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Feedback in living systems | https://www.youtube.com/watch?v=eHsYuPEYXgE | vtt | https://www.youtube.com/api/timedtext?v=eHsYuPEYXgE&ei=3FWUZeDkEp2ep-oPgJme-Ao&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=7C2B54531ACB5149EC571AA85A35CE7F264EDE70.79F8A2C07B3503BB6CD2167E51C096EF7FE25562&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.520 --> 00:00:02.300
- [Instructor] So last
weekend, my family and I
00:00:02.300 --> 00:00:04.410
went out hiking in the desert.
00:00:04.410 --> 00:00:06.070
And as you can tell from these pictures
00:00:06.070 --> 00:00:09.410
I snapped along the way,
it was a gorgeous hike.
00:00:09.410 --> 00:00:13.340
We made our way to this lake
around a small canyon range
00:00:13.340 --> 00:00:15.430
and up and down this mountain trail.
00:00:15.430 --> 00:00:17.460
Now, all of this was really great,
00:00:17.460 --> 00:00:19.360
but there was just one problem.
00:00:19.360 --> 00:00:21.500
It got super hot.
00:00:21.500 --> 00:00:24.340
And because we were
exercising out in the hot sun,
00:00:24.340 --> 00:00:26.470
we started sweating buckets.
00:00:26.470 --> 00:00:29.580
And all I wanted to do after
a while was to find some water
00:00:29.580 --> 00:00:31.910
and shade as soon as possible.
00:00:31.910 --> 00:00:34.320
So finally, after we sat down to have
00:00:34.320 --> 00:00:35.940
a nice picnic in the shade
00:00:35.940 --> 00:00:39.160
and our sweat provided
some evaporative cooling,
00:00:39.160 --> 00:00:42.590
our bodies were able to cool
down without overheating.
00:00:42.590 --> 00:00:45.140
So you might be wondering
why did our bodies
00:00:45.140 --> 00:00:47.350
in our behavior respond that way?
00:00:47.350 --> 00:00:49.730
Why did we sweat and want to find shade?
00:00:49.730 --> 00:00:53.670
Well, the answer is our bodies
were protecting us from harm.
00:00:53.670 --> 00:00:55.810
The human body isn't able to function
00:00:55.810 --> 00:00:57.460
at too high of a temperature.
00:00:57.460 --> 00:01:00.580
So our bodies helped cool us
down through a combination
00:01:00.580 --> 00:01:04.220
of physiological and behavioral responses.
00:01:04.220 --> 00:01:07.087
Physiological responses
being the internal, chemical,
00:01:07.087 --> 00:01:09.270
and physical changes that our bodies
00:01:09.270 --> 00:01:11.160
carry out unconsciously,
00:01:11.160 --> 00:01:13.530
and behavioral responses being the actions
00:01:13.530 --> 00:01:17.490
we carry out consciously in
response to what our body needs.
00:01:17.490 --> 00:01:19.980
So in this case, the
physiological response
00:01:19.980 --> 00:01:22.130
would be sweating, which our body does
00:01:22.130 --> 00:01:23.860
in order to cool itself down.
00:01:23.860 --> 00:01:27.570
And in addition to sweating,
other physiological responses
00:01:27.570 --> 00:01:31.400
were also happening such as,
our blood vessels were dilating
00:01:31.400 --> 00:01:33.500
and we were getting thirsty.
00:01:33.500 --> 00:01:35.940
And the behavioral
responses were our attempts
00:01:35.940 --> 00:01:39.823
to find shade and get out of
the sun and to drink water.
00:01:40.780 --> 00:01:45.080
This tendency of an organism
to maintain internal conditions
00:01:45.080 --> 00:01:48.350
within an acceptable range despite changes
00:01:48.350 --> 00:01:52.840
in its external environment
is called homeostasis.
00:01:52.840 --> 00:01:54.700
And I'll write down our definition.
00:01:54.700 --> 00:01:59.700
So it's the tendency to
maintain internal conditions
00:02:00.060 --> 00:02:04.320
despite changes in external conditions.
00:02:04.320 --> 00:02:08.360
So homeostasis is incredibly
important because without it,
00:02:08.360 --> 00:02:12.170
we could have overheated
and been in real danger.
00:02:12.170 --> 00:02:15.300
So in other words,
homeostasis is necessary
00:02:15.300 --> 00:02:17.870
in order for organisms to survive.
00:02:17.870 --> 00:02:20.550
Now, you might also be
wondering how living things
00:02:20.550 --> 00:02:24.600
generally maintain this
homeostatic condition of theirs.
00:02:24.600 --> 00:02:28.500
And this usually involves
negative feedback loops.
00:02:28.500 --> 00:02:30.160
So let me draw this diagram for us.
00:02:30.160 --> 00:02:33.070
We have our stimulus, we have a detection
00:02:33.070 --> 00:02:34.953
and then a response.
00:02:37.400 --> 00:02:42.330
So in negative feedback, a
stimulus or a detectable change
00:02:42.330 --> 00:02:45.950
in internal conditions
triggers the body to carry out
00:02:45.950 --> 00:02:50.190
a response that will counteract
or oppose this change.
00:02:50.190 --> 00:02:53.990
So it'll bring conditions
back within an ideal range.
00:02:53.990 --> 00:02:56.100
And this is what is represented right here
00:02:56.100 --> 00:02:58.873
by this blocking symbol in the diagram.
00:02:59.890 --> 00:03:01.990
So going back to my family's hiking trip,
00:03:01.990 --> 00:03:04.590
we can say that the
stimulus was the increase
00:03:04.590 --> 00:03:06.920
in our body temperatures as a result
00:03:06.920 --> 00:03:09.110
of hiking in the hot desert.
00:03:09.110 --> 00:03:11.980
Our bodies detected that
our internal temperature
00:03:11.980 --> 00:03:15.220
was moving outside of
the acceptable range,
00:03:15.220 --> 00:03:18.410
which typically falls between 97.7
00:03:18.410 --> 00:03:23.410
to 99.5 degrees Fahrenheit or
36.5 to 37.5 degrees Celsius.
00:03:26.850 --> 00:03:28.130
And the cool thing is that,
00:03:28.130 --> 00:03:30.570
once our bodies detected the stimulus,
00:03:30.570 --> 00:03:33.230
they produced a response to counteract
00:03:33.230 --> 00:03:35.800
this change through negative feedback.
00:03:35.800 --> 00:03:38.970
We were hot, so we wanted
to become less hot.
00:03:38.970 --> 00:03:41.120
And in this case, the
negative feedback loop
00:03:41.120 --> 00:03:44.310
caused responses like sweating that helped
00:03:44.310 --> 00:03:45.890
cool our body temperatures down
00:03:45.890 --> 00:03:49.580
to the acceptable or the ideal range.
00:03:49.580 --> 00:03:51.280
It's also worth noting that our bodies
00:03:51.280 --> 00:03:54.870
can elicit negative feedback
mechanisms in response
00:03:54.870 --> 00:03:57.940
to our body temperature dropping too low.
00:03:57.940 --> 00:04:01.300
So if our body temperature
drops below the ideal range
00:04:01.300 --> 00:04:03.800
or our body temperature decreases,
00:04:03.800 --> 00:04:06.590
then the body counteracts
this change through responses
00:04:06.590 --> 00:04:09.850
like shivering and blood
vessel constriction,
00:04:09.850 --> 00:04:12.520
all with a goal of
helping to keep us warm.
00:04:12.520 --> 00:04:15.320
So negative feedback
mechanisms help cool us down
00:04:15.320 --> 00:04:19.760
when we get too hot or they
warm us up when we get too cold.
00:04:19.760 --> 00:04:23.330
So they help to keep our
body temperatures just right.
00:04:23.330 --> 00:04:25.890
And this process of
maintaining body temperature,
00:04:25.890 --> 00:04:28.660
otherwise known as thermoregulation,
00:04:28.660 --> 00:04:30.230
let me write that out for us,
00:04:30.230 --> 00:04:33.340
it can be seen in all
different kinds of organisms.
00:04:33.340 --> 00:04:36.120
You might've seen dogs
pant when they're hot
00:04:36.120 --> 00:04:39.030
or spotted lizards
sunbathing to stay warm.
00:04:39.030 --> 00:04:41.260
And these are all homeostatic responses
00:04:41.260 --> 00:04:43.960
that help keep the
organism's body temperature
00:04:43.960 --> 00:04:47.190
within the acceptable
range that we talked about.
00:04:47.190 --> 00:04:50.170
Another really awesome example
of a negative feedback loop
00:04:50.170 --> 00:04:53.940
is osmoregulation, specifically in salmon.
00:04:53.940 --> 00:04:55.810
And here's a picture.
00:04:55.810 --> 00:04:59.270
Now, salmon spend part of their
lives in freshwater streams
00:04:59.270 --> 00:05:02.540
and the other part of their
lives in salt-water oceans.
00:05:02.540 --> 00:05:05.800
So in fresh water, the salt
concentration of the water
00:05:05.800 --> 00:05:08.630
is lower than the salt
concentration you would find
00:05:08.630 --> 00:05:11.500
in the fish's internal body fluid.
00:05:11.500 --> 00:05:14.760
While in saltwater, the salt
concentration of the water
00:05:14.760 --> 00:05:18.930
is higher than this fish's
internal salt concentration.
00:05:18.930 --> 00:05:20.830
So this means that in fresh water,
00:05:20.830 --> 00:05:23.140
the fish will tend to absorb water
00:05:23.140 --> 00:05:25.290
and lose salts through their skin.
00:05:25.290 --> 00:05:28.340
Well, the opposite is true in saltwater.
00:05:28.340 --> 00:05:31.110
Any large change in a fish's internal salt
00:05:31.110 --> 00:05:33.440
or water levels could be fatal.
00:05:33.440 --> 00:05:35.810
So how exactly can salmon tolerate
00:05:35.810 --> 00:05:39.280
these extremely different
environmental conditions?
00:05:39.280 --> 00:05:42.960
Well, they also use negative
feedback mechanisms.
00:05:42.960 --> 00:05:45.560
So salmon have a negative feedback system,
00:05:45.560 --> 00:05:49.100
which detects changes in
internal salt concentrations
00:05:49.100 --> 00:05:52.380
and causes a response that
involves either taking up
00:05:52.380 --> 00:05:54.940
or excreting salt through the gills
00:05:54.940 --> 00:05:57.650
or having more or less dilute urine
00:05:57.650 --> 00:06:01.600
in order to reestablish ideal
internal salt concentrations.
00:06:01.600 --> 00:06:05.840
And this is otherwise
known as osmoregulation.
00:06:05.840 --> 00:06:08.320
So again, we have a
feedback loop that acts
00:06:08.320 --> 00:06:11.110
to oppose a stimulus, which in this case
00:06:11.110 --> 00:06:14.750
is the change in internal
salt concentrations.
00:06:14.750 --> 00:06:17.620
So now we know that homeostatic mechanisms
00:06:17.620 --> 00:06:20.250
usually involve negative feedback loops,
00:06:20.250 --> 00:06:22.720
but what about positive feedback loops?
00:06:22.720 --> 00:06:25.890
Well, many organisms actually
use positive feedback loops
00:06:25.890 --> 00:06:28.490
to bring processes to completion.
00:06:28.490 --> 00:06:31.590
So while negative feedback
loops dampen stimuli
00:06:31.590 --> 00:06:35.730
or oppose stimuli, positive
feedback loops do the opposite.
00:06:35.730 --> 00:06:38.450
They amplify stimuli.
00:06:38.450 --> 00:06:40.700
And as you can tell from this diagram,
00:06:40.700 --> 00:06:43.380
instead of having a blocking symbol here,
00:06:43.380 --> 00:06:45.210
we have an arrow to indicate
00:06:45.210 --> 00:06:48.000
the amplification of the stimulus.
00:06:48.000 --> 00:06:51.090
So in humans for instance,
a positive feedback loop
00:06:51.090 --> 00:06:53.060
is used for childbirth.
00:06:53.060 --> 00:06:54.940
So as you can see from this diagram,
00:06:54.940 --> 00:06:57.740
the stimulus in childbirth
comes from the baby's head,
00:06:57.740 --> 00:07:00.610
which presses against the cervix here.
00:07:00.610 --> 00:07:03.340
And this stimulates neurons in the cervix,
00:07:03.340 --> 00:07:06.070
which send a signal for
the brain to release
00:07:06.070 --> 00:07:09.200
a special kind of hormone called oxytocin.
00:07:09.200 --> 00:07:11.920
Now, oxytocin is responsible for causing
00:07:11.920 --> 00:07:15.151
the uterus to contract,
which as you might've guessed
00:07:15.151 --> 00:07:17.670
causes more pressure on the cervix
00:07:17.670 --> 00:07:19.660
which sends more neural signals,
00:07:19.660 --> 00:07:22.050
which releases more oxytocin.
00:07:22.050 --> 00:07:24.750
And this loop continues on and on
00:07:24.750 --> 00:07:28.070
all the way until the baby is born.
00:07:28.070 --> 00:07:31.050
So when the baby is born,
because the baby's head
00:07:31.050 --> 00:07:33.400
isn't pressing up against the cervix
00:07:33.400 --> 00:07:35.380
and the pelvic floor anymore,
00:07:35.380 --> 00:07:37.200
the neuron stops sending the signal
00:07:37.200 --> 00:07:38.720
and the brain stops triggering
00:07:38.720 --> 00:07:41.190
the release of so much oxytocin.
00:07:41.190 --> 00:07:44.593
So that's how the loop will
eventually come to an end.
00:07:45.950 --> 00:07:48.150
So to recap on what we've talked about.
00:07:48.150 --> 00:07:50.320
Today, we learned that organisms maintain
00:07:50.320 --> 00:07:53.660
their internal conditions
through homeostasis.
00:07:53.660 --> 00:07:55.060
And this is usually accomplished
00:07:55.060 --> 00:07:56.820
through negative feedback loops,
00:07:56.820 --> 00:08:00.420
which dampen or oppose
stimuli as we talked about
00:08:00.420 --> 00:08:04.000
with thermoregulation and osmoregulation.
00:08:04.000 --> 00:08:06.730
But on the other hand
as we saw in childbirth,
00:08:06.730 --> 00:08:10.200
positive feedback loops
work to amplify stimuli
00:08:10.200 --> 00:08:13.103
in order to bring processes to completion.
|
Inertial Mass vs. Gravitational Mass | https://www.youtube.com/watch?v=Ws3yB3QsKY4 | vtt | https://www.youtube.com/api/timedtext?v=Ws3yB3QsKY4&ei=3FWUZeP5ArK2vdIP2ua60A0&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=D40D3EE7F5E277DE16AEFF253FDDB0FCF9EA5155.138C2A91079077BCD442CF4B5546AABFE687C8A1&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.180 --> 00:00:01.520
- [Instructor] Knowing
the mass of an object
00:00:01.520 --> 00:00:05.110
actually tells you two independent
things about that object.
00:00:05.110 --> 00:00:08.610
For instance, if you knew that
this truck had a large mass
00:00:08.610 --> 00:00:11.000
you'd know that it has a
large amount of inertia,
00:00:11.000 --> 00:00:11.890
that is to say,
00:00:11.890 --> 00:00:14.310
it'd be very reluctant
to being accelerated.
00:00:14.310 --> 00:00:16.120
It'd be difficult to speed up.
00:00:16.120 --> 00:00:17.570
And once you got it up to speed,
00:00:17.570 --> 00:00:19.160
it'd be very difficult to stop.
00:00:19.160 --> 00:00:20.880
It would take a large amount of force
00:00:20.880 --> 00:00:23.910
that's 'cause it has a large
amount of inertial mass.
00:00:23.910 --> 00:00:27.240
And this idea of inertial
mass is best exemplified
00:00:27.240 --> 00:00:29.180
with Newton's second law.
00:00:29.180 --> 00:00:34.170
So acceleration equals the
net force divided by M.
00:00:34.170 --> 00:00:36.830
This M right here, down
here in the denominator,
00:00:36.830 --> 00:00:39.670
this is the inertial mass,
00:00:39.670 --> 00:00:41.920
because it's telling you
how reluctant that thing is
00:00:41.920 --> 00:00:43.070
to being accelerated more.
00:00:43.070 --> 00:00:46.340
Inertial mass would give
you less acceleration,
00:00:46.340 --> 00:00:48.110
but mass also tells you something else.
00:00:48.110 --> 00:00:51.080
It tells you how much that
object is gonna interact
00:00:51.080 --> 00:00:52.020
via gravity.
00:00:52.020 --> 00:00:55.280
So if this truck has a large
mass that also tells you
00:00:55.280 --> 00:00:58.430
its force of gravity is
going to be very large.
00:00:58.430 --> 00:01:02.880
So the force of gravity FG
on this truck is equal to MG
00:01:02.880 --> 00:01:06.320
that this M right here
is not inertial mass.
00:01:06.320 --> 00:01:09.350
This M here, is telling you
how much this truck interacts
00:01:09.350 --> 00:01:11.430
via gravity with other objects.
00:01:11.430 --> 00:01:14.120
And that means this is
the gravitational mass.
00:01:14.120 --> 00:01:16.750
Now in our universe for a given object,
00:01:16.750 --> 00:01:19.860
these two values inertial
mass and gravitational mass
00:01:19.860 --> 00:01:20.810
are gonna be the same.
00:01:20.810 --> 00:01:24.410
So this trucks, inertial
mass measured in kilograms
00:01:24.410 --> 00:01:27.930
is gonna be the exact
same value as this trucks,
00:01:27.930 --> 00:01:30.920
gravitational mass measured in kilograms,
00:01:30.920 --> 00:01:32.300
but it didn't have to be that way.
00:01:32.300 --> 00:01:35.100
I mean, these two ideas
are conceptually different.
00:01:35.100 --> 00:01:37.530
One, the inertial mass
tells you how much inertia
00:01:37.530 --> 00:01:39.850
or reluctance to
acceleration something has,
00:01:39.850 --> 00:01:42.140
but the gravitational mass
tells you how much that object
00:01:42.140 --> 00:01:43.580
interacts via gravity.
00:01:43.580 --> 00:01:45.410
So you could imagine a universe
00:01:45.410 --> 00:01:47.900
or maybe there's no force gravity,
00:01:47.900 --> 00:01:49.620
but objects still have a reluctance
00:01:49.620 --> 00:01:52.240
to being accelerated by other forces.
00:01:52.240 --> 00:01:54.280
Or maybe you can imagine a universe
00:01:54.280 --> 00:01:56.200
where there is a force of gravity,
00:01:56.200 --> 00:01:57.510
but the number that tells you
00:01:57.510 --> 00:01:59.970
how much something interacts via gravity,
00:01:59.970 --> 00:02:02.150
could have been different
from the number that tells you
00:02:02.150 --> 00:02:04.890
how reluctant that object
is to being accelerated.
00:02:04.890 --> 00:02:07.920
But for our universe, these
two numbers are the same.
00:02:07.920 --> 00:02:09.420
I mean, scientists to this day
00:02:09.420 --> 00:02:11.750
are still doing very delicate experiments
00:02:11.750 --> 00:02:14.400
to try to decern any small differences
00:02:14.400 --> 00:02:15.770
between these two.
00:02:15.770 --> 00:02:19.110
But as far I can tell, to the
best experiments up to date,
00:02:19.110 --> 00:02:21.020
these two numbers are exactly the same
00:02:21.020 --> 00:02:23.380
even though they're
conceptually different.
00:02:23.380 --> 00:02:24.900
So this is good to keep in mind.
00:02:24.900 --> 00:02:26.290
If you're gonna do an experiment,
00:02:26.290 --> 00:02:28.390
you're gonna be measuring
either inertial mass,
00:02:28.390 --> 00:02:31.390
or gravitational mass
typically, how would you know
00:02:31.390 --> 00:02:34.010
in a given experiment if you
measured one or the other?
00:02:34.010 --> 00:02:35.920
Well, I mean, if you just
use a simple experiment,
00:02:35.920 --> 00:02:39.700
like take a spring scale,
measure the force you're exerting
00:02:39.700 --> 00:02:42.600
on a cart and then measure
the acceleration of that cart
00:02:42.600 --> 00:02:46.310
using meter sticks and
stopwatches or a motion sensor.
00:02:46.310 --> 00:02:48.810
And if you just plug this
into Newton's second law,
00:02:48.810 --> 00:02:52.120
so if you know that acceleration
from a motion detector,
00:02:52.120 --> 00:02:53.640
stopwatches and rulers,
00:02:53.640 --> 00:02:55.870
and you measure the force
with the spring scale
00:02:55.870 --> 00:02:58.760
and you solve for this M well,
00:02:58.760 --> 00:03:01.650
this is the denominator
of Newton's second law.
00:03:01.650 --> 00:03:04.540
That means you just
solve for inertial mass,
00:03:04.540 --> 00:03:08.030
'cause you solved in a formula
that contained inertial mass.
00:03:08.030 --> 00:03:09.940
How would you experimentally determine
00:03:09.940 --> 00:03:12.020
the gravitational mass of this cart?
00:03:12.020 --> 00:03:13.300
Well, it's even easier.
00:03:13.300 --> 00:03:15.320
All you have to do take a scale, you know,
00:03:15.320 --> 00:03:17.930
just a digital scale, take your cart,
00:03:17.930 --> 00:03:19.900
put your cart on the digital scale
00:03:19.900 --> 00:03:21.820
and just measure how much the scale reads
00:03:21.820 --> 00:03:24.020
because you know that the force of gravity
00:03:24.020 --> 00:03:25.870
is gonna be measured by the scale.
00:03:25.870 --> 00:03:28.030
That's the number you
get out of the scales
00:03:28.030 --> 00:03:30.500
telling you how much
weight this object has.
00:03:30.500 --> 00:03:32.350
So the scale would just read this
00:03:32.350 --> 00:03:33.560
and if you know what planet you're on,
00:03:33.560 --> 00:03:34.550
you know what G you've got.
00:03:34.550 --> 00:03:37.960
So if you know, G is 9.8
and you solve for this M,
00:03:37.960 --> 00:03:40.300
well, look at you solve
for the gravitational mass,
00:03:40.300 --> 00:03:42.690
how much this thing interacts via gravity.
00:03:42.690 --> 00:03:44.230
So whenever you put something on a scale,
00:03:44.230 --> 00:03:46.370
weigh it like that and get M,
00:03:46.370 --> 00:03:47.810
you're getting gravitational mass.
00:03:47.810 --> 00:03:49.690
If you do the other way
with Newton's second law,
00:03:49.690 --> 00:03:51.550
you're getting inertial mass.
00:03:51.550 --> 00:03:53.710
People get this mixed
up, but it's pretty easy.
00:03:53.710 --> 00:03:56.510
If you ever use a formula
that involves little G
00:03:56.510 --> 00:03:59.620
or like big G, gravitational
constant big G,
00:03:59.620 --> 00:04:02.440
that means you've solved M in that formula
00:04:02.440 --> 00:04:03.920
for gravitational mass.
00:04:03.920 --> 00:04:06.960
If there isn't a G, then you're
solving for inertial mass.
00:04:06.960 --> 00:04:08.490
So for instance, (mumbles)
00:04:08.490 --> 00:04:10.930
you do some experiment where
you try to very delicately
00:04:10.930 --> 00:04:13.940
measure the force of
gravity between two spheres.
00:04:13.940 --> 00:04:14.773
This would be hard.
00:04:14.773 --> 00:04:15.840
You probably wouldn't set it up like this.
00:04:15.840 --> 00:04:17.200
You'd have to be more sophisticated,
00:04:17.200 --> 00:04:19.890
but let's say you could just
measure the force of gravity.
00:04:19.890 --> 00:04:22.220
These two spheres exert on each other.
00:04:22.220 --> 00:04:24.850
The formula for that would be big G, M one
00:04:24.850 --> 00:04:27.330
times M of the other
divided by the distance
00:04:27.330 --> 00:04:28.720
between them squared.
00:04:28.720 --> 00:04:30.280
You'd have to know one of the masses,
00:04:30.280 --> 00:04:32.370
but the spring scale
could give you the force.
00:04:32.370 --> 00:04:35.090
You can measure the distance
between them with a ruler
00:04:35.090 --> 00:04:37.720
big G you know, it's a
constant of the universe.
00:04:37.720 --> 00:04:41.490
If you knew one of the other
masses and solved for this one,
00:04:41.490 --> 00:04:43.297
you'd be getting the gravitational mass
00:04:43.297 --> 00:04:46.120
you could use the
formula that's got big G.
00:04:46.120 --> 00:04:49.140
Any formula with big G or with little G
00:04:49.140 --> 00:04:52.060
like force of gravity is MG.
00:04:52.060 --> 00:04:55.010
These are all formulas that
tell you how much the object M
00:04:55.010 --> 00:04:57.380
is gonna interact via gravity.
00:04:57.380 --> 00:05:01.300
Or you could even imagine
gravitational field is big GM
00:05:02.630 --> 00:05:03.910
over R squared.
00:05:03.910 --> 00:05:05.440
All of these M's here,
00:05:05.440 --> 00:05:08.560
this M here, that M there, that M there,
00:05:08.560 --> 00:05:11.170
and this M here all gravitational mass,
00:05:11.170 --> 00:05:13.370
'cause there's either big G or little G
00:05:13.370 --> 00:05:16.240
involved in that fundamental equation.
00:05:16.240 --> 00:05:18.340
If there's a fundamental
equation that doesn't have big G
00:05:18.340 --> 00:05:19.270
or little G,
00:05:19.270 --> 00:05:21.530
you're not talking about how
something interacts by gravity,
00:05:21.530 --> 00:05:23.090
you're talking about it's inertia,
00:05:23.090 --> 00:05:24.310
and that would be a natural mass.
00:05:24.310 --> 00:05:26.350
So for instance, if you
did some other experiment
00:05:26.350 --> 00:05:28.190
maybe you slam two carts together
00:05:28.190 --> 00:05:31.240
and use conservation of
momentum to solve for M
00:05:31.240 --> 00:05:33.540
well, momentum is MV.
00:05:33.540 --> 00:05:36.250
This formula has nothing to
do with little G or big G,
00:05:36.250 --> 00:05:38.060
no gravitational constants here.
00:05:38.060 --> 00:05:40.340
So if you use this collision experiment
00:05:40.340 --> 00:05:42.150
and solve for the mass
of one of the carts,
00:05:42.150 --> 00:05:45.190
you've solved for the
inertial mass of the cart.
00:05:45.190 --> 00:05:47.500
Similarly, if you use kinetic energy,
00:05:47.500 --> 00:05:50.630
this formula has nothing
fundamentally to do with gravity.
00:05:50.630 --> 00:05:53.150
One half MV squared,
there's no big G or little G
00:05:53.150 --> 00:05:55.700
this M here would be inertial mass.
00:05:55.700 --> 00:05:58.190
If you did the period
of a mass on a spring,
00:05:58.190 --> 00:06:01.400
is two PI root M over K.
00:06:01.400 --> 00:06:03.810
There's no little G or
big G to be found in here.
00:06:03.810 --> 00:06:06.330
That means this is also inertial mass.
00:06:06.330 --> 00:06:07.980
So unless there's a little G or big G
00:06:07.980 --> 00:06:10.760
in your fundamental equation
here, your basic equation,
00:06:10.760 --> 00:06:12.540
that mass is gonna be inertial mass
00:06:12.540 --> 00:06:13.960
if there is a little G or big G
00:06:13.960 --> 00:06:15.920
you're talking about gravitational mass.
00:06:15.920 --> 00:06:16.900
Now, if you're clever,
00:06:16.900 --> 00:06:19.700
you could do a single
experiment with two phases
00:06:19.700 --> 00:06:22.820
and get both masses at once for instance,
00:06:22.820 --> 00:06:25.130
let's say you got a spring
of known spring constant
00:06:25.130 --> 00:06:26.470
and you hung a block on it
00:06:26.470 --> 00:06:28.930
and you lowered it gently until it hangs
00:06:28.930 --> 00:06:31.140
at a certain distance,
unless you measured.
00:06:31.140 --> 00:06:33.100
How much did this thing stretch?
00:06:33.100 --> 00:06:34.600
Well, if you measure that with a ruler,
00:06:34.600 --> 00:06:38.740
then you know it this
position, the spring force KX
00:06:38.740 --> 00:06:42.600
had better be equal to the
gravitational force, MG.
00:06:42.600 --> 00:06:45.030
And so KX would just equal MG
00:06:45.030 --> 00:06:46.730
if the spring constance known
00:06:46.730 --> 00:06:48.520
and you measured X with a ruler,
00:06:48.520 --> 00:06:49.590
and you know what planning you're on
00:06:49.590 --> 00:06:51.090
'cause G is 9.8 on earth.
00:06:51.090 --> 00:06:53.470
If you solve for this and
look at G is right here,
00:06:53.470 --> 00:06:55.530
you multiplied by the G and this formulate
00:06:55.530 --> 00:06:57.300
came from a gravitational formula,
00:06:57.300 --> 00:07:00.130
you would have sold
for gravitational mass.
00:07:00.130 --> 00:07:02.260
And now you know the
gravitational mass of the object,
00:07:02.260 --> 00:07:04.080
how could you get the inertial mass?
00:07:04.080 --> 00:07:06.380
Well, let's say you just
pull down a little extra.
00:07:06.380 --> 00:07:08.390
You pull this down a
little extra, you let go.
00:07:08.390 --> 00:07:10.830
And then it's gonna oscillate
at a certain period.
00:07:10.830 --> 00:07:12.990
Let's say you measure that
period with a stopwatch.
00:07:12.990 --> 00:07:16.090
You measure how long it takes
to go through one full cycle.
00:07:16.090 --> 00:07:19.690
That's got to equal two PI, root M over K.
00:07:19.690 --> 00:07:21.670
Now, there's no little G or big G here.
00:07:21.670 --> 00:07:23.000
This has nothing to do with gravity.
00:07:23.000 --> 00:07:24.890
So if you measure this
period with a stopwatch
00:07:24.890 --> 00:07:26.320
and you know the spring constant
00:07:26.320 --> 00:07:28.160
and you solve for this M,
00:07:28.160 --> 00:07:32.030
well, now you've solved for the
inertial mass of that block.
00:07:32.030 --> 00:07:33.010
And now you know both.
00:07:33.010 --> 00:07:35.300
One stage got us the gravitational mass,
00:07:35.300 --> 00:07:37.780
'cause it came from MG the M did.
00:07:37.780 --> 00:07:39.480
The second stage, got us the inertial mass
00:07:39.480 --> 00:07:42.020
'cause it comes from
two PI, root M over K,
00:07:42.020 --> 00:07:43.970
and this formula has
nothing to do with gravity.
00:07:43.970 --> 00:07:46.720
So this would be a way you
could find both masses at once.
00:07:46.720 --> 00:07:49.670
So recapping, inertial
mass and gravitational mass
00:07:49.670 --> 00:07:53.190
are identical numbers, but
different conceptually.
00:07:53.190 --> 00:07:55.870
One, tells you how reluctant an object is
00:07:55.870 --> 00:07:57.200
to being accelerated.
00:07:57.200 --> 00:07:59.630
And the other tells you how
much the object will interact
00:07:59.630 --> 00:08:00.700
via gravity.
00:08:00.700 --> 00:08:03.160
And if the mass shows
up in a basic formula
00:08:03.160 --> 00:08:05.540
that involves little G or big G
00:08:05.540 --> 00:08:07.890
that's gonna be the gravitational mass.
00:08:07.890 --> 00:08:10.773
Otherwise it's gonna be the inertial mass.
|
Work-Energy Principle Example | https://www.youtube.com/watch?v=BYkxKrbETb4 | vtt | https://www.youtube.com/api/timedtext?v=BYkxKrbETb4&ei=3FWUZZG6CPmbvdIP5ve2iAo&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=B4A96385004CE1F8ABF20C05D63990031F8A1B92.9716367128E1D7AAFC7052E314B8E56C195739AF&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.180 --> 00:00:01.310
- [Instructor] So, the
work-energy principle
00:00:01.310 --> 00:00:03.700
states that the net work done on an object
00:00:03.700 --> 00:00:06.800
is gonna equal the changing
kinetic energy of that object.
00:00:06.800 --> 00:00:08.680
And this works for systems as well.
00:00:08.680 --> 00:00:10.949
So, the net work done
on a system of objects
00:00:10.949 --> 00:00:14.250
is gonna equal the change
in the total kinetic energy
00:00:14.250 --> 00:00:16.030
of the objects in that system.
00:00:16.030 --> 00:00:18.480
Now, that sounds really
complicated and technical,
00:00:18.480 --> 00:00:19.313
but I like to think
00:00:19.313 --> 00:00:21.420
about the work-energy
principle's a shortcut.
00:00:21.420 --> 00:00:23.500
This is a really nice
shortcut that lets me
00:00:23.500 --> 00:00:26.500
determine the change in kinetic
energy without having to do
00:00:26.500 --> 00:00:29.720
a bunch of complicated
conservation of energy equations
00:00:29.720 --> 00:00:31.530
or kinematic formulas.
00:00:31.530 --> 00:00:33.040
The catch is that I need to know
00:00:33.040 --> 00:00:35.410
how to figure out what the net work is.
00:00:35.410 --> 00:00:36.960
So, how do you figure out net work?
00:00:36.960 --> 00:00:40.010
Well, the formula for work
done is F d cosine theta.
00:00:40.010 --> 00:00:42.020
Since this formula, work-energy principle,
00:00:42.020 --> 00:00:43.400
relies on net work,
00:00:43.400 --> 00:00:45.840
this has to be magnitude of the net force
00:00:45.840 --> 00:00:48.000
times magnitude of the distance traveled
00:00:48.000 --> 00:00:49.470
times cosine of theta.
00:00:49.470 --> 00:00:53.500
Remember this theta has to be
angle between, not any angle,
00:00:53.500 --> 00:00:55.810
angle between the net force direction
00:00:55.810 --> 00:00:57.286
and the direction of motion.
00:00:57.286 --> 00:00:59.190
And so, let's try this out.
00:00:59.190 --> 00:01:00.330
How do you use this thing?
00:01:00.330 --> 00:01:01.860
Let's kick the tires.
00:01:01.860 --> 00:01:03.050
Let's say there's a satellite.
00:01:03.050 --> 00:01:04.320
It's moving to the right
00:01:04.320 --> 00:01:06.690
and there's a net force on this satellite.
00:01:06.690 --> 00:01:08.940
Now, this net force could
go in any direction.
00:01:08.940 --> 00:01:11.909
If the net force has a component
in the direction of motion,
00:01:11.909 --> 00:01:14.560
then, the net work is gonna be positive.
00:01:14.560 --> 00:01:17.570
And if so, anything here
from like negative 90,
00:01:17.570 --> 00:01:20.120
well, like it's negative 89.9,
00:01:20.120 --> 00:01:21.670
because 90 would be
perpendicular for many,
00:01:21.670 --> 00:01:25.640
for like 89.9 negative to positive 89.9,
00:01:25.640 --> 00:01:28.440
you've got a component in
the direction of motion.
00:01:28.440 --> 00:01:30.857
That means you're gonna be
doing positive net work.
00:01:30.857 --> 00:01:32.660
And that means the
change of kinetic energy
00:01:32.660 --> 00:01:35.180
will be positive because
it just equals that number.
00:01:35.180 --> 00:01:37.290
That means kinetic energy increases.
00:01:37.290 --> 00:01:38.300
You're gonna be speeding up
00:01:38.300 --> 00:01:40.420
And that kind of, it
makes sense intuitively.
00:01:40.420 --> 00:01:42.570
If your force is in the
direction of motion,
00:01:42.570 --> 00:01:43.780
you're speeding up.
00:01:43.780 --> 00:01:44.760
What about the other case?
00:01:44.760 --> 00:01:45.900
What if your net force points
00:01:45.900 --> 00:01:47.430
in the opposite direction of motion?
00:01:47.430 --> 00:01:49.540
Well, now, the net work
is gonna be negative.
00:01:49.540 --> 00:01:52.490
You'll have a negative
change in kinetic energy.
00:01:52.490 --> 00:01:54.500
In other words, you're gonna slow down
00:01:54.500 --> 00:01:56.900
and if the net force points perpendicular,
00:01:56.900 --> 00:01:58.490
well, then, you're not doing any work
00:01:58.490 --> 00:02:01.430
because cosine of 90 is gonna be zero.
00:02:01.430 --> 00:02:03.040
No net work would be done.
00:02:03.040 --> 00:02:04.920
There's gonna be no
change in kinetic energy.
00:02:04.920 --> 00:02:05.890
That doesn't mean you stop.
00:02:05.890 --> 00:02:08.860
It just means you're not going
to speed up or slow down.
00:02:08.860 --> 00:02:09.693
This does something.
00:02:09.693 --> 00:02:10.650
You might be like,
"Don't you do something?"
00:02:10.650 --> 00:02:11.810
Yeah, you're gonna drift upward.
00:02:11.810 --> 00:02:13.740
You're gonna start
changing your direction,
00:02:13.740 --> 00:02:16.090
but this is not gonna
be doing any work on you
00:02:16.950 --> 00:02:18.890
at that moment.
00:02:18.890 --> 00:02:20.280
And so, just to be clear, I mean,
00:02:20.280 --> 00:02:21.920
let's just try a complicated one here.
00:02:21.920 --> 00:02:24.280
Let's say this force
goes in some direction.
00:02:24.280 --> 00:02:25.790
Let's say your velocity even goes down.
00:02:25.790 --> 00:02:28.400
So, maybe your satellite's
heading downward
00:02:28.400 --> 00:02:30.810
and your force is gonna
go in any direction.
00:02:30.810 --> 00:02:32.580
Well, if it goes this way,
00:02:32.580 --> 00:02:35.370
exactly backwards, it's gonna be 180.
00:02:35.370 --> 00:02:37.040
You're gonna be doing negative work.
00:02:37.040 --> 00:02:39.250
You're gonna be slowing down,
decreasing kinetic energy.
00:02:39.250 --> 00:02:41.130
And you're not gonna change direction.
00:02:41.130 --> 00:02:44.120
If you're like this, you
have a component opposite.
00:02:44.120 --> 00:02:47.271
So, you're gonna be slowing
down and changing direction.
00:02:47.271 --> 00:02:49.360
This will just be changing direction.
00:02:49.360 --> 00:02:51.676
You're not speeding up or
slowing down at that moment.
00:02:51.676 --> 00:02:54.890
This will speed you up
and change your direction.
00:02:54.890 --> 00:02:57.320
And finally, this will
just be speeding you up
00:02:57.320 --> 00:02:59.430
and you will not be
changing your direction.
00:02:59.430 --> 00:03:01.670
So, the work-energy principle's convenient
00:03:01.670 --> 00:03:04.120
to just get a conceptual
or qualitative idea
00:03:04.120 --> 00:03:05.050
of what's going on.
00:03:05.050 --> 00:03:07.510
And it can obviously also give you an idea
00:03:07.510 --> 00:03:09.380
of how to calculate things.
00:03:09.380 --> 00:03:11.970
So, let's try one where you
actually have to get a number.
00:03:11.970 --> 00:03:14.000
So, let's say there's a hot air balloon
00:03:14.000 --> 00:03:16.350
and it's a 300 kilogram hot air balloon.
00:03:16.350 --> 00:03:17.230
Drifting to the left,
00:03:17.230 --> 00:03:19.970
it had an initial speed of
seven meters per second,
00:03:19.970 --> 00:03:22.170
and it's traveling a total of 50 meters
00:03:22.170 --> 00:03:24.150
to the left during this journey.
00:03:24.150 --> 00:03:25.930
Now, there's gonna be forces
on this hot air balloon.
00:03:25.930 --> 00:03:29.010
Obviously, there's gonna be
gravity and some buoyant force,
00:03:29.010 --> 00:03:31.250
but because these are perpendicular
00:03:31.250 --> 00:03:32.510
to the direction of motion,
00:03:32.510 --> 00:03:33.420
they do no work.
00:03:33.420 --> 00:03:35.650
And so, when we're gonna use
this work-energy principle,
00:03:35.650 --> 00:03:36.690
they're not even gonna factor in.
00:03:36.690 --> 00:03:38.120
We don't even have to know these
00:03:38.120 --> 00:03:40.160
since they were perpendicular
and did no work.
00:03:40.160 --> 00:03:42.727
You only consider the forces
in the direction of motion.
00:03:42.727 --> 00:03:44.730
So, let's say there was a wind gust
00:03:44.730 --> 00:03:47.330
helping you to the left
here of 200 newtons,
00:03:47.330 --> 00:03:50.150
but this is a big, bulky
balloon, not that aerodynamic.
00:03:50.150 --> 00:03:51.890
And so, there was a drag force
00:03:51.890 --> 00:03:55.100
from air resistance of
104 newtons to the right.
00:03:55.100 --> 00:03:57.530
And what we wanna know
is we wanna determine
00:03:57.530 --> 00:03:59.150
the final speed of the hot air balloon
00:03:59.150 --> 00:04:02.170
after it travels 50 meters
directly to the left
00:04:02.170 --> 00:04:03.560
with the forces shown.
00:04:03.560 --> 00:04:05.490
Now, there's lots of
different ways to do this.
00:04:05.490 --> 00:04:06.820
You know, Newton's laws,
00:04:06.820 --> 00:04:10.330
you can do a kinematic formula,
there's all kinds of stuff,
00:04:10.330 --> 00:04:12.170
even momentum, technically, impulse,
00:04:12.170 --> 00:04:14.399
but the easiest, I'm pretty
sure the easiest way to do this
00:04:14.399 --> 00:04:17.310
is just gonna be the
work-energy principle,
00:04:17.310 --> 00:04:19.900
which states that the net work done
00:04:19.900 --> 00:04:22.690
is gonna equal the
change in kinetic energy.
00:04:22.690 --> 00:04:23.620
So, let's go ahead and do it.
00:04:23.620 --> 00:04:25.430
So, we know that net work is equal
00:04:25.430 --> 00:04:27.360
to the magnitude of the net force
00:04:27.360 --> 00:04:29.580
times the magnitude of
the distance traveled
00:04:29.580 --> 00:04:31.490
times cosine of the angle between them.
00:04:31.490 --> 00:04:33.050
What's change in kinetic energy mean?
00:04:33.050 --> 00:04:35.970
Well, change in anything
is final minus initial.
00:04:35.970 --> 00:04:39.530
So, since kinetic energy
is 1/2 m v squared,
00:04:39.530 --> 00:04:42.530
this is just gonna be
1/2 m v final squared,
00:04:42.530 --> 00:04:46.710
minus 1/2 m v initial squared.
00:04:46.710 --> 00:04:48.470
So, that's gonna be the
change in kinetic energy,
00:04:48.470 --> 00:04:49.760
final minus initial.
00:04:49.760 --> 00:04:50.910
All right, let's plug in numbers here.
00:04:50.910 --> 00:04:52.660
So, net force, how do we get that?
00:04:52.660 --> 00:04:53.580
Vertical pieces don't matter.
00:04:53.580 --> 00:04:54.860
We're just looking horizontally here.
00:04:54.860 --> 00:04:56.340
Those were the only ones
that are gonna affect it.
00:04:56.340 --> 00:04:58.040
These vertical ones just cancel.
00:04:58.040 --> 00:05:01.180
So, we have 200 to the
left, 104 to the right.
00:05:01.180 --> 00:05:02.320
So, we're gonna have to subtract those
00:05:02.320 --> 00:05:04.270
to get 96 to the left.
00:05:04.270 --> 00:05:05.370
And we just want magnitude.
00:05:05.370 --> 00:05:09.280
So, I'm gonna get 96 newtons to the left,
00:05:09.280 --> 00:05:11.770
not negative or anything,
I'm just taking magnitude,
00:05:11.770 --> 00:05:13.020
times the distance traveled.
00:05:13.020 --> 00:05:14.207
We know that's 50.
00:05:14.207 --> 00:05:18.720
So, we get times 50 meters,
cosine of the angle.
00:05:18.720 --> 00:05:19.553
Now, this is careful.
00:05:19.553 --> 00:05:20.860
You might be like, "Oh 180 here."
00:05:20.860 --> 00:05:23.330
But no, the net force points to the left.
00:05:23.330 --> 00:05:25.060
This 200 is winning here.
00:05:25.060 --> 00:05:27.570
So, leftward net force and
the leftward direction,
00:05:27.570 --> 00:05:29.468
the angle between those two is zero,
00:05:29.468 --> 00:05:31.820
cosine of zero is just one.
00:05:31.820 --> 00:05:33.010
We're maxed out here.
00:05:33.010 --> 00:05:36.200
So, net force points in
the direction of motion.
00:05:36.200 --> 00:05:38.797
So, equals, let's plug
in the rest of this,
00:05:38.797 --> 00:05:42.410
1/2, the mass is 300 kilograms,
00:05:42.410 --> 00:05:44.040
times v final squared,
00:05:44.040 --> 00:05:45.570
that's what we wanna determine,
00:05:45.570 --> 00:05:49.883
minus 1/2, 300 kilograms,
00:05:51.630 --> 00:05:54.890
times the initial speed is
seven meters per second.
00:05:54.890 --> 00:05:58.359
So, we got seven meters per squared.
00:05:58.359 --> 00:06:01.467
Well, 96 times 50 is
gonna come out to 4,800.
00:06:02.590 --> 00:06:04.960
That means that's the net work done.
00:06:04.960 --> 00:06:06.370
Notice that's joules.
00:06:06.370 --> 00:06:08.210
That's how much energy we've added.
00:06:08.210 --> 00:06:09.840
That's the change in kinetic energy.
00:06:09.840 --> 00:06:11.790
So, we know the net work is
change in kinetic energy.
00:06:11.790 --> 00:06:14.864
We've added 4,800 joules
of kinetic energy.
00:06:14.864 --> 00:06:19.864
That's gonna have to equal,
half of 300 is 150 kilograms,
00:06:21.160 --> 00:06:23.630
times v final squared,
00:06:23.630 --> 00:06:28.630
minus, if you take a half
of 300 times seven squared,
00:06:28.700 --> 00:06:31.710
you're gonna get 7,350.
00:06:31.710 --> 00:06:32.890
So, this is how much energy
00:06:32.890 --> 00:06:35.410
the hot air balloon
started with initially.
00:06:35.410 --> 00:06:36.650
So, after we moved that to the left,
00:06:36.650 --> 00:06:38.070
we add those together.
00:06:38.070 --> 00:06:41.760
I'm gonna get 12,150 joules
00:06:41.760 --> 00:06:45.050
is how much kinetic energy
the balloon ends with.
00:06:45.050 --> 00:06:48.740
And that's gotta equal 150 kilograms
00:06:48.740 --> 00:06:50.800
times v final squared.
00:06:50.800 --> 00:06:55.800
I could divide 12,150 by
150 and you get exactly 81
00:06:56.743 --> 00:06:59.530
and that's gonna equal v final squared.
00:06:59.530 --> 00:07:01.050
And if you take a square root of that,
00:07:01.050 --> 00:07:02.440
you get exactly nine.
00:07:02.440 --> 00:07:04.664
So, the final velocity
of this hot air balloon
00:07:04.664 --> 00:07:06.970
is nine meters per second.
00:07:06.970 --> 00:07:07.894
It sped up.
00:07:07.894 --> 00:07:09.630
That's not surprising.
00:07:09.630 --> 00:07:11.850
This net force was directed leftward
00:07:11.850 --> 00:07:13.890
and the object was moving leftward.
00:07:13.890 --> 00:07:14.930
So, we're doing positive work.
00:07:14.930 --> 00:07:16.640
We're increasing the kinetic energy.
00:07:16.640 --> 00:07:17.928
We started with seven meters per second.
00:07:17.928 --> 00:07:20.210
We ended up with nine meters per second.
00:07:20.210 --> 00:07:21.043
And this is an example
00:07:21.043 --> 00:07:23.180
of how you use the work-energy principle.
00:07:23.180 --> 00:07:24.160
So, to recap,
00:07:24.160 --> 00:07:25.470
the work-energy principle states,
00:07:25.470 --> 00:07:28.110
the net work is equal to the
change in kinetic energy.
00:07:28.110 --> 00:07:29.520
This can help you just conceptually
00:07:29.520 --> 00:07:31.350
or qualitatively determine
00:07:31.350 --> 00:07:33.200
whether something is
gonna speed up, slow down,
00:07:33.200 --> 00:07:34.960
or change direction or both.
00:07:34.960 --> 00:07:36.010
And then, quantitatively,
00:07:36.010 --> 00:07:37.930
you can use this to specifically solve
00:07:37.930 --> 00:07:40.140
for the change in kinetic energy,
00:07:40.140 --> 00:07:42.830
as well as the final or initial speed
00:07:42.830 --> 00:07:44.053
something might've had.
|
Changes in Momentum Worked Examples | https://www.youtube.com/watch?v=5_bdL_g-X9I | vtt | https://www.youtube.com/api/timedtext?v=5_bdL_g-X9I&ei=2VWUZZPdNtu3mLAPuP2hyAU&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245321&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=375DC510BF8E9A0E6A93AC0745ED304EBAC8F289.DF32C7FD8721BF58AD1468B5709550EE9A1844A6&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.250 --> 00:00:01.430
- [Instructor] So, here's a pink ball
00:00:01.430 --> 00:00:03.610
rolling toward a green cube
00:00:03.610 --> 00:00:05.878
that's sitting at rest on
a frictionless surface.
00:00:05.878 --> 00:00:09.920
When the pink ball hits and
slams into the green cube,
00:00:09.920 --> 00:00:12.490
it's gonna exert a force to
the right on the green cube
00:00:12.490 --> 00:00:14.270
and the green cube's gonna speed up.
00:00:14.270 --> 00:00:16.250
But because of Newton's third law,
00:00:16.250 --> 00:00:17.970
whatever force the pink ball
00:00:17.970 --> 00:00:19.860
exerts on the green cube to the right
00:00:19.860 --> 00:00:22.090
has to be equal and opposite to the force
00:00:22.090 --> 00:00:25.600
the green cube exerts
backward on the pink ball.
00:00:25.600 --> 00:00:27.860
So, the green cube's
gonna gain some momentum,
00:00:27.860 --> 00:00:29.800
but the pink ball is
gonna lose some momentum.
00:00:29.800 --> 00:00:31.520
And here's the cool thing.
00:00:31.520 --> 00:00:34.390
Whatever momentum is
gained by this green cube
00:00:34.390 --> 00:00:36.310
has to be the same amount of momentum
00:00:36.310 --> 00:00:38.410
that's lost by the pink ball.
00:00:38.410 --> 00:00:40.510
So, if the green cube gained
00:00:40.510 --> 00:00:42.560
three units of momentum to the right,
00:00:42.560 --> 00:00:44.210
and then, the pink ball has to lose
00:00:44.210 --> 00:00:45.870
three units of momentum to the right.
00:00:45.870 --> 00:00:46.960
And this is true,
00:00:46.960 --> 00:00:49.540
whether these are the same
mass or different masses,
00:00:49.540 --> 00:00:50.760
or whether the green cube
00:00:50.760 --> 00:00:52.890
was moving left to
start or right to start.
00:00:52.890 --> 00:00:53.840
However they collide,
00:00:53.840 --> 00:00:55.340
if two objects collide,
00:00:55.340 --> 00:00:57.670
the change in momentum
between the two objects
00:00:57.670 --> 00:00:59.760
has to be equal and opposite.
00:00:59.760 --> 00:01:01.300
And this is why we love momentum.
00:01:01.300 --> 00:01:02.750
Whatever momentum is gained by one
00:01:02.750 --> 00:01:04.230
has to be lost by the other.
00:01:04.230 --> 00:01:05.840
And so, how is that possible?
00:01:05.840 --> 00:01:07.000
You might be like, "How can that work?"
00:01:07.000 --> 00:01:08.250
Well, let's go up here.
00:01:08.250 --> 00:01:09.620
Think about these forces.
00:01:09.620 --> 00:01:12.150
The forces on each object
are equal and opposite.
00:01:12.150 --> 00:01:13.300
Here's the cool part though.
00:01:13.300 --> 00:01:17.150
The time they're in contact
also has to be equal
00:01:17.150 --> 00:01:19.786
because as soon as one of them
loses contact with the other,
00:01:19.786 --> 00:01:22.580
the other loses contact with the one.
00:01:22.580 --> 00:01:26.050
And in physics, force times
time is called the impulse.
00:01:26.050 --> 00:01:28.260
Now, this is the change in momentum.
00:01:28.260 --> 00:01:29.870
This will equal the change in momentum.
00:01:29.870 --> 00:01:31.100
So, if you wanna know how much momentum
00:01:31.100 --> 00:01:33.508
was gained by this green cube,
00:01:33.508 --> 00:01:36.490
multiply the force
exerted on it by the time,
00:01:36.490 --> 00:01:38.630
you'll get the change in
momentum of the green cube.
00:01:38.630 --> 00:01:39.780
That's true for this pink ball.
00:01:39.780 --> 00:01:41.710
And look, the force is backwards.
00:01:41.710 --> 00:01:44.368
It's just the negative
of this other impulse.
00:01:44.368 --> 00:01:46.900
So, this is why the pink ball,
00:01:46.900 --> 00:01:49.170
no matter what it's mass
or how fast it's going,
00:01:49.170 --> 00:01:50.244
same with green cube,
00:01:50.244 --> 00:01:54.300
these changes in momentum
must be equal and opposite
00:01:54.300 --> 00:01:56.980
simply due to Newton's third law.
00:01:56.980 --> 00:01:58.520
So, to be clear, what I'm saying is this.
00:01:58.520 --> 00:02:00.490
If you are to graph the momentum,
00:02:00.490 --> 00:02:03.340
this pink ball would have
started off with some momentum.
00:02:03.340 --> 00:02:05.600
And that would have been
constant before the collision
00:02:05.600 --> 00:02:07.520
if there's no friction or resistance.
00:02:07.520 --> 00:02:08.840
But then, it lost some momentum.
00:02:08.840 --> 00:02:11.520
So, this goes down and
maybe end up right here.
00:02:11.520 --> 00:02:13.160
And then, afterward, it'll maintain
00:02:13.160 --> 00:02:14.910
a constant amount of momentum.
00:02:14.910 --> 00:02:17.220
The green box, the green cube here,
00:02:17.220 --> 00:02:19.188
started with zero
momentum, it was at rest.
00:02:19.188 --> 00:02:21.980
During this collision,
it gained some momentum.
00:02:21.980 --> 00:02:24.110
So, it's gonna jump up maybe to here.
00:02:24.110 --> 00:02:27.430
What I'm saying is that, and
afterward, it stays constant,
00:02:27.430 --> 00:02:29.759
what I'm saying is that
these two jumps are the same.
00:02:29.759 --> 00:02:31.780
You know, if this thing lost,
00:02:31.780 --> 00:02:34.900
let's say it lost four units of momentum,
00:02:34.900 --> 00:02:37.140
well then, this green cube has to gain
00:02:37.140 --> 00:02:38.357
four units of momentum.
00:02:38.357 --> 00:02:40.010
And you might be like,
"Okay, I don't care."
00:02:40.010 --> 00:02:41.190
But here's why you should care.
00:02:41.190 --> 00:02:44.260
If you are to graph the total momentum,
00:02:44.260 --> 00:02:47.010
what this means is that
the total momentum,
00:02:47.010 --> 00:02:48.930
which was just the pink ball initially,
00:02:48.930 --> 00:02:51.150
is gonna remain constant the whole time.
00:02:51.150 --> 00:02:55.450
It's as if the momentum never
realized a collision occurred.
00:02:55.450 --> 00:02:58.660
This total momentum just remains constant.
00:02:58.660 --> 00:03:01.400
And this is why conservation
and momentum is a thing.
00:03:01.400 --> 00:03:02.750
It is why it's really useful.
00:03:02.750 --> 00:03:05.600
The total initial momentum in a system,
00:03:05.600 --> 00:03:09.000
even if a collision occurs
between objects in that system,
00:03:09.000 --> 00:03:11.460
the total initial momentum must be equal
00:03:11.460 --> 00:03:13.690
to the total final momentum.
00:03:13.690 --> 00:03:16.330
As long as the forces are only internal,
00:03:16.330 --> 00:03:18.277
that is to say between
objects in the system,
00:03:18.277 --> 00:03:20.280
and there's no external forces,
00:03:20.280 --> 00:03:21.820
then, this will always be true.
00:03:21.820 --> 00:03:24.160
So, this is a super powerful tool
00:03:24.160 --> 00:03:26.110
we can use to problem-solve.
00:03:26.110 --> 00:03:28.070
This saves us a lot of time and trouble.
00:03:28.070 --> 00:03:29.240
If a collision is occurring,
00:03:29.240 --> 00:03:32.060
this is one of our best
methods to solve for things
00:03:32.060 --> 00:03:33.825
is conservation of momentum.
00:03:33.825 --> 00:03:35.170
Now, keep in mind.
00:03:35.170 --> 00:03:37.350
Even though the total momentum in a system
00:03:37.350 --> 00:03:38.461
has to stay the same,
00:03:38.461 --> 00:03:40.730
the momentum of an individual object
00:03:40.730 --> 00:03:42.220
does not have to stay the same.
00:03:42.220 --> 00:03:44.679
These objects can exchange
momentum, but again,
00:03:44.679 --> 00:03:47.010
the reason this is gonna be conserved
00:03:47.010 --> 00:03:48.500
is that they do so equally.
00:03:48.500 --> 00:03:51.540
If one gains five, the
other loses five and so on,
00:03:51.540 --> 00:03:53.550
and the total amount stays the same.
00:03:53.550 --> 00:03:55.230
So, let me show you how
this works real quick.
00:03:55.230 --> 00:03:57.200
So, to give you an idea numerically here.
00:03:57.200 --> 00:03:59.450
So, let's say the pink
ball was two kilograms
00:03:59.450 --> 00:04:01.565
and it was going five
meters per second start.
00:04:01.565 --> 00:04:05.330
And the green cube had a
mass, m, and afterward,
00:04:05.330 --> 00:04:08.110
let's say the pink ball's
going four meters per seconds.
00:04:08.110 --> 00:04:09.040
So, it's slowed down.
00:04:09.040 --> 00:04:10.650
And the green cubes speeds up.
00:04:10.650 --> 00:04:12.620
Let's say, it's going
eight meters per second.
00:04:12.620 --> 00:04:14.640
You might think, "Wait,
this isn't conserved.
00:04:14.640 --> 00:04:18.310
The pink ball only lost one, five to four,
00:04:18.310 --> 00:04:20.130
but the green cube gained eight."
00:04:20.130 --> 00:04:22.040
But, remember, we're
not conserving velocity.
00:04:22.040 --> 00:04:24.130
We're conserving momentum.
00:04:24.130 --> 00:04:26.690
So, momentum is m times v,
00:04:26.690 --> 00:04:28.740
momentum is mv,
00:04:28.740 --> 00:04:30.060
and it's a vector, you gotta be careful.
00:04:30.060 --> 00:04:31.430
It has a direction.
00:04:31.430 --> 00:04:33.620
So, I'm not saying the amount
of velocity is conserved
00:04:33.620 --> 00:04:34.453
or anything like that.
00:04:34.453 --> 00:04:35.520
I'm saying momentum is conserved.
00:04:35.520 --> 00:04:38.270
So, what I'm saying is
that p initial total
00:04:38.270 --> 00:04:41.040
has to equal p final total.
00:04:41.040 --> 00:04:43.560
So, only the pink ball
had momentum initially.
00:04:43.560 --> 00:04:46.370
So, it had two kilograms
00:04:46.370 --> 00:04:49.920
times five meters per second of momentum.
00:04:49.920 --> 00:04:52.520
To start with, the green cube had none.
00:04:52.520 --> 00:04:53.978
So, this has gotta equal.
00:04:53.978 --> 00:04:57.390
Afterward, the pink ball has two kilograms
00:04:57.390 --> 00:05:00.170
times four meters per second.
00:05:00.170 --> 00:05:02.320
And the green cube does
have momentum afterward.
00:05:02.320 --> 00:05:03.153
Now, we gotta add it up.
00:05:03.153 --> 00:05:04.130
There's gotta be the total momentum.
00:05:04.130 --> 00:05:06.800
So, plus mass of the cube
00:05:06.800 --> 00:05:09.570
times its eight meters per second.
00:05:09.570 --> 00:05:10.640
Well, so this isn't too hard.
00:05:10.640 --> 00:05:11.473
The math here is easy.
00:05:11.473 --> 00:05:13.080
So, this is gonna be 10 units of momentum,
00:05:13.080 --> 00:05:15.410
10 kilogram meters per second
00:05:15.410 --> 00:05:17.160
is what the ball started with.
00:05:17.160 --> 00:05:18.020
And then, the ball is gonna end
00:05:18.020 --> 00:05:21.220
with eight kilogram meters per second.
00:05:21.220 --> 00:05:22.053
So, we can see right here,
00:05:22.053 --> 00:05:24.330
the ball lost two units of momentum.
00:05:24.330 --> 00:05:26.500
That means the green cube better gain
00:05:26.500 --> 00:05:27.333
two units of momentum.
00:05:27.333 --> 00:05:29.980
So, it's gonna be plus m times eight.
00:05:29.980 --> 00:05:30.813
And so, this is what I mean
00:05:30.813 --> 00:05:32.200
when this can help you solve problems,
00:05:32.200 --> 00:05:33.360
we can just solve for the mass now.
00:05:33.360 --> 00:05:35.530
Now, we can know what the
mass of the cube had to be.
00:05:35.530 --> 00:05:38.600
So, 10 minus eight,
it's gonna be two units.
00:05:38.600 --> 00:05:41.976
It's how much momentum this
green cube has to gain.
00:05:41.976 --> 00:05:44.530
And if we divide two by eight,
00:05:44.530 --> 00:05:46.740
we get that the mass of the green cube
00:05:46.740 --> 00:05:50.610
had to be .25 kilograms.
00:05:50.610 --> 00:05:55.436
So, indeed, if we took the
.25 kilograms times the eight
00:05:55.436 --> 00:05:58.130
that this cube ended with, .25 times eight
00:05:58.130 --> 00:06:00.140
really does give us two, positive two,
00:06:00.140 --> 00:06:03.270
it gained two units of momentum.
00:06:03.270 --> 00:06:05.660
This is why momentum is conserved.
00:06:05.660 --> 00:06:07.434
Whatever a gain in
momentum one thing gets,
00:06:07.434 --> 00:06:09.709
there's a corresponding loss in the other.
00:06:09.709 --> 00:06:12.190
And so, this is gonna be equal.
00:06:12.190 --> 00:06:15.770
Now, how could you ever make
it so that this was not equal?
00:06:15.770 --> 00:06:17.580
Well, this will always be equal
00:06:17.580 --> 00:06:19.140
if the only force is being exerted
00:06:19.140 --> 00:06:20.480
are internal to your system.
00:06:20.480 --> 00:06:23.320
The only way you make this nonequal
00:06:23.320 --> 00:06:25.420
is to have external forces.
00:06:25.420 --> 00:06:26.530
What would that look like?
00:06:26.530 --> 00:06:30.300
Well, imagine the ball and
the cube were on a ramp now.
00:06:30.300 --> 00:06:32.220
So, now that this thing's inclined,
00:06:32.220 --> 00:06:35.370
gravity is gonna be
exerting an external force.
00:06:35.370 --> 00:06:37.150
Let's say it sit like 30 degrees.
00:06:37.150 --> 00:06:40.222
And if we graph the total
momentum of the ball and cube,
00:06:40.222 --> 00:06:42.740
it's not gonna be a straight line anymore.
00:06:42.740 --> 00:06:44.770
It is not gonna look like this.
00:06:44.770 --> 00:06:45.780
That's what it looked like before
00:06:45.780 --> 00:06:47.470
when there were no external forces.
00:06:47.470 --> 00:06:49.540
This time, it's gonna be angled up.
00:06:49.540 --> 00:06:51.430
Let's just call down the ramp positive.
00:06:51.430 --> 00:06:53.270
This time, it's gonna look like this.
00:06:53.270 --> 00:06:55.330
Gravity's pulling down the ramp.
00:06:55.330 --> 00:06:57.100
Let's call that the positive direction.
00:06:57.100 --> 00:06:58.860
If we're measuring the momentum
00:06:58.860 --> 00:07:00.993
in that parallel to the ramp direction,
00:07:00.993 --> 00:07:03.690
we're gonna see an increase
in momentum that direction,
00:07:03.690 --> 00:07:04.523
because that's the way
00:07:04.523 --> 00:07:07.856
that this external
force of gravity points.
00:07:07.856 --> 00:07:09.810
So, how much will this increase?
00:07:09.810 --> 00:07:11.840
How could you figure out what the change
00:07:11.840 --> 00:07:14.120
in the total momentum is gonna be?
00:07:14.120 --> 00:07:16.040
One way to do it is to find the impulse.
00:07:16.040 --> 00:07:19.770
So, remember, force times time
would give you the impulse.
00:07:19.770 --> 00:07:21.550
Let's just say we were looking at this
00:07:21.550 --> 00:07:23.730
for about one second of the time
00:07:23.730 --> 00:07:25.130
that these were on the ramp.
00:07:25.130 --> 00:07:26.820
And let's say they have
the values they did before.
00:07:26.820 --> 00:07:30.620
So, two kilograms and .25 kilograms.
00:07:30.620 --> 00:07:34.790
That would mean the force down
the ramp is mg sine theta.
00:07:34.790 --> 00:07:38.060
So, the force along this
parallel direction is m,
00:07:38.060 --> 00:07:42.440
which the total mass of our
system is 2.25 kilograms.
00:07:42.440 --> 00:07:47.380
So, m times g, 9.8, times sine of 30.
00:07:47.380 --> 00:07:48.940
So, you need to take this sine of 30
00:07:48.940 --> 00:07:50.640
if you wanna know the change in momentum
00:07:50.640 --> 00:07:52.090
along this ramp direction.
00:07:52.090 --> 00:07:57.030
So, the force of gravity
parallel is mg sine theta.
00:07:57.030 --> 00:07:58.220
And then, that's the force.
00:07:58.220 --> 00:07:59.670
So, that's the force parallel to the ramp.
00:07:59.670 --> 00:08:01.970
That would give us the
change in momentum parallel.
00:08:01.970 --> 00:08:04.803
We just have to multiply by
the time, which is one second.
00:08:04.803 --> 00:08:09.140
And that gives us about
11 units of momentum.
00:08:09.140 --> 00:08:12.690
So, this system would
gain 11 units of momentum.
00:08:12.690 --> 00:08:13.673
That doesn't tell you who's gonna get it.
00:08:13.673 --> 00:08:15.520
It's not like the two gets all of it,
00:08:15.520 --> 00:08:17.260
or the .25 gets all of it.
00:08:17.260 --> 00:08:18.470
But the total system,
00:08:18.470 --> 00:08:19.860
if you watched for a second,
00:08:19.860 --> 00:08:21.689
while it's on this
ramp, frictionless ramp,
00:08:21.689 --> 00:08:23.448
it would increase its momentum.
00:08:23.448 --> 00:08:25.397
It'd be changing its total momentum
00:08:25.397 --> 00:08:28.780
because there was an external force.
00:08:28.780 --> 00:08:32.090
So, recapping, if there are no
external forces on a system,
00:08:32.090 --> 00:08:33.534
then, the total momentum initial
00:08:33.534 --> 00:08:37.110
will equal the total momentum final.
00:08:37.110 --> 00:08:39.520
So, using p equals mv,
00:08:39.520 --> 00:08:41.380
you can add up these contributions
00:08:41.380 --> 00:08:43.070
and set them equal to problem-solve.
00:08:43.070 --> 00:08:46.020
And in a case where there
is an external force,
00:08:46.020 --> 00:08:48.040
you can find how much that system
00:08:48.040 --> 00:08:50.030
will gain or lose in momentum
00:08:50.030 --> 00:08:52.100
by taking that external force
00:08:52.100 --> 00:08:54.550
times the time that force was applied.
00:08:54.550 --> 00:08:57.140
That would give you the
total change in momentum
00:08:57.140 --> 00:08:59.153
of that system over that time.
|
Torque Basics | https://www.youtube.com/watch?v=TQQXpFhACSU | vtt | https://www.youtube.com/api/timedtext?v=TQQXpFhACSU&ei=3FWUZcrGC4qRvdIPrMyc6AU&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=37F4CAFA0F9E170721DD6EDE552B512E0D8D3C04.D0AC6A5B2487A6FD83B3AD3E879423894B48D57F&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.250 --> 00:00:01.540
- [Instructor] Imagine
you've got a door here
00:00:01.540 --> 00:00:03.310
with a blue door knob.
00:00:03.310 --> 00:00:05.370
Any one of these 10 newton forces
00:00:05.370 --> 00:00:09.170
will cause the door to rotate
around the hinge or the axis,
00:00:09.170 --> 00:00:11.320
or sometimes this is
called the pivot point.
00:00:11.320 --> 00:00:13.930
Any one of these forces will
cause the door to rotate.
00:00:13.930 --> 00:00:16.090
My question is, if you
could insert one of these
00:00:16.090 --> 00:00:17.640
in one of these locations,
00:00:17.640 --> 00:00:19.650
which one of these forces, if any,
00:00:19.650 --> 00:00:23.310
would cause the most angular
acceleration of this door?
00:00:23.310 --> 00:00:26.070
And you might think, "Oh,
well, 10 newtons is 10 newtons.
00:00:26.070 --> 00:00:28.750
They'll all cause the same
amount," but that's not true.
00:00:28.750 --> 00:00:30.080
It turns out we put door knobs
00:00:30.080 --> 00:00:32.210
at the end of doors for a reason.
00:00:32.210 --> 00:00:34.280
This red 10 newtons at the outside edge
00:00:34.280 --> 00:00:36.840
will cause the most angular acceleration.
00:00:36.840 --> 00:00:39.570
It'll cause this door to
speed up most rapidly.
00:00:39.570 --> 00:00:40.630
And this used to bother me.
00:00:40.630 --> 00:00:43.230
I was like, "How come this
is getting an advantage?"
00:00:43.230 --> 00:00:45.010
I think the best way to
think about it is this.
00:00:45.010 --> 00:00:46.930
Even though these forces
are all going through
00:00:46.930 --> 00:00:49.597
the same angle, so they've
gone through 20 degrees,
00:00:49.597 --> 00:00:51.870
and now they've all
gone through 30 degrees,
00:00:51.870 --> 00:00:55.760
now they've all gone
through 45, 60 and 90.
00:00:55.760 --> 00:00:57.120
Even though these forces
00:00:57.120 --> 00:00:58.710
have all gone through the same angle,
00:00:58.710 --> 00:01:01.320
they have not gone
through the same distance.
00:01:01.320 --> 00:01:02.153
Some of these forces
00:01:02.153 --> 00:01:03.860
have been exerted through
a larger distance.
00:01:03.860 --> 00:01:04.760
So just look at it.
00:01:04.760 --> 00:01:06.830
If you imagine rotating this thing,
00:01:06.830 --> 00:01:09.770
that red force, this
outside pink force here
00:01:09.770 --> 00:01:12.230
goes through a much larger distance
00:01:12.230 --> 00:01:14.410
than that inner yellow force.
00:01:14.410 --> 00:01:17.190
This force has gone through
very little distance whatsoever.
00:01:17.190 --> 00:01:18.840
And you might think, well,
why does that matter?
00:01:18.840 --> 00:01:22.260
Well, it matters because
if you remember work done.
00:01:22.260 --> 00:01:24.670
Work done is proportional
to the amount of force,
00:01:24.670 --> 00:01:25.780
but these are all 10 newtons
00:01:25.780 --> 00:01:27.370
so that doesn't really matter here.
00:01:27.370 --> 00:01:29.560
And it's also proportional
to the amount of distance
00:01:29.560 --> 00:01:31.280
through which that force is applied.
00:01:31.280 --> 00:01:33.360
And because this outside force
00:01:33.360 --> 00:01:35.590
has gone through so much more distance
00:01:35.590 --> 00:01:37.440
than these inner forces,
00:01:37.440 --> 00:01:40.240
it's done more work over the same angle.
00:01:40.240 --> 00:01:42.180
And if you do more work,
00:01:42.180 --> 00:01:44.930
you input more kinetic
energy into the door,
00:01:44.930 --> 00:01:48.560
it's gonna be moving
faster for the same angle
00:01:48.560 --> 00:01:51.610
compared to what's caused
by these other forces here.
00:01:51.610 --> 00:01:53.550
And this is why in angular mechanics
00:01:53.550 --> 00:01:55.370
you can't just think about forces,
00:01:55.370 --> 00:01:58.160
you have to think about
something called torque.
00:01:58.160 --> 00:02:00.880
The symbol for torque is this fancy T.
00:02:00.880 --> 00:02:02.820
It's the Greek letter tau.
00:02:02.820 --> 00:02:05.210
And the amount of torque
caused by a force,
00:02:05.210 --> 00:02:07.380
so you need a force to cause a torque,
00:02:07.380 --> 00:02:08.740
but it's more than just force.
00:02:08.740 --> 00:02:10.620
You have to multiply r,
00:02:10.620 --> 00:02:13.190
the distance from the access to the force
00:02:13.190 --> 00:02:15.170
by the amount of force
00:02:15.170 --> 00:02:17.790
in order to find how much
torque is being exerted
00:02:17.790 --> 00:02:19.350
by a given force.
00:02:19.350 --> 00:02:21.220
The more torque that's exerted,
00:02:21.220 --> 00:02:23.900
the more angular acceleration you'd get,
00:02:23.900 --> 00:02:25.960
the faster you'd get
something to speed up.
00:02:25.960 --> 00:02:26.793
Now you might wonder like,
00:02:26.793 --> 00:02:29.210
"Okay, I get that more
force gives me more torque,
00:02:29.210 --> 00:02:31.690
how come this is just r
and not like r squared?
00:02:31.690 --> 00:02:34.100
It seems kind of random, maybe
its like square root of r."
00:02:34.100 --> 00:02:37.240
Well, if you remember arc
lengths from back in the day,
00:02:37.240 --> 00:02:39.550
arc length is r times theta.
00:02:39.550 --> 00:02:42.650
So if I'm twice as far away from an axis,
00:02:42.650 --> 00:02:44.400
I get twice the arc length.
00:02:44.400 --> 00:02:47.170
If I get twice the arc length,
I get twice the work done.
00:02:47.170 --> 00:02:48.180
You get twice the work done,
00:02:48.180 --> 00:02:50.350
you get twice the input kinetic energy
00:02:50.350 --> 00:02:52.470
and it turns out twice the kinetic energy
00:02:52.470 --> 00:02:54.940
will give you twice the
angular acceleration.
00:02:54.940 --> 00:02:57.680
This is why everything
is just proportional to r
00:02:57.680 --> 00:03:00.510
in terms of torque, it's
not like r squared here.
00:03:00.510 --> 00:03:03.830
So for example, let's just say
the distance from the axis,
00:03:03.830 --> 00:03:04.663
because that's what matters,
00:03:04.663 --> 00:03:07.080
to this 10 newtons here was one meter.
00:03:07.080 --> 00:03:10.210
And from the access to the
purple force was two meters.
00:03:10.210 --> 00:03:14.180
And from the access to this
doorknob force was three meters.
00:03:14.180 --> 00:03:16.070
What this torque formula
means is that even though
00:03:16.070 --> 00:03:17.330
these are all 10 newtons,
00:03:17.330 --> 00:03:19.170
they'd all be exerting
different amounts of torque.
00:03:19.170 --> 00:03:21.680
I'd have to take the one
meter times 10 newtons
00:03:21.680 --> 00:03:24.160
would give me 10 newton meters.
00:03:24.160 --> 00:03:27.710
So the unit for torque
is meters times newtons,
00:03:27.710 --> 00:03:29.970
but we usually write it as newton meters.
00:03:29.970 --> 00:03:31.240
If you buy a torque wrench,
00:03:31.240 --> 00:03:34.170
you could set it in newton
meters or in foot pounds,
00:03:34.170 --> 00:03:36.470
if you're doing the US system.
00:03:36.470 --> 00:03:38.420
And then this purple force,
even though it's 10 newtons,
00:03:38.420 --> 00:03:41.360
you'd have to take two
meters times 10 newtons.
00:03:41.360 --> 00:03:45.290
This would exert a torque
of 20 newton meters
00:03:45.290 --> 00:03:47.280
and the doorknob force wins the battle
00:03:47.280 --> 00:03:51.100
because it would have three
times 10 would exert a torque
00:03:51.100 --> 00:03:53.140
of 30 newton meters.
00:03:53.140 --> 00:03:56.070
So the same size force can
exert a different amount
00:03:56.070 --> 00:03:59.070
of torque, depending on how
far away it is from the axis.
00:03:59.070 --> 00:04:01.020
So one area you have to
be careful of this torque
00:04:01.020 --> 00:04:02.480
technically is a vector.
00:04:02.480 --> 00:04:03.313
It has a direction,
00:04:03.313 --> 00:04:04.710
it could be positive or negative.
00:04:04.710 --> 00:04:07.690
If you're doing full-blown
engineering 3D physics,
00:04:07.690 --> 00:04:10.450
technically these torques would
point out of the screen here
00:04:10.450 --> 00:04:13.350
out of the page, but for
intro algebra-based physics,
00:04:13.350 --> 00:04:15.700
and for most problems, you
can usually get away with
00:04:15.700 --> 00:04:19.730
just considering
counterclockwise or clockwise
00:04:19.730 --> 00:04:21.810
as being the direction of the torque.
00:04:21.810 --> 00:04:25.410
That is to say these forces
were making this object rotate
00:04:25.410 --> 00:04:27.840
in the counterclockwise direction,
00:04:27.840 --> 00:04:29.630
so they were all at the same sign.
00:04:29.630 --> 00:04:32.590
The convention is to call
counterclockwise positive.
00:04:32.590 --> 00:04:34.230
So we'd call these all positive.
00:04:34.230 --> 00:04:37.440
If there were any forces that
tried to rotate the system
00:04:37.440 --> 00:04:40.140
clockwise, you'd call
those torques negative.
00:04:40.140 --> 00:04:42.600
You can do it either way, as
long as you're consistent.
00:04:42.600 --> 00:04:44.740
Most books pick this as
the convention though,
00:04:44.740 --> 00:04:45.890
so you should be aware of that.
00:04:45.890 --> 00:04:47.560
And then the last little
bit to be careful about,
00:04:47.560 --> 00:04:50.180
I'm drawing all these forces
nice and perpendicular
00:04:50.180 --> 00:04:53.960
to the r, and if that's the
case, you just do r times F.
00:04:53.960 --> 00:04:56.200
If your force has different components,
00:04:56.200 --> 00:04:58.080
you need to make sure
that the only component
00:04:58.080 --> 00:05:00.360
you plug in here is the
perpendicular piece.
00:05:00.360 --> 00:05:02.360
So if this had some weird angle here,
00:05:02.360 --> 00:05:05.420
you'd only want the piece
that was directly into
00:05:05.420 --> 00:05:10.060
this perpendicular lever arm
here at a perpendicular angle.
00:05:10.060 --> 00:05:11.480
We'll talk about that more later.
00:05:11.480 --> 00:05:13.980
For now, let's just try some
problems to kick the tires
00:05:13.980 --> 00:05:15.560
and get used to this formula.
00:05:15.560 --> 00:05:16.850
So imagine this example here
00:05:16.850 --> 00:05:18.900
where you've got the fancy door, you know,
00:05:18.900 --> 00:05:20.520
with a fancy hotel or restaurant
00:05:20.520 --> 00:05:22.930
that's a rotating circle and you can go in
00:05:22.930 --> 00:05:23.840
from either direction.
00:05:23.840 --> 00:05:25.470
This would be a bird's-eye view.
00:05:25.470 --> 00:05:27.550
Now, imagine you go into the hotel,
00:05:27.550 --> 00:05:28.383
you're pushing over here,
00:05:28.383 --> 00:05:29.670
you took physics, you know what to do.
00:05:29.670 --> 00:05:31.410
So you exert this 20 newtons over here.
00:05:31.410 --> 00:05:33.310
Let's say someone else comes
in from the other edge.
00:05:33.310 --> 00:05:35.680
It's all awkward and they're
trying to go in the other way
00:05:35.680 --> 00:05:36.740
and it's a stalemate.
00:05:36.740 --> 00:05:39.920
You're both pushing with
forces, but nothing's happening.
00:05:39.920 --> 00:05:41.810
And that doesn't mean
the two forces are equal.
00:05:41.810 --> 00:05:44.650
If you're in a stalemate here
in terms of angular motion,
00:05:44.650 --> 00:05:47.660
that means your torques
are equal and opposite.
00:05:47.660 --> 00:05:49.890
They're opposed, they
have the same magnitude,
00:05:49.890 --> 00:05:51.630
but they'll have opposite
directions of torque.
00:05:51.630 --> 00:05:53.180
So if you're locked in a stalemate here,
00:05:53.180 --> 00:05:55.950
that means the torque that
you exert with your 20 newtons
00:05:55.950 --> 00:05:59.650
has to be equal to the
torque from the other person.
00:05:59.650 --> 00:06:01.370
So let's try to figure out how much force
00:06:01.370 --> 00:06:02.860
would this person have to exert?
00:06:02.860 --> 00:06:04.600
It's not gonna be 20 newtons.
00:06:04.600 --> 00:06:06.480
They're pushing closer to the axis here
00:06:06.480 --> 00:06:08.110
so they're gonna have
to push with more force.
00:06:08.110 --> 00:06:09.230
How much more force?
00:06:09.230 --> 00:06:11.810
Well, we can use the formula
for torque to find it.
00:06:11.810 --> 00:06:13.060
The torques have to be equal.
00:06:13.060 --> 00:06:15.240
If there's no rotation
here, you're balanced out.
00:06:15.240 --> 00:06:16.630
If your force is 20 newtons,
00:06:16.630 --> 00:06:19.910
you're exerting a force three
meters away from the axis.
00:06:19.910 --> 00:06:22.170
That's your r, would be three meters
00:06:22.170 --> 00:06:25.770
times 20 newtons means you're
exerting 20 times three,
00:06:25.770 --> 00:06:27.970
so 60 newton meters of torque.
00:06:27.970 --> 00:06:29.940
That means the other
person has to be exerting
00:06:29.940 --> 00:06:33.000
60 newton meters of torque,
but there r isn't two.
00:06:33.000 --> 00:06:35.140
Be careful here, you always
have to measure from the axis,
00:06:35.140 --> 00:06:36.560
the point where you're rotating about.
00:06:36.560 --> 00:06:38.640
That'd be one meter.
00:06:38.640 --> 00:06:40.210
This door's all symmetric here.
00:06:40.210 --> 00:06:42.590
So it'd be one meter times F.
00:06:42.590 --> 00:06:45.410
And if you take this 60 newton meters
00:06:45.410 --> 00:06:47.260
and you divide by one meter,
00:06:47.260 --> 00:06:48.450
you're gonna get that this force here
00:06:48.450 --> 00:06:50.040
is gonna have to be 60 newtons.
00:06:50.040 --> 00:06:52.040
So this person is gonna
have to exert more force.
00:06:52.040 --> 00:06:55.280
In fact, they pushed three
times closer to the axis,
00:06:55.280 --> 00:06:57.010
so they're gonna have to exert three times
00:06:57.010 --> 00:06:58.310
the force that you do.
00:06:58.310 --> 00:07:02.030
You have a three times advantage
here in holding this door
00:07:02.030 --> 00:07:03.770
compared to the other person.
00:07:03.770 --> 00:07:05.070
All right, let's try one more
00:07:05.070 --> 00:07:06.590
just to make sure we understand it.
00:07:06.590 --> 00:07:08.190
Let's say it's now rush hour, you know,
00:07:08.190 --> 00:07:10.410
bird's eye view here, same circular door.
00:07:10.410 --> 00:07:12.240
Three people are trying
to go through at once.
00:07:12.240 --> 00:07:13.660
It's gonna be a mad house.
00:07:13.660 --> 00:07:16.020
This time I want to know,
it's not gonna be a stalemate.
00:07:16.020 --> 00:07:17.780
This door is gonna
rotate in some direction.
00:07:17.780 --> 00:07:20.130
I want to know what the net torque is.
00:07:20.130 --> 00:07:21.660
So just like you can find net force,
00:07:21.660 --> 00:07:24.120
you can find the net torque,
but you gotta be careful.
00:07:24.120 --> 00:07:25.290
These might have different signs,
00:07:25.290 --> 00:07:27.320
you gotta add or subtract accordingly.
00:07:27.320 --> 00:07:28.370
So start over here.
00:07:28.370 --> 00:07:31.020
How much torque would
be from this 10 newtons?
00:07:31.020 --> 00:07:34.600
Well, it's exerted three
meters away from the axis,
00:07:34.600 --> 00:07:35.990
so it's r is three meters.
00:07:35.990 --> 00:07:38.750
So the torque from that
force would be three meters
00:07:38.750 --> 00:07:42.010
times 10 newtons, and
since this is directed
00:07:42.010 --> 00:07:45.270
counterclockwise, I'm just
gonna call that positive
00:07:45.270 --> 00:07:47.110
and I'll have to be
consistent with that choice.
00:07:47.110 --> 00:07:48.700
So now let's consider this eight newtons.
00:07:48.700 --> 00:07:50.960
You might think it would
have an oppositely directed
00:07:50.960 --> 00:07:53.120
sign of torque from this 10 newtons
00:07:53.120 --> 00:07:54.880
'cause the eight is down, the 10 is up,
00:07:54.880 --> 00:07:57.440
but it's also trying to rotate this door
00:07:57.440 --> 00:07:59.270
in the counterclockwise direction.
00:07:59.270 --> 00:08:00.780
So in terms of forces,
00:08:00.780 --> 00:08:03.560
this 10 newton and eight
newton are oppositely directed,
00:08:03.560 --> 00:08:06.220
but in terms of torques,
they are the same direction.
00:08:06.220 --> 00:08:08.890
They're both causing
rotation counterclockwise.
00:08:08.890 --> 00:08:11.770
So if I called this torque
from the 10 newtons positive,
00:08:11.770 --> 00:08:14.620
I've gotta call the torque from
this eight newtons positive
00:08:14.620 --> 00:08:16.780
'cause it's trying to exert a
torque in the same direction.
00:08:16.780 --> 00:08:20.080
So I'd have one meter
is the r for the eight
00:08:20.080 --> 00:08:22.780
times eight newtons would be the torque
00:08:22.780 --> 00:08:24.250
from the eight newtons.
00:08:24.250 --> 00:08:25.500
And then I have one more force here.
00:08:25.500 --> 00:08:28.960
This five newton is trying
to rotate clockwise.
00:08:28.960 --> 00:08:31.130
Since I called counterclockwise positive,
00:08:31.130 --> 00:08:32.760
I'm gonna have to make
this a negative torque,
00:08:32.760 --> 00:08:36.470
so minus three meters,
the r from the access
00:08:36.470 --> 00:08:39.180
to this five newtons is three meters
00:08:39.180 --> 00:08:41.250
multiplied by five newtons.
00:08:41.250 --> 00:08:44.360
And if you take 30 plus eight minus 15,
00:08:44.360 --> 00:08:45.230
you're gonna get a total
00:08:45.230 --> 00:08:48.760
of positive 23 newton meters of torque,
00:08:48.760 --> 00:08:49.930
so this is not a stalemate.
00:08:49.930 --> 00:08:52.920
There will be an amount
of angular acceleration
00:08:52.920 --> 00:08:55.120
caused by this net torque.
00:08:55.120 --> 00:08:58.410
So to recap, just like net forces
00:08:58.410 --> 00:09:01.010
can cause regular acceleration,
00:09:01.010 --> 00:09:04.140
net torques can cause
angular acceleration.
00:09:04.140 --> 00:09:05.400
If there is no net torque,
00:09:05.400 --> 00:09:07.950
that means there is no
angular acceleration.
00:09:07.950 --> 00:09:10.820
The way you find the
torque from a given force
00:09:10.820 --> 00:09:13.880
is you take r, the distance from the axis
00:09:13.880 --> 00:09:16.360
to where that force is
applied and you multiply
00:09:16.360 --> 00:09:19.970
by the amount of force, as long
as it's that amount of force
00:09:19.970 --> 00:09:23.170
that runs perpendicular to this lever arm
00:09:23.170 --> 00:09:25.240
or this r direction.
00:09:25.240 --> 00:09:27.240
Be careful that torque is a vector.
00:09:27.240 --> 00:09:30.840
We typically count
counterclockwise as positive
00:09:30.840 --> 00:09:34.610
and clockwise as negative,
but if you're consistent,
00:09:34.610 --> 00:09:36.050
you can call whichever one of these
00:09:36.050 --> 00:09:37.450
you want to be positive
00:09:37.450 --> 00:09:39.600
as long as you call
the other one negative.
|
Period of a Pendulum | https://www.youtube.com/watch?v=mzatvUid9Pw | vtt | https://www.youtube.com/api/timedtext?v=mzatvUid9Pw&ei=3FWUZYiKD6CsmLAP75iC0AQ&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=201A549503A22AB95F92B45F0727E4170B235EFE.EEF60365923DB329951F27E772A36B98C3E1C8DF&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.150 --> 00:00:01.310
- [Instructor] So, a simple pendulum
00:00:01.310 --> 00:00:03.540
is just a mass hanging from a string.
00:00:03.540 --> 00:00:05.210
And if you are to pull this mass,
00:00:05.210 --> 00:00:07.004
sometimes it's called a pendulum bob,
00:00:07.004 --> 00:00:09.380
if you are to pull it
back and then let go,
00:00:09.380 --> 00:00:11.860
gravity would act as a restoring force
00:00:11.860 --> 00:00:15.310
and this mass would swing
back and forth over and over.
00:00:15.310 --> 00:00:17.220
And because this simple pendulum
00:00:17.220 --> 00:00:19.920
is a simple harmonic
oscillator, it's motion.
00:00:19.920 --> 00:00:21.552
Its angle as a function of time
00:00:21.552 --> 00:00:25.320
would be accurately described
by a sine or a cosine graph.
00:00:25.320 --> 00:00:26.153
So, in other words,
00:00:26.153 --> 00:00:30.120
if you are to pull this back
initially by 15 degrees,
00:00:30.120 --> 00:00:32.600
you might get a graph that
looks something like this.
00:00:32.600 --> 00:00:34.840
Now, every simple harmonic oscillator
00:00:34.840 --> 00:00:38.010
has a characteristic period of motion.
00:00:38.010 --> 00:00:40.670
Now, the period of motion
is the time it takes
00:00:40.670 --> 00:00:42.800
to complete one full cycle.
00:00:42.800 --> 00:00:45.210
So, the time it takes to swing from here
00:00:45.210 --> 00:00:46.043
all the way to there,
00:00:46.043 --> 00:00:47.330
all the way back to here,
00:00:47.330 --> 00:00:49.660
would be one full period.
00:00:49.660 --> 00:00:52.570
And in this graph, I've
written it as .5 seconds,
00:00:52.570 --> 00:00:54.690
but the period of every simple pendulum
00:00:54.690 --> 00:00:56.290
is not gonna be .5 seconds.
00:00:56.290 --> 00:00:57.930
The period of a simple pendulum
00:00:57.930 --> 00:01:00.687
depends on the characteristics
of that pendulum
00:01:00.687 --> 00:01:02.520
and the environment that it's in.
00:01:02.520 --> 00:01:05.760
So, to derive this formula
for the period of a pendulum,
00:01:05.760 --> 00:01:07.300
you would need calculus.
00:01:07.300 --> 00:01:08.420
So, I'm just gonna write it down
00:01:08.420 --> 00:01:10.390
and give you a quick tour and compare it
00:01:10.390 --> 00:01:12.560
with the period formula
for a mass on a spring,
00:01:12.560 --> 00:01:13.600
to the period of a pendulum
00:01:13.600 --> 00:01:18.600
is gonna be equal to two
pi times the square root
00:01:18.740 --> 00:01:21.870
of the ratio of the
length of the pendulum, L,
00:01:21.870 --> 00:01:25.070
so the length of that
string here, the length L,
00:01:25.070 --> 00:01:28.145
divided by g, the
gravitational acceleration
00:01:28.145 --> 00:01:31.530
of the planet that the
pendulum is being used on.
00:01:31.530 --> 00:01:32.510
Now, if you look at this
00:01:32.510 --> 00:01:33.830
and you've been paying
attention in physics,
00:01:33.830 --> 00:01:35.800
you might be like, "Wait,
that looks really similar
00:01:35.800 --> 00:01:38.620
to the formula for the period
of a mass on a spring."
00:01:38.620 --> 00:01:40.199
So, if you are to take a mass on a spring,
00:01:40.199 --> 00:01:42.130
displace it 15 centimeters,
00:01:42.130 --> 00:01:44.098
you'd get a similar graph
00:01:44.098 --> 00:01:47.880
and this would also have a
characteristic period of motion.
00:01:47.880 --> 00:01:51.020
And if you wrote down the
period for a mass on a spring,
00:01:51.020 --> 00:01:53.590
it looks like this, its
period for a mass on a spring
00:01:53.590 --> 00:01:56.470
is also two pi, so that's identical.
00:01:56.470 --> 00:01:59.120
And then, it's also the
square root of a ratio,
00:01:59.120 --> 00:02:02.294
but instead of L over g
for the mass on a spring,
00:02:02.294 --> 00:02:06.340
it's m, the mass of the block
connected to the spring,
00:02:06.340 --> 00:02:10.690
divided by k, the spring
constant of the spring.
00:02:10.690 --> 00:02:13.021
So, one obvious similarity
between these two formulas
00:02:13.021 --> 00:02:14.630
is just their format.
00:02:14.630 --> 00:02:18.110
They're both a two pi times
a square root of a ratio,
00:02:18.110 --> 00:02:20.810
but another important
similarity between these
00:02:20.810 --> 00:02:22.140
that might not be evident
00:02:22.140 --> 00:02:23.840
is that neither of these formulas
00:02:23.840 --> 00:02:26.090
depend on the amplitude of the motion.
00:02:26.090 --> 00:02:28.090
So, the period of a pendulum
00:02:28.090 --> 00:02:30.360
does not depend on the
amplitude of the motion
00:02:30.360 --> 00:02:32.000
and the period of a mass on a spring
00:02:32.000 --> 00:02:35.020
also does not depend on the
amplitude of the motion.
00:02:35.020 --> 00:02:35.853
What I mean by that
00:02:35.853 --> 00:02:37.850
is if you are to pull this pendulum back,
00:02:37.850 --> 00:02:38.920
instead of 15 degrees,
00:02:38.920 --> 00:02:41.370
pull it back 20 degrees and let go,
00:02:41.370 --> 00:02:43.100
it would have farther to swing.
00:02:43.100 --> 00:02:45.350
So, its motion might
look something like this,
00:02:45.350 --> 00:02:47.830
and we get down farther
and it would get back up,
00:02:47.830 --> 00:02:50.120
but it would take the
exact same amount of time.
00:02:50.120 --> 00:02:51.790
The period would not change
00:02:51.790 --> 00:02:54.320
if you pull this amplitude back farther.
00:02:54.320 --> 00:02:56.490
Same goes with this mass on a spring.
00:02:56.490 --> 00:02:58.300
Instead of pulling it 15 centimeters,
00:02:58.300 --> 00:03:00.630
let's say you pulled it
20 centimeters, again,
00:03:00.630 --> 00:03:02.060
this would start up higher.
00:03:02.060 --> 00:03:03.960
It would get down lower.
00:03:03.960 --> 00:03:06.900
But the time it takes to
complete one full cycle
00:03:06.900 --> 00:03:09.730
would not vary as you vary this amplitude.
00:03:09.730 --> 00:03:10.690
And that might seem weird.
00:03:10.690 --> 00:03:12.410
You're like, "Wait, don't these objects
00:03:12.410 --> 00:03:14.210
have farther to go now
00:03:14.210 --> 00:03:15.990
that you've pulled it back
to a larger amplitude?"
00:03:15.990 --> 00:03:18.780
That's true, they'll both
have farther to travel,
00:03:18.780 --> 00:03:20.550
but they'll be going faster now.
00:03:20.550 --> 00:03:24.632
And faster motion over a bigger
distance is gonna offset.
00:03:24.632 --> 00:03:27.499
And the amplitude does
not affect the period
00:03:27.499 --> 00:03:30.760
of the motion of a pendulum
or of a mass on a spring.
00:03:30.760 --> 00:03:33.220
As for the differences, well,
00:03:33.220 --> 00:03:35.370
the denominator here
for the mass on a spring
00:03:35.370 --> 00:03:38.690
depends on k, and that's
the spring constant k,
00:03:38.690 --> 00:03:39.710
and that should make sense.
00:03:39.710 --> 00:03:43.150
More spring constant means
you get more restoring force,
00:03:43.150 --> 00:03:45.400
the spring force is the
restoring force here.
00:03:45.400 --> 00:03:47.170
More restoring force means this mass
00:03:47.170 --> 00:03:48.800
is gonna be moving faster.
00:03:48.800 --> 00:03:51.280
That means it's gonna take less time
00:03:51.280 --> 00:03:52.940
to go through a full period.
00:03:52.940 --> 00:03:56.000
So, dividing by a bigger
number, bigger spring k,
00:03:56.000 --> 00:03:57.520
gives you less period.
00:03:57.520 --> 00:03:59.660
That's also true here but it's not k.
00:03:59.660 --> 00:04:02.270
The force that's the
restoring force for a pendulum
00:04:02.270 --> 00:04:04.980
isn't a spring, it's the force of gravity.
00:04:04.980 --> 00:04:07.220
So, mg depends on the g.
00:04:07.220 --> 00:04:10.810
So, a bigger g would give
you a bigger restoring force
00:04:10.810 --> 00:04:12.310
over here for the pendulum.
00:04:12.310 --> 00:04:14.700
That means the pendulum
could be moving faster.
00:04:14.700 --> 00:04:17.400
Moving faster means it's
gonna take less time
00:04:17.400 --> 00:04:18.920
to complete a full period.
00:04:18.920 --> 00:04:21.250
So, dividing by a bigger g,
if you took this pendulum
00:04:21.250 --> 00:04:23.570
to the surface of Jupiter or something,
00:04:23.570 --> 00:04:25.070
where the g is bigger,
00:04:25.070 --> 00:04:27.480
it would swing back and forth faster.
00:04:27.480 --> 00:04:29.560
It would take less time to complete it
00:04:29.560 --> 00:04:31.420
because that restoring force is bigger.
00:04:31.420 --> 00:04:33.890
So, even though these denominators
are different letters,
00:04:33.890 --> 00:04:35.760
they're arriving from the same source.
00:04:35.760 --> 00:04:38.880
They're both arriving
because the restoring force
00:04:38.880 --> 00:04:41.520
is larger when you increase
these denominators,
00:04:41.520 --> 00:04:43.460
which increases the speed of the object.
00:04:43.460 --> 00:04:45.320
Now, maybe the biggest difference here
00:04:45.320 --> 00:04:47.610
is that the numerator here
00:04:47.610 --> 00:04:49.620
for the mass on a spring depends on mass,
00:04:49.620 --> 00:04:51.730
but nowhere is mass to be found
00:04:51.730 --> 00:04:53.010
in this period of a pendulum.
00:04:53.010 --> 00:04:56.020
The period of the pendulum
does not depend on the mass.
00:04:56.020 --> 00:04:57.480
Now, this is kind of interesting.
00:04:57.480 --> 00:05:00.520
So, you know, really big,
heavy person gets on a swing,
00:05:00.520 --> 00:05:01.730
swings back and forth,
00:05:01.730 --> 00:05:04.240
very light child gets on the same swing,
00:05:04.240 --> 00:05:06.240
they will take the same amount of time
00:05:06.240 --> 00:05:07.730
to complete a full cycle.
00:05:07.730 --> 00:05:09.800
Their mass does not factor in here
00:05:09.800 --> 00:05:10.790
to the period of pendulum,
00:05:10.790 --> 00:05:13.840
but it does for the mass
on a spring, why is that?
00:05:13.840 --> 00:05:16.440
Well, bigger mass on a spring
00:05:16.440 --> 00:05:18.770
gives you more inertia in the system.
00:05:18.770 --> 00:05:20.430
If you have more inertia in the system,
00:05:20.430 --> 00:05:22.130
it's more sluggish to movement.
00:05:22.130 --> 00:05:23.510
It's gonna go slower.
00:05:23.510 --> 00:05:25.460
That means it's gonna take more time
00:05:25.460 --> 00:05:27.210
to complete a full cycle.
00:05:27.210 --> 00:05:28.490
Now, you might think, "Wait a minute.
00:05:28.490 --> 00:05:29.660
don't that hold true up here?
00:05:29.660 --> 00:05:33.470
Look, if we have a
bigger mass pendulum bob,
00:05:33.470 --> 00:05:35.982
that should increase
the rotational inertia.
00:05:35.982 --> 00:05:37.970
And so, that should make this take longer.
00:05:37.970 --> 00:05:39.560
It should be more sluggish to movement.
00:05:39.560 --> 00:05:41.680
It should take longer to
go through a full period."
00:05:41.680 --> 00:05:45.370
But look at the restoring
force is also, for a pendulum,
00:05:45.370 --> 00:05:46.970
proportional to mass.
00:05:46.970 --> 00:05:48.510
So, if you increase the
mass of this pendulum,
00:05:48.510 --> 00:05:49.810
you do get more inertia,
00:05:49.810 --> 00:05:51.370
but you're getting more restoring force
00:05:51.370 --> 00:05:53.120
because the restoring force is gravity.
00:05:53.120 --> 00:05:54.084
Those completely offset
00:05:54.084 --> 00:05:57.930
mass does not end up showing
up into this pendulum formula,
00:05:57.930 --> 00:05:59.730
even though it does down here.
00:05:59.730 --> 00:06:02.140
So, the spring force is
not proportional to mass.
00:06:02.140 --> 00:06:03.510
Spring force is kx.
00:06:03.510 --> 00:06:06.487
Increasing the mass of
this block on the end
00:06:06.487 --> 00:06:09.140
does not increase the
spring restoring force.
00:06:09.140 --> 00:06:11.020
So, this mass stays in the numerator here,
00:06:11.020 --> 00:06:13.640
but it does not affect
the period of a pendulum.
00:06:13.640 --> 00:06:15.590
So, why does this L show up then?
00:06:15.590 --> 00:06:18.210
Why is it length of the
pendulum in the numerator?
00:06:18.210 --> 00:06:20.880
Well, the rotational
inertia does get increased
00:06:20.880 --> 00:06:23.280
when you increase the
length of the pendulum.
00:06:23.280 --> 00:06:24.210
But increasing that length
00:06:24.210 --> 00:06:26.550
that does not increase
the force of gravity.
00:06:26.550 --> 00:06:27.940
If you wanna get technical,
00:06:27.940 --> 00:06:31.270
rotational inertia is
proportional to length squared,
00:06:31.270 --> 00:06:33.840
but the torque would only
be proportional to length.
00:06:33.840 --> 00:06:36.040
That's why only one L shows up here.
00:06:36.040 --> 00:06:39.920
Long story short, if you increase
the length of a pendulum,
00:06:39.920 --> 00:06:42.150
you're gonna increase the
inertia of that pendulum.
00:06:42.150 --> 00:06:43.380
That's gonna make it take longer
00:06:43.380 --> 00:06:44.730
to go through a full cycle.
00:06:44.730 --> 00:06:45.900
This is while I go into the park
00:06:45.900 --> 00:06:47.650
and finding the long swings.
00:06:47.650 --> 00:06:50.410
The longer the swing, the
longer it actually takes,
00:06:50.410 --> 00:06:52.670
the more time it actually
takes to swing back and forth.
00:06:52.670 --> 00:06:55.480
I think that's more fun
than the little short swings
00:06:55.480 --> 00:06:57.380
that go back and forth really quick.
00:06:57.380 --> 00:06:58.670
So, let's try a sample problem
00:06:58.670 --> 00:07:01.160
to see how this period formula works.
00:07:01.160 --> 00:07:02.660
Let's say you went to the park.
00:07:02.660 --> 00:07:03.900
You're 60 kilograms.
00:07:03.900 --> 00:07:04.990
You're swinging on a swing
00:07:04.990 --> 00:07:07.880
and your friend pulls you back 20 degrees
00:07:07.880 --> 00:07:10.370
on a swing that's one meter in length.
00:07:10.370 --> 00:07:12.370
Let's find the period of the motion.
00:07:12.370 --> 00:07:13.680
So, in other words, the time it takes
00:07:13.680 --> 00:07:15.150
to go all the way to here
00:07:15.150 --> 00:07:16.720
and then all the way back to there.
00:07:16.720 --> 00:07:19.710
We use the period formula for a pendulum.
00:07:19.710 --> 00:07:23.600
It's two pi, root L over g.
00:07:23.600 --> 00:07:27.670
And so, we would do two
pi times the square root,
00:07:27.670 --> 00:07:29.860
the length here is the
length of the string here.
00:07:29.860 --> 00:07:31.800
So, one meter, technically,
00:07:31.800 --> 00:07:34.040
it'd be to wherever
your center of mass is,
00:07:34.040 --> 00:07:35.820
but we're gonna assume our center mass
00:07:35.820 --> 00:07:37.250
is right here at the end,
00:07:37.250 --> 00:07:40.260
divided by g, well, we're
on earth, I'm assuming,
00:07:40.260 --> 00:07:43.420
so, 9.8 meters per second squared.
00:07:43.420 --> 00:07:44.359
If you solve all of that,
00:07:44.359 --> 00:07:48.070
you get a period of about
two seconds exactly.
00:07:48.070 --> 00:07:51.490
So, this swing would have a
period of about two seconds.
00:07:51.490 --> 00:07:54.480
Now, notice we did not
use this 20 degrees.
00:07:54.480 --> 00:07:55.670
That's the amplitude.
00:07:55.670 --> 00:07:58.020
This period does not
depend on the amplitude.
00:07:58.020 --> 00:08:01.200
We also did not use the fact
that I was 60 kilograms.
00:08:01.200 --> 00:08:03.410
The period of a pendulum
also does not depend
00:08:03.410 --> 00:08:06.250
on the mass of the bob at
the end of the pendulum.
00:08:06.250 --> 00:08:08.640
We only use the length
and if you're on earth,
00:08:08.640 --> 00:08:11.260
the denominator here
is always gonna be 9.8.
00:08:11.260 --> 00:08:14.310
Now, one thing I should be
clear about is that a pendulum
00:08:14.310 --> 00:08:17.100
is technically not a perfect
simple harmonic oscillator.
00:08:17.100 --> 00:08:19.760
It's only approximately a
simple harmonic oscillator.
00:08:19.760 --> 00:08:22.780
So, this formula here is
only approximately correct,
00:08:22.780 --> 00:08:25.400
but for small angles, it's almost perfect.
00:08:25.400 --> 00:08:26.560
So, at 20 degrees,
00:08:26.560 --> 00:08:28.610
this formula is only gonna be off.
00:08:28.610 --> 00:08:31.066
The error's only going to be about 1%,
00:08:31.066 --> 00:08:32.230
which isn't bad.
00:08:32.230 --> 00:08:34.420
If you get this back to like 70 degrees,
00:08:34.420 --> 00:08:37.920
even then, the error's only around 10%.
00:08:37.920 --> 00:08:41.190
So, this is a really,
really good approximation
00:08:41.190 --> 00:08:44.710
if you're in small angles,
like around 20 to 30 degrees.
00:08:44.710 --> 00:08:46.340
The bigger the angle gets though,
00:08:46.340 --> 00:08:47.960
the worst the approximation gets.
00:08:47.960 --> 00:08:51.310
For small angles, most
physicists just treat a pendulum
00:08:51.310 --> 00:08:53.656
as if it's a perfect
simple harmonic oscillator.
00:08:53.656 --> 00:08:55.560
As you get to those higher angles though,
00:08:55.560 --> 00:08:56.700
you gotta be careful.
00:08:56.700 --> 00:08:59.470
This can start deviating
more significantly
00:08:59.470 --> 00:09:00.870
from the actual value.
00:09:00.870 --> 00:09:02.860
So, to recap, the period of a pendulum
00:09:02.860 --> 00:09:04.930
depends on the length of the pendulum
00:09:04.930 --> 00:09:07.650
and the surface gravity of
the planet that you're on.
00:09:07.650 --> 00:09:10.110
It does not depend on the amplitude
00:09:10.110 --> 00:09:12.040
or the mass of the pendulum.
00:09:12.040 --> 00:09:13.940
And the form it takes is very similar
00:09:13.940 --> 00:09:16.070
to the period of a mass on a spring
00:09:16.070 --> 00:09:17.890
where the numerator increases
00:09:17.890 --> 00:09:19.530
due to increased inertia
00:09:19.530 --> 00:09:21.680
and the denominator increases
00:09:21.680 --> 00:09:24.253
due to increased restoring force.
|
Dihybrid cross and the Law of Independent Assortment | https://www.youtube.com/watch?v=ZkyX3TmmMag | vtt | https://www.youtube.com/api/timedtext?v=ZkyX3TmmMag&ei=3FWUZcG6BcSkvdIPuJW6uAs&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=58F3E661750ACB523C38CDDACC06C84974860328.5C17A64722736B620D5DE8EA4833EA5689C52D7C&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.300 --> 00:00:02.070
- [Instructor] In this
video, we're going to build
00:00:02.070 --> 00:00:03.977
on our understanding of Mendelian genetics
00:00:03.977 --> 00:00:05.390
and Punnett squares
00:00:05.390 --> 00:00:08.340
by starting to think
about two different genes.
00:00:08.340 --> 00:00:09.820
So we're going back to the pea plant,
00:00:09.820 --> 00:00:12.070
and we're gonna think about
the gene for pea color
00:00:12.070 --> 00:00:15.090
and the gene for pea shape.
00:00:15.090 --> 00:00:18.430
So let's say that in
the parental generation,
00:00:18.430 --> 00:00:21.640
you have one parent that
is homozygous dominant
00:00:21.640 --> 00:00:24.210
for both of these genes.
00:00:24.210 --> 00:00:28.500
So their genotype is capital Y, capital Y,
00:00:28.500 --> 00:00:32.260
and capital R, capital R.
00:00:32.260 --> 00:00:35.640
So their phenotype for sure
is going to be yellow round,
00:00:35.640 --> 00:00:36.840
and we also see the genotype.
00:00:36.840 --> 00:00:39.680
We see which alleles it has.
00:00:39.680 --> 00:00:41.270
Now, let's say that that is crossed
00:00:41.270 --> 00:00:44.100
with the homozygous recessive parent.
00:00:44.100 --> 00:00:47.710
So in this case, it's going
to be green-colored peas.
00:00:47.710 --> 00:00:49.950
It's counterintuitive
to write green with a y,
00:00:49.950 --> 00:00:52.350
a lowercase y in the color yellow,
00:00:52.350 --> 00:00:54.730
but the lowercase y represents green.
00:00:54.730 --> 00:00:57.930
And also these are wrinkled green peas.
00:00:57.930 --> 00:01:01.410
So I will write that with
the lowercase r here.
00:01:01.410 --> 00:01:03.370
And so the phenotype here is going
00:01:03.370 --> 00:01:06.900
to be green and wrinkled for sure.
00:01:06.900 --> 00:01:09.320
Now, what's going to
happen when they cross?
00:01:09.320 --> 00:01:12.110
What does the F1 generation look like?
00:01:12.110 --> 00:01:15.460
Well, we know from
Mendel's law of segregation
00:01:15.460 --> 00:01:19.180
for each of these genes, that
when a gamete is created,
00:01:19.180 --> 00:01:23.290
it randomly gets one copy
of each of these genes.
00:01:23.290 --> 00:01:24.123
So for this first one,
00:01:24.123 --> 00:01:27.150
it's going to randomly get
one of these capital Ys.
00:01:27.150 --> 00:01:29.430
So it's going to get a capital Y for sure
00:01:29.430 --> 00:01:30.620
from this first parent.
00:01:30.620 --> 00:01:34.460
And it's also going to randomly
get one of these capital Rs.
00:01:34.460 --> 00:01:36.860
So it's going to get a capital R for sure
00:01:36.860 --> 00:01:38.370
from that first parent.
00:01:38.370 --> 00:01:40.370
And then by the same logic,
00:01:40.370 --> 00:01:43.340
it's going to randomly get one
of these two lowercase y's.
00:01:43.340 --> 00:01:46.390
So it's going to get a
lowercase y for sure,
00:01:46.390 --> 00:01:47.900
and it's going to randomly get one
00:01:47.900 --> 00:01:49.650
of these two lowercase r's,
00:01:49.650 --> 00:01:52.470
so it's going to get a
lowercase r for sure.
00:01:52.470 --> 00:01:57.060
So this is the genotype for
all of the F1 generation.
00:01:57.060 --> 00:01:58.893
This is often known as a dihybrid.
00:01:59.976 --> 00:02:03.120
It is heterozygous in both genes.
00:02:03.120 --> 00:02:04.830
Now, what's the phenotype here?
00:02:04.830 --> 00:02:06.450
Well, we know yellow is dominant,
00:02:06.450 --> 00:02:08.050
and we know round is dominant.
00:02:08.050 --> 00:02:10.210
So if we looked at these
plants right over here,
00:02:10.210 --> 00:02:12.430
their peas would still be yellow round,
00:02:12.430 --> 00:02:15.380
just like this homozygous
parent over here.
00:02:15.380 --> 00:02:17.080
Now, what's interesting is when you do
00:02:17.080 --> 00:02:19.760
what's known as a dihybrid cross
00:02:19.760 --> 00:02:22.890
when you cross one of this F1 generation
00:02:22.890 --> 00:02:25.130
with itself or with each other.
00:02:25.130 --> 00:02:26.020
And to do that,
00:02:26.020 --> 00:02:30.440
I'm gonna create a four by
four Punnett square here.
00:02:30.440 --> 00:02:34.210
And so one parent here
is going to be hybrid in
00:02:34.210 --> 00:02:37.540
or heterozygous in the color gene
00:02:37.540 --> 00:02:40.470
and also heterozygous in the shape gene.
00:02:40.470 --> 00:02:42.900
And that's going to be true
of the other parent as well.
00:02:42.900 --> 00:02:46.380
Heterozygous or hybrid in the color gene
00:02:46.380 --> 00:02:49.890
and also heterozygous in the shape gene.
00:02:49.890 --> 00:02:52.160
And so that's why this is
called a dihybrid cross.
00:02:52.160 --> 00:02:53.300
You're crossing things
00:02:53.300 --> 00:02:56.330
that are hybrid in two different genes.
00:02:56.330 --> 00:02:59.300
Now, we've already talked
about the law of segregation.
00:02:59.300 --> 00:03:03.320
The gamete is randomly going
to get one copy of each gene.
00:03:03.320 --> 00:03:07.190
Now, Mendel also has the law
of independent assortment,
00:03:07.190 --> 00:03:08.580
which tells us the alleles
00:03:08.580 --> 00:03:12.100
of different genes
segregate independently.
00:03:12.100 --> 00:03:14.020
So for this parent here,
00:03:14.020 --> 00:03:17.230
whether it contributes a
capital Y or a lowercase y
00:03:17.230 --> 00:03:19.910
is independent of whether
it contribute a capital R
00:03:19.910 --> 00:03:21.330
or a lowercase r.
00:03:21.330 --> 00:03:22.920
Now, there is a little bit of a asterisk,
00:03:22.920 --> 00:03:24.490
a little caveat on there.
00:03:24.490 --> 00:03:27.020
We now know that genes sit on chromosomes.
00:03:27.020 --> 00:03:28.810
One chromosome will have many genes on it.
00:03:28.810 --> 00:03:31.630
And this law of independent
assortment only applies
00:03:31.630 --> 00:03:34.690
to genes that are actually
sitting on different chromosomes.
00:03:34.690 --> 00:03:36.710
If they sit on the same chromosome,
00:03:36.710 --> 00:03:40.230
they generally are not going
to assort independently.
00:03:40.230 --> 00:03:43.040
But let's just assume the
law of independent assortment
00:03:43.040 --> 00:03:45.380
'cause this is true for most genes.
00:03:45.380 --> 00:03:49.920
So this first parent can
contribute a capital Y
00:03:49.920 --> 00:03:51.530
out of this first gene
00:03:51.530 --> 00:03:54.900
and a capital R out of the second gene,
00:03:54.900 --> 00:03:57.380
or they could contribute
the lowercase copy
00:03:57.380 --> 00:03:58.600
of the first gene
00:03:58.600 --> 00:04:02.780
and the capital R copy of the second gene,
00:04:02.780 --> 00:04:06.000
this capital R, the round
allele of the second gene.
00:04:06.000 --> 00:04:08.210
And we could go through
every combination here.
00:04:08.210 --> 00:04:12.580
It could also contribute the yellow allele
00:04:12.580 --> 00:04:14.363
and the wrinkled allele.
00:04:15.490 --> 00:04:20.290
Or it could contribute the green allele
00:04:20.290 --> 00:04:22.543
and the wrinkled allele as well.
00:04:23.540 --> 00:04:26.000
And the same would be true
for this other dihybrid,
00:04:26.000 --> 00:04:28.130
this other parent right over here.
00:04:28.130 --> 00:04:29.510
So let me just write that down.
00:04:29.510 --> 00:04:33.440
They could contribute capital
Y in two of the scenarios.
00:04:33.440 --> 00:04:35.270
They could contribute a lowercase y
00:04:35.270 --> 00:04:37.590
or the green allele in
two of the scenarios.
00:04:37.590 --> 00:04:39.920
And they could contribute a capital R
00:04:39.920 --> 00:04:42.360
in two of the scenarios, a round allele,
00:04:42.360 --> 00:04:44.700
or a lowercase r in two of the scenarios,
00:04:44.700 --> 00:04:46.100
a wrinkled allele.
00:04:46.100 --> 00:04:48.050
So you have all of the
different combinations
00:04:48.050 --> 00:04:49.690
that each of them can contribute.
00:04:49.690 --> 00:04:51.730
Once again, whether you get the yellow
00:04:51.730 --> 00:04:53.110
or the green is independent
00:04:53.110 --> 00:04:55.260
of whether you get the
round or the wrinkled.
00:04:55.260 --> 00:04:58.083
So these are all equally
probably right over here.
00:04:59.100 --> 00:05:01.270
When the two gametes from
these two parents merge,
00:05:01.270 --> 00:05:03.000
we can then look at what the genotype
00:05:03.000 --> 00:05:04.350
of the offspring is going to be,
00:05:04.350 --> 00:05:06.900
really the genotype of the F2 generation
00:05:06.900 --> 00:05:10.470
'cause we're crossing two
members of the F1 generation.
00:05:10.470 --> 00:05:12.210
So I encourage you to pause this video
00:05:12.210 --> 00:05:13.720
and fill in this grid.
00:05:13.720 --> 00:05:15.820
See if you can figure
the different genotypes
00:05:15.820 --> 00:05:16.803
that will result.
00:05:18.140 --> 00:05:20.270
All right, now let's do this together.
00:05:20.270 --> 00:05:21.710
So this scenario right over here,
00:05:21.710 --> 00:05:25.060
you're getting a capital
Y from both parents,
00:05:25.060 --> 00:05:29.810
and you're getting a
capital R from both parents.
00:05:29.810 --> 00:05:30.730
This scenario over here,
00:05:30.730 --> 00:05:33.330
you're getting a capital
Y from this parent,
00:05:33.330 --> 00:05:35.840
lowercase y from that parent,
00:05:35.840 --> 00:05:38.663
and then you're getting
a capital R from both.
00:05:39.650 --> 00:05:43.940
This scenario over here,
capital Y from both parents.
00:05:43.940 --> 00:05:45.500
Capital Y, capital Y.
00:05:45.500 --> 00:05:49.940
And you're getting a
capital R from this parent
00:05:49.940 --> 00:05:52.480
and a lowercase r from that parent.
00:05:52.480 --> 00:05:54.460
And then this scenario over here,
00:05:54.460 --> 00:05:57.550
you're getting gonna capital
Y allele from this parent
00:05:57.550 --> 00:05:59.640
and lowercase y from that parent,
00:05:59.640 --> 00:06:03.130
and you're getting a
capital R from this parent
00:06:03.130 --> 00:06:05.630
and a lowercase r from that parent.
00:06:05.630 --> 00:06:07.810
And now I'm just going
to speed up the video
00:06:07.810 --> 00:06:10.923
and just fill in the rest of
these using the same logic.
00:06:14.440 --> 00:06:17.080
All right, now that we've
filled out this Punnett square,
00:06:17.080 --> 00:06:19.470
let's think about the
different phenotypes.
00:06:19.470 --> 00:06:20.530
How many of these plants are going
00:06:20.530 --> 00:06:22.560
to produce yellow round peas?
00:06:22.560 --> 00:06:24.310
Pause the video and think about it.
00:06:25.320 --> 00:06:27.310
Well, it's yellow and round.
00:06:27.310 --> 00:06:31.260
It has to have at least one
capital Y and one capital R.
00:06:31.260 --> 00:06:33.620
So that one's going to
be yellow and round.
00:06:33.620 --> 00:06:35.560
This is going to be yellow and round.
00:06:35.560 --> 00:06:37.970
This is going to be yellow and round.
00:06:37.970 --> 00:06:40.270
That's yellow and round as well.
00:06:40.270 --> 00:06:42.500
This is yellow and round.
00:06:42.500 --> 00:06:44.500
That's yellow and round.
00:06:44.500 --> 00:06:46.610
This is yellow and round.
00:06:46.610 --> 00:06:49.560
And that one is yellow and round.
00:06:49.560 --> 00:06:53.040
And then last but not least,
I think this is the last one
00:06:53.040 --> 00:06:55.430
that is both yellow and round.
00:06:55.430 --> 00:06:57.090
And actually let me make
a little color code here.
00:06:57.090 --> 00:07:00.240
Yellow plus round.
00:07:00.240 --> 00:07:01.850
And here we're talking
about the phenotype.
00:07:01.850 --> 00:07:03.840
You can see we have
different genotypes here,
00:07:03.840 --> 00:07:06.730
but because both yellow
and round are dominant,
00:07:06.730 --> 00:07:09.170
as long as you have at
least one Y and one R,
00:07:09.170 --> 00:07:10.340
you're going to have a yellow
00:07:10.340 --> 00:07:12.330
plus round phenotype over here.
00:07:12.330 --> 00:07:14.300
So you have one, two, three, four,
00:07:14.300 --> 00:07:16.540
five, six, seven, eight, nine.
00:07:16.540 --> 00:07:19.580
And I will say there's
nine of these over here.
00:07:19.580 --> 00:07:24.580
Now, how many of these are going
to be yellow plus wrinkled?
00:07:25.490 --> 00:07:28.820
Pause the video and think
about that, that phenotype.
00:07:28.820 --> 00:07:30.000
So yellow and wrinkled,
00:07:30.000 --> 00:07:32.300
you're going to have to have a capital Y
00:07:32.300 --> 00:07:35.610
and two lowercase r's
in order to be wrinkled.
00:07:35.610 --> 00:07:39.310
So you have at least one
capital Y and two lowercase r's,
00:07:39.310 --> 00:07:42.860
and least one capital Y
and two lowercase r's.
00:07:42.860 --> 00:07:47.170
Let's see, at least one capital
Y and two lowercase r's.
00:07:47.170 --> 00:07:50.390
It looks like you have
exactly three of them,
00:07:50.390 --> 00:07:51.550
that phenotype.
00:07:51.550 --> 00:07:54.390
And then what about the other way around?
00:07:54.390 --> 00:07:58.410
What if we are looking for,
I'll do it in this green color,
00:07:58.410 --> 00:08:03.410
green plus round?
00:08:03.840 --> 00:08:06.180
How many of them exhibit that phenotype?
00:08:06.180 --> 00:08:07.450
Well, to be green and round,
00:08:07.450 --> 00:08:09.590
you have to have two lowercase y's,
00:08:09.590 --> 00:08:12.370
and you have to have
at least one capital R.
00:08:12.370 --> 00:08:15.950
So this would be green and round.
00:08:15.950 --> 00:08:18.090
This would be green and round.
00:08:18.090 --> 00:08:20.270
And then this would be
green and round as well.
00:08:20.270 --> 00:08:21.800
So you have three of those.
00:08:21.800 --> 00:08:23.300
And then how many of them are going
00:08:23.300 --> 00:08:25.430
to be both green and wrinkled?
00:08:25.430 --> 00:08:28.290
Well, I think you see that
one scenario over here
00:08:28.290 --> 00:08:30.020
that is both green and wrinkled,
00:08:30.020 --> 00:08:33.450
having that homozygous
recessive phenotype.
00:08:33.450 --> 00:08:35.290
And so if you were to do this many times,
00:08:35.290 --> 00:08:37.870
you'd expect the ratios between
these various phenotypes
00:08:37.870 --> 00:08:41.400
to be nine to three to three to one.
00:08:41.400 --> 00:08:43.000
And when Mendel and many other people
00:08:43.000 --> 00:08:45.180
since Mendel have done
these types of experiments,
00:08:45.180 --> 00:08:47.060
they have seen that statistically,
00:08:47.060 --> 00:08:49.870
this is what you see
in that F2 generation.
00:08:49.870 --> 00:08:51.820
Now, you're unlikely to get exactly a nine
00:08:51.820 --> 00:08:53.590
to three to three to one ratio.
00:08:53.590 --> 00:08:54.950
It's all probabilistic.
00:08:54.950 --> 00:08:58.650
Every one of these 16
scenarios are equally likely,
00:08:58.650 --> 00:09:00.530
so you would expect this nine to three
00:09:00.530 --> 00:09:01.950
to three to one ratio,
00:09:01.950 --> 00:09:04.870
but you're not always going
to get that exact ratio.
00:09:04.870 --> 00:09:06.970
You'll probably get something close to it.
|
Energy at the microscopic scale | https://www.youtube.com/watch?v=VeueBB5Abt4 | vtt | https://www.youtube.com/api/timedtext?v=VeueBB5Abt4&ei=3FWUZeSaDLWvvdIPzsKD-Aw&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=1C2CE84C6708A498AA6DA31CAE0C6CA6B1E8CA4E.407CDB4CF072C219B270648D8A2B351FB83A9F8D&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.400 --> 00:00:01.560
- [Instructor] Welcome.
00:00:01.560 --> 00:00:04.300
Today, we're going to take
a look at forms of energy,
00:00:04.300 --> 00:00:07.270
such as kinetic, electrical, thermal,
00:00:07.270 --> 00:00:09.370
gravitational, potential energy.
00:00:09.370 --> 00:00:11.300
It turns out when you start thinking
00:00:11.300 --> 00:00:15.230
about energy on smaller scales,
or the microscopic level,
00:00:15.230 --> 00:00:17.930
all of these forms of energy
are basically two things:
00:00:17.930 --> 00:00:21.380
one, kinetic energy,
particles moving around,
00:00:21.380 --> 00:00:25.170
and two, potential energy,
energy stored by a field,
00:00:25.170 --> 00:00:27.713
such as electric,
magnetic or gravitational.
00:00:28.800 --> 00:00:30.980
Let's start with a
deceivingly simple example
00:00:30.980 --> 00:00:33.693
and explore properties
of energy as we zoom in.
00:00:36.830 --> 00:00:38.563
I'm drawing a glass of water.
00:00:39.450 --> 00:00:40.900
This water has a temperature.
00:00:41.830 --> 00:00:44.310
I can warm up the water by adding energy
00:00:44.310 --> 00:00:45.813
from an electric stove,
00:00:46.710 --> 00:00:49.850
or cool down the water by
putting it in the fridge,
00:00:49.850 --> 00:00:52.920
thus removing energy in the liquid water.
00:00:52.920 --> 00:00:55.210
From this example, we
can see that temperature
00:00:55.210 --> 00:00:56.830
is related to energy.
00:00:56.830 --> 00:01:00.083
But how is it related to
kinetic or potential energy?
00:01:01.010 --> 00:01:02.620
Hmm.
00:01:02.620 --> 00:01:05.110
This big picture, the macroscopic scale,
00:01:05.110 --> 00:01:07.500
allows us to look at energy
in terms of temperature.
00:01:07.500 --> 00:01:09.830
But let's go to the
microscopic or small-scale
00:01:09.830 --> 00:01:12.293
to get a better picture
of the physics at play.
00:01:14.330 --> 00:01:16.130
As we look inside this liquid,
00:01:16.130 --> 00:01:19.103
we see lots of water
molecules moving around.
00:01:20.070 --> 00:01:21.740
Zoom, zoom, zoom.
00:01:21.740 --> 00:01:23.690
Well, they don't actually make a sound.
00:01:25.950 --> 00:01:28.650
The average speed at
which these molecules move
00:01:28.650 --> 00:01:31.160
is related to their kinetic
energy and its temperature.
00:01:31.160 --> 00:01:32.543
This is thermal motion.
00:01:34.220 --> 00:01:38.700
If we zoom in again, we can
look into the strong chemical
00:01:38.700 --> 00:01:40.710
bonds within molecules.
00:01:40.710 --> 00:01:44.130
Here, the individual atoms,
in this case for water,
00:01:44.130 --> 00:01:46.420
is hydrogen and oxygen.
00:01:46.420 --> 00:01:49.160
They can vibrate back
and forth and rotate,
00:01:49.160 --> 00:01:50.883
so they also have kinetic energy.
00:01:51.740 --> 00:01:52.900
Let's look at another example
00:01:52.900 --> 00:01:55.773
between macro and microscale
energy interactions.
00:01:56.710 --> 00:01:59.660
When you burn something, think of a fire.
00:01:59.660 --> 00:02:01.400
A chemical reaction takes place,
00:02:01.400 --> 00:02:03.310
and it releases a lot of energy.
00:02:03.310 --> 00:02:04.960
How does it do that?
00:02:04.960 --> 00:02:08.220
Let's look at the microscopic
scale to find out.
00:02:08.220 --> 00:02:10.520
In this example, I'm
gonna burn methane gas,
00:02:10.520 --> 00:02:12.530
and the chemical reaction that takes place
00:02:12.530 --> 00:02:17.380
is methane, CH4, and oxygen, O2.
00:02:17.380 --> 00:02:20.910
They rearrange to create water, H2O,
00:02:20.910 --> 00:02:24.103
and carbon dioxide, CO2, plus energy.
00:02:25.750 --> 00:02:26.860
Before the reaction,
00:02:26.860 --> 00:02:28.720
there is a greater
chemical potential energy
00:02:28.720 --> 00:02:29.730
than afterwards.
00:02:29.730 --> 00:02:30.563
But don't worry.
00:02:30.563 --> 00:02:32.970
Energy is still conserved
because that potential energy
00:02:32.970 --> 00:02:35.383
is converted to kinetic
energy and radiation.
00:02:37.330 --> 00:02:40.600
What is the source of
chemical potential energy?
00:02:40.600 --> 00:02:43.040
At this level, we can
think of individual bonds
00:02:43.040 --> 00:02:44.920
between atoms storing energy
00:02:44.920 --> 00:02:47.670
so that energy can be absorbed or released
00:02:47.670 --> 00:02:49.803
as bonds are broken and reformed.
00:02:50.750 --> 00:02:54.280
But where does the energy
and chemical bonds come from?
00:02:54.280 --> 00:02:55.793
We need to zoom in again.
00:02:57.260 --> 00:02:58.410
In a single atom,
00:02:58.410 --> 00:03:02.530
there's a nucleus that
contains protons and neutrons
00:03:02.530 --> 00:03:05.200
and overall has a positive charge.
00:03:05.200 --> 00:03:07.113
This creates an electromagnetic field.
00:03:07.950 --> 00:03:10.600
The interaction of
other charged particles,
00:03:10.600 --> 00:03:12.430
like negatively charged electrons
00:03:12.430 --> 00:03:15.130
relatively far away from the nucleus,
00:03:15.130 --> 00:03:18.140
with this field provide potential energy.
00:03:18.140 --> 00:03:19.950
You can think of this
electric potential energy
00:03:19.950 --> 00:03:22.480
as the same kind of concept
as a potential energy
00:03:22.480 --> 00:03:24.583
of a mass and a gravitational field.
00:03:25.700 --> 00:03:28.550
Zooming back out, each
molecule has its own
00:03:28.550 --> 00:03:30.640
particular configuration
of charged particles
00:03:30.640 --> 00:03:33.700
within the electromagnetic fields, right?
00:03:33.700 --> 00:03:36.603
This means it has an
associated potential energy.
00:03:37.570 --> 00:03:39.960
As we've seen, this
chemical potential energy
00:03:39.960 --> 00:03:42.513
is the result of energy stored in fields.
00:03:43.790 --> 00:03:46.210
Okay, so we've covered
electrical, chemical,
00:03:46.210 --> 00:03:47.250
thermal types of energy,
00:03:47.250 --> 00:03:49.300
but there's other forms out there, right?
00:03:50.220 --> 00:03:52.600
For instance, what about sound waves?
00:03:52.600 --> 00:03:56.023
Here's a speaker and an ear.
00:03:57.890 --> 00:04:00.070
The energy in sound waves is transferred
00:04:00.070 --> 00:04:01.060
through the vibrations,
00:04:01.060 --> 00:04:03.840
a back and forth motion
of molecules in the air.
00:04:03.840 --> 00:04:07.370
Another example could be
elastic potential energy
00:04:07.370 --> 00:04:09.470
or the energy stored in a spring.
00:04:09.470 --> 00:04:11.010
At the microscopic level,
00:04:11.010 --> 00:04:12.750
as you stretch the spring,
00:04:12.750 --> 00:04:14.490
see the hand stretching the spring?
00:04:14.490 --> 00:04:17.140
The atoms are being pulled out
of their equilibrium position
00:04:17.140 --> 00:04:20.330
within a solid and thus
gain potential energy
00:04:20.330 --> 00:04:21.610
from the electromagnetic force
00:04:21.610 --> 00:04:23.670
that holds the solid together.
00:04:23.670 --> 00:04:24.810
How neat is this?
00:04:24.810 --> 00:04:27.170
We can describe all these energies
00:04:27.170 --> 00:04:29.363
as just kinetic or potential.
00:04:30.370 --> 00:04:32.470
So there's one more
microscopic form of energy
00:04:32.470 --> 00:04:33.730
that we need to talk about,
00:04:33.730 --> 00:04:36.350
and it might seem a little
complicated at first.
00:04:36.350 --> 00:04:38.010
Let's go back to the combustion example
00:04:38.010 --> 00:04:39.780
we talked about earlier.
00:04:39.780 --> 00:04:43.860
As I said before, this process
releases radiant energy.
00:04:43.860 --> 00:04:45.210
We can see burning objects.
00:04:45.210 --> 00:04:46.430
They glow brightly.
00:04:46.430 --> 00:04:48.690
We can also put our hand
near the burning object.
00:04:48.690 --> 00:04:49.620
Don't touch it!
00:04:49.620 --> 00:04:51.690
And feel the radiant heat.
00:04:51.690 --> 00:04:54.653
This radiation that's emitted
carries energy with it.
00:04:55.650 --> 00:04:58.630
So how do we explain the radiant energy?
00:04:58.630 --> 00:05:00.590
Does it fit it into one
of these two categories,
00:05:00.590 --> 00:05:02.460
either kinetic or potential energy
00:05:02.460 --> 00:05:03.810
that we've been discussing?
00:05:04.690 --> 00:05:08.500
Well, it turns out it sort
of fits into both groups.
00:05:08.500 --> 00:05:12.500
Whoa, electromagnetic
radiation, such as light,
00:05:12.500 --> 00:05:14.830
can be modeled in a
couple of different ways,
00:05:14.830 --> 00:05:17.410
which we'll go into more
detail in another video.
00:05:17.410 --> 00:05:19.320
But one way to model the light
00:05:19.320 --> 00:05:22.423
is as a wave of electric
and magnetic fields.
00:05:23.830 --> 00:05:26.240
Another way to think about light
00:05:26.240 --> 00:05:28.800
is being made up of
particles called photons.
00:05:28.800 --> 00:05:31.410
In this instance, the particles
are carrying the energy.
00:05:31.410 --> 00:05:32.850
So with both of these models,
00:05:32.850 --> 00:05:34.480
radiant energy can be explained
00:05:34.480 --> 00:05:36.550
by the same microscopic interactions
00:05:36.550 --> 00:05:39.110
that cause the other forms of energy.
00:05:39.110 --> 00:05:41.960
In conclusion, we can see
energy at the macroscopic scale,
00:05:41.960 --> 00:05:44.240
like temperature or light being emitted.
00:05:44.240 --> 00:05:46.500
However, we must look at the microscale
00:05:46.500 --> 00:05:49.010
to observe the different forms of energy
00:05:49.010 --> 00:05:51.550
that we experience are
really just the result
00:05:51.550 --> 00:05:54.750
of kinetic and potential
energy of particles.
00:05:54.750 --> 00:05:55.883
How cool!
|
Energy and fields | https://www.youtube.com/watch?v=rMNJfR168_U | vtt | https://www.youtube.com/api/timedtext?v=rMNJfR168_U&ei=3FWUZbStDYmpp-oP-7iHkAs&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=7EAFEA599A0FFA0F55AE8BFFCECC87B714FB7CED.A6E336A330632F9BAC43E8B6D5616183FEC482B2&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.410 --> 00:00:02.850
- [Instructor] In previous
videos we have already defined
00:00:02.850 --> 00:00:04.920
or provided a definition for energy
00:00:04.920 --> 00:00:07.780
as the capacity to do work.
00:00:07.780 --> 00:00:11.870
We have also talked about
the notion of a field.
00:00:11.870 --> 00:00:14.460
We have talked about things
like an electric field
00:00:14.460 --> 00:00:16.710
or a gravitational field.
00:00:16.710 --> 00:00:19.080
And these are really mental constructs
00:00:19.080 --> 00:00:23.700
that we have produced to
explain force at a distance.
00:00:23.700 --> 00:00:26.910
For example, if I have a planet here
00:00:26.910 --> 00:00:30.830
and then I have some other
object here that has some mass,
00:00:30.830 --> 00:00:35.830
we know that these are going
to exert forces on each other,
00:00:36.030 --> 00:00:38.830
and actually equal and
opposite forces on each other.
00:00:38.830 --> 00:00:41.680
And scientists said, well,
they're not touching each other.
00:00:41.680 --> 00:00:44.130
How are they exerting
forces on each other?
00:00:44.130 --> 00:00:46.660
And so they introduced
this notion of a field
00:00:46.660 --> 00:00:49.480
that each of these objects produce,
00:00:49.480 --> 00:00:52.230
a gravitational field of sorts.
00:00:52.230 --> 00:00:53.980
Now Einstein came later and said,
00:00:53.980 --> 00:00:56.530
well, actually they're
warping space, time,
00:00:56.530 --> 00:00:57.363
et cetera, et cetera.
00:00:57.363 --> 00:00:59.760
But a field is one way to think
00:00:59.760 --> 00:01:02.860
about how they're able to induce a force
00:01:02.860 --> 00:01:04.670
so to speak in each other.
00:01:04.670 --> 00:01:08.060
Similarly, if you have
two electric charges,
00:01:08.060 --> 00:01:11.650
let's say you have two negative
point charges like that.
00:01:11.650 --> 00:01:14.370
We know that they push away on each other,
00:01:14.370 --> 00:01:16.850
that like charges repel.
00:01:16.850 --> 00:01:18.110
Well, they're not touching each other.
00:01:18.110 --> 00:01:20.757
How do they know to have
a force being applied
00:01:20.757 --> 00:01:23.160
to them in opposite directions?
00:01:23.160 --> 00:01:25.140
So once again, there's this idea
00:01:25.140 --> 00:01:27.460
that each of these produces a field,
00:01:27.460 --> 00:01:30.830
the other one is in the
other electric charges field.
00:01:30.830 --> 00:01:35.090
And then that field
somehow applies that force
00:01:35.090 --> 00:01:37.720
or makes that force
happen to the other thing.
00:01:37.720 --> 00:01:39.840
Notice, the field is a useful concept
00:01:39.840 --> 00:01:41.490
to predict what will happen
00:01:41.490 --> 00:01:43.327
and to quantify how it could happen.
00:01:43.327 --> 00:01:45.600
But it really is just something
00:01:45.600 --> 00:01:48.794
in our minds to make
sense of the universe.
00:01:48.794 --> 00:01:50.180
So with that out of the way,
00:01:50.180 --> 00:01:52.410
let's look at this water
wheel right over here.
00:01:52.410 --> 00:01:55.290
You can see that the
water comes down from here
00:01:55.290 --> 00:01:56.610
and then it falls.
00:01:56.610 --> 00:01:58.460
And as it falls, it pushes,
00:01:58.460 --> 00:02:00.640
it fills up these things right over here
00:02:00.640 --> 00:02:01.840
which then pushes it down.
00:02:01.840 --> 00:02:03.800
And then the whole wheel turns.
00:02:03.800 --> 00:02:07.470
And then that wheel could do work.
00:02:07.470 --> 00:02:09.180
Actually could do useful work.
00:02:09.180 --> 00:02:12.086
In a physics context, not all
work is necessarily useful.
00:02:12.086 --> 00:02:14.780
But this could actually do useful work.
00:02:14.780 --> 00:02:18.660
So what I wanna think about is
two different drops of water.
00:02:18.660 --> 00:02:19.870
I have a drop of water here,
00:02:19.870 --> 00:02:21.445
maybe the same drop of water.
00:02:21.445 --> 00:02:26.310
When it's up here versus once
it has gone all the way down
00:02:26.310 --> 00:02:28.030
and has been dumped into what I'm assuming
00:02:28.030 --> 00:02:31.150
is a stream down here.
00:02:31.150 --> 00:02:35.380
Now, which one has a
higher capacity to do work?
00:02:35.380 --> 00:02:37.280
Pause this video and think about that.
00:02:39.490 --> 00:02:42.880
Well, I just told you that
when the water drop is up here,
00:02:42.880 --> 00:02:45.650
it has the capacity as it falls
00:02:45.650 --> 00:02:48.080
because of the gravitational field,
00:02:48.080 --> 00:02:49.850
which is pulling down on it.
00:02:49.850 --> 00:02:52.360
And by the way, if the gravitational field
00:02:52.360 --> 00:02:54.020
is pulling down on the water drop,
00:02:54.020 --> 00:02:57.328
that water drop is also
pulling up on earth.
00:02:57.328 --> 00:02:59.780
But this gravitational field of earth
00:02:59.780 --> 00:03:02.000
is pulling down on that water drop.
00:03:02.000 --> 00:03:03.310
And because of that,
00:03:03.310 --> 00:03:05.570
if the water drop is not supported
00:03:05.570 --> 00:03:07.947
it can actually do work in this example
00:03:07.947 --> 00:03:12.700
on its way to being in this
position right over here.
00:03:12.700 --> 00:03:14.050
Now this position right over here,
00:03:14.050 --> 00:03:16.640
in theory, it could maybe still do work.
00:03:16.640 --> 00:03:19.050
Maybe there's a cliff right over here
00:03:19.050 --> 00:03:20.640
and it can continue to pour down.
00:03:20.640 --> 00:03:22.890
But the water drop up here
clearly has the capacity
00:03:22.890 --> 00:03:25.330
to do more work because
it has the potential work
00:03:25.330 --> 00:03:28.210
that it can do from
going from here to here.
00:03:28.210 --> 00:03:29.930
And then obviously it could then continue
00:03:29.930 --> 00:03:33.270
to do any work that this
position would allow it to have.
00:03:33.270 --> 00:03:35.887
So we would say that this water drop
00:03:35.887 --> 00:03:38.289
by virtue of its position,
00:03:38.289 --> 00:03:42.180
has a higher capacity to do
work and has more energy.
00:03:42.180 --> 00:03:43.840
And what is a form of that energy?
00:03:43.840 --> 00:03:47.100
Well, in this case, it's
gravitational potential energy.
00:03:47.100 --> 00:03:49.930
It's energy that is stored.
00:03:49.930 --> 00:03:51.100
And I put that in quotes
00:03:51.100 --> 00:03:52.380
because it's not like
you're going to be able
00:03:52.380 --> 00:03:54.940
to open that water drop and
all of a sudden see energy,
00:03:54.940 --> 00:03:58.500
but it's energy that's stored
by virtue of its position.
00:03:58.500 --> 00:03:59.840
Another way to think about it
00:03:59.840 --> 00:04:01.890
is instead of imagining that the energy
00:04:01.890 --> 00:04:03.340
is stored in the water drop,
00:04:03.340 --> 00:04:05.520
and it is really happening in our minds,
00:04:05.520 --> 00:04:08.770
is to say that that energy
is stored in the field.
00:04:08.770 --> 00:04:11.810
In this case, this gravitational field.
00:04:11.810 --> 00:04:15.070
Now the gravitational field
is pulling on this water drop.
00:04:15.070 --> 00:04:16.900
So the direction of motion
00:04:16.900 --> 00:04:19.950
would actually reduce
the energy in the field.
00:04:19.950 --> 00:04:23.550
So if we just let things happen,
earth's gravitational field
00:04:23.550 --> 00:04:25.810
is going to pull on this water drop.
00:04:25.810 --> 00:04:28.020
And actually that water drop
has a gravitational field
00:04:28.020 --> 00:04:29.480
that's going to pull up on earth,
00:04:29.480 --> 00:04:32.420
but as that water drop gets pulled down,
00:04:32.420 --> 00:04:34.580
the total amount of energy stored
00:04:34.580 --> 00:04:36.640
in the field is going to go down.
00:04:36.640 --> 00:04:37.790
Now what happened to that energy?
00:04:37.790 --> 00:04:40.280
That energy gets
transferred out of the field
00:04:40.280 --> 00:04:42.470
into kinetic energy of this wheel,
00:04:42.470 --> 00:04:44.970
which could then be
transferred into other things.
|
What is energy? | https://www.youtube.com/watch?v=zKb3QRyIDnM | vtt | https://www.youtube.com/api/timedtext?v=zKb3QRyIDnM&ei=3FWUZeGQDPe1vdIPot2CsA0&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=8B2C683DA7166F5147C682D4FE3DF45C52E632EB.16A03906BA077B0ECB888F25E80DBE41FB8709B6&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.120 --> 00:00:02.160
- [Instructor] Energy is a
word we hear all the time
00:00:02.160 --> 00:00:03.560
in seemingly different contexts,
00:00:03.560 --> 00:00:04.900
almost every single day.
00:00:04.900 --> 00:00:07.170
We hear about renewable
energy on the news,
00:00:07.170 --> 00:00:08.630
and particularly in the winter,
00:00:08.630 --> 00:00:10.400
we hear people talking
about their energy bills,
00:00:10.400 --> 00:00:11.500
because they're worried
00:00:11.500 --> 00:00:13.830
about how much it's going
to cost to heat their homes.
00:00:13.830 --> 00:00:14.950
So this brings about the question
00:00:14.950 --> 00:00:18.530
of what is energy that we
can talk about it so often
00:00:18.530 --> 00:00:20.890
and in seemingly such different ways?
00:00:20.890 --> 00:00:23.590
So in physics, we actually
have a specific definition
00:00:23.590 --> 00:00:25.040
of what energy is,
00:00:25.040 --> 00:00:26.470
and you'll see it's
really not that different
00:00:26.470 --> 00:00:29.060
from how we talk about energy day to day.
00:00:29.060 --> 00:00:33.130
Energy in physics is defined
as the ability to do work.
00:00:33.130 --> 00:00:35.800
We can't talk about energy
without talking about work,
00:00:35.800 --> 00:00:37.890
so we should probably
define that right now,
00:00:37.890 --> 00:00:39.550
because work is another one of these words
00:00:39.550 --> 00:00:41.730
that we use an awful lot, but once again,
00:00:41.730 --> 00:00:44.193
physics has a specific definition for it.
00:00:45.130 --> 00:00:47.010
In physics, work is performed
00:00:47.010 --> 00:00:50.120
when you apply force over a distance.
00:00:50.120 --> 00:00:52.170
We can actually write this as an equation,
00:00:52.170 --> 00:00:56.140
W equals F times d, where
W is work, F is force,
00:00:56.140 --> 00:00:58.323
and d is distance or displacement.
00:00:59.260 --> 00:01:01.130
If you've ever moved a box, a suitcase,
00:01:01.130 --> 00:01:03.780
or really any object in
your room across the floor
00:01:03.780 --> 00:01:06.590
just to get it out of your
way, you performed work.
00:01:06.590 --> 00:01:09.170
You had to apply force
to that box to move it
00:01:09.170 --> 00:01:11.490
whatever distance it took
to get out of your way.
00:01:11.490 --> 00:01:13.030
If it was a short distance,
00:01:13.030 --> 00:01:14.380
you can see from the equation,
00:01:14.380 --> 00:01:16.330
that that's going to be less work
00:01:16.330 --> 00:01:18.650
than if you have to move
it across your entire room,
00:01:18.650 --> 00:01:21.070
down the hall, into another room.
00:01:21.070 --> 00:01:23.240
And in order to perform
this work to move the box
00:01:23.240 --> 00:01:25.910
out of your way, you had
to have energy available.
00:01:25.910 --> 00:01:27.710
That energy is enabling
you to do the work,
00:01:27.710 --> 00:01:29.570
because you're going
to transfer the energy
00:01:29.570 --> 00:01:32.930
from yourself to that
box in order to move it.
00:01:32.930 --> 00:01:35.670
So, another way that we can
think about work and energy
00:01:35.670 --> 00:01:38.240
is that the change in
energy of the system,
00:01:38.240 --> 00:01:39.700
in this case, you and the box,
00:01:39.700 --> 00:01:42.250
is actually equal to the work done.
00:01:42.250 --> 00:01:43.990
When we define energy this way,
00:01:43.990 --> 00:01:46.850
it allows us to do a lot
of interesting things.
00:01:46.850 --> 00:01:49.800
We've set up a way to
measure and calculate energy,
00:01:49.800 --> 00:01:52.890
so it's actually a quantifiable property.
00:01:52.890 --> 00:01:54.870
Let's go back to the example of a box,
00:01:54.870 --> 00:01:57.480
and let's say that instead
of just trying to move a box
00:01:57.480 --> 00:01:58.940
out of your way in your room,
00:01:58.940 --> 00:02:01.010
you're actually going to pack
up everything in your room,
00:02:01.010 --> 00:02:02.120
because you're going to move
00:02:02.120 --> 00:02:03.660
to a completely different house.
00:02:03.660 --> 00:02:06.000
And now you have 10 boxes to move.
00:02:06.000 --> 00:02:09.320
We can actually calculate
the energy required
00:02:09.320 --> 00:02:12.000
to move all of those boxes.
00:02:12.000 --> 00:02:14.500
You might be saying to
yourself, "Wait a minute.
00:02:14.500 --> 00:02:16.230
I'm now moving 10 boxes.
00:02:16.230 --> 00:02:18.030
That actually sounds kind of tiring.
00:02:18.900 --> 00:02:20.150
And if I'm getting tired,
00:02:20.150 --> 00:02:22.550
does that mean I'm
actually losing energy?"
00:02:22.550 --> 00:02:25.560
It turns out that energy
is coming from somewhere,
00:02:25.560 --> 00:02:27.750
and in this case, it's
going to come from food.
00:02:27.750 --> 00:02:29.440
So as you're moving these boxes,
00:02:29.440 --> 00:02:31.310
you may find yourself getting hungry,
00:02:31.310 --> 00:02:33.090
so you should probably grab a snack,
00:02:33.090 --> 00:02:35.620
something like, I don't know, an apple,
00:02:35.620 --> 00:02:37.920
let's pretend that's
what I've drawn there,
00:02:37.920 --> 00:02:39.730
so that you can get more energy
00:02:39.730 --> 00:02:41.913
to move the rest of those 10 boxes.
00:02:43.070 --> 00:02:46.530
And you might be thinking
now, "Wait a minute.
00:02:46.530 --> 00:02:50.290
This energy coming from
food to me seems different
00:02:50.290 --> 00:02:52.970
than energy between me and moving a box."
00:02:52.970 --> 00:02:56.060
And that's because you can
actually see the box moving,
00:02:56.060 --> 00:02:58.410
which brings us to our next point,
00:02:58.410 --> 00:03:00.130
energy comes in various forms
00:03:00.130 --> 00:03:02.330
and they don't all look the same.
00:03:02.330 --> 00:03:04.740
We have equations to quantify the energy
00:03:04.740 --> 00:03:05.810
of these various forms,
00:03:05.810 --> 00:03:08.300
and we'll talk about
those in another video,
00:03:08.300 --> 00:03:10.610
but the key here is that energy
00:03:10.610 --> 00:03:12.450
can transfer between objects
00:03:12.450 --> 00:03:14.750
and it can also convert
between different forms,
00:03:14.750 --> 00:03:18.240
such as when you eat and
get energy from that apple,
00:03:18.240 --> 00:03:21.510
and then you use that
energy to move a box.
00:03:21.510 --> 00:03:25.530
So to summarize, energy
is the ability to do work.
00:03:25.530 --> 00:03:28.810
Work is done when you apply
force across a distance,
00:03:28.810 --> 00:03:31.090
and we can write that as an equation.
00:03:31.090 --> 00:03:33.010
And because we can calculate the energy
00:03:33.010 --> 00:03:35.040
of a system using equations,
00:03:35.040 --> 00:03:37.883
we now know that energy is
a quantifiable property.
|
Calculating gravitational potential energy | https://www.youtube.com/watch?v=VafUJehX48w | vtt | https://www.youtube.com/api/timedtext?v=VafUJehX48w&ei=3FWUZcXnLIDoxN8PgpamyAs&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=EF4CFC08AAC10E86F83383D048C05682CB1AF526.D3710B0541DD23313F681BD4985577A0C1804166&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:01.260 --> 00:00:02.400
- [Instructor] In previous videos,
00:00:02.400 --> 00:00:05.640
we have introduced the idea of energy
00:00:05.640 --> 00:00:08.770
as the capacity to do work
00:00:08.770 --> 00:00:11.820
and we have talked about
multiple types of energies.
00:00:11.820 --> 00:00:14.830
We've talked about kinetic
energy, energy due to motion.
00:00:14.830 --> 00:00:17.330
We've talked about potential energy,
00:00:17.330 --> 00:00:21.150
which is energy by virtue of position.
00:00:21.150 --> 00:00:23.570
And when we're talking
about potential energy,
00:00:23.570 --> 00:00:27.130
we're talking about it relative
to some other position.
00:00:27.130 --> 00:00:29.150
And in particular, in this video,
00:00:29.150 --> 00:00:31.980
we're going to talk about
gravitational potential energy,
00:00:31.980 --> 00:00:34.300
which is potential energy due to position
00:00:34.300 --> 00:00:36.660
in a gravitational field.
00:00:36.660 --> 00:00:41.000
So let's say that this is
the surface of the earth.
00:00:41.000 --> 00:00:46.000
Let's say that I have a five
kilogram mass right over here,
00:00:47.650 --> 00:00:52.650
and let's say that it is 10 meters above
00:00:53.840 --> 00:00:55.300
the surface of the earth.
00:00:55.300 --> 00:00:58.780
My question to you is how
much more potential energy
00:00:58.780 --> 00:01:00.400
does it have in this position
00:01:00.400 --> 00:01:03.210
than when it is in this position,
00:01:03.210 --> 00:01:06.310
when it is sitting on
the surface of the earth,
00:01:06.310 --> 00:01:08.430
10 meters lower?
00:01:08.430 --> 00:01:10.630
Pause the video and try
to think about that.
00:01:12.610 --> 00:01:15.350
All right, now let's
work on this together.
00:01:15.350 --> 00:01:19.300
So our gravitational potential
energy is going to be equal
00:01:19.300 --> 00:01:22.950
to our mass times lowercase g,
00:01:22.950 --> 00:01:25.210
which you can view as the constant
00:01:25.210 --> 00:01:28.660
for earth's gravitational field
near the surface of earth.
00:01:28.660 --> 00:01:31.060
And the reason why I say
near the surface of earth
00:01:31.060 --> 00:01:33.550
is as you get further
and further from earth,
00:01:33.550 --> 00:01:35.330
this thing could actually change,
00:01:35.330 --> 00:01:37.030
but near the surface of the earth,
00:01:37.030 --> 00:01:39.460
we assume that it is roughly constant,
00:01:39.460 --> 00:01:43.560
and then you multiply
that times your height.
00:01:43.560 --> 00:01:46.070
So calculating this is
pretty straightforward
00:01:46.070 --> 00:01:48.270
as long as you know what g is.
00:01:48.270 --> 00:01:53.270
G, we can approximate it as
9.8 meters per second squared.
00:01:55.240 --> 00:01:57.310
So when you multiply all of this out,
00:01:57.310 --> 00:01:59.970
this is going to be equal to your mass,
00:01:59.970 --> 00:02:01.983
which is five kilograms,
00:02:03.240 --> 00:02:06.310
times the gravitational field constant,
00:02:06.310 --> 00:02:09.980
so times 9.8 meters per second squared,
00:02:14.400 --> 00:02:15.560
times your height,
00:02:15.560 --> 00:02:18.010
which in this situation is 10 meters,
00:02:18.010 --> 00:02:20.750
so times 10 meters.
00:02:20.750 --> 00:02:25.653
And so this is going to be
equal to five times 9.8 is 49,
00:02:26.530 --> 00:02:30.110
times 10 is 490.
00:02:30.110 --> 00:02:31.453
We have kilograms,
00:02:32.540 --> 00:02:34.810
and then we have meters times meters,
00:02:34.810 --> 00:02:39.280
so times meters squared
per second squared.
00:02:39.280 --> 00:02:41.160
And these might seem like strange units,
00:02:41.160 --> 00:02:42.510
but you might recognize this
00:02:42.510 --> 00:02:45.960
as also the units of force times distance,
00:02:45.960 --> 00:02:49.420
which we could also
express in terms of joules.
00:02:49.420 --> 00:02:52.340
So this is 490 joules,
00:02:52.340 --> 00:02:57.120
which is our units both for
energy and our unit for work.
00:02:57.120 --> 00:03:00.320
Now, let's make sure that
this is intuitive sense.
00:03:00.320 --> 00:03:01.680
Well, one way to think about it is
00:03:01.680 --> 00:03:05.990
how much work would it take
to go from here to here?
00:03:05.990 --> 00:03:10.380
Well, you're going to be lifting
it a distance of 10 meters,
00:03:10.380 --> 00:03:13.180
and as you're lifting it
a distance of 10 meters,
00:03:13.180 --> 00:03:15.410
what is the force you're
going to have to apply?
00:03:15.410 --> 00:03:16.640
Well, the force you're
going to have to apply
00:03:16.640 --> 00:03:18.250
is going to be the weight of the object.
00:03:18.250 --> 00:03:21.430
The weight is its mass times
the gravitational field.
00:03:21.430 --> 00:03:24.570
So in order to put it in that
position from the ground,
00:03:24.570 --> 00:03:27.320
you're going to have to do
its weight times the height,
00:03:27.320 --> 00:03:30.120
or 490 joules of work.
00:03:30.120 --> 00:03:33.930
And so you can do 490 joules
of work to get it there
00:03:33.930 --> 00:03:35.300
and then you can think about it
00:03:35.300 --> 00:03:37.830
as that energy being stored this way.
00:03:37.830 --> 00:03:39.460
And now it can then do that work.
00:03:39.460 --> 00:03:40.800
How could it do that work?
00:03:40.800 --> 00:03:42.750
Well, there's a bunch
of ways you could do it.
00:03:42.750 --> 00:03:47.750
You could have this attached
to maybe a pulley of some kind
00:03:47.850 --> 00:03:51.650
and then if it had another
weight right over here,
00:03:51.650 --> 00:03:55.420
and let's just, for simplicity,
assume it has the same mass,
00:03:55.420 --> 00:03:59.000
well, if you let this
first purple mass go,
00:03:59.000 --> 00:04:00.370
it's going to go down.
00:04:00.370 --> 00:04:02.430
And if you assume that this pulley
00:04:02.430 --> 00:04:04.010
is completely frictionless,
00:04:04.010 --> 00:04:07.130
this mass is going to
be lifted by 10 meters.
00:04:07.130 --> 00:04:09.750
And so if you have a five kilogram mass
00:04:09.750 --> 00:04:13.470
that is lifted by 10 meters in
Earth's gravitational field,
00:04:13.470 --> 00:04:15.060
near the surface of the earth,
00:04:15.060 --> 00:04:18.270
you would have just
done 490 joules of work.
00:04:18.270 --> 00:04:19.890
So hopefully this makes sense
00:04:19.890 --> 00:04:21.490
why you're just really taking the weight
00:04:21.490 --> 00:04:23.040
of the object times its height.
00:04:23.040 --> 00:04:24.700
And hopefully it also makes sense
00:04:24.700 --> 00:04:28.100
that it then has the capacity
to do that amount of work.
00:04:28.100 --> 00:04:31.953
And in this case, we said
relative to sitting on the ground.
|
Calculating kinetic energy | https://www.youtube.com/watch?v=3FIFHRrut2s | vtt | https://www.youtube.com/api/timedtext?v=3FIFHRrut2s&ei=3FWUZcL3LN3ixN8P_6C02A0&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=5CA164B51A6044FE01594A6FBB1DA6E48D8B0C13.11122D7DA475A85922F46E10C1D8CDB36D6F0865&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.560 --> 00:00:01.410
- [Instructor] In this video,
00:00:01.410 --> 00:00:03.420
we're gonna talk about kinetic energy
00:00:03.420 --> 00:00:06.540
and we're also gonna think
about how to calculate it.
00:00:06.540 --> 00:00:09.020
So you can already imagine
based on the word kinetic,
00:00:09.020 --> 00:00:10.780
which is referring to motion
00:00:10.780 --> 00:00:13.560
that this is the energy that an object has
00:00:13.560 --> 00:00:15.650
by virtue of its motion.
00:00:15.650 --> 00:00:17.100
And when we talk about energy,
00:00:17.100 --> 00:00:20.570
we're talking about its
capacity to do work.
00:00:20.570 --> 00:00:24.390
So just based on that early
definition of kinetic energy,
00:00:24.390 --> 00:00:26.300
which of these two running backs
00:00:26.300 --> 00:00:28.920
do you think has more kinetic energy,
00:00:28.920 --> 00:00:33.010
this gentleman on the left
whose mass is a 100 kilograms
00:00:33.010 --> 00:00:36.290
and who is traveling at a
speed of two meters per second,
00:00:36.290 --> 00:00:37.470
or the gentleman on the right,
00:00:37.470 --> 00:00:39.660
who has a mass of 25 kilograms
00:00:39.660 --> 00:00:43.120
and who's traveling with a
speed of four meters per second?
00:00:43.120 --> 00:00:45.020
Pause this video and think about that.
00:00:46.240 --> 00:00:48.550
All right, now let's
think about this together.
00:00:48.550 --> 00:00:50.530
So I'm first just gonna
give you the formula
00:00:50.530 --> 00:00:53.620
for kinetic energy, but then
we are going to derive it.
00:00:53.620 --> 00:00:56.510
So the formula for kinetic
energy is that it's equal
00:00:56.510 --> 00:00:59.480
to 1/2 times the mass of the object,
00:00:59.480 --> 00:01:02.250
times the magnitude of
its velocity squared,
00:01:02.250 --> 00:01:03.250
or another way to think about it,
00:01:03.250 --> 00:01:05.240
its speed squared.
00:01:05.240 --> 00:01:08.390
And so given this formula, pause the video
00:01:08.390 --> 00:01:10.330
and see if you can
calculate the kinetic energy
00:01:10.330 --> 00:01:11.930
for each of these running backs.
00:01:13.100 --> 00:01:15.911
All right, let's calculate
the kinetic energy
00:01:15.911 --> 00:01:18.210
for this guy on the left.
00:01:18.210 --> 00:01:22.430
It's gonna be 1/2 times his mass,
00:01:22.430 --> 00:01:27.430
which is 100 kilograms, times
the square of the speed,
00:01:28.000 --> 00:01:32.610
so times four meters
squared per second squared,
00:01:32.610 --> 00:01:35.010
have to make sure that we
square the units as well.
00:01:35.010 --> 00:01:37.570
And this is going to be
equal to 1/2 times 100
00:01:37.570 --> 00:01:42.334
is 50 times four is 200 and
then the units are kilogram
00:01:42.334 --> 00:01:45.960
meter squared per second squared.
00:01:45.960 --> 00:01:48.150
And you might already recognize
that this is the same thing
00:01:48.150 --> 00:01:52.500
as kilogram meter per
second squared times meters,
00:01:52.500 --> 00:01:56.450
or these are really the units
of force times distance,
00:01:56.450 --> 00:01:58.520
or this is the units of energy
00:01:58.520 --> 00:02:01.700
which we can write as 200 joules.
00:02:01.700 --> 00:02:04.540
Now let's do the same
thing for this running back
00:02:04.540 --> 00:02:06.330
that has less mass.
00:02:06.330 --> 00:02:10.170
Kinetic energy here is
gonna be 1/2 times the mass,
00:02:10.170 --> 00:02:14.580
25 kilograms times the
square of the speed here,
00:02:14.580 --> 00:02:19.220
so that's gonna be 16 meters
squared per second squared.
00:02:19.220 --> 00:02:20.930
And then that gets us.
00:02:20.930 --> 00:02:25.120
We're essentially gonna have
1/2 times 16 is eight times 25,
00:02:25.120 --> 00:02:27.600
200, and we get the exact same units
00:02:27.600 --> 00:02:29.960
and so we can go straight to 200 joules.
00:02:29.960 --> 00:02:31.620
So it turns out that they have
00:02:31.620 --> 00:02:33.900
the exact same kinetic energy.
00:02:33.900 --> 00:02:36.610
Even though the gentleman
on the right has one fourth
00:02:36.610 --> 00:02:39.270
the mass and only twice the speed,
00:02:39.270 --> 00:02:42.640
we see that we square
the speed right over here
00:02:42.640 --> 00:02:44.120
so that makes a huge difference.
00:02:44.120 --> 00:02:46.730
And so their energy due to their motion,
00:02:46.730 --> 00:02:50.360
they have the same capacity to do work.
00:02:50.360 --> 00:02:51.540
Now, some of you are thinking,
00:02:51.540 --> 00:02:53.970
where does this formula come from?
00:02:53.970 --> 00:02:55.930
And one way to think about work and energy
00:02:55.930 --> 00:03:00.310
is that you can use
work to transfer energy
00:03:00.310 --> 00:03:02.830
to a system or to an object somehow.
00:03:02.830 --> 00:03:05.710
And then that energy is
that object's capacity
00:03:05.710 --> 00:03:07.380
to do work again.
00:03:07.380 --> 00:03:10.710
So let's imagine some
object that has a mass m
00:03:10.710 --> 00:03:14.830
and the magnitude of its
velocity or its speed is v.
00:03:14.830 --> 00:03:17.920
So what would be the work necessary
00:03:17.920 --> 00:03:20.730
to bring that object that has mass m
00:03:20.730 --> 00:03:25.730
to a speed of v, assuming
it's starting at a standstill?
00:03:25.740 --> 00:03:27.840
Well, let's think about it a little bit.
00:03:27.840 --> 00:03:31.360
Work is equal to the magnitude of force
00:03:31.360 --> 00:03:32.720
in a certain direction,
00:03:32.720 --> 00:03:36.860
times the magnitude of the
displacement in that direction,
00:03:36.860 --> 00:03:37.810
which we could write like that.
00:03:37.810 --> 00:03:40.290
Sometimes they use s for the magnitude
00:03:40.290 --> 00:03:42.090
of displacement as well.
00:03:42.090 --> 00:03:45.130
And so what is the
force the same thing as?
00:03:45.130 --> 00:03:48.050
We know that the force is the same thing
00:03:48.050 --> 00:03:51.970
as mass times the acceleration.
00:03:51.970 --> 00:03:52.980
And we're going to assume
00:03:52.980 --> 00:03:54.500
that we have constant acceleration
00:03:54.500 --> 00:03:57.510
just so that we can simplify
our derivation here.
00:03:57.510 --> 00:03:59.960
And then what's the distance
that we're gonna travel.
00:03:59.960 --> 00:04:02.530
Well, the distance is gonna
be the average magnitude
00:04:02.530 --> 00:04:04.690
of the velocity, or we
could say the average speed,
00:04:04.690 --> 00:04:06.420
so I'll write it like this,
00:04:06.420 --> 00:04:11.420
times the time that it takes
to accelerate the object
00:04:11.420 --> 00:04:13.640
to a velocity of v.
00:04:13.640 --> 00:04:15.970
Well, how long does it take
to accelerate an object
00:04:15.970 --> 00:04:19.130
to a velocity of v if
you're accelerating it at a?
00:04:19.130 --> 00:04:22.080
Well, this is just gonna
be the velocity divided
00:04:22.080 --> 00:04:23.120
by the acceleration.
00:04:23.120 --> 00:04:23.953
Think about it.
00:04:23.953 --> 00:04:25.820
If you're going, trying
to get to a velocity
00:04:25.820 --> 00:04:28.230
of four meters per second,
and you're accelerating
00:04:28.230 --> 00:04:30.780
at two meters per second, per second,
00:04:30.780 --> 00:04:34.939
four divided by two is gonna
leave you with two seconds.
00:04:34.939 --> 00:04:37.750
And if you're starting at a speed of zero
00:04:37.750 --> 00:04:40.080
and you're going to a
magnitude of a velocity
00:04:40.080 --> 00:04:44.180
or a speed of v, and you're
assuming constant acceleration,
00:04:44.180 --> 00:04:48.870
your average velocity is
just gonna be v over two.
00:04:48.870 --> 00:04:51.710
So this is just v over two.
00:04:51.710 --> 00:04:54.990
And then we get a little bit
of a drum roll right over here.
00:04:54.990 --> 00:04:57.890
We see that acceleration
cancels with acceleration,
00:04:57.890 --> 00:05:02.890
and we are left with mass
times v squared over two,
00:05:03.460 --> 00:05:05.470
mv squared over two,
00:05:05.470 --> 00:05:08.440
which is exactly what
we had right over here.
00:05:08.440 --> 00:05:11.540
So the work necessary
to accelerate an object
00:05:11.540 --> 00:05:16.540
of mass m from zero speed to
a speed of v is exactly this.
00:05:17.490 --> 00:05:19.790
And that's how much energy is then stored
00:05:19.790 --> 00:05:22.730
in that object by virtue of its motion.
00:05:22.730 --> 00:05:24.400
And if you don't have energy loss
00:05:24.400 --> 00:05:27.313
it could in theory, do this much work.
|
Energy in fields | https://www.youtube.com/watch?v=waw8-hFq1cc | vtt | https://www.youtube.com/api/timedtext?v=waw8-hFq1cc&ei=3FWUZf7XHJXxmLAPw_W_0AI&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=3B1EEF227C22794E80FB74E872F605437133A8ED.E4403D141FE7FBB8C4D8C1220ABE0208D62C23DE&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.530 --> 00:00:01.660
- [Presenter] In this
video, we're gonna talk
00:00:01.660 --> 00:00:04.290
about how energy is stored in field
00:00:04.290 --> 00:00:07.530
and in particular, how if we
change the position of things
00:00:07.530 --> 00:00:11.090
within that field, how it
might change the energy.
00:00:11.090 --> 00:00:13.060
So, just as a bit of a refresher,
00:00:13.060 --> 00:00:15.910
let's remind ourselves what energy is.
00:00:15.910 --> 00:00:20.910
It is the capacity to do work.
00:00:21.160 --> 00:00:23.330
And we've also seen that work,
00:00:23.330 --> 00:00:26.320
we can view it as equal
to the magnitude of force
00:00:26.320 --> 00:00:30.600
times the displacement in
the direction of that force.
00:00:30.600 --> 00:00:34.040
And then we can also remind
ourselves what a field is.
00:00:34.040 --> 00:00:35.810
And I'm not just talking about a big lawn
00:00:35.810 --> 00:00:37.970
or something like that, a football field.
00:00:37.970 --> 00:00:40.900
I'm talking about a general
idea in physics that's used.
00:00:40.900 --> 00:00:44.040
It's really just a concept
that allows us to predict
00:00:44.040 --> 00:00:48.680
and explain how to things that
are not touching each other
00:00:48.680 --> 00:00:49.940
are still interacting,
00:00:49.940 --> 00:00:52.640
are still able to exert
forces on each other.
00:00:52.640 --> 00:00:54.500
And in other videos, I've
also talked about that.
00:00:54.500 --> 00:00:56.670
Really nothing in this
universe is touching.
00:00:56.670 --> 00:00:59.850
We just conceptualize
that sometimes they are.
00:00:59.850 --> 00:01:01.520
But just as an example of a field,
00:01:01.520 --> 00:01:02.770
we have an electric field here.
00:01:02.770 --> 00:01:04.500
I could have done another type of field,
00:01:04.500 --> 00:01:06.520
we could have done a magnetic field,
00:01:06.520 --> 00:01:08.800
we could have done a gravitational field.
00:01:08.800 --> 00:01:11.160
Although when you study general relativity
00:01:11.160 --> 00:01:12.650
which Einstein gave us,
00:01:12.650 --> 00:01:16.090
we realize that it might
not exactly be optimal
00:01:16.090 --> 00:01:17.630
to think about it as a field.
00:01:17.630 --> 00:01:19.250
But in an electric field, right over here,
00:01:19.250 --> 00:01:21.810
we have a positive charge,
we have a negative charge.
00:01:21.810 --> 00:01:23.820
We know from experience
00:01:23.820 --> 00:01:26.420
that these two things attract each other
00:01:26.420 --> 00:01:29.610
and the convention is to
draw these field lines
00:01:29.610 --> 00:01:33.120
that go from the positive
towards the negative.
00:01:33.120 --> 00:01:37.150
Now, if we were to just let
go of these two point charges
00:01:37.150 --> 00:01:38.980
over here, what would happen?
00:01:38.980 --> 00:01:42.300
Well, we know that due to the
electric field constructed
00:01:42.300 --> 00:01:44.310
or created or that we imagined was created
00:01:44.310 --> 00:01:46.260
by this negative point charge,
00:01:46.260 --> 00:01:49.450
this positive charge would have a force
00:01:49.450 --> 00:01:51.310
acting on it towards the negative charge
00:01:51.310 --> 00:01:53.610
and vice versa due to the electric field
00:01:53.610 --> 00:01:56.370
that is created by the positive charge.
00:01:56.370 --> 00:01:59.330
The negative charge is
going to also be attracted
00:01:59.330 --> 00:02:00.170
to the positive charge.
00:02:00.170 --> 00:02:02.840
They're both going to
move towards each other.
00:02:02.840 --> 00:02:05.280
And so, when we talk
about energy in fields
00:02:05.280 --> 00:02:08.863
or energy stored in fields,
in our initial configuration,
00:02:10.582 --> 00:02:12.590
how is there energy in this field?
00:02:12.590 --> 00:02:14.820
How is their capacity to do work?
00:02:14.820 --> 00:02:16.720
Pause this video and think about that.
00:02:17.910 --> 00:02:19.100
Well, think about it this way.
00:02:19.100 --> 00:02:23.480
Imagine if each of these
charges were attached
00:02:23.480 --> 00:02:25.280
to some type of a mass,
00:02:25.280 --> 00:02:27.670
let me do this in a color
you can actually see.
00:02:27.670 --> 00:02:30.540
So, let's say that this is
towing some type of a mass
00:02:30.540 --> 00:02:35.290
and this is towing some type
of a mass right over here.
00:02:35.290 --> 00:02:38.590
Well, when you let go and
the forces are exerted
00:02:38.590 --> 00:02:40.570
on each of these point charges,
00:02:40.570 --> 00:02:42.530
assuming that the forces are large enough,
00:02:42.530 --> 00:02:45.060
they're going to be able
to pull these masses
00:02:45.060 --> 00:02:46.000
towards each other.
00:02:46.000 --> 00:02:48.790
So, there's a potential amount
of work that could be done
00:02:48.790 --> 00:02:50.300
and it would essentially keep happening
00:02:50.300 --> 00:02:52.750
until these point charges touch.
00:02:52.750 --> 00:02:55.070
And I used air quotes with my hand
00:02:55.070 --> 00:02:56.310
even though you can't see it,
00:02:56.310 --> 00:02:58.490
or until they can't get
any closer to each other
00:02:58.490 --> 00:03:01.920
or some other is keeping
them from getting any closer
00:03:01.920 --> 00:03:03.020
to each other.
00:03:03.020 --> 00:03:06.840
So now, let me think about how
could I increase the energy
00:03:06.840 --> 00:03:09.210
that is stored in this field.
00:03:09.210 --> 00:03:11.093
Pause the video and think about that.
00:03:12.750 --> 00:03:15.710
Well, what if I were to
keep the positive charge
00:03:15.710 --> 00:03:19.350
where it is, but if I were
to take the negative charge
00:03:19.350 --> 00:03:22.040
and if I were to move it
in a direction opposite
00:03:22.040 --> 00:03:25.940
from the force direction that
the field is trying to exert.
00:03:25.940 --> 00:03:27.660
So, instead of the negative charge there,
00:03:27.660 --> 00:03:30.830
what if I moved it all the way out there?
00:03:30.830 --> 00:03:34.080
Once again, let me do that in
a color you can actually see.
00:03:34.080 --> 00:03:35.580
Well, if I moved it out here
00:03:35.580 --> 00:03:39.270
and we're still towing
some type of a mass,
00:03:39.270 --> 00:03:42.680
you can see that when I moved
it against the direction
00:03:42.680 --> 00:03:46.070
that the force of the
field is trying to exert,
00:03:46.070 --> 00:03:48.300
that I've increased
the energy in the field
00:03:48.300 --> 00:03:50.410
because now I can do more work.
00:03:50.410 --> 00:03:55.410
I can drag this potential
mass over a larger distance.
00:03:55.410 --> 00:03:57.530
So, we have a general principle here.
00:03:57.530 --> 00:04:02.120
If we let these charges go in
the direction of the forces
00:04:02.120 --> 00:04:04.350
that are being exerted
on them due to the field,
00:04:04.350 --> 00:04:07.530
we're going to reduce
the energy in the field.
00:04:07.530 --> 00:04:11.430
But then if we are able to
move them against the forces
00:04:11.430 --> 00:04:13.190
of the field, and as you can imagine,
00:04:13.190 --> 00:04:14.420
we're going to have to put energy
00:04:14.420 --> 00:04:16.850
into the system to do that.
00:04:16.850 --> 00:04:20.010
But if we do that, then
we're storing more energy
00:04:20.010 --> 00:04:22.990
in this field because in that case,
00:04:22.990 --> 00:04:25.300
they're going to be further
away from each other
00:04:25.300 --> 00:04:28.410
and so they could drag their little masses
00:04:28.410 --> 00:04:30.553
that they're towing even further.
|
Electromagnetic radiation emission | https://www.youtube.com/watch?v=WsSMMeYh8jU | vtt | https://www.youtube.com/api/timedtext?v=WsSMMeYh8jU&ei=3FWUZZ2ULIy1xN8P6OCNkAo&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=9FA9112FF0B9EAE4E7BDFE688335B063F50AD7CC.846BCD7533A50579410BF55B8C344E1DC860811B&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.320 --> 00:00:03.040
- [Norm] Let me ask you a
seemingly simple question.
00:00:03.040 --> 00:00:06.060
I have a picture of fire
here, and my question is,
00:00:06.060 --> 00:00:08.310
what is fire?
00:00:08.310 --> 00:00:11.190
Well, what would you say if
I were to tell you that fire,
00:00:11.190 --> 00:00:13.560
as we see it, these flickering flames,
00:00:13.560 --> 00:00:16.050
it is nothing but hot air?
00:00:16.050 --> 00:00:17.460
And I know what you might be thinking.
00:00:17.460 --> 00:00:18.527
Hot air?
00:00:18.527 --> 00:00:20.140
"Norm, I've seen air that's hot,
00:00:20.140 --> 00:00:21.700
or I experienced air that's hot
00:00:21.700 --> 00:00:24.370
and I don't oftentimes even see the air,
00:00:24.370 --> 00:00:26.460
but here I clearly see something bright,
00:00:26.460 --> 00:00:28.070
something that's emitting light,
00:00:28.070 --> 00:00:31.350
something that's emitting
electromagnetic radiation."
00:00:31.350 --> 00:00:33.400
And then what I would say to you,
00:00:33.400 --> 00:00:34.550
if you were thinking that,
00:00:34.550 --> 00:00:38.490
is it actually turns out
that anything in our universe
00:00:38.490 --> 00:00:42.480
that has a temperature above
absolute zero, zero Kelvin,
00:00:42.480 --> 00:00:43.680
which is pretty much anything
00:00:43.680 --> 00:00:45.970
that you will ever come
across in your life,
00:00:45.970 --> 00:00:48.420
emits electromagnetic radiation.
00:00:48.420 --> 00:00:50.740
Objects with temperature
aren't the only way
00:00:50.740 --> 00:00:52.700
to create electromagnetic radiation,
00:00:52.700 --> 00:00:55.840
but it is a major way that's
happening all around us.
00:00:55.840 --> 00:00:57.960
Even if you were in a pitch-black room,
00:00:57.960 --> 00:01:01.000
you would be emitting
electromagnetic radiation.
00:01:01.000 --> 00:01:03.450
A tree outside, even
if it was dark outside,
00:01:03.450 --> 00:01:05.810
is emitting electromagnetic radiation.
00:01:05.810 --> 00:01:07.600
You might say, "Wait, but
I don't see the tree,"
00:01:07.600 --> 00:01:08.900
and that's because your eyes
00:01:08.900 --> 00:01:11.410
can only detect certain frequencies
00:01:11.410 --> 00:01:13.790
of electromagnetic radiation.
00:01:13.790 --> 00:01:16.440
If we look at this
diagram right over here,
00:01:16.440 --> 00:01:19.730
we can see how we've categorized
many of the frequencies,
00:01:19.730 --> 00:01:21.140
and you can see that up here,
00:01:21.140 --> 00:01:23.060
this is the frequency,
this is the wavelength,
00:01:23.060 --> 00:01:25.410
and these are in powers of 10.
00:01:25.410 --> 00:01:28.480
So you can really view this
as a logarithmic scale.
00:01:28.480 --> 00:01:29.530
And just over here,
00:01:29.530 --> 00:01:32.300
you can see that our
eyes can only visibly see
00:01:32.300 --> 00:01:37.300
a small section of this
logarithmic scale of frequencies.
00:01:37.480 --> 00:01:38.760
One of the things I like to wonder,
00:01:38.760 --> 00:01:40.620
if humans didn't have eyes,
00:01:40.620 --> 00:01:42.970
if we weren't able to detect
even the small segment
00:01:42.970 --> 00:01:44.590
of the electromagnetic spectrum,
00:01:44.590 --> 00:01:45.720
would we even know
00:01:45.720 --> 00:01:49.300
that something like
electromagnetic waves existed?
00:01:49.300 --> 00:01:52.160
But we can see you have
gamma rays, x-rays, UV rays,
00:01:52.160 --> 00:01:55.760
infrared rays, microwave,
FM, AM radio waves,
00:01:55.760 --> 00:01:57.570
long radio waves.
00:01:57.570 --> 00:01:59.430
In most hot air,
00:01:59.430 --> 00:02:02.570
the frequency isn't high
enough for us to see it.
00:02:02.570 --> 00:02:06.610
So most hot air is going to
be in the infrared range.
00:02:06.610 --> 00:02:10.380
Only if it gets hot enough
will we start to see it,
00:02:10.380 --> 00:02:13.080
and that's what's happening
with this fire here.
00:02:13.080 --> 00:02:15.800
And if you look closely at a fire,
00:02:15.800 --> 00:02:18.230
you might actually see that the location
00:02:18.230 --> 00:02:20.800
where the combustion
reaction is happening,
00:02:20.800 --> 00:02:22.800
that that actually might be dark.
00:02:22.800 --> 00:02:25.660
And then right above that,
you'll see some blue flame,
00:02:25.660 --> 00:02:28.220
and then you'll see,
maybe if you look closely,
00:02:28.220 --> 00:02:30.270
some green or yellow flame,
00:02:30.270 --> 00:02:32.740
and then you will see the orange flame,
00:02:32.740 --> 00:02:34.970
and then you will see the red flame.
00:02:34.970 --> 00:02:37.400
And the reason why it
might be dark right where
00:02:37.400 --> 00:02:39.180
the combustion reaction is happening
00:02:39.180 --> 00:02:43.210
is that might be very high
energy electromagnetic waves.
00:02:43.210 --> 00:02:45.880
That would be in the UV spectrum.
00:02:45.880 --> 00:02:47.930
That would be at a higher
frequency than what's visible,
00:02:47.930 --> 00:02:49.250
so to our eyes, it looks dark.
00:02:49.250 --> 00:02:52.190
And then as it cools, it goes
through the visible spectrum.
00:02:52.190 --> 00:02:54.870
And then if it cools
enough, it goes to infrared.
00:02:54.870 --> 00:02:57.060
But we human beings have
built the capability
00:02:57.060 --> 00:03:00.970
to see beyond what our
regular eyes can see.
00:03:00.970 --> 00:03:02.510
For example,
00:03:02.510 --> 00:03:05.560
these are what are often
known as thermal images,
00:03:05.560 --> 00:03:08.660
but they're really just
detecting the infrared range.
00:03:08.660 --> 00:03:10.700
So this is a picture of two dogs.
00:03:10.700 --> 00:03:12.270
It could be pitch-black outside.
00:03:12.270 --> 00:03:13.910
I mean, it could be the
middle of the night,
00:03:13.910 --> 00:03:15.760
but because they have temperature,
00:03:15.760 --> 00:03:17.980
they are releasing electromagnetic waves,
00:03:17.980 --> 00:03:18.960
which we can detect.
00:03:18.960 --> 00:03:20.440
And this over here has a scale
00:03:20.440 --> 00:03:21.850
of what the temperature must be.
00:03:21.850 --> 00:03:23.950
So you can see the eyes of the dog
00:03:23.950 --> 00:03:26.090
are the hottest part right over here.
00:03:26.090 --> 00:03:28.990
You can also see thermal
imaging of not only a hand,
00:03:28.990 --> 00:03:31.010
but after a hand has touched a wall.
00:03:31.010 --> 00:03:32.830
With our eyes, if you were to touch a wall
00:03:32.830 --> 00:03:34.250
for say 30 seconds,
00:03:34.250 --> 00:03:36.800
it doesn't look like the
wall has changed at all,
00:03:36.800 --> 00:03:38.380
but if you were to look at the infrared,
00:03:38.380 --> 00:03:40.160
you would see that you
would have heated up parts
00:03:40.160 --> 00:03:41.330
of the wall and you would be able
00:03:41.330 --> 00:03:43.350
to see the shape of the hand.
00:03:43.350 --> 00:03:45.610
And so you can imagine, we human beings,
00:03:45.610 --> 00:03:48.100
because of our ability to
detect electromagnetic waves
00:03:48.100 --> 00:03:50.250
and explore electromagnetic waves,
00:03:50.250 --> 00:03:52.360
we've been able to
leverage them more and more
00:03:52.360 --> 00:03:53.620
in our everyday lives.
00:03:53.620 --> 00:03:56.430
Thermal imaging itself
has a lot of applications.
00:03:56.430 --> 00:03:58.450
Firefighters use it to find people,
00:03:58.450 --> 00:04:01.640
or to find flames in the
middle of a lot of smoke.
00:04:01.640 --> 00:04:03.820
We have things like x-rays,
00:04:03.820 --> 00:04:05.920
which are high energy
electromagnetic waves,
00:04:05.920 --> 00:04:08.610
which we can use to see
through soft tissues.
00:04:08.610 --> 00:04:09.960
So we can see bones.
00:04:09.960 --> 00:04:11.820
This is an old image and
it looks like they're using
00:04:11.820 --> 00:04:13.580
the x-rays kind of carelessly.
00:04:13.580 --> 00:04:15.940
You don't wanna be throwing
that radiation around,
00:04:15.940 --> 00:04:16.773
but even today.
00:04:16.773 --> 00:04:18.970
I got an x-ray of my
teeth just the other day
00:04:18.970 --> 00:04:20.470
when I went to the dentist.
00:04:20.470 --> 00:04:21.960
When you talk on your cell phone,
00:04:21.960 --> 00:04:24.060
the way that your cell
phone is able to communicate
00:04:24.060 --> 00:04:26.543
is leveraging electromagnetic waves.
00:04:27.390 --> 00:04:29.180
This is another thing
that's mind blowing to me,
00:04:29.180 --> 00:04:30.750
is that my little cell phone
00:04:30.750 --> 00:04:33.020
can actually emit electromagnetic waves
00:04:33.020 --> 00:04:36.180
in the radio part of
the spectrum far enough
00:04:36.180 --> 00:04:38.080
to be received by a cell
tower that could be 10,
00:04:38.080 --> 00:04:42.750
20, and in certain cases,
30 or 40 miles away.
00:04:42.750 --> 00:04:45.990
Microwave ovens literally
released microwaves,
00:04:45.990 --> 00:04:49.240
which are absorbed by our
food, which heats up the food.
00:04:49.240 --> 00:04:51.140
And so I'll leave you there.
00:04:51.140 --> 00:04:53.400
The big picture here is
that electromagnetic waves
00:04:53.400 --> 00:04:54.730
are all around us.
00:04:54.730 --> 00:04:57.810
It's most obvious to us
in the visible spectrum,
00:04:57.810 --> 00:04:59.670
because that's what we can see.
00:04:59.670 --> 00:05:03.570
But there is a large continuum
of different frequencies
00:05:03.570 --> 00:05:05.820
that the visible is only a part of.
00:05:05.820 --> 00:05:09.620
And we human beings have
leveraged this phenomenon
00:05:09.620 --> 00:05:11.630
in all sorts of interesting ways,
00:05:11.630 --> 00:05:14.160
and I would suspect that
we're just at the beginning
00:05:14.160 --> 00:05:15.140
of this exploration.
00:05:15.140 --> 00:05:18.230
Maybe you will come up
with a new application
00:05:18.230 --> 00:05:20.163
of electromagnetic waves.
|
pH and solubility | https://www.youtube.com/watch?v=Z2bDnvDGQHQ | vtt | https://www.youtube.com/api/timedtext?v=Z2bDnvDGQHQ&ei=3FWUZcnjEoG3p-oP4qCB8Ak&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=5D194F1C634A2EFEDBA7EC13522A75304A839532.AE68E506F75106B89BCC2764E30393D25A82E1D9&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.570 --> 00:00:02.270
- [Instructor] Changing
the pH of a solution
00:00:02.270 --> 00:00:06.150
can affect the solubility
of a slightly soluble salt.
00:00:06.150 --> 00:00:09.610
For example, if we took some
solid lead two fluoride,
00:00:09.610 --> 00:00:11.120
which is a white solid,
00:00:11.120 --> 00:00:13.180
and we put it in some distilled water,
00:00:13.180 --> 00:00:15.440
the solid is going to reach an equilibrium
00:00:15.440 --> 00:00:17.700
with the ions in solution.
00:00:17.700 --> 00:00:19.970
Lead two fluoride forms lead two plus ions
00:00:19.970 --> 00:00:24.160
and fluoride anions in
a one to two mole ratio.
00:00:24.160 --> 00:00:27.230
So if we have two lead two
plus ions in this diagram,
00:00:27.230 --> 00:00:30.160
we need four fluoride anions.
00:00:30.160 --> 00:00:32.270
At equilibrium, the rate of this solution
00:00:32.270 --> 00:00:34.530
is equal to the rate of precipitation,
00:00:34.530 --> 00:00:37.000
and therefore, the amount of solid
00:00:37.000 --> 00:00:41.090
and the concentration of ions
in solution remains constant.
00:00:41.090 --> 00:00:45.700
And this forms a saturated
solution of lead two fluoride.
00:00:45.700 --> 00:00:47.580
To the system at equilibrium,
00:00:47.580 --> 00:00:49.790
we're gonna add some H plus ions.
00:00:49.790 --> 00:00:51.580
So by increasing the concentration
00:00:51.580 --> 00:00:53.580
of H plus ions in solution,
00:00:53.580 --> 00:00:57.440
we're decreasing the pH of the solution.
00:00:57.440 --> 00:00:59.930
When the H plus ions are
added to the solution,
00:00:59.930 --> 00:01:01.990
most of them react with
the fluoride anions
00:01:01.990 --> 00:01:03.120
that are present.
00:01:03.120 --> 00:01:06.680
So H plus plus F minus forms HF.
00:01:06.680 --> 00:01:09.760
Comparing the first diagram
to the second diagram,
00:01:09.760 --> 00:01:12.360
I just happened to add three H plus ions,
00:01:12.360 --> 00:01:15.130
which will react with three
of the fluoride anions
00:01:15.130 --> 00:01:18.320
that are present to produce three HF.
00:01:18.320 --> 00:01:19.950
Notice how the concentration
00:01:19.950 --> 00:01:22.240
of fluoride anions in solution
00:01:22.240 --> 00:01:25.270
has decreased from the first
diagram to the second diagram,
00:01:25.270 --> 00:01:28.750
because of the addition
of the H plus ions.
00:01:28.750 --> 00:01:30.950
So the system was at equilibrium
00:01:30.950 --> 00:01:35.100
and the concentration of
fluoride anions was decreased.
00:01:35.100 --> 00:01:37.210
According to Le Chatelier's Principle,
00:01:37.210 --> 00:01:39.490
the system will shift in the direction
00:01:39.490 --> 00:01:41.460
that decreases the stress.
00:01:41.460 --> 00:01:42.910
So if the stress is decreased
00:01:42.910 --> 00:01:44.880
concentration of fluoride anions,
00:01:44.880 --> 00:01:46.870
the system will shift to the right
00:01:46.870 --> 00:01:49.990
to make more fluoride anions.
00:01:49.990 --> 00:01:51.920
And when the system shifts to the right,
00:01:51.920 --> 00:01:54.100
more lead two fluoride dissolves
00:01:54.100 --> 00:01:56.680
to increase the
concentration of Pb two plus
00:01:56.680 --> 00:01:58.710
and fluoride anion.
00:01:58.710 --> 00:02:01.060
We can see that comparing
the second diagram
00:02:01.060 --> 00:02:03.220
to the third diagram,
00:02:03.220 --> 00:02:05.850
so the amount of solid has gotten smaller,
00:02:05.850 --> 00:02:08.390
since some of that lead
two fluoride dissolved,
00:02:08.390 --> 00:02:11.550
and we've increased the
concentration of Pb two plus
00:02:11.550 --> 00:02:14.160
and F minus in solution.
00:02:14.160 --> 00:02:15.730
The solid keeps dissolving
00:02:15.730 --> 00:02:19.520
and the concentration of ions
keeps increasing in solution
00:02:19.520 --> 00:02:23.120
until the system reaches equilibrium.
00:02:23.120 --> 00:02:24.400
So for a saturated solution
00:02:24.400 --> 00:02:26.830
of lead two fluoride at equilibrium,
00:02:26.830 --> 00:02:29.830
decreasing the pH or making
the solution more acidic
00:02:29.830 --> 00:02:32.780
by increasing the
concentration of H plus ions,
00:02:32.780 --> 00:02:36.410
increases the solubility
of lead two fluoride,
00:02:36.410 --> 00:02:39.210
which is why we saw more
of the solid dissolve
00:02:39.210 --> 00:02:41.540
when the H plus ions were added.
00:02:41.540 --> 00:02:43.280
This effect of decreasing the pH
00:02:43.280 --> 00:02:46.500
and increasing the solubility
of a slightly soluble salt
00:02:46.500 --> 00:02:49.350
happens whenever the slightly soluble salt
00:02:49.350 --> 00:02:52.260
contains a basic anion.
00:02:52.260 --> 00:02:55.610
For this example, the basic
anion is the fluoride anion,
00:02:55.610 --> 00:02:58.530
which reacts with the added H plus ions.
00:02:58.530 --> 00:03:00.850
And when the basic anion reacts,
00:03:00.850 --> 00:03:04.160
that decreases the concentration
of that basic anion,
00:03:04.160 --> 00:03:07.720
which caused the equilibrium
to shift to the right.
00:03:07.720 --> 00:03:10.460
And there are many other
examples of basic anions,
00:03:10.460 --> 00:03:12.660
two more would be the hydroxide anion
00:03:12.660 --> 00:03:14.870
and the carbonate anion.
00:03:14.870 --> 00:03:17.790
And if a compound contains a basic anion,
00:03:17.790 --> 00:03:21.840
such as the hydroxide anion,
hydroxide functions as a base
00:03:21.840 --> 00:03:25.460
and reacts with H plus ions to form H2O.
00:03:25.460 --> 00:03:27.870
So therefore, the solubility of a compound
00:03:27.870 --> 00:03:31.180
containing a hydroxide ion would increase
00:03:31.180 --> 00:03:34.820
as H plus ions are added to the solution.
00:03:34.820 --> 00:03:35.910
It's also important to note
00:03:35.910 --> 00:03:38.010
for this lead two fluoride problem,
00:03:38.010 --> 00:03:42.070
if the pH is decreased at
a constant temperature,
00:03:42.070 --> 00:03:46.930
the Ksp value for PbF
two remains constant.
00:03:46.930 --> 00:03:50.220
So the molar solubility does increase,
00:03:50.220 --> 00:03:53.530
but the Ksp value remains the same.
00:03:53.530 --> 00:03:55.450
This time, instead of lead two fluoride,
00:03:55.450 --> 00:03:57.790
let's look at lead two chloride.
00:03:57.790 --> 00:04:00.380
Lead two chloride is also a white solid.
00:04:00.380 --> 00:04:02.570
So if we dissolve some in solution,
00:04:02.570 --> 00:04:04.690
eventually, we would reach an equilibrium
00:04:04.690 --> 00:04:07.550
between the solid and
the ions in solution.
00:04:07.550 --> 00:04:10.930
So this diagram here
shows a saturated solution
00:04:10.930 --> 00:04:14.620
of lead two chloride and the
system is at equilibrium.
00:04:14.620 --> 00:04:16.290
And to the system at equilibrium,
00:04:16.290 --> 00:04:21.290
we decrease the pH by adding
H plus ions to the solution.
00:04:21.490 --> 00:04:23.570
In this case, the chloride anions
00:04:23.570 --> 00:04:26.870
aren't basic enough to
react with the H plus ions.
00:04:26.870 --> 00:04:29.310
Therefore, we do not form HCl
00:04:29.310 --> 00:04:32.440
and the concentration of chloride anions
00:04:32.440 --> 00:04:36.360
remains the same as it was
in the original diagram.
00:04:36.360 --> 00:04:39.330
So if the concentration of
chloride ions remains the same
00:04:39.330 --> 00:04:41.230
and the concentration
of lead two plus ions
00:04:41.230 --> 00:04:44.810
would remain the same, the
system is still at equilibrium
00:04:44.810 --> 00:04:47.630
and decrease in the pH had no effect
00:04:47.630 --> 00:04:50.330
on the solubility of the solids.
00:04:50.330 --> 00:04:54.010
So we have the same amount
of lead two chloride solid
00:04:54.010 --> 00:04:57.050
on the bottom of the
beaker in both diagrams.
00:04:57.050 --> 00:04:59.690
So whenever an anion has
an extremely weak base,
00:04:59.690 --> 00:05:01.440
like the chloride anion,
00:05:01.440 --> 00:05:05.530
we say that this is an
anion of negligible basicity
00:05:05.530 --> 00:05:07.230
and the solubility of salts
00:05:07.230 --> 00:05:10.010
with anions of negligible basicity
00:05:10.010 --> 00:05:13.353
is unaffected by changes in pH.
|
The common-ion effect | https://www.youtube.com/watch?v=fI3U9T7LigY | vtt | https://www.youtube.com/api/timedtext?v=fI3U9T7LigY&ei=3FWUZYnbLYq5vdIPxYm3yAI&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=931B35B438DA656512B3A7AA036C2042D04B5E46.29B1E8FAE14A372E7CCCA9D1FD3B7B516073159C&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.360 --> 00:00:02.140
- [Instructor] The
presence of a common ion
00:00:02.140 --> 00:00:05.040
can affect a solubility equilibrium.
00:00:05.040 --> 00:00:05.873
For example,
00:00:05.873 --> 00:00:09.530
let's say we have a saturated
solution of lead II chloride.
00:00:09.530 --> 00:00:11.950
Lead II chloride is a white solid,
00:00:11.950 --> 00:00:14.360
so here's the white solid
on the bottom of the beaker.
00:00:14.360 --> 00:00:18.100
And the solid's at equilibrium
with the ions in solution.
00:00:18.100 --> 00:00:22.210
So that would be Pb2+ and Cl-.
00:00:22.210 --> 00:00:26.890
Notice how the mole ratio is
one-to-two of Pb2+ to 2Cl-.
00:00:26.890 --> 00:00:30.590
So if we have two Pb2+
ions in our diagram,
00:00:30.590 --> 00:00:33.320
there should be twice
as many chloride anions.
00:00:33.320 --> 00:00:36.350
At equilibrium, the rate
of dissolution is equal to
00:00:36.350 --> 00:00:38.510
the rate of precipitation.
00:00:38.510 --> 00:00:41.250
Therefore, the concentration
of ions in solution
00:00:41.250 --> 00:00:43.180
remains constant.
00:00:43.180 --> 00:00:45.220
So our system is at equilibrium.
00:00:45.220 --> 00:00:48.570
And let's add some solid
potassium chloride.
00:00:48.570 --> 00:00:50.780
Potassium chloride is a soluble salt.
00:00:50.780 --> 00:00:55.780
So it will dissociate and turn
into K+ and Cl- in solution.
00:00:56.320 --> 00:00:58.650
Adding a source of chloride anion means
00:00:58.650 --> 00:01:01.360
the system is no longer at equilibrium.
00:01:01.360 --> 00:01:02.193
So let me write in here,
00:01:02.193 --> 00:01:05.950
not at equilibrium at that moment in time.
00:01:05.950 --> 00:01:07.730
So the system was at equilibrium
00:01:07.730 --> 00:01:10.320
and a stress was added to the system.
00:01:10.320 --> 00:01:13.500
In this case, the stress was
increased chloride anion.
00:01:13.500 --> 00:01:17.527
So there's an increase in
the concentration of Cl-.
00:01:18.471 --> 00:01:20.410
According to Le Chatelier's principle,
00:01:20.410 --> 00:01:21.980
the system will move in the direction
00:01:21.980 --> 00:01:23.980
that decreases the stress.
00:01:23.980 --> 00:01:25.060
So if the stress is
00:01:25.060 --> 00:01:27.810
increased concentration of chloride anion,
00:01:27.810 --> 00:01:29.610
the system will move to the left
00:01:29.610 --> 00:01:33.000
to get rid of some of
that extra chloride anion.
00:01:33.000 --> 00:01:34.720
When the system moves to the left,
00:01:34.720 --> 00:01:39.720
Pb2+ ions will combine with
chloride anions to form PbCl2.
00:01:39.747 --> 00:01:42.290
And we can see that down
here in the diagram.
00:01:42.290 --> 00:01:43.123
So imagine,
00:01:43.123 --> 00:01:47.480
say this Pb2+ ion combined
with these two chloride anions
00:01:47.480 --> 00:01:50.180
to form some more of the white solid.
00:01:50.180 --> 00:01:51.610
Looking at the third diagram,
00:01:51.610 --> 00:01:53.580
the amount of white solid has increased
00:01:53.580 --> 00:01:55.280
from the second diagram,
00:01:55.280 --> 00:01:59.859
and we've lost this Pb2+ ion
and these two chloride anions.
00:01:59.859 --> 00:02:02.450
And the amount of our precipitate PbCl2
00:02:02.450 --> 00:02:06.180
will keep forming until
equilibrium is reached.
00:02:06.180 --> 00:02:07.700
Let's just say this third diagram,
00:02:07.700 --> 00:02:10.470
it does represent the
system at equilibrium.
00:02:10.470 --> 00:02:13.410
So I'll write on here, at equilibrium.
00:02:13.410 --> 00:02:16.750
This is an example of
the common ion effect.
00:02:16.750 --> 00:02:20.310
For this problem, the common
ion is the chloride anion,
00:02:20.310 --> 00:02:22.640
because there were two sources of it.
00:02:22.640 --> 00:02:25.750
One was from the disillusion of PbCl2.
00:02:25.750 --> 00:02:28.720
If we had dissolved some solid
to make a saturated solution,
00:02:28.720 --> 00:02:32.340
the source of these chloride
anions would be from PbCl2.
00:02:32.340 --> 00:02:35.470
And the second source
is from the added KCl,
00:02:35.470 --> 00:02:38.490
which of course dissolved
to form chloride anion.
00:02:38.490 --> 00:02:42.090
So the chloride anion is the common ion.
00:02:42.090 --> 00:02:43.830
And we use Le Chatelier's principle
00:02:43.830 --> 00:02:46.360
to predict the system
will move to the left
00:02:46.360 --> 00:02:49.650
to get rid of the extra chloride anion.
00:02:49.650 --> 00:02:50.950
When the system moved to the left,
00:02:50.950 --> 00:02:53.550
we formed more of the solid PbCl2.
00:02:53.550 --> 00:02:55.830
And that's why this amount
got bigger over here.
00:02:55.830 --> 00:03:00.040
So if we compare the first
diagram with the third diagram,
00:03:00.040 --> 00:03:03.050
the first diagram has more of
00:03:03.050 --> 00:03:05.600
the lead II chloride in solution.
00:03:05.600 --> 00:03:07.830
And the third diagram has less of it.
00:03:07.830 --> 00:03:11.850
Therefore, the addition of the
common ion of chloride anion,
00:03:11.850 --> 00:03:16.650
that decreased the solubility
of lead II chloride.
00:03:16.650 --> 00:03:18.380
So the common ion effect says that
00:03:18.380 --> 00:03:21.130
the solubility of a slightly soluble salt,
00:03:21.130 --> 00:03:22.610
like lead II chloride,
00:03:22.610 --> 00:03:26.490
is decreased by the
presence of a common ion.
00:03:26.490 --> 00:03:28.360
Another way to think about this is using
00:03:28.360 --> 00:03:30.490
the reaction quotient, Q.
00:03:30.490 --> 00:03:34.140
For the diagram on the
left, we're at equilibrium.
00:03:34.140 --> 00:03:38.560
Therefore the reaction
quotient Qsp is equal to
00:03:38.560 --> 00:03:41.630
the Ksp value for lead II chloride,
00:03:41.630 --> 00:03:44.620
which means the system is at equilibrium.
00:03:44.620 --> 00:03:48.600
Adding chloride anion
increases the value for Qsp.
00:03:48.600 --> 00:03:51.790
So now Qsp is greater than Ksp
00:03:51.790 --> 00:03:54.340
and the system is not at equilibrium.
00:03:54.340 --> 00:03:56.700
In order to decrease the value for Q,
00:03:56.700 --> 00:03:59.290
the system needs to move to the left.
00:03:59.290 --> 00:04:01.920
And the system will
continue to move to the left
00:04:01.920 --> 00:04:05.890
until Qsp is equal to Ksp again
00:04:05.890 --> 00:04:08.550
and the system is at equilibrium.
00:04:08.550 --> 00:04:13.320
A shift to the left means an
increase in the amount of PbCl2
00:04:13.320 --> 00:04:18.030
which therefore decreases
the solubility of PbCl2.
00:04:18.030 --> 00:04:20.918
But it doesn't change the value for Ksp.
00:04:20.918 --> 00:04:25.918
Ksp for PbCl2 stays the same
at the same temperature.
00:04:26.530 --> 00:04:29.360
Next, let's see how the
presence of a common ion affects
00:04:29.360 --> 00:04:32.740
the molar solubility of lead II chloride.
00:04:32.740 --> 00:04:33.573
And to do that,
00:04:33.573 --> 00:04:36.100
let's calculate the molar
solubility of lead II chloride
00:04:36.100 --> 00:04:38.110
at 25 degrees Celsius
00:04:38.110 --> 00:04:43.010
in a solution that is 0.10
molar in potassium chloride.
00:04:43.010 --> 00:04:47.464
The Ksp value for lead II
chloride at 25 degrees Celsius is
00:04:47.464 --> 00:04:50.490
1.7 times 10 to the negative fifth.
00:04:50.490 --> 00:04:52.500
To help us calculate the molar solubility,
00:04:52.500 --> 00:04:53.920
we're going to use an ICE table,
00:04:53.920 --> 00:04:56.070
where I stands for the
initial concentration,
00:04:56.070 --> 00:04:57.880
C is the change in concentration,
00:04:57.880 --> 00:05:00.870
and E is the equilibrium concentration.
00:05:00.870 --> 00:05:01.750
First, let's say that
00:05:01.750 --> 00:05:04.420
none of the lead II
chloride has dissolved yet.
00:05:04.420 --> 00:05:05.350
And if that's true,
00:05:05.350 --> 00:05:09.200
the concentration of lead
II plus ions would be zero,
00:05:09.200 --> 00:05:11.890
and the concentration of chloride anions
00:05:11.890 --> 00:05:15.600
from the lead II chloride
would also be zero.
00:05:15.600 --> 00:05:18.200
However, there's another
source of chloride anions,
00:05:18.200 --> 00:05:22.320
and that's because our
solution is 0.10 molar in KCl.
00:05:22.320 --> 00:05:25.200
KCl is a soluble salt.
00:05:25.200 --> 00:05:30.190
So KCl associates completely
to turn to K+ and Cl-.
00:05:30.190 --> 00:05:34.570
Therefore, if the concentration
of KCl is 0.10 molar,
00:05:34.570 --> 00:05:38.830
that's also the concentration
of Cl- from the KCl.
00:05:38.830 --> 00:05:43.570
So we can add here plus 0.10 molar.
00:05:43.570 --> 00:05:47.000
And think about that
as being from our KCl.
00:05:47.000 --> 00:05:48.560
So there are two sources.
00:05:48.560 --> 00:05:51.340
There's going to be two sources
of chloride anions here.
00:05:51.340 --> 00:05:55.450
And so the Cl anion and is our common ion.
00:05:55.450 --> 00:05:58.570
The other source of
chloride anion is PbCl2
00:05:58.570 --> 00:05:59.780
when it dissolves.
00:05:59.780 --> 00:06:02.320
So some of the PbCl2 will dissolve,
00:06:02.320 --> 00:06:06.120
we don't know how much, so
I like to write -X in here.
00:06:06.120 --> 00:06:07.510
And if some of that dissolves,
00:06:07.510 --> 00:06:12.510
the mole ratio of PbCl2 to Pb2+
is a one-to-one mole ratio.
00:06:12.700 --> 00:06:17.700
So if we're losing X for PbCl2,
we're gaining X for Pb2+.
00:06:18.530 --> 00:06:20.100
And looking at our mole ratios,
00:06:20.100 --> 00:06:22.150
if we're gaining X for Pb2+
00:06:22.150 --> 00:06:24.860
and it's a one-to-two mole ratio,
00:06:24.860 --> 00:06:29.460
we would write in here +2X
for the chloride anion.
00:06:29.460 --> 00:06:33.120
So for the equilibrium
concentration of Pb2+,
00:06:33.120 --> 00:06:36.400
it would be zero plus X, or just X.
00:06:36.400 --> 00:06:39.590
And for the equilibrium
concentration of the chloride anion,
00:06:39.590 --> 00:06:42.830
it would be 0.10 plus 2X.
00:06:42.830 --> 00:06:47.830
So the 0.10 came from
the potassium chloride,
00:06:48.000 --> 00:06:52.350
and the 2X came from the
dissolution of lead II chloride.
00:06:52.350 --> 00:06:54.410
Next, we need to write a Ksp expression,
00:06:54.410 --> 00:06:57.200
which we can get from
the disillusion equation.
00:06:57.200 --> 00:07:02.200
So, Ksp is equal to the
concentration of lead II plus ions
00:07:02.850 --> 00:07:05.280
raised to the first power
00:07:05.280 --> 00:07:07.440
times the concentration
of chloride anions.
00:07:07.440 --> 00:07:09.550
And since there's a two as a coefficient
00:07:09.550 --> 00:07:10.690
in the balanced equation,
00:07:10.690 --> 00:07:14.020
we need to raise that
concentration to the second power.
00:07:14.020 --> 00:07:15.330
Pure solids are left out of
00:07:15.330 --> 00:07:17.080
equilibrium constant expressions.
00:07:17.080 --> 00:07:20.150
So we don't write anything for PbCl2.
00:07:20.150 --> 00:07:22.950
Next, we plug in our
equilibrium concentrations.
00:07:22.950 --> 00:07:27.100
So for lead II plus, the
equilibrium concentration is X.
00:07:27.100 --> 00:07:29.010
And for the chloride anion,
00:07:29.010 --> 00:07:32.933
the equilibrium concentration
is 0.10 plus 2X.
00:07:34.270 --> 00:07:38.860
We also need to plug in the
Ksp value for lead II chloride.
00:07:38.860 --> 00:07:41.270
Here we have the Ksp value plugged in.
00:07:41.270 --> 00:07:44.490
X and 0.10 plus 2X.
00:07:44.490 --> 00:07:49.000
And let's think about 0.10
plus 2X for a second here.
00:07:49.000 --> 00:07:50.961
With a very low value for Ksp,
00:07:50.961 --> 00:07:53.440
1.7 times 10 to the negative fifth,
00:07:53.440 --> 00:07:57.450
that means that not very much
of the PbCl2 will dissolve.
00:07:57.450 --> 00:08:00.380
And if that's true, X is
a pretty small number.
00:08:00.380 --> 00:08:04.090
And if X is a small number,
2X is also pretty small.
00:08:04.090 --> 00:08:05.960
So we're going to make an approximation
00:08:05.960 --> 00:08:09.140
and say that 0.10 plus
a pretty small number
00:08:09.140 --> 00:08:12.550
is approximately equal to just 0.10.
00:08:12.550 --> 00:08:15.130
And that's going to make
the math easier on us.
00:08:15.130 --> 00:08:18.320
So instead of writing
0.10 plus 2X squared,
00:08:18.320 --> 00:08:20.643
we just have 0.10 squared.
00:08:21.880 --> 00:08:26.450
Solving for X, we find
that X is equal to 0.0017,
00:08:27.580 --> 00:08:28.623
which we could just write as
00:08:28.623 --> 00:08:33.623
1.7 times 10 to the negative third molar.
00:08:34.240 --> 00:08:35.530
It's okay to write molar here
00:08:35.530 --> 00:08:38.010
because this X value represents
00:08:38.010 --> 00:08:42.120
the equilibrium concentration of Pb2+.
00:08:42.120 --> 00:08:45.670
And if that's the equilibrium
concentration of Pb2+,
00:08:45.670 --> 00:08:48.030
that's also the concentration
of lead to chloride
00:08:48.030 --> 00:08:48.920
that dissolved.
00:08:48.920 --> 00:08:51.290
So this number, this concentration,
00:08:51.290 --> 00:08:55.320
is the molar solubility
of lead II chloride
00:08:55.320 --> 00:08:57.160
in a solution at 25 degrees
00:08:57.160 --> 00:09:00.810
where the solution is 0.10 molar in KCl.
00:09:00.810 --> 00:09:04.040
Most textbooks leave this
-X out of their ICE tables
00:09:04.040 --> 00:09:06.810
because the concentration
of a solid doesn't change.
00:09:06.810 --> 00:09:08.250
I like to just leave it in here though
00:09:08.250 --> 00:09:10.550
to remind me that X represents
00:09:10.550 --> 00:09:14.840
the molar solubility of
the slightly soluble salt.
00:09:14.840 --> 00:09:16.010
Finally, if we'd calculate
00:09:16.010 --> 00:09:17.990
the molar solubility of lead II chloride
00:09:17.990 --> 00:09:20.620
without the presence of a common ion,
00:09:20.620 --> 00:09:23.310
this 0.10 would have been
gone from everything.
00:09:23.310 --> 00:09:25.720
And doing the math that way,
we would have found that
00:09:25.720 --> 00:09:29.150
the molar solubility at 25 degrees Celsius
00:09:29.150 --> 00:09:31.820
and using this value for the Ksp,
00:09:31.820 --> 00:09:36.820
the molar solubility
comes out to 0.016 molar.
00:09:37.720 --> 00:09:40.300
So comparing these two
smaller solubilities,
00:09:40.300 --> 00:09:43.210
0.016 molar versus 0.0017,
00:09:45.150 --> 00:09:48.120
that's approximately a factor of 10.
00:09:48.120 --> 00:09:50.980
Therefore the addition of a common ion
00:09:50.980 --> 00:09:55.980
decreased the solubility by
approximately a factor of 10.
00:09:56.980 --> 00:09:59.970
So doing the common ion
effect in a quantitative way
00:09:59.970 --> 00:10:01.750
also shows a decrease in
00:10:01.750 --> 00:10:04.280
the solubility of a slightly soluble salt
00:10:05.412 --> 00:10:07.553
because of the presence of a common ion.
|
Worked example: Predicting whether a precipitate forms by comparing Q and Kₛₚ | https://www.youtube.com/watch?v=vyENVkttVtw | vtt | https://www.youtube.com/api/timedtext?v=vyENVkttVtw&ei=3FWUZcusLK39mLAP25eRiAM&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=B11E3A2E7158ED8FCD2FF9BCCF3F3DB4BF9BAF40.53023259B4220ED7135130989861F1B1177B34C1&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.330 --> 00:00:02.020
- [Instructor] For this problem,
our goal is to figure out
00:00:02.020 --> 00:00:04.160
whether or not a precipitate will form
00:00:04.160 --> 00:00:08.810
if we mix 0.20 liters over
4.0 times 10 to the negative
00:00:08.810 --> 00:00:12.140
third Molar solution of lead two nitrate,
00:00:12.140 --> 00:00:16.410
with 0.80 liters of an 8.0
times 10 to the negative third
00:00:16.410 --> 00:00:19.530
Molar solution of sodium sulfate.
00:00:19.530 --> 00:00:21.690
The first step is to
figure out the identity
00:00:21.690 --> 00:00:23.840
of the precipitate that might form.
00:00:23.840 --> 00:00:26.630
So we're mixing an aqueous
solution of lead two nitrate
00:00:26.630 --> 00:00:30.360
with an aqueous solution
of sodium sulfate.
00:00:30.360 --> 00:00:33.228
In the lead two nitrate
solution they're lead two plus
00:00:33.228 --> 00:00:37.046
cations and nitrate anions.
00:00:37.046 --> 00:00:39.330
In the sodium sulfate aqueous solution,
00:00:39.330 --> 00:00:43.643
there are sodium cations
and sulfate anions.
00:00:44.540 --> 00:00:48.210
So we take the cation from one
and the anion from the other.
00:00:48.210 --> 00:00:51.350
So one possible product
would be lead sulfate.
00:00:51.350 --> 00:00:55.450
So let's write on here,
PbSO4, after we cross over
00:00:55.450 --> 00:01:00.450
our charges and we take the
other cation and the other anion
00:01:01.070 --> 00:01:05.080
and so the other product
would be sodium nitrate.
00:01:05.080 --> 00:01:07.033
So we write it in here and a NaNO3.
00:01:08.170 --> 00:01:12.930
To balance the equation, we
need a two in front of NANO3.
00:01:12.930 --> 00:01:16.962
Since nitrates are soluble,
sodium nitrate is an aqueous
00:01:16.962 --> 00:01:21.962
solution and lead sulfate would
be our possible precipitate.
00:01:22.120 --> 00:01:24.130
Now that we know are possible precipitate,
00:01:24.130 --> 00:01:26.360
let's go ahead and write
a net ionic equation
00:01:26.360 --> 00:01:29.920
showing the formation of that precipitate.
00:01:29.920 --> 00:01:34.040
So lead two plus ions, would
come together with sulfate
00:01:34.040 --> 00:01:39.040
anions to form PBSO4.
00:01:39.090 --> 00:01:43.870
So PBSO4 is the possible precipitate.
00:01:43.870 --> 00:01:46.260
Since lead sulfate is
our possible precipitate,
00:01:46.260 --> 00:01:50.070
we really only care about the
concentration of lead two plus
00:01:50.070 --> 00:01:52.810
ions and sulfate anions in solution.
00:01:52.810 --> 00:01:56.610
We don't need to worry about
sodium cations or nitrate
00:01:56.610 --> 00:02:00.180
anions because those
are the spectator ions
00:02:00.180 --> 00:02:02.760
in our overall reaction.
00:02:02.760 --> 00:02:05.880
Running the overall equation,
and the net ionic equation
00:02:05.880 --> 00:02:08.470
are really optional for
a problem like this.
00:02:08.470 --> 00:02:11.350
But we really need to do
is identify the precipitate
00:02:11.350 --> 00:02:14.230
and then write out the
disillusion equation.
00:02:14.230 --> 00:02:19.230
So PBSO4 would be our
possible precipitate.
00:02:19.430 --> 00:02:24.360
And if it dissolves in water,
we would form lead two plus
00:02:24.360 --> 00:02:29.360
cations in aqueous solution,
and sulfates anions
00:02:29.530 --> 00:02:31.257
in aqueous solutions, right?
00:02:31.257 --> 00:02:33.470
aq over here.
00:02:33.470 --> 00:02:36.180
The reason why it's important
to write out the dissolution
00:02:36.180 --> 00:02:40.030
equation is because we
can write a KSP expression
00:02:40.030 --> 00:02:40.940
from it.
00:02:40.940 --> 00:02:44.250
So KSP is equal to, it
would be the concentration
00:02:44.250 --> 00:02:46.600
of lead two plus raised to the first power
00:02:46.600 --> 00:02:48.100
because we have a coefficient of one
00:02:48.100 --> 00:02:49.710
in the balanced equation,
00:02:49.710 --> 00:02:52.990
times the concentration
of sulfate also raised
00:02:52.990 --> 00:02:56.680
to the first power and
pure solids are left out
00:02:56.680 --> 00:02:58.680
of equilibrium, constant expressions.
00:02:58.680 --> 00:03:02.830
Therefore we're not going
to include lead sulfate.
00:03:02.830 --> 00:03:07.830
For lead two sulfate KSP
is equal to 6.3 times 10
00:03:09.380 --> 00:03:14.380
to the negative seven
at 25 degrees Celsius.
00:03:15.420 --> 00:03:19.310
The concentrations of lead two
plus and sulfate in the KSP
00:03:19.310 --> 00:03:23.060
expression, are
equilibrium concentrations.
00:03:23.060 --> 00:03:25.840
For our problem, we're
gonna calculate QSP,
00:03:25.840 --> 00:03:27.980
which has the same form as KSP,
00:03:27.980 --> 00:03:29.930
the differences the concentrations can be
00:03:29.930 --> 00:03:31.980
at any moment in time.
00:03:31.980 --> 00:03:34.080
And we're gonna calculate
QSP at the moment,
00:03:34.080 --> 00:03:35.960
our two solutions are mixed,
00:03:35.960 --> 00:03:40.200
and then we're going
to compare QSP to KSP.
00:03:40.200 --> 00:03:42.640
I've drawn out some diagrams
to help us understand
00:03:42.640 --> 00:03:45.720
how QSP compares to
KSP and what that means
00:03:45.720 --> 00:03:46.890
for the solution.
00:03:46.890 --> 00:03:49.020
However, these aren't perfect diagrams
00:03:49.020 --> 00:03:51.330
they're just to help get the point across.
00:03:51.330 --> 00:03:55.470
If QSP is less than KSP,
the solution is unsaturated,
00:03:55.470 --> 00:03:58.400
which means no precipitate would form.
00:03:58.400 --> 00:03:59.880
For an unsaturated solution,
00:03:59.880 --> 00:04:02.300
you can dissolve more
led two sulfate in it.
00:04:02.300 --> 00:04:05.000
So lead two sulfate as a white solid,
00:04:05.000 --> 00:04:08.130
so if we were to put a small
amount of lead two sulfate
00:04:08.130 --> 00:04:10.980
in our unsaturated
solution, it would dissolve,
00:04:10.980 --> 00:04:15.980
and it would continue to dissolve
until QSP is equal to KSP.
00:04:16.450 --> 00:04:19.760
And the system is at equilibrium.
00:04:19.760 --> 00:04:22.760
At equilibrium, the solid
is turning into the ions
00:04:22.760 --> 00:04:26.760
at the same rate, the ions are
turning back into the solid.
00:04:26.760 --> 00:04:29.780
Since the rate of dissolution
is equal to the rate
00:04:29.780 --> 00:04:32.880
of precipitation when the
system is at equilibrium,
00:04:32.880 --> 00:04:34.990
the concentrations of lead two plus ions
00:04:34.990 --> 00:04:37.070
and sulfate ions are constant,
00:04:37.070 --> 00:04:40.740
and this represents a saturated solution.
00:04:40.740 --> 00:04:43.300
And since the solution is
saturated at equilibrium,
00:04:43.300 --> 00:04:46.060
if we tried to add some
more lead two sulfate
00:04:46.060 --> 00:04:47.730
at the same temperature,
00:04:47.730 --> 00:04:49.850
we wouldn't be able to dissolve any more,
00:04:49.850 --> 00:04:52.220
we would just increase the
pile of lead two sulfate
00:04:52.220 --> 00:04:54.310
on the bottom of the beaker.
00:04:54.310 --> 00:04:58.180
That concept helps us
understand what happens when QSP
00:04:58.180 --> 00:05:00.320
is greater than KSP.
00:05:00.320 --> 00:05:04.730
When QSP is greater than KSP,
the solution is oversaturated.
00:05:04.730 --> 00:05:07.490
So it's exceeded the limit
of what can dissolve,
00:05:07.490 --> 00:05:10.640
and therefore you can imagine
some lead two plus ions
00:05:10.640 --> 00:05:15.290
combining with some sulfate
ions to form a precipitate.
00:05:15.290 --> 00:05:18.470
Therefore, when QSP is greater than KSP,
00:05:18.470 --> 00:05:20.600
a precipitate will form.
00:05:20.600 --> 00:05:23.100
The precipitate will continue to form,
00:05:23.100 --> 00:05:25.940
until QSP is equal to KSP,
00:05:25.940 --> 00:05:28.620
and the system reaches equilibrium.
00:05:28.620 --> 00:05:30.840
Next, we need to go back
to what we were given
00:05:30.840 --> 00:05:32.240
in our initial problem,
00:05:32.240 --> 00:05:34.750
when we mixed our two solutions together.
00:05:34.750 --> 00:05:37.090
Remember we only cared about
the concentration of lead
00:05:37.090 --> 00:05:39.510
two plus ions and sulfate ions.
00:05:39.510 --> 00:05:42.330
So we're gonna calculate the
concentration of those two ions
00:05:42.330 --> 00:05:45.950
at the moment in time, when
the two solutions are mixed.
00:05:45.950 --> 00:05:48.450
First let's calculate the
concentration of lead two
00:05:48.450 --> 00:05:49.790
plus ions.
00:05:49.790 --> 00:05:53.110
The original solution of lead two nitrate
00:05:53.110 --> 00:05:56.280
had a concentration of 4.0
times 10 to the negative
00:05:56.280 --> 00:05:57.610
third Molar.
00:05:57.610 --> 00:06:00.200
So molarity is equal to moles over liters.
00:06:00.200 --> 00:06:02.190
So we can plug in the concentration,
00:06:02.190 --> 00:06:04.550
and we can also plug in the
volume of that solution,
00:06:04.550 --> 00:06:08.580
which was 0.20 liters, and solve for X,
00:06:08.580 --> 00:06:13.130
X equal to 8.0 times 10 to
the negative fourth moles.
00:06:13.130 --> 00:06:14.930
That's how many moles of lead two nitrate
00:06:14.930 --> 00:06:17.870
there are and that's also
how many moles of lead two
00:06:17.870 --> 00:06:19.760
plus ions there are.
00:06:19.760 --> 00:06:22.440
Therefore to find the
concentration of lead two plus ions
00:06:22.440 --> 00:06:23.760
after the solutions are mixed,
00:06:23.760 --> 00:06:27.060
we plug in 8.0 times 10 to
the negative fourth moles,
00:06:27.060 --> 00:06:30.010
and for the volume we're
adding these two solutions
00:06:30.010 --> 00:06:32.430
together, so the total
volume of the solution
00:06:32.430 --> 00:06:34.573
is 0.20 plus 0.80.
00:06:35.534 --> 00:06:37.870
So the concentration of lead two plus ions
00:06:37.870 --> 00:06:42.400
will be equal to 8.0 times 10
to the negative fourth Molar.
00:06:42.400 --> 00:06:44.100
We can do the same type of calculation
00:06:44.100 --> 00:06:46.400
to find the concentration of sulfate ions
00:06:46.400 --> 00:06:49.140
after the two solutions have been mixed.
00:06:49.140 --> 00:06:51.560
So we take the concentration
of the original solution
00:06:51.560 --> 00:06:54.970
of sodium sulfate and plug that
into the molarity equation,
00:06:54.970 --> 00:06:59.110
plug in the volume solve for
X and 6.4 times 10 to negative
00:06:59.110 --> 00:07:02.770
third moles is how many moles
of sodium sulfate there are.
00:07:02.770 --> 00:07:05.510
That's also how many moles
of sulfate ions there are,
00:07:05.510 --> 00:07:08.930
so we plug in that number
into the concentration
00:07:08.930 --> 00:07:11.220
for sulfate, and once
again, since we're adding
00:07:11.220 --> 00:07:13.470
the two solutions together,
we divide that by the total
00:07:13.470 --> 00:07:16.430
volume to get a
concentration of sulfate ions
00:07:16.430 --> 00:07:20.220
of 6.4 times 10 to the
negative third Molar.
00:07:20.220 --> 00:07:22.850
Now that we know the concentrations
of lead two plus ions
00:07:22.850 --> 00:07:26.080
and sulfate ions, after the
two solutions have been mixed,
00:07:26.080 --> 00:07:29.930
we can plug those concentrations
into our QSP expression
00:07:29.930 --> 00:07:31.990
and solve for QSP.
00:07:31.990 --> 00:07:36.050
So at this moment in time,
QSP is equal to 5.1 times 10
00:07:36.050 --> 00:07:37.760
to the negative six.
00:07:37.760 --> 00:07:41.560
At 25 degrees Celsius, the
KSP value for lead two sulfate
00:07:41.560 --> 00:07:45.120
is equal to 6.3 times 10
to the negative seventh.
00:07:45.120 --> 00:07:48.160
QSP at this moment in time is 5.1 times 10
00:07:48.160 --> 00:07:49.690
to the negative six.
00:07:49.690 --> 00:07:54.357
Therefore QSP is greater than KSP.
00:07:55.980 --> 00:08:00.210
Since QSP is greater than
KSP, we've exceeded the limit
00:08:00.210 --> 00:08:02.930
of what can dissolve and
therefore the solution
00:08:02.930 --> 00:08:05.220
is oversaturated.
00:08:05.220 --> 00:08:09.550
So yes, a precipitate will
form and the precipitate
00:08:09.550 --> 00:08:12.190
of lead two sulfate will continue to form
00:08:12.190 --> 00:08:15.493
until QSP is equal to KSP.
|
Worked example: Calculating solubility from Kₛₚ | https://www.youtube.com/watch?v=Ywvw32DaxUk | vtt | https://www.youtube.com/api/timedtext?v=Ywvw32DaxUk&ei=3FWUZffxLKfxvdIP1cyokAo&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=A54865589E4C3C877EECFEBE4CB272C32F4BBB21.D7CC41F3D442C56FEB7314D8BB40B3FE01478C84&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.170 --> 00:00:01.003
- [Instructor] Let's calculate
00:00:01.003 --> 00:00:03.270
the molar solubility of calcium fluoride
00:00:03.270 --> 00:00:05.620
if the Ksp value for calcium fluoride is
00:00:05.620 --> 00:00:10.540
3.9 times 10 to the negative
11th at 25 degrees Celsius.
00:00:10.540 --> 00:00:11.400
The first step is
00:00:11.400 --> 00:00:15.710
to write the dissolution
equation for calcium fluoride.
00:00:15.710 --> 00:00:20.170
So, solid calcium fluoride
will dissolve in solution
00:00:20.170 --> 00:00:25.170
to form aqueous calcium two
plus ions and fluoride anions.
00:00:26.100 --> 00:00:28.960
And to balance that out,
we need to make sure
00:00:28.960 --> 00:00:32.840
and include a two in front
of the fluoride anions.
00:00:32.840 --> 00:00:34.900
The next step is to set up an ICE table,
00:00:34.900 --> 00:00:38.260
where I stands for initial concentration,
00:00:38.260 --> 00:00:40.930
C stands for the change in concentration,
00:00:40.930 --> 00:00:44.910
and E stands for
equilibrium concentration.
00:00:44.910 --> 00:00:47.420
Before any of the solid
calcium fluoride dissolves,
00:00:47.420 --> 00:00:50.190
the initial concentrations
of calcium two plus ions
00:00:50.190 --> 00:00:52.970
and fluoride anions in solution is zero.
00:00:52.970 --> 00:00:54.830
So we can go ahead and put a zero in here
00:00:54.830 --> 00:00:58.740
for the initial concentration
of the ions in solution.
00:00:58.740 --> 00:01:00.680
Some of the calcium
fluoride will dissolve,
00:01:00.680 --> 00:01:02.070
and we don't know how much.
00:01:02.070 --> 00:01:06.500
So I like to represent that by
writing -X on the ICE table,
00:01:06.500 --> 00:01:09.090
where X is the concentration
of calcium fluoride
00:01:09.090 --> 00:01:10.400
that dissolves.
00:01:10.400 --> 00:01:13.350
Looking at the mole ratios,
it's a one-to-one mole ratio
00:01:13.350 --> 00:01:16.720
between calcium fluoride
and calcium two plus ions.
00:01:16.720 --> 00:01:17.990
So if we're losing X
00:01:17.990 --> 00:01:20.100
for the concentration of calcium fluoride,
00:01:20.100 --> 00:01:21.570
we must be gaining X
00:01:21.570 --> 00:01:24.650
for the concentration of
calcium two plus ions.
00:01:24.650 --> 00:01:27.180
And since it's a one-to-two mole ratio
00:01:27.180 --> 00:01:30.300
for calcium two plus
ions to fluoride anions,
00:01:30.300 --> 00:01:33.250
if we're gaining +X for calcium two plus,
00:01:33.250 --> 00:01:35.350
we must gain plus +2X for fluoride anions.
00:01:36.890 --> 00:01:40.790
So the equilibrium concentration
of calcium two plus ions is
00:01:40.790 --> 00:01:42.930
zero plus X, or just X,
00:01:42.930 --> 00:01:45.870
and the equilibrium concentration
of fluoride anions will be
00:01:45.870 --> 00:01:49.070
zero plus 2X, or just 2X.
00:01:49.070 --> 00:01:51.730
The next step is to
write the Ksp expression
00:01:51.730 --> 00:01:53.460
from the balanced equation.
00:01:53.460 --> 00:01:55.360
So Ksp is equal to
00:01:55.360 --> 00:01:58.910
the concentration of
calcium two plus ions,
00:01:58.910 --> 00:02:00.800
and since there's a coefficient of one
00:02:00.800 --> 00:02:01.883
in the balanced equation,
00:02:01.883 --> 00:02:04.015
that's the concentration
of calcium two plus ions
00:02:04.015 --> 00:02:05.865
raised to the first power,
00:02:05.865 --> 00:02:08.906
times the concentration
of fluoride anions,
00:02:08.906 --> 00:02:10.615
and since there is a coefficient of two
00:02:10.615 --> 00:02:12.136
in the balanced equation,
00:02:12.136 --> 00:02:14.610
it's the concentration of
fluoride anions raised to
00:02:14.610 --> 00:02:16.040
the second power.
00:02:16.040 --> 00:02:17.790
Pure solids are not included
00:02:17.790 --> 00:02:19.760
in equilibrium constant expression.
00:02:19.760 --> 00:02:21.830
So we're going to leave calcium fluoride
00:02:21.830 --> 00:02:24.540
out of the Ksp expression.
00:02:24.540 --> 00:02:27.150
The concentration of ions
in our Ksp expression
00:02:27.150 --> 00:02:29.740
are equilibrium concentrations.
00:02:29.740 --> 00:02:31.220
Therefore we can plug in X
00:02:31.220 --> 00:02:34.360
for the equilibrium
concentration of calcium two plus
00:02:34.360 --> 00:02:39.000
and 2X for the equilibrium
concentration of fluoride anions.
00:02:39.000 --> 00:02:44.000
We can also plug in the Ksp
value for calcium fluoride.
00:02:44.490 --> 00:02:45.390
So that would give us
00:02:45.390 --> 00:02:50.390
3.9 times 10 to the
negative 11th is equal to
00:02:50.740 --> 00:02:55.330
X times 2X squared.
00:02:55.330 --> 00:02:57.190
Next we need to solve for X.
00:02:57.190 --> 00:03:01.410
So, 3.9 times 10 to the
negative 11th is equal to
00:03:01.410 --> 00:03:03.130
X times 2X squared.
00:03:03.130 --> 00:03:04.570
Well, 2X squared is equal to
00:03:04.570 --> 00:03:08.910
4X squared times X is equal to 4X cubed.
00:03:08.910 --> 00:03:13.410
So to solve for X, we need
to divide both sides by four
00:03:13.410 --> 00:03:17.980
and then take the cube root of both sides.
00:03:17.980 --> 00:03:21.100
So we'd take the cube
root of the left side
00:03:21.100 --> 00:03:25.683
and the cube root of X cubed.
00:03:26.620 --> 00:03:28.562
That gives us X is equal to
00:03:28.562 --> 00:03:33.562
2.1 times 10 to the negative fourth.
00:03:33.980 --> 00:03:36.100
And looking at our ICE table, X represents
00:03:36.100 --> 00:03:39.740
the equilibrium concentration
of calcium two plus ions.
00:03:39.740 --> 00:03:43.010
So 2.1 times 10 to the
negative fourth molar is
00:03:43.010 --> 00:03:46.700
the equilibrium concentration
of calcium two plus ions.
00:03:46.700 --> 00:03:48.110
For the fluoride anions,
00:03:48.110 --> 00:03:50.620
the equilibrium concentration is 2X.
00:03:50.620 --> 00:03:55.620
So two times 2.1 times 10 to
the negative fourth is 4.2,
00:03:55.690 --> 00:03:56.832
let me go ahead and write that down here,
00:03:56.832 --> 00:04:00.210
4.2 times 10 to the negative fourth molar
00:04:00.210 --> 00:04:03.860
for the equilibrium
concentration of fluoride anions.
00:04:03.860 --> 00:04:04.900
Our goal was to calculate
00:04:04.900 --> 00:04:07.410
the molar solubility of calcium fluoride.
00:04:07.410 --> 00:04:09.300
And molar solubility refers to
00:04:09.300 --> 00:04:12.470
the concentration of
our salt that dissolved
00:04:12.470 --> 00:04:16.030
to form a saturated
solution at equilibrium.
00:04:16.030 --> 00:04:17.460
So if X refers to
00:04:17.460 --> 00:04:21.430
the concentration of calcium
two plus ions at equilibrium,
00:04:21.430 --> 00:04:23.620
looking at our mole ratios, that's also
00:04:23.620 --> 00:04:26.790
the concentration of calcium
fluoride that dissolved.
00:04:26.790 --> 00:04:30.020
Therefore, 2.1 times 10 to
the negative fourth molar
00:04:30.020 --> 00:04:34.640
is also the molar solubility
of calcium fluoride.
00:04:34.640 --> 00:04:37.770
Technically at a constant
temperature of 25 degrees,
00:04:37.770 --> 00:04:40.690
the concentration of a
solid doesn't change.
00:04:40.690 --> 00:04:44.170
And so you'll see most
textbooks not to put in -X
00:04:44.170 --> 00:04:46.580
on the ICE table. I like
to just put it in though
00:04:46.580 --> 00:04:49.630
to remind me that X in
this case does refer to
00:04:49.630 --> 00:04:51.263
the molar solubility.
|
Introduction to solubility equilibria | https://www.youtube.com/watch?v=N9a2r01ToZk | vtt | https://www.youtube.com/api/timedtext?v=N9a2r01ToZk&ei=3FWUZeb8GNH2mLAPm6ij6A4&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=2456109890004492CA9A294C4877CE22068ECF97.1C4DE7A8987CF3CDF2D1BB7AD36F521CDCE2C971&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.610 --> 00:00:01.870
- [Instructor] Let's say we have a beaker
00:00:01.870 --> 00:00:04.700
of distilled water at 25 degrees Celsius.
00:00:04.700 --> 00:00:07.750
And to the beaker, we
add some barium sulfate.
00:00:07.750 --> 00:00:10.810
Barium sulfate is a white solid.
00:00:10.810 --> 00:00:12.420
A small amount of the barium sulfate
00:00:12.420 --> 00:00:15.870
dissolves in the water and
forms Ba2+ ions in solution
00:00:15.870 --> 00:00:17.980
and sulfate ions in solution.
00:00:17.980 --> 00:00:20.350
So let me draw those in on our diagrams.
00:00:20.350 --> 00:00:22.520
So we're gonna form some Ba2+ ions
00:00:22.520 --> 00:00:25.530
and some sulfate anions.
00:00:25.530 --> 00:00:28.620
But most of the barium
sulfate remains undissolved
00:00:28.620 --> 00:00:31.180
and so we'll draw that
here sitting on the bottom
00:00:31.180 --> 00:00:33.040
of the beaker.
00:00:33.040 --> 00:00:36.650
So barium sulfate can
dissolve to form Ba2+ ions
00:00:36.650 --> 00:00:38.820
and sulfate anions in solution.
00:00:38.820 --> 00:00:41.440
And it's possible for the Ba2+ ion
00:00:41.440 --> 00:00:44.850
to combine with the sulfate
anion to form a precipitate,
00:00:44.850 --> 00:00:46.460
of barium sulfate.
00:00:46.460 --> 00:00:49.470
When the rate of dissolution
is equal to the rate of
00:00:49.470 --> 00:00:53.690
precipitation, the
system is at equilibrium.
00:00:53.690 --> 00:00:55.740
These types of equilibria are referred
00:00:55.740 --> 00:00:58.880
to as solubility equilibria.
00:00:58.880 --> 00:01:00.950
And when the system is at equilibrium,
00:01:00.950 --> 00:01:04.060
the concentrations of Ba2+
ions and sulfate anions
00:01:04.060 --> 00:01:05.630
solution are constant.
00:01:05.630 --> 00:01:08.780
And the amount of solid is constant too.
00:01:08.780 --> 00:01:11.170
And this forms a saturated solution.
00:01:11.170 --> 00:01:13.370
The balanced equation
shows the dissolution
00:01:13.370 --> 00:01:15.730
of a salt barium sulfate.
00:01:15.730 --> 00:01:17.070
And from the balanced equation,
00:01:17.070 --> 00:01:20.170
we can write an equilibrium
constant expression.
00:01:20.170 --> 00:01:23.015
So we would write the
equilibrium constant K
00:01:23.015 --> 00:01:27.410
is equal to the concentration of Ba2+
00:01:27.410 --> 00:01:29.470
and since there's a coefficient of one
00:01:29.470 --> 00:01:30.620
in the balanced equation,
00:01:30.620 --> 00:01:33.200
it'd be the concentration
raised to the first power
00:01:33.200 --> 00:01:35.640
times the concentration of sulfate
00:01:35.640 --> 00:01:39.000
also raised to the first power.
00:01:39.000 --> 00:01:42.110
And since pure solids are left
out of equilibrium constant
00:01:42.110 --> 00:01:46.510
expressions, we would not
include the solid barium sulfate.
00:01:46.510 --> 00:01:48.510
For solubility equilibria,
00:01:48.510 --> 00:01:53.510
we would write Ksp where sp
stands for solubility product.
00:01:53.630 --> 00:01:58.372
The solubility product constant
Ksp has only one value for a
00:01:58.372 --> 00:02:01.180
given salt at a specific temperature.
00:02:01.180 --> 00:02:04.340
That temperature is
usually 25 degrees Celsius.
00:02:04.340 --> 00:02:08.940
And Ksp indicates how much
of that salt will dissolve.
00:02:08.940 --> 00:02:11.430
For example, at 25 degrees Celsius,
00:02:11.430 --> 00:02:13.960
the Ksp value for barium sulfate
00:02:13.960 --> 00:02:16.930
is 1.1 times 10 to the negative 10th.
00:02:16.930 --> 00:02:19.670
When the Ksp value is much less than one,
00:02:19.670 --> 00:02:22.120
that indicates the salt
is not very soluble.
00:02:22.120 --> 00:02:25.440
So barium sulfate is not a soluble salt.
00:02:25.440 --> 00:02:28.610
If the Ksp value is greater than one,
00:02:28.610 --> 00:02:31.640
like it is for something
like sodium chloride,
00:02:31.640 --> 00:02:33.610
that indicates a soluble salt
00:02:33.610 --> 00:02:36.070
that dissolves easily in water.
00:02:36.070 --> 00:02:39.880
The solubility of a substance
refers to the amount of solid
00:02:39.880 --> 00:02:42.930
that dissolves to form
a saturated solution.
00:02:42.930 --> 00:02:47.930
Usually the units for solubility
are in grams per liter.
00:02:48.440 --> 00:02:52.140
Molar solubility refers to the
number of moles of the solid
00:02:52.140 --> 00:02:55.460
that dissolve to form one litter
of the saturated solution.
00:02:55.460 --> 00:02:59.550
And therefore the units
would be moles per one liter
00:02:59.550 --> 00:03:01.133
or you could just write M.
00:03:03.680 --> 00:03:07.030
Ksp values can be used to
predict the relative solubilities
00:03:07.030 --> 00:03:11.030
of salts that produce the same
number of ions in solution.
00:03:11.030 --> 00:03:13.560
For example, silver
chloride, silver bromide,
00:03:13.560 --> 00:03:17.750
and silver iodide all
produce two ions in solution.
00:03:17.750 --> 00:03:20.880
Let's look at the dissolution
equation for silver chloride
00:03:20.880 --> 00:03:22.470
to see why this is true.
00:03:22.470 --> 00:03:24.720
Solid silver chloride
turns into Ag+ and Cl-.
00:03:26.500 --> 00:03:30.370
So that's one Ag+ ion and
one Cl- ion for a total
00:03:30.370 --> 00:03:32.590
of two ions in solution.
00:03:32.590 --> 00:03:35.140
And we could write out similar
equations for silver bromide
00:03:35.140 --> 00:03:38.920
and silver iodide, so they all
produce two ions in solution.
00:03:38.920 --> 00:03:41.500
However, a salt like Lead(II)chloride
00:03:41.500 --> 00:03:43.940
produces three ions in solution.
00:03:43.940 --> 00:03:47.210
So Lead(II)chloride
would give one Pb2+ ion
00:03:47.210 --> 00:03:49.680
and two chloride anions in solution.
00:03:49.680 --> 00:03:51.900
One plus two is three ions.
00:03:51.900 --> 00:03:55.890
Since Lead(II)chloride produces
three ions in solution,
00:03:55.890 --> 00:03:59.360
we can determine its solubility
relative to the other
00:03:59.360 --> 00:04:02.040
three by comparing Ksp values.
00:04:02.040 --> 00:04:04.390
Here are the Ksp values
for the three salts
00:04:04.390 --> 00:04:06.250
at 25 degrees Celsius.
00:04:06.250 --> 00:04:09.530
For silver chloride, it's 1.8
times 10 to the negative 10th,
00:04:09.530 --> 00:04:12.950
for silver bromide, it's 5.0
times 10 to the negative 13th.
00:04:12.950 --> 00:04:15.246
And for silver iodide, it's 8.3 times 10
00:04:15.246 --> 00:04:17.270
to the negative 17th.
00:04:17.270 --> 00:04:20.130
When comparing salts that
produce the same number of ions,
00:04:20.130 --> 00:04:22.030
the higher the value of Ksp,
00:04:22.030 --> 00:04:25.020
the higher the solubility of the salt.
00:04:25.020 --> 00:04:29.190
And since silver chloride has
the highest Ksp value of these
00:04:29.190 --> 00:04:33.520
three, silver chloride is
the most soluble salts.
00:04:33.520 --> 00:04:35.340
For some insight into why this is true,
00:04:35.340 --> 00:04:38.200
let's look at the Ksp
expression for silver chloride,
00:04:38.200 --> 00:04:40.990
which we can get from
the balanced equation.
00:04:40.990 --> 00:04:43.010
The higher the value for Ksp,
00:04:43.010 --> 00:04:46.290
the higher the concentration
of these ions at equilibrium,
00:04:46.290 --> 00:04:49.490
which means that more of the
solid must have dissolved.
00:04:49.490 --> 00:04:52.540
Therefore, silver chloride
has the highest solubility
00:04:52.540 --> 00:04:54.680
out of these three salts.
00:04:54.680 --> 00:04:58.030
Let's say we have some solid
calcium fluoride that we add to
00:04:58.030 --> 00:05:01.300
pure water at 25 degrees Celsius.
00:05:01.300 --> 00:05:04.830
Eventually equilibrium is
reached and the equilibrium
00:05:04.830 --> 00:05:07.523
concentration of Ca2+ ions is measured
00:05:07.523 --> 00:05:11.290
to be 2.1 times 10 to the negative 4th M.
00:05:11.290 --> 00:05:15.040
Our goal is to calculate
the Ksp for calcium fluoride
00:05:15.040 --> 00:05:17.490
at 25 degrees Celsius.
00:05:17.490 --> 00:05:19.240
The first step is to write out the
00:05:19.240 --> 00:05:22.730
dissolution equation for calcium fluoride.
00:05:22.730 --> 00:05:27.180
So we would write CaF2 solid,
and we know that calcium forms
00:05:27.180 --> 00:05:32.180
a 2+ cation, so we would
write Ca2+ in aqueous solution
00:05:34.040 --> 00:05:37.210
and to balance everything
we'd need two fluoride anions.
00:05:37.210 --> 00:05:41.770
So 2F- also in aqueous solution.
00:05:41.770 --> 00:05:43.790
The next step is to use
the balanced equation
00:05:43.790 --> 00:05:45.950
to write the Ksp expression.
00:05:45.950 --> 00:05:50.180
So Ksp is equal to, there's
a one as a coefficient
00:05:50.180 --> 00:05:53.000
in front of Ca2+ so it'd
be the concentration
00:05:53.000 --> 00:05:56.360
of Ca2+ raise to the first power,
00:05:56.360 --> 00:05:59.220
times the concentration of fluoride anion
00:05:59.220 --> 00:06:01.160
and since there's a two as a coefficient,
00:06:01.160 --> 00:06:04.490
this is the concentration
of fluoride anion squared.
00:06:04.490 --> 00:06:08.800
For a Ksp expression, these
are equilibrium concentrations,
00:06:08.800 --> 00:06:12.260
and we already know the
concentration of Ca2+
00:06:12.260 --> 00:06:16.260
at equilibrium is 2.1 times
10 to the negative 4th.
00:06:16.260 --> 00:06:17.750
So that can be plugged in for the
00:06:17.750 --> 00:06:21.160
equilibrium concentration of Ca2+.
00:06:21.160 --> 00:06:23.760
So here's our expression with 2.1 times 10
00:06:23.760 --> 00:06:25.450
to the negative 4th plugged in,
00:06:25.450 --> 00:06:27.540
and next we need to
plug in the equilibrium
00:06:27.540 --> 00:06:30.090
concentration of fluoride anion.
00:06:30.090 --> 00:06:32.370
We're looking at the disillusion equation,
00:06:32.370 --> 00:06:37.370
the mole ratio of Ca2+
to fluoride anion is 1:2.
00:06:37.650 --> 00:06:40.300
Therefore, at equilibrium,
there's twice as many
00:06:40.300 --> 00:06:44.440
fluoride ions in solution
as there are Ca2+ ions.
00:06:44.440 --> 00:06:47.190
Therefore the equilibrium
concentration of the fluoride
00:06:47.190 --> 00:06:51.960
anion would just be twice
this concentration for Ca2+.
00:06:51.960 --> 00:06:55.490
So the equilibrium
concentration of fluoride anion
00:06:55.490 --> 00:06:59.533
must be 4.2 times 10
to the negative 4th M.
00:07:00.986 --> 00:07:03.360
And when you do the math, you get that Ksp
00:07:03.360 --> 00:07:06.750
for calcium fluoride is
equal to 3.7 times 10
00:07:06.750 --> 00:07:10.690
to the negative 11th
at 25 degrees Celsius.
00:07:10.690 --> 00:07:13.320
Ksp values can be difficult to measure
00:07:13.320 --> 00:07:16.060
and therefore different sources
often give different values
00:07:16.060 --> 00:07:18.990
for Ksp at the same temperature.
00:07:18.990 --> 00:07:22.690
For example, for calcium
fluoride at 25 degrees Celsius,
00:07:22.690 --> 00:07:26.110
one source had Ksp equal to 3.5 times 10
00:07:26.110 --> 00:07:27.520
to the negative 11th.
00:07:27.520 --> 00:07:32.090
Another one had 3.9 times
10 to the negative 11th.
00:07:32.090 --> 00:07:35.332
Since we got 3.7 times
10 to the negative 11th,
00:07:35.332 --> 00:07:38.140
this sounds like a pretty good
calculation for the numbers
00:07:38.140 --> 00:07:40.390
that we used for our problem.
00:07:40.390 --> 00:07:42.950
Finally, let's think
about the molar solubility
00:07:42.950 --> 00:07:44.260
of calcium fluoride.
00:07:44.260 --> 00:07:47.480
So how many moles of our
salt dissolve to form
00:07:47.480 --> 00:07:50.460
one litter of our saturated solution?
00:07:50.460 --> 00:07:53.267
Well, the mole ratio of Ca2+ ions
00:07:53.267 --> 00:07:56.349
to calcium fluoride is 1:1.
00:07:56.349 --> 00:08:01.349
Therefore, the concentration
of Ca2+ ions in solution 2.1
00:08:01.420 --> 00:08:03.770
times 10 to the negative 4th M,
00:08:03.770 --> 00:08:06.278
that number must also
be the molar solubility
00:08:06.278 --> 00:08:08.340
of calcium fluoride.
00:08:08.340 --> 00:08:10.420
Therefore, for this problem,
we could say that we use the
00:08:10.420 --> 00:08:13.100
molar solubility of calcium
fluoride to calculate
00:08:13.100 --> 00:08:15.673
the Ksp value for calcium fluoride.
|
Worked example: Using Le Chȃtelier’s principle to predict shifts in equilibrium | https://www.youtube.com/watch?v=YBEoLzMWCdM | vtt | https://www.youtube.com/api/timedtext?v=YBEoLzMWCdM&ei=3FWUZfK9LKehp-oPzdGm0Ag&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245324&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=BC11856950A2E50058EF02B5305D83130BF26C1E.3741E16A631516276DCD8BB05D36A1D84344DFE4&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.490 --> 00:00:03.210
- [Instructor] Carbon monoxide
will react with hydrogen gas
00:00:03.210 --> 00:00:05.650
to produce methanol.
00:00:05.650 --> 00:00:07.770
Let's say that the
reaction is at equilibrium
00:00:07.770 --> 00:00:09.310
and our job is to figure out
00:00:09.310 --> 00:00:11.100
which direction the
equilibrium will shift,
00:00:11.100 --> 00:00:13.620
to the left, to the right, or not at all,
00:00:13.620 --> 00:00:17.390
as we try to make changes to
the reaction at equilibrium.
00:00:17.390 --> 00:00:19.640
For example, if we add some hydrogen gas
00:00:19.640 --> 00:00:21.650
to our reaction at equilibrium,
00:00:21.650 --> 00:00:25.690
we're increasing the concentration
of one of our reactants.
00:00:25.690 --> 00:00:27.360
According to the Le Chatelier's principle,
00:00:27.360 --> 00:00:29.130
the net reaction will
move in the direction
00:00:29.130 --> 00:00:32.420
that decreases the stress
placed on the system.
00:00:32.420 --> 00:00:34.170
So if the stress is increased amount
00:00:34.170 --> 00:00:35.860
of one of the reactants,
00:00:35.860 --> 00:00:37.900
the equilibrium will shift to the right
00:00:37.900 --> 00:00:40.610
to get rid of some of that reactant.
00:00:40.610 --> 00:00:43.370
In part B, some methanol is removed.
00:00:43.370 --> 00:00:47.790
So if we're decreasing the
concentration of our product,
00:00:47.790 --> 00:00:51.150
the equilibrium's gonna shift
to make more of our product,
00:00:51.150 --> 00:00:54.840
therefore, the equilibrium
will shift to the right.
00:00:54.840 --> 00:00:56.620
Next, the volume is increased
00:00:56.620 --> 00:00:58.780
on the reaction at equilibrium.
00:00:58.780 --> 00:01:03.660
And if we increase the volume,
we decrease the pressure,
00:01:03.660 --> 00:01:05.440
therefore, we could consider the stress
00:01:05.440 --> 00:01:07.280
to be decreased pressure.
00:01:07.280 --> 00:01:09.850
Le Chatelier's principle says
the net reaction is gonna go
00:01:09.850 --> 00:01:11.640
in the direction that relieves the stress.
00:01:11.640 --> 00:01:13.890
So if the stress is decreased pressure,
00:01:13.890 --> 00:01:18.140
the net reaction is going to
shift to increase the pressure.
00:01:18.140 --> 00:01:19.790
And we can figure out
which direction that is
00:01:19.790 --> 00:01:21.760
by looking at the balanced equation.
00:01:21.760 --> 00:01:23.000
On the reactant side,
00:01:23.000 --> 00:01:25.340
there's one mole of gas
and two moles of gas
00:01:25.340 --> 00:01:27.310
for a total of three moles of gas.
00:01:27.310 --> 00:01:30.040
On the product side, there's
only one mole of gas.
00:01:30.040 --> 00:01:32.280
So there's three moles of gas on the left
00:01:32.280 --> 00:01:34.760
and only one mole of gas on the right.
00:01:34.760 --> 00:01:36.940
Since the net reaction is going to try
00:01:36.940 --> 00:01:38.740
to increase the pressure,
00:01:38.740 --> 00:01:41.420
the equilibrium shifts to the left,
00:01:41.420 --> 00:01:44.520
toward the side that's gonna
form more moles of gas,
00:01:44.520 --> 00:01:47.300
therefore increasing the pressure.
00:01:47.300 --> 00:01:49.070
Next, we try adding some neon gas
00:01:49.070 --> 00:01:52.020
to our reaction mixture at equilibrium.
00:01:52.020 --> 00:01:53.850
Well, neon gas is an inert gas,
00:01:53.850 --> 00:01:55.010
which means it doesn't react
00:01:55.010 --> 00:01:57.200
with any of our reactants or products.
00:01:57.200 --> 00:01:59.010
And if we look at the expression
00:01:59.010 --> 00:02:01.160
for the reaction quotient Qp,
00:02:01.160 --> 00:02:03.160
neon gas is not included.
00:02:03.160 --> 00:02:05.300
Therefore, adding neon gas is not going
00:02:05.300 --> 00:02:07.590
to change the value for Qp,
00:02:07.590 --> 00:02:10.500
so the reaction remains at equilibrium.
00:02:10.500 --> 00:02:12.470
So the answer is there's no shift
00:02:12.470 --> 00:02:15.280
when an inert gas is added.
00:02:15.280 --> 00:02:17.190
And that might sound a
little strange at first
00:02:17.190 --> 00:02:18.980
because adding neon gas means
00:02:18.980 --> 00:02:21.540
that the total pressure would increase,
00:02:21.540 --> 00:02:24.080
the total pressure since
we're adding a gas.
00:02:24.080 --> 00:02:26.700
However, the partial
pressures stay the same.
00:02:26.700 --> 00:02:29.320
So the partial pressures for methanol
00:02:29.320 --> 00:02:32.290
and carbon monoxide and hydrogen
gas actually stay the same
00:02:32.290 --> 00:02:34.760
and therefore Q doesn't change.
00:02:34.760 --> 00:02:38.000
Next, we add a catalyst to
our reaction at equilibrium.
00:02:38.000 --> 00:02:39.300
Catalysts speed up reactions
00:02:39.300 --> 00:02:41.420
by lowering deactivation energy.
00:02:41.420 --> 00:02:43.970
However, the catalyst is gonna
speed up that the forward
00:02:43.970 --> 00:02:46.310
and the reverse reactions
by the same amount
00:02:46.310 --> 00:02:49.720
and therefore the reaction
remains at equilibrium.
00:02:49.720 --> 00:02:52.190
So there's no shift
when a catalyst is added
00:02:52.190 --> 00:02:54.700
to a reaction at equilibrium.
00:02:54.700 --> 00:02:55.690
And then in part F,
00:02:55.690 --> 00:02:57.580
let's try decreasing the temperature
00:02:57.580 --> 00:02:59.930
on the reaction at equilibrium.
00:02:59.930 --> 00:03:01.740
Well, this reaction is exothermic
00:03:01.740 --> 00:03:03.920
because Delta H is less than 0,
00:03:03.920 --> 00:03:06.680
so we can treat heat as a product.
00:03:06.680 --> 00:03:09.900
So we go ahead and write
heat on the product side.
00:03:09.900 --> 00:03:11.880
If we treat heat like a product,
00:03:11.880 --> 00:03:15.210
decreasing the temperature
is like decreasing the amount
00:03:15.210 --> 00:03:16.850
of our product, therefore,
00:03:16.850 --> 00:03:19.230
the net reaction will move to the right
00:03:19.230 --> 00:03:21.410
to make more of the product.
00:03:21.410 --> 00:03:23.110
Whether that reaction moves to the right,
00:03:23.110 --> 00:03:25.080
you can think about that being an increase
00:03:25.080 --> 00:03:26.550
in the amount of products
00:03:26.550 --> 00:03:29.740
and therefore a decrease
in the amount of reactants.
00:03:29.740 --> 00:03:31.200
And when you increase the products
00:03:31.200 --> 00:03:32.750
and decrease the reactants,
00:03:32.750 --> 00:03:36.130
you increase the value for
the equilibrium constant.
00:03:36.130 --> 00:03:40.020
Therefore, lowering the
temperature causes an increase
00:03:40.020 --> 00:03:44.390
in the equilibrium constant
for an exothermic reaction.
00:03:44.390 --> 00:03:45.740
Note that changing the temperature
00:03:45.740 --> 00:03:48.180
in part F is the only change
00:03:48.180 --> 00:03:50.710
that actually changed
the equilibrium constant.
00:03:50.710 --> 00:03:53.250
So in all the other ones, in A through E,
00:03:53.250 --> 00:03:57.233
the equilibrium constant
stayed the same value.
|
Worked example: Calculating the equilibrium total pressure after a change in volume | https://www.youtube.com/watch?v=2q5UPN4tF20 | vtt | https://www.youtube.com/api/timedtext?v=2q5UPN4tF20&ei=3VWUZcWoK7S1vdIPoLuoUA&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245325&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=240899D2F9B3EDB3257E8FA27053432487AE6637.EE5F946941335656CAAC6FAE8A79AF29F73B448C&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.220 --> 00:00:02.610
- [Instructor] Phosphorus
pentachloride will decompose
00:00:02.610 --> 00:00:06.220
into phosphorus trichloride
and chlorine gas.
00:00:06.220 --> 00:00:10.930
Kp for this reaction is
equal to .500 at 500 Kelvin.
00:00:10.930 --> 00:00:13.090
Let's say that this
reaction is at equilibrium
00:00:13.090 --> 00:00:16.370
and a reaction vessel that
has a volume of 2.0 liters
00:00:16.370 --> 00:00:18.450
and the equilibrium partial pressure,
00:00:18.450 --> 00:00:22.100
of PCl5 is equal to .980 atmospheres.
00:00:22.100 --> 00:00:24.670
The equilibrium partial pressure of PCl3
00:00:24.670 --> 00:00:27.310
is equal to .700 atmospheres.
00:00:27.310 --> 00:00:29.840
And the equilibrium partial
pressure of chlorine gas
00:00:29.840 --> 00:00:32.930
is equal to .700 atmospheres.
00:00:32.930 --> 00:00:35.090
If we add up those
three partial pressures,
00:00:35.090 --> 00:00:38.800
we get the total pressure of
the gas mixture at equilibrium,
00:00:38.800 --> 00:00:41.860
which is equal to 2.38 atmospheres.
00:00:41.860 --> 00:00:45.150
And we're gonna call
this total pressure, P1.
00:00:45.150 --> 00:00:47.730
If we decrease the volume from two liters
00:00:47.730 --> 00:00:48.950
down to one liter,
00:00:48.950 --> 00:00:52.840
and we keep the temperature
constant at 500 Kelvin,
00:00:52.840 --> 00:00:55.360
we decrease the volume by a factor of two,
00:00:55.360 --> 00:00:59.290
which means we increase the
pressure by a factor of two.
00:00:59.290 --> 00:01:02.930
So, all of the partial
pressures of our gases double,
00:01:02.930 --> 00:01:05.130
and there's a new total pressure,
00:01:05.130 --> 00:01:07.420
which is twice the
original total pressure.
00:01:07.420 --> 00:01:11.160
And this new total pressure
is equal to 4.76 atmospheres.
00:01:11.160 --> 00:01:14.580
And from now on, we'll call
this total pressure, P2.
00:01:14.580 --> 00:01:16.320
So, when the volume was two liters,
00:01:16.320 --> 00:01:18.780
the reaction started out at equilibrium
00:01:18.780 --> 00:01:21.430
and by decreasing the volume to one liter,
00:01:21.430 --> 00:01:22.850
and by doubling the pressure,
00:01:22.850 --> 00:01:25.870
we've introduced a stress to the system.
00:01:25.870 --> 00:01:27.300
And so, at this moment in time,
00:01:27.300 --> 00:01:28.910
when these are the partial pressures,
00:01:28.910 --> 00:01:32.173
the reaction is not at equilibrium.
00:01:33.210 --> 00:01:35.380
Le Chatelier's principle
says the net reaction
00:01:35.380 --> 00:01:38.290
will move in the direction
that decreases the stress.
00:01:38.290 --> 00:01:41.150
So, if the stress is an
increase in the pressure,
00:01:41.150 --> 00:01:43.210
the net reaction will
move in the direction
00:01:43.210 --> 00:01:45.500
that decreases the pressure.
00:01:45.500 --> 00:01:46.910
Looking at the balanced equation,
00:01:46.910 --> 00:01:49.320
there's one mole of gas
on the reactant side,
00:01:49.320 --> 00:01:52.960
and there are two moles of
gas on the product side.
00:01:52.960 --> 00:01:54.154
So, if the net reaction goes
00:01:54.154 --> 00:01:56.560
from the products to the reactants,
00:01:56.560 --> 00:01:58.581
if the net reaction goes to the left,
00:01:58.581 --> 00:02:00.960
the net reaction is going to the side
00:02:00.960 --> 00:02:03.890
with the smaller number of moles of gas,
00:02:03.890 --> 00:02:07.540
which would decrease the
pressure and relieve the stress.
00:02:07.540 --> 00:02:09.493
The net reaction keeps moving to the left
00:02:09.493 --> 00:02:13.110
until equilibrium is reestablished.
00:02:13.110 --> 00:02:15.160
And when equilibrium is reestablished,
00:02:15.160 --> 00:02:18.860
there'll be a new total
pressure, which we'll call P3.
00:02:18.860 --> 00:02:22.890
So, our goal is to calculate P3,
00:02:22.890 --> 00:02:26.670
so we can compare it to P1 and P2.
00:02:26.670 --> 00:02:29.210
And we're gonna do this
in a quantitative way
00:02:29.210 --> 00:02:31.730
and in a more qualitative way.
00:02:31.730 --> 00:02:32.920
Let's use an ICE table
00:02:32.920 --> 00:02:36.590
to help us figure out the
final total pressure, P3.
00:02:36.590 --> 00:02:37.423
In an ICE table,
00:02:37.423 --> 00:02:40.210
I stands for the initial
partial pressure in this case,
00:02:40.210 --> 00:02:43.700
C is the change and E is the
equilibrium partial pressure.
00:02:43.700 --> 00:02:46.360
The initial partial pressure of PCl5,
00:02:46.360 --> 00:02:48.667
after the volume was reduced to one liter,
00:02:48.667 --> 00:02:51.280
was 1.96 atmospheres.
00:02:51.280 --> 00:02:53.890
And the partial pressures of PCl3 and Cl2
00:02:53.890 --> 00:02:57.090
were both 1.40 atmospheres.
00:02:57.090 --> 00:02:58.938
We already used Le Chatelier's principle
00:02:58.938 --> 00:03:03.000
to realize the net reaction's
going to go to the left,
00:03:03.000 --> 00:03:04.880
which means we're going to decrease
00:03:04.880 --> 00:03:06.150
in the amount of our products,
00:03:06.150 --> 00:03:09.061
and we're going to increase
the amount of the reactants.
00:03:09.061 --> 00:03:12.310
So, if we're gonna increase
the amount of PCl5,
00:03:12.310 --> 00:03:13.880
we don't know how much
we're gonna increase,
00:03:13.880 --> 00:03:15.080
we're gonna call that x.
00:03:15.080 --> 00:03:16.570
But we know it's going to increase,
00:03:16.570 --> 00:03:20.110
so we write plus x under the
change part on the ICE table.
00:03:20.110 --> 00:03:24.450
And since our mole ratio of
PCl5 to PCl3 is one to one,
00:03:24.450 --> 00:03:26.930
if we're gaining x for PCl5,
00:03:26.930 --> 00:03:29.860
we must be losing x for PCl3.
00:03:29.860 --> 00:03:31.570
And the same goes for Cl2,
00:03:31.570 --> 00:03:33.170
since there's a coefficient of one.
00:03:33.170 --> 00:03:36.370
So, we write minus x in our ICE table.
00:03:36.370 --> 00:03:39.340
Therefore, the equilibrium
partial pressure of PCl5
00:03:39.340 --> 00:03:43.986
would be 1.96 plus x.
00:03:43.986 --> 00:03:46.820
The equilibrium partial pressure of PCl3
00:03:46.820 --> 00:03:50.140
would be 1.40 minus x.
00:03:50.140 --> 00:03:52.500
And the equilibrium
partial pressure of Cl2
00:03:52.500 --> 00:03:56.120
would also be 1.40 minus x.
00:03:56.120 --> 00:03:58.381
Next, we can plug in the
equilibrium partial pressures
00:03:58.381 --> 00:04:00.869
into our Kp expression.
00:04:00.869 --> 00:04:03.970
So, we can plug in 1.40 minus x
00:04:03.970 --> 00:04:06.793
for the equilibrium
partial pressure of PCl3,
00:04:06.793 --> 00:04:11.460
1.40 minus x for the equilibrium
partial pressure of Cl2,
00:04:11.460 --> 00:04:14.010
and 1.96 plus x
00:04:14.010 --> 00:04:17.514
for the equilibrium
partial pressure of PCl5.
00:04:17.514 --> 00:04:19.930
And we can also plug in the value
00:04:19.930 --> 00:04:22.630
for the equilibrium constant, Kp.
00:04:22.630 --> 00:04:25.360
Here's what our equilibrium
constant expression looks like
00:04:25.360 --> 00:04:27.130
with everything plugged in.
00:04:27.130 --> 00:04:29.780
And next, we would need to solve for x,
00:04:29.780 --> 00:04:32.610
which would involve the use
of a quadratic equation.
00:04:32.610 --> 00:04:34.100
And when you do all that math,
00:04:34.100 --> 00:04:36.890
you find that x is equal to .330.
00:04:40.140 --> 00:04:42.810
Now that we know x is equal to .33,
00:04:42.810 --> 00:04:45.440
we can solve for the
equilibrium partial pressures.
00:04:45.440 --> 00:04:49.760
1.96 plus .33 is equal to 2.29.
00:04:49.760 --> 00:04:52.660
Therefore, the equilibrium
partial pressure of PCl5
00:04:52.660 --> 00:04:54.970
is 2.29 atmospheres,
00:04:54.970 --> 00:04:58.003
for PCl3, it's 1.40 minus x,
00:04:58.003 --> 00:05:02.510
1.40 minus 0.33 is equal to 1.07.
00:05:02.510 --> 00:05:05.150
Therefore, the equilibrium
partial pressure of PCl3
00:05:05.150 --> 00:05:07.520
is equal to 1.07 atmospheres.
00:05:07.520 --> 00:05:09.990
And it's the same math for Cl2.
00:05:09.990 --> 00:05:13.000
So, the equilibrium
partial pressure of Cl2
00:05:13.000 --> 00:05:16.640
is also 1.07 atmospheres.
00:05:16.640 --> 00:05:18.840
So, to find the total pressure, P3,
00:05:18.840 --> 00:05:22.680
we simply need to add up the
individual partial pressures.
00:05:22.680 --> 00:05:27.680
So, 2.29 plus 1.07 plus 1.07
is equal to 4.43 atmospheres.
00:05:30.295 --> 00:05:33.878
Therefore, P3 is equal
to 4.43 atmospheres.
00:05:38.940 --> 00:05:40.830
Doing the math helps us realize that x
00:05:40.830 --> 00:05:42.295
is not a very large number.
00:05:42.295 --> 00:05:44.730
And the reason why x is
not a very large number
00:05:44.730 --> 00:05:49.210
is because the Kp value is
equal to .500 for this reaction.
00:05:49.210 --> 00:05:51.270
And when K is close to one,
00:05:51.270 --> 00:05:52.670
there's an appreciable amount
00:05:52.670 --> 00:05:55.410
of both reactants and
products at equilibrium.
00:05:55.410 --> 00:05:58.630
And we can see that with our
equilibrium partial pressures.
00:05:58.630 --> 00:06:01.200
There's an appreciable
amount of both of them.
00:06:01.200 --> 00:06:02.860
And since there has to be a decent amount
00:06:02.860 --> 00:06:05.133
of both reactants and
products at equilibrium,
00:06:05.133 --> 00:06:06.900
we're not gonna see huge change
00:06:06.900 --> 00:06:09.580
from these initial partial pressures.
00:06:09.580 --> 00:06:12.860
So, there will definitely
be a shift to the left
00:06:12.860 --> 00:06:14.950
to decrease the pressure.
00:06:14.950 --> 00:06:17.236
And when these were the partial pressures,
00:06:17.236 --> 00:06:21.150
if you remember P2 was equal to 4.76,
00:06:21.150 --> 00:06:23.260
so there's gonna be a
decrease of pressure.
00:06:23.260 --> 00:06:24.440
So, there's gonna be a decrease,
00:06:24.440 --> 00:06:27.550
so the pressure is going
to go down from 4.76,
00:06:27.550 --> 00:06:29.480
but since there's not a large change,
00:06:29.480 --> 00:06:31.660
it's not gonna be a huge change.
00:06:31.660 --> 00:06:36.480
And that's why we saw P3 only
dropped to 4.43 atmospheres.
00:06:36.480 --> 00:06:38.240
So, if you go back to
the original problem,
00:06:38.240 --> 00:06:40.800
and our goal is to figure out P3
00:06:40.800 --> 00:06:43.320
in relation to P1 and to P2,
00:06:43.320 --> 00:06:45.400
without doing all of that math,
00:06:45.400 --> 00:06:46.560
we could think to ourselves,
00:06:46.560 --> 00:06:49.120
okay, so, we decrease the
volume by a factor of two,
00:06:49.120 --> 00:06:51.470
which doubled the total pressure.
00:06:51.470 --> 00:06:53.340
But then, the net
reaction moves to the left
00:06:53.340 --> 00:06:54.873
to decrease the pressure.
00:06:54.873 --> 00:06:57.682
Since it's not gonna
move much to the left,
00:06:57.682 --> 00:07:00.270
it's not gonna decrease
the pressure by a lot.
00:07:00.270 --> 00:07:03.190
Therefore, the final pressure P3
00:07:03.190 --> 00:07:06.095
is going to be a little less than 4.76,
00:07:06.095 --> 00:07:09.953
but greater than 2.38 atmospheres.
|
Le Chȃtelier’s principle: Changing temperature | https://www.youtube.com/watch?v=j7FOzKIDrg8 | vtt | https://www.youtube.com/api/timedtext?v=j7FOzKIDrg8&ei=3VWUZdSiKdDGp-oP56wx&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245325&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=CB70553246BBC57D0B519928726AA93763637E79.DA84EC5E1F0CA66ADE2425BCC12F008539016060&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.260 --> 00:00:02.720
- [Instructor] Le Chateliers's
Principle says if a stress
00:00:02.720 --> 00:00:05.260
is applied to a reaction at equilibrium,
00:00:05.260 --> 00:00:07.710
the net reaction goes in
the direction that relieves
00:00:07.710 --> 00:00:09.060
the stress.
00:00:09.060 --> 00:00:11.580
One possible stress is
to change the temperature
00:00:11.580 --> 00:00:13.840
of the reaction at equilibrium.
00:00:13.840 --> 00:00:16.560
As an example, let's look
at the hypothetical reaction
00:00:16.560 --> 00:00:20.070
where gas A turns into gas B.
00:00:20.070 --> 00:00:22.980
Delta H for this reaction
is less than zero,
00:00:22.980 --> 00:00:27.170
which tells us this is
an exothermic reaction.
00:00:27.170 --> 00:00:30.070
And for an exothermic
reaction, heat is given off,
00:00:30.070 --> 00:00:31.110
heat is released.
00:00:31.110 --> 00:00:33.520
Therefore we can go
ahead and write plus heat
00:00:33.520 --> 00:00:35.620
on the product side.
00:00:35.620 --> 00:00:38.820
Let's say that our hypothetical
reaction is at equilibrium,
00:00:38.820 --> 00:00:40.560
and then we change the temperature,
00:00:40.560 --> 00:00:44.350
so we're going to
increase the temperature.
00:00:44.350 --> 00:00:45.980
According to Le Chatelier's Principal,
00:00:45.980 --> 00:00:47.750
the net reaction is
gonna go in the direction
00:00:47.750 --> 00:00:49.350
that decreases the stress.
00:00:49.350 --> 00:00:52.940
And if we treat heat if
we treat like a product
00:00:52.940 --> 00:00:55.140
and we've increased the temperature,
00:00:55.140 --> 00:00:58.260
it says if we've increased the
amount of one of our products
00:00:58.260 --> 00:01:01.100
and therefore the net reaction
is going to shift to the left
00:01:01.100 --> 00:01:03.670
to decrease a product.
00:01:03.670 --> 00:01:06.720
Let's use particulate diagrams
and the reaction quotient Q
00:01:06.720 --> 00:01:09.660
to explain what's going on when
we increase the temperature
00:01:09.660 --> 00:01:12.060
on our reaction at equilibrium.
00:01:12.060 --> 00:01:14.360
The first particular
diagram shows the reaction
00:01:14.360 --> 00:01:17.680
at equilibrium, and let's
prove that by calculating QC
00:01:17.680 --> 00:01:19.360
at this moment in time.
00:01:19.360 --> 00:01:21.820
We can get the expression
for the reaction quotient,
00:01:21.820 --> 00:01:24.680
QC by looking at the balanced equation.
00:01:24.680 --> 00:01:26.770
So we have coefficients
of one in front of A
00:01:26.770 --> 00:01:29.400
and in front of B, therefore QC is equal
00:01:29.400 --> 00:01:31.440
to the concentration
of B to the first power
00:01:31.440 --> 00:01:33.350
divided by the concentration of A,
00:01:33.350 --> 00:01:35.070
also to the first power.
00:01:35.070 --> 00:01:37.400
To find the concentration
of B, we know that B
00:01:37.400 --> 00:01:39.230
is represented by blue spheres,
00:01:39.230 --> 00:01:42.150
so there are 1, 2, 3 blue spheres,
00:01:42.150 --> 00:01:45.390
And if each sphere represents
0.1 moles of a substance
00:01:45.390 --> 00:01:49.430
three times 0.1 is equal to 0.3 moles of B
00:01:49.430 --> 00:01:52.644
and at the volumes equal to 1.0 liter,
00:01:52.644 --> 00:01:56.770
0.3 divided by 1.0 liter is 0.3 Molar.
00:01:56.770 --> 00:02:01.770
So the concentration of
B is equal to 0.3 Molar.
00:02:02.390 --> 00:02:05.210
There are also three particles of A
00:02:05.210 --> 00:02:07.030
therefore the concentration of A
00:02:07.030 --> 00:02:11.270
is also equal to 0.3 Molar.
00:02:11.270 --> 00:02:13.410
0.3 divided by 0.3 is equal to one.
00:02:13.410 --> 00:02:16.670
So QC at this moment of
time is equal to one.
00:02:16.670 --> 00:02:21.100
KC for this reaction is equal
to one at 25 degrees Celsius.
00:02:21.100 --> 00:02:24.070
So QC is equal to KC.
00:02:24.070 --> 00:02:28.970
And when QC is equal to KC,
the reaction is at equilibrium.
00:02:28.970 --> 00:02:31.570
So for this first particular diagram,
00:02:31.570 --> 00:02:33.353
the reaction's at equilibrium.
00:02:34.200 --> 00:02:36.300
Next, we introduced the
stress to the reaction
00:02:36.300 --> 00:02:39.700
at equilibrium and the
stress is an increase
00:02:39.700 --> 00:02:41.330
in the temperature.
00:02:41.330 --> 00:02:44.430
In general, for an exothermic reaction,
00:02:44.430 --> 00:02:46.840
increasing the temperature
lowers the value
00:02:46.840 --> 00:02:48.930
for the equilibrium constant.
00:02:48.930 --> 00:02:52.440
So for this hypothetical
reaction at 25 degrees Celsius,
00:02:52.440 --> 00:02:55.500
KC is equal to one, but
since we've increased
00:02:55.500 --> 00:02:59.120
the temperature, the value
for the equilibrium constant
00:02:59.120 --> 00:03:00.370
is going to decrease.
00:03:00.370 --> 00:03:04.990
So let's say it goes 2.5, if
we increase the temperature
00:03:04.990 --> 00:03:07.863
to 30 degrees Celsius.
00:03:08.770 --> 00:03:13.520
So if we calculate QC for our
second particular diagram,
00:03:13.520 --> 00:03:16.270
we still have three blues and three reds,
00:03:16.270 --> 00:03:17.730
and the volume is still the same,
00:03:17.730 --> 00:03:21.740
therefore QC is still equal to one,
00:03:21.740 --> 00:03:24.280
but the difference is KC has now changed,
00:03:24.280 --> 00:03:27.020
so QC is not equal to KC,
00:03:27.020 --> 00:03:30.170
so we are not at equilibrium.
00:03:30.170 --> 00:03:33.830
And in this case, QC is greater than KC
00:03:33.830 --> 00:03:36.583
'cause QC is equal to one
and KC is equal to 0.5.
00:03:37.660 --> 00:03:42.660
And when QC is greater than
KC, there are too many products
00:03:42.960 --> 00:03:44.890
and not enough reactants.
00:03:44.890 --> 00:03:49.890
And therefore the net
reaction goes to the left.
00:03:49.890 --> 00:03:52.030
When the net reaction goes to the left,
00:03:52.030 --> 00:03:55.430
we're going to have be turned into A.
00:03:55.430 --> 00:04:00.120
So we should see one blue
sphere turn into one red sphere.
00:04:00.120 --> 00:04:03.190
So if we have three blues and three reds,
00:04:03.190 --> 00:04:08.010
and one blue turns into a red,
that gives us only two blues
00:04:08.010 --> 00:04:10.550
and four reds now.
00:04:10.550 --> 00:04:13.810
So when we calculate QC for
our third particular diagram,
00:04:13.810 --> 00:04:17.440
the concentration of B would be 0.2 Molar,
00:04:17.440 --> 00:04:21.650
and the concentration
of A would be 0.4 Molar.
00:04:21.650 --> 00:04:26.650
So 0.2 divided by 0.4 is equal to 0.5.
00:04:27.010 --> 00:04:30.890
Well, KC is also equal to 0.5.
00:04:30.890 --> 00:04:34.580
Therefore QC is equal to KC,
00:04:34.580 --> 00:04:37.850
and the reaction is at equilibrium.
00:04:37.850 --> 00:04:39.740
And when a reaction is at equilibrium,
00:04:39.740 --> 00:04:43.830
the concentrations of reactants
and products are constant.
00:04:43.830 --> 00:04:46.980
Let's go back to our hypothetical
reaction at equilibrium,
00:04:46.980 --> 00:04:50.060
but this time we're going
to decrease the temperature.
00:04:50.060 --> 00:04:53.130
If we treat heat like a product
decrease in the temperature
00:04:53.130 --> 00:04:56.060
is like decreasing the amount
of one of the products.
00:04:56.060 --> 00:04:58.460
Therefore the net reaction
will go to the right
00:04:58.460 --> 00:05:00.490
to make more product.
00:05:00.490 --> 00:05:02.820
If we approach this problem
by thinking about the reaction
00:05:02.820 --> 00:05:06.100
quotient Q for an exothermic reaction,
00:05:06.100 --> 00:05:09.840
a decrease in temperature in
general causes an increase
00:05:09.840 --> 00:05:11.930
in the equilibrium constants.
00:05:11.930 --> 00:05:14.570
And if the equilibrium constant increases,
00:05:14.570 --> 00:05:17.130
then Q would be less than K.
00:05:17.130 --> 00:05:19.340
And when Q is less than K,
00:05:19.340 --> 00:05:22.850
the net reaction goes to the right.
00:05:22.850 --> 00:05:25.010
The net reaction would
continue to go to the right
00:05:25.010 --> 00:05:26.700
until Q is equal to K,
00:05:26.700 --> 00:05:29.990
and equilibrium has been re-established.
00:05:29.990 --> 00:05:32.240
Next let's look at an endothermic reaction
00:05:32.240 --> 00:05:34.800
where Delta H is greater than zero.
00:05:34.800 --> 00:05:39.140
When six water molecules
complex to a Cobalt two plus ion
00:05:39.140 --> 00:05:42.800
the resulting complex
ion is pink in color.
00:05:42.800 --> 00:05:46.440
And when for chloride anions
complex to a cobalt two plus
00:05:46.440 --> 00:05:50.910
ion, the resulting complex
ion is blue in color.
00:05:50.910 --> 00:05:53.830
When the pink ion reacts
with four chloride anions,
00:05:53.830 --> 00:05:55.850
the blue ion is formed.
00:05:55.850 --> 00:05:58.050
And since this reaction is endothermic,
00:05:58.050 --> 00:06:01.363
we can put heat on the reactant side.
00:06:02.500 --> 00:06:04.770
We're gonna use these
particular diagrams down here
00:06:04.770 --> 00:06:07.210
to help us understand what
happens to an endothermic
00:06:07.210 --> 00:06:10.340
reaction at equilibrium when
the temperature changes,
00:06:10.340 --> 00:06:12.640
however, these drawings aren't
designed to be completely
00:06:12.640 --> 00:06:14.560
accurate for this particular reaction.
00:06:14.560 --> 00:06:18.160
They're just to help us understand
what color we would see.
00:06:18.160 --> 00:06:21.410
For example, let's say that
this middle particulate diagram
00:06:21.410 --> 00:06:23.870
represents the reaction at equilibrium.
00:06:23.870 --> 00:06:26.710
And if there are decent
amounts of both the blue ion
00:06:26.710 --> 00:06:29.070
and the pink ion at equilibrium,
00:06:29.070 --> 00:06:31.280
the resulting equilibrium mixture,
00:06:31.280 --> 00:06:33.170
so this is an aqueous solution
00:06:33.170 --> 00:06:36.343
would appear to be purple or violet.
00:06:38.060 --> 00:06:40.950
If we were to increase the temperature
00:06:40.950 --> 00:06:42.650
for this endothermic reaction,
00:06:42.650 --> 00:06:45.270
we treat heat like a reactant.
00:06:45.270 --> 00:06:47.880
So increasing the temperature
is like increasing
00:06:47.880 --> 00:06:49.860
the amount of a reactant.
00:06:49.860 --> 00:06:53.730
And therefore the net reaction
will shift to the right
00:06:53.730 --> 00:06:56.620
to get rid of some of that reactant.
00:06:56.620 --> 00:06:58.210
Whether the net reaction
goes to the right,
00:06:58.210 --> 00:07:00.800
we're gonna increase in
the amount of blue ion,
00:07:00.800 --> 00:07:04.460
and we're going to decrease
in the amount of pink ion.
00:07:04.460 --> 00:07:08.240
Therefore looking at this
particular diagram on the right
00:07:08.240 --> 00:07:12.720
there are now more blue ions
than there are pink ions
00:07:12.720 --> 00:07:16.000
compared to our equilibrium
mixture in the middle.
00:07:16.000 --> 00:07:18.480
Therefore for this third
particular diagram,
00:07:18.480 --> 00:07:22.420
the resulting aqueous solution
is going to look blue.
00:07:22.420 --> 00:07:25.260
If we think about those
using Q in general,
00:07:25.260 --> 00:07:28.670
for an endothermic reaction,
an increase in temperature
00:07:28.670 --> 00:07:32.490
causes an increase in the
equilibrium constant K.
00:07:32.490 --> 00:07:37.490
And if K increases, then
the reaction quotient Q
00:07:37.500 --> 00:07:39.410
is less than K.
00:07:39.410 --> 00:07:40.970
And when Q is less than K,
00:07:40.970 --> 00:07:44.180
the net reaction goes to the right.
00:07:44.180 --> 00:07:47.720
Now let's go back to the
middle particular diagram.
00:07:47.720 --> 00:07:49.790
And so there are reactions at equilibrium
00:07:49.790 --> 00:07:53.000
and this time we're going
to decrease the temperature.
00:07:53.000 --> 00:07:55.090
If we treat heat as a reactant,
00:07:55.090 --> 00:07:56.660
and we decrease the temperature,
00:07:56.660 --> 00:07:59.000
it's like we're decreasing
one of our reactants.
00:07:59.000 --> 00:08:01.430
Therefore the net reaction
will shift to the left
00:08:01.430 --> 00:08:03.920
to make more of our reactant.
00:08:03.920 --> 00:08:05.840
And when that reaction goes to the left,
00:08:05.840 --> 00:08:08.320
we're gonna decrease in
the amount of the blue ion,
00:08:08.320 --> 00:08:12.110
and we're going to increase
in the amount of the pink ion.
00:08:12.110 --> 00:08:14.930
So when we compare the
middle particulate diagram
00:08:14.930 --> 00:08:17.110
to the one on the left
and the one that left,
00:08:17.110 --> 00:08:19.230
there's a lot more of the pink ion,
00:08:19.230 --> 00:08:20.970
then there is of the blue ion.
00:08:20.970 --> 00:08:23.860
Therefore the overall solution,
00:08:23.860 --> 00:08:27.380
the overall aqueous solution
is going to appear pink.
00:08:27.380 --> 00:08:29.990
If we think about what's happening using Q
00:08:29.990 --> 00:08:33.020
for an endothermic reaction in general,
00:08:33.020 --> 00:08:34.540
when you decrease the temperature,
00:08:34.540 --> 00:08:37.040
you decrease the equilibrium constant.
00:08:37.040 --> 00:08:40.030
And if the equilibrium constant decreases
00:08:40.030 --> 00:08:42.680
now, Q would be greater than K,
00:08:42.680 --> 00:08:45.410
which means too many products
and not enough reactance.
00:08:45.410 --> 00:08:48.670
Therefore the net reaction
would go to the left.
00:08:48.670 --> 00:08:51.400
Let's go back to our exothermic reaction.
00:08:51.400 --> 00:08:54.270
At this time let's pretend like
we're starting with only A,
00:08:54.270 --> 00:08:56.710
so we start with only A
and we have none of B.
00:08:56.710 --> 00:08:59.970
And our goal is to make
as much as we possibly can
00:08:59.970 --> 00:09:02.440
and to do it as fast as possible.
00:09:02.440 --> 00:09:05.160
One way to increase the rate of a reaction
00:09:05.160 --> 00:09:07.930
would be to increase the temperature.
00:09:07.930 --> 00:09:10.420
However, for an exothermic reaction,
00:09:10.420 --> 00:09:13.960
increasing the temperature
decreases the equilibrium
00:09:13.960 --> 00:09:15.170
constant K.
00:09:15.170 --> 00:09:17.870
And if you decrease the
equilibrium constant K,
00:09:17.870 --> 00:09:20.280
you would decrease the amount of B
00:09:20.280 --> 00:09:23.290
that you would have when
you reach equilibrium.
00:09:23.290 --> 00:09:25.490
So we can't run our hypothetical reaction
00:09:25.490 --> 00:09:27.770
at too high of a temperature
because that would decrease
00:09:27.770 --> 00:09:29.820
the equilibrium constant.
00:09:29.820 --> 00:09:32.250
So instead to speed up
the rate of the reaction,
00:09:32.250 --> 00:09:34.633
we could add a catalyst,
00:09:36.110 --> 00:09:39.760
let's look at a graph of
concentration of B versus time,
00:09:39.760 --> 00:09:41.970
and we're gonna start
with this blue curve here,
00:09:41.970 --> 00:09:44.890
which represents the hypothetical reaction
00:09:44.890 --> 00:09:48.530
without a catalyst, so
the uncatalyzed reaction.
00:09:48.530 --> 00:09:51.760
When time is equal to zero,
the concentration of B is zero
00:09:51.760 --> 00:09:53.620
because we start with only A.
00:09:53.620 --> 00:09:57.790
And as A turns into B the
concentration of B increases
00:09:57.790 --> 00:10:00.810
over time, and eventually
the concentration of B
00:10:00.810 --> 00:10:02.360
becomes constant.
00:10:02.360 --> 00:10:04.710
And when the concentration
of B becomes constant,
00:10:04.710 --> 00:10:06.710
the reaction reaches equilibrium.
00:10:06.710 --> 00:10:10.740
So this dotted line here
represents the concentration of B
00:10:10.740 --> 00:10:12.490
at equilibrium.
00:10:12.490 --> 00:10:14.950
The yellow line represents the reaction
00:10:14.950 --> 00:10:16.760
with a catalyst added.
00:10:16.760 --> 00:10:18.810
So once again, we're starting with only A,
00:10:18.810 --> 00:10:20.190
so when time is equal to zero,
00:10:20.190 --> 00:10:22.410
the concentration of B is equal to zero.
00:10:22.410 --> 00:10:24.850
And as time increases A turns into B,
00:10:24.850 --> 00:10:27.290
so the concentration of B increases
00:10:27.290 --> 00:10:30.860
and eventually the concentration
of B becomes constant.
00:10:30.860 --> 00:10:33.390
And the reaction reaches equilibrium.
00:10:33.390 --> 00:10:36.540
Notice that the reaction
reached equilibrium much faster
00:10:36.540 --> 00:10:38.410
with the addition of the catalyst
00:10:38.410 --> 00:10:40.900
than it did without the catalyst.
00:10:40.900 --> 00:10:43.730
So the addition of a
catalyst allows a reaction
00:10:43.730 --> 00:10:46.340
to reach equilibrium faster.
00:10:46.340 --> 00:10:49.810
However, notice that the final
equilibrium concentration
00:10:49.810 --> 00:10:53.220
of B is the same for both
the uncatalyzed reaction
00:10:53.220 --> 00:10:55.150
and the catalyzed reaction.
00:10:55.150 --> 00:10:57.730
Therefore, the addition of
a catalyst does not change
00:10:57.730 --> 00:11:01.570
the composition of the
equilibrium mixture.
00:11:01.570 --> 00:11:03.710
And that's because the catalyst speeds up
00:11:03.710 --> 00:11:07.920
both the forward reaction
and the reverse reaction,
00:11:07.920 --> 00:11:10.150
but the rates are still equal.
00:11:10.150 --> 00:11:11.490
And since the rates are equal,
00:11:11.490 --> 00:11:13.350
there's no change in the composition
00:11:13.350 --> 00:11:15.153
of the equilibrium mixture.
|
Le Chȃtelier’s principle: Changing volume | https://www.youtube.com/watch?v=FmqyKCQo7Tk | vtt | https://www.youtube.com/api/timedtext?v=FmqyKCQo7Tk&ei=3VWUZdKnLMa3mLAPw_eH8Ak&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245325&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=6C8BB02CBFC39ED0B2025952A55561427C339CE2.8E23B625FBA715930CA985EEE5BB5025D5805C48&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.955 --> 00:00:02.840
- [Tutor] Le Chatelier's
principle says that
00:00:02.840 --> 00:00:06.490
if a stress is applied to a
reaction mixture at equilibrium,
00:00:06.490 --> 00:00:08.500
the net reaction goes in the direction
00:00:08.500 --> 00:00:10.730
that relieves the stress.
00:00:10.730 --> 00:00:14.030
One possible stress that we
could do is to change the volume
00:00:14.030 --> 00:00:16.590
on our reaction at equilibrium.
00:00:16.590 --> 00:00:20.180
Let's say we have a hypothetical
reaction, where solid A,
00:00:20.180 --> 00:00:23.500
which is symbolized by red
in our particular diagram,
00:00:23.500 --> 00:00:27.370
turns into solid B, which
is symbolized by a blue
00:00:27.370 --> 00:00:29.620
and also C, which is a gas
00:00:29.620 --> 00:00:33.000
and C will be symbolized by white spheres.
00:00:33.000 --> 00:00:35.650
The equilibrium constant
Kc for this reaction,
00:00:35.650 --> 00:00:39.750
is equal to 0.4 at 25 degrees Celsius.
00:00:39.750 --> 00:00:40.930
The first particular diagram
00:00:40.930 --> 00:00:43.240
shows the reaction at equilibrium,
00:00:43.240 --> 00:00:46.380
and we can see there's some
solid A and some solid B
00:00:46.380 --> 00:00:48.070
at the bottom of the container,
00:00:48.070 --> 00:00:51.930
and there's also some
gaseous particles of C.
00:00:51.930 --> 00:00:53.330
Let's introduce a stress,
00:00:53.330 --> 00:00:55.970
to our reaction mixture at equilibrium.
00:00:55.970 --> 00:00:58.870
Let's decrease the
volume of the container.
00:00:58.870 --> 00:01:01.970
So looking from the first
particular diagram to the second,
00:01:01.970 --> 00:01:03.530
we can see there's been a decrease
00:01:03.530 --> 00:01:05.370
in the volume of the container.
00:01:05.370 --> 00:01:08.790
That's gonna cause an
increase in the pressure
00:01:08.790 --> 00:01:11.140
because pressure comes
from these gas particles
00:01:11.140 --> 00:01:13.830
slamming into the sides of the container.
00:01:13.830 --> 00:01:15.940
And if we decrease the volume,
00:01:15.940 --> 00:01:18.860
now there's less distance
for these particles to travel
00:01:18.860 --> 00:01:21.040
before they slam into the
sides of the container,
00:01:21.040 --> 00:01:23.970
which means we increase
the collision frequency.
00:01:23.970 --> 00:01:27.130
And therefore the pressure increases.
00:01:27.130 --> 00:01:29.060
According to Le Chatelier's principle,
00:01:29.060 --> 00:01:30.990
the net reaction is gonna
go in the direction,
00:01:30.990 --> 00:01:32.750
that relieves the stress.
00:01:32.750 --> 00:01:35.310
So if the stress is increased pressure,
00:01:35.310 --> 00:01:37.690
the net reaction is going to
try to move in the direction
00:01:37.690 --> 00:01:40.420
that decreases the pressure.
00:01:40.420 --> 00:01:43.070
Looking at the equation for
this hypothetical reaction,
00:01:43.070 --> 00:01:46.110
the two solids aren't really
contributing to the pressure.
00:01:46.110 --> 00:01:49.000
So it's only gas C that
we need to worry about.
00:01:49.000 --> 00:01:52.770
And there's one mole of
gas C on the product side,
00:01:52.770 --> 00:01:56.810
and there are zero moles of
gas on the reactant side.
00:01:56.810 --> 00:01:58.530
So if the net reaction went to the right,
00:01:58.530 --> 00:02:01.530
we'd be going from zero moles
of gas to one mole of gas.
00:02:01.530 --> 00:02:04.210
So going to the right would
increase the moles of gas,
00:02:04.210 --> 00:02:06.450
which would increase the pressure.
00:02:06.450 --> 00:02:08.720
However, that's not what
the reaction wants to do.
00:02:08.720 --> 00:02:11.350
The goal of the reaction
is to relieve the stress
00:02:11.350 --> 00:02:14.830
and therefore the reaction
wants to decrease the pressure.
00:02:14.830 --> 00:02:17.210
So the reactions gonna go to the left,
00:02:17.210 --> 00:02:19.250
to get rid of some of that gas
00:02:19.250 --> 00:02:23.250
and decreasing the amount of
gas will decrease the pressure,
00:02:23.250 --> 00:02:26.380
therefore relieving the stress.
00:02:26.380 --> 00:02:28.670
If the net reaction moves to the left,
00:02:28.670 --> 00:02:30.470
we're gonna lose some of our products.
00:02:30.470 --> 00:02:32.220
So we're gonna decrease the amount of C
00:02:32.220 --> 00:02:34.860
and we're gonna decrease
in the amount of B
00:02:34.860 --> 00:02:37.270
and we're going to gain
some of our reactants.
00:02:37.270 --> 00:02:39.630
So we're gonna increase
in the amount of A,
00:02:39.630 --> 00:02:42.810
and we can see all that and
the third particulate diagram.
00:02:42.810 --> 00:02:44.530
So going from the second
particular diagram
00:02:44.530 --> 00:02:46.150
to the third particular diagram,
00:02:46.150 --> 00:02:47.630
we've decreased the amount of C,
00:02:47.630 --> 00:02:49.370
we've gone from four particles of C
00:02:49.370 --> 00:02:51.110
to only two particles of C.
00:02:51.110 --> 00:02:52.900
We've also decreased the amount of B.
00:02:52.900 --> 00:02:54.790
You can see that this blue,
00:02:54.790 --> 00:02:56.870
this blue solid has gotten smaller,
00:02:56.870 --> 00:03:00.040
and we've increased the amount of A.
00:03:00.040 --> 00:03:02.870
So A, is this, A, is this red sphere here,
00:03:02.870 --> 00:03:04.390
and you can see how it's gotten bigger
00:03:04.390 --> 00:03:07.320
from the second particulate
diagram to the third.
00:03:07.320 --> 00:03:09.630
And by going from four particles of C,
00:03:09.630 --> 00:03:11.680
to only two particles of C,
00:03:11.680 --> 00:03:14.150
we've decreased the amount of the gas,
00:03:14.150 --> 00:03:17.000
and therefore we've
decreased the pressure.
00:03:17.000 --> 00:03:19.290
To better understand what
happens to a reaction mixture
00:03:19.290 --> 00:03:21.590
at equilibrium when a
stress is placed on it,
00:03:21.590 --> 00:03:24.140
let's calculate the reaction quotient Q
00:03:24.140 --> 00:03:26.160
for these three particular diagrams,
00:03:26.160 --> 00:03:28.820
for the same hypothetical reaction.
00:03:28.820 --> 00:03:31.550
The expression for the
reaction quotient Qc,
00:03:31.550 --> 00:03:35.010
has the same form as the
equilibrium constant expression
00:03:35.010 --> 00:03:36.330
for Kc.
00:03:36.330 --> 00:03:37.860
So since solids are left out
00:03:37.860 --> 00:03:40.320
of the equilibrium constant expression,
00:03:40.320 --> 00:03:43.420
we only need to include the
concentration of the gas.
00:03:43.420 --> 00:03:45.910
And since there's a coefficient
of one in front of C,
00:03:45.910 --> 00:03:48.070
Qc is equal to the concentration of C
00:03:48.070 --> 00:03:50.060
raised to the first power.
00:03:50.060 --> 00:03:51.610
Since there are four particles of C
00:03:51.610 --> 00:03:53.280
in the first particular diagram,
00:03:53.280 --> 00:03:56.430
and if each particle
represents 0.1 moles of C,
00:03:56.430 --> 00:03:58.046
four times, 0.1
00:03:58.046 --> 00:03:59.710
is equal to 0.4
00:03:59.710 --> 00:04:00.760
moles of C.
00:04:00.760 --> 00:04:02.650
So to find the concentration of C,
00:04:02.650 --> 00:04:04.100
we take the moles and divide that
00:04:04.100 --> 00:04:07.530
by the volume of the
container, which is 1.0 liter.
00:04:07.530 --> 00:04:09.730
So 0.4 divided by 1.0
00:04:09.730 --> 00:04:10.691
is equal to
00:04:10.691 --> 00:04:11.770
0.4
00:04:11.770 --> 00:04:12.603
molar.
00:04:12.603 --> 00:04:14.130
So that's the concentration of C
00:04:14.130 --> 00:04:16.200
in the first particular diagram.
00:04:16.200 --> 00:04:19.170
We plugged that into our expression for Q.
00:04:19.170 --> 00:04:20.240
So Qc
00:04:20.240 --> 00:04:21.073
is equal
00:04:21.073 --> 00:04:21.963
to
00:04:21.963 --> 00:04:23.150
0.4
00:04:23.150 --> 00:04:24.177
and notice that
00:04:24.177 --> 00:04:25.010
Kc
00:04:25.010 --> 00:04:25.843
is also
00:04:25.843 --> 00:04:26.676
equal to
00:04:26.676 --> 00:04:27.509
0.4.
00:04:27.509 --> 00:04:31.100
So at this moment in
time, Qc is equal to Kc,
00:04:31.100 --> 00:04:34.940
which tells us the
reaction is at equilibrium.
00:04:34.940 --> 00:04:37.170
Next, we think about the
stress that was applied
00:04:37.170 --> 00:04:38.900
to the reaction at equilibrium.
00:04:38.900 --> 00:04:41.070
We decreased the volume.
00:04:41.070 --> 00:04:42.410
And if we look at the volumes here,
00:04:42.410 --> 00:04:46.180
we're going from 1.0 liters to 0.5 liters.
00:04:46.180 --> 00:04:49.080
So we're decreasing the
volume by a factor of two,
00:04:49.080 --> 00:04:51.520
which would cause an
increase in the pressure
00:04:51.520 --> 00:04:53.850
by a factor of two.
00:04:53.850 --> 00:04:57.010
And changing the volume would
change the concentration.
00:04:57.010 --> 00:05:00.167
So instead of 0.4, divided by 1.0,
00:05:00.167 --> 00:05:01.243
it'd be 0.4
00:05:01.243 --> 00:05:02.440
divided by
00:05:02.440 --> 00:05:03.600
0.5,
00:05:03.600 --> 00:05:05.084
which is equal to
00:05:05.084 --> 00:05:06.210
0.8
00:05:06.210 --> 00:05:07.043
molar.
00:05:07.043 --> 00:05:09.890
So the concentration has doubled.
00:05:09.890 --> 00:05:13.710
So if we calculate Q for our
second particular diagram,
00:05:13.710 --> 00:05:16.970
we plug in the concentration
of C, which is 0.8 molar.
00:05:16.970 --> 00:05:17.910
So Qc
00:05:17.910 --> 00:05:19.363
is equal to
00:05:19.363 --> 00:05:20.450
0.8,
00:05:20.450 --> 00:05:21.440
K is equal
00:05:21.440 --> 00:05:22.530
to 0.4.
00:05:22.530 --> 00:05:24.580
So Q is not equal to K,
00:05:24.580 --> 00:05:27.730
therefore the reaction
is not at equilibrium
00:05:27.730 --> 00:05:29.357
for our second particular diagram.
00:05:29.357 --> 00:05:34.040
Let me write in here, not at equilibrium.
00:05:34.040 --> 00:05:34.873
In this case,
00:05:34.873 --> 00:05:35.890
Qc
00:05:35.890 --> 00:05:37.690
is greater than Kc,
00:05:37.690 --> 00:05:39.850
which tells us we have too many products
00:05:39.850 --> 00:05:41.340
and not enough reactants.
00:05:41.340 --> 00:05:43.860
Therefore the net
reaction goes to the left
00:05:43.860 --> 00:05:45.580
to get rid of some of the products
00:05:45.580 --> 00:05:48.950
and to increase the amount of reactants.
00:05:48.950 --> 00:05:50.890
The net reaction keeps going to the left
00:05:50.890 --> 00:05:53.440
until we reach equilibrium again.
00:05:53.440 --> 00:05:55.330
So if we calculate the concentration of C
00:05:55.330 --> 00:05:57.100
in the third particular diagram,
00:05:57.100 --> 00:05:58.870
here there are only two particles.
00:05:58.870 --> 00:05:59.930
So that'd be
00:05:59.930 --> 00:06:00.763
0.2
00:06:00.763 --> 00:06:01.750
moles
00:06:01.750 --> 00:06:04.780
divided by a volume of 0.5 liters.
00:06:04.780 --> 00:06:05.690
So 0.2
00:06:05.690 --> 00:06:07.150
divided by 0.5
00:06:07.150 --> 00:06:08.660
is equal to
00:06:08.660 --> 00:06:09.493
0.4
00:06:09.493 --> 00:06:10.326
molar.
00:06:10.326 --> 00:06:11.230
So Qc
00:06:11.230 --> 00:06:12.063
is equal
00:06:12.063 --> 00:06:13.100
to 0.4.
00:06:13.100 --> 00:06:17.083
And since Qc is equal
to 0.4, Kc is still 0.4.
00:06:18.650 --> 00:06:22.560
So Qc is equal to Kc and
we're at equilibrium.
00:06:22.560 --> 00:06:26.180
So equilibrium has been re-established.
00:06:26.180 --> 00:06:27.900
Since the reaction is at equilibrium
00:06:27.900 --> 00:06:29.940
in a third particular diagram,
00:06:29.940 --> 00:06:31.700
the net reaction stops going to the left
00:06:31.700 --> 00:06:35.020
and the concentration
of C remains constant.
00:06:35.020 --> 00:06:37.150
Let's apply what we've
learned to another reaction,
00:06:37.150 --> 00:06:41.360
the synthesis of ammonia from
nitrogen gas and hydrogen gas.
00:06:41.360 --> 00:06:43.940
If we have a mixture of
these gases at equilibrium,
00:06:43.940 --> 00:06:45.230
and we introduce a stress,
00:06:45.230 --> 00:06:47.770
the system like a decrease in volume,
00:06:47.770 --> 00:06:49.560
the decrease in the
volume of the container
00:06:49.560 --> 00:06:52.150
would cause an increase in the pressure.
00:06:52.150 --> 00:06:54.080
And according to Le Chatelier's principle,
00:06:54.080 --> 00:06:55.940
the net reaction is
gonna go in the direction
00:06:55.940 --> 00:06:59.280
that relieves the stress that
was placed on the system.
00:06:59.280 --> 00:07:02.120
So if the stress is increased pressure,
00:07:02.120 --> 00:07:03.360
the net reaction says,
00:07:03.360 --> 00:07:06.350
I wanna move in the direction
that decreases that pressure.
00:07:06.350 --> 00:07:09.320
So the net reaction moves to the right,
00:07:09.320 --> 00:07:11.900
because there are four
moles of gas on the left
00:07:11.900 --> 00:07:13.970
and only two moles of gas on the right.
00:07:13.970 --> 00:07:15.790
And by moving to the right,
00:07:15.790 --> 00:07:18.020
that goes from four moles
of gas to two moles of gas,
00:07:18.020 --> 00:07:20.010
which decreases the amount of gas
00:07:20.010 --> 00:07:23.220
and causes a decrease in the pressure.
00:07:23.220 --> 00:07:26.370
If we had a mixture of
these gases at equilibrium,
00:07:26.370 --> 00:07:29.530
and we increased the volume
and increase in the volume
00:07:29.530 --> 00:07:32.190
would cause a decrease in the pressure.
00:07:32.190 --> 00:07:35.440
So the stress this time,
is decreased pressure.
00:07:35.440 --> 00:07:37.780
To relieve the stress, the net reaction,
00:07:37.780 --> 00:07:41.020
wants to move in the direction
that increases the pressure.
00:07:41.020 --> 00:07:43.860
Therefore, the net reaction
is going to move to the left
00:07:43.860 --> 00:07:45.140
because if it moves to the left,
00:07:45.140 --> 00:07:47.160
we're going from two
moles of gas in the right
00:07:47.160 --> 00:07:49.080
to four moles of gas on the left.
00:07:49.080 --> 00:07:52.000
So that's an increase in the moles of gas
00:07:52.000 --> 00:07:53.800
and increase in the amount of gas,
00:07:53.800 --> 00:07:56.730
causes an increase in the pressure.
00:07:56.730 --> 00:07:57.780
Now let's see what happens,
00:07:57.780 --> 00:07:59.584
when we have equal amounts of moles of gas
00:07:59.584 --> 00:08:01.930
on both sides of the equation.
00:08:01.930 --> 00:08:04.630
For example, for the
hypothetical reaction,
00:08:04.630 --> 00:08:06.530
where gas A turns into gas B,
00:08:06.530 --> 00:08:09.200
there's one mole of gas
on the reactant side,
00:08:09.200 --> 00:08:12.230
and there's one mole of
gas on the product side,
00:08:12.230 --> 00:08:15.460
and let's use particular
diagrams and reaction quotients
00:08:15.460 --> 00:08:17.080
to understand what's going on here.
00:08:17.080 --> 00:08:19.490
So for our first particular diagram,
00:08:19.490 --> 00:08:21.200
here's the Qc expression.
00:08:21.200 --> 00:08:23.520
It's equal to the concentration
of B to the first power,
00:08:23.520 --> 00:08:26.270
divided by the concentration
of A to the first power
00:08:26.270 --> 00:08:28.850
and the concentration
of B since B is blue,
00:08:28.850 --> 00:08:32.700
there's two blue spheres in
this first particular diagram.
00:08:32.700 --> 00:08:36.040
So two times 0.1 moles
is 0.2 moles of blue
00:08:36.040 --> 00:08:38.430
divided by a volume of one liter.
00:08:38.430 --> 00:08:43.350
Therefore the concentration
of B is equal to 0.2.
00:08:43.350 --> 00:08:46.700
The concentration of A would
also be equal to 0.2 molar
00:08:46.700 --> 00:08:50.040
because there's two
particles of A in here.
00:08:50.040 --> 00:08:52.360
So 0.2 divided by 0.2
00:08:52.360 --> 00:08:53.560
is equal to
00:08:53.560 --> 00:08:54.730
one.
00:08:54.730 --> 00:08:58.360
And since K is equal to
one for this reaction,
00:08:58.360 --> 00:09:01.240
Kc is equal to one at 25 degrees Celsius.
00:09:01.240 --> 00:09:04.950
Qc is equal to Kc at this moment in time.
00:09:04.950 --> 00:09:07.940
Therefore the reaction is at equilibrium
00:09:07.940 --> 00:09:10.220
in this first particular diagram.
00:09:10.220 --> 00:09:13.010
If you introduce a stress to
our system at equilibrium,
00:09:13.010 --> 00:09:16.080
let's decrease the volume
by a factor of two.
00:09:16.080 --> 00:09:20.050
So we're going from one,
one liter to 0.5 liters.
00:09:20.050 --> 00:09:23.190
That's gonna increase the
pressure by a factor of two.
00:09:23.190 --> 00:09:26.350
And it's also going to
double the concentrations.
00:09:26.350 --> 00:09:28.130
So the concentration of B
00:09:28.130 --> 00:09:29.310
is now
00:09:29.310 --> 00:09:30.143
0.4
00:09:30.143 --> 00:09:30.976
molar
00:09:30.976 --> 00:09:34.620
and the concentration
of A is also 0.4 molar.
00:09:34.620 --> 00:09:36.660
So 0.4 divided by 0.4
00:09:36.660 --> 00:09:37.493
is equal
00:09:37.493 --> 00:09:38.326
to
00:09:38.326 --> 00:09:39.159
one.
00:09:39.159 --> 00:09:40.310
So Qc
00:09:40.310 --> 00:09:41.250
is still
00:09:41.250 --> 00:09:42.540
equal to Kc.
00:09:42.540 --> 00:09:46.160
The reaction is still at equilibrium.
00:09:46.160 --> 00:09:49.150
Since changing the volume
didn't change the value for Q,
00:09:49.150 --> 00:09:51.320
Qc is still equal to Kc.
00:09:51.320 --> 00:09:53.960
And since there's no change,
there's no net reaction
00:09:53.960 --> 00:09:57.080
to the left and there's no
net reaction to the right.
00:09:57.080 --> 00:10:00.080
Therefore changing the volume
on a reaction at equilibrium,
00:10:00.080 --> 00:10:03.060
when there are equal amounts
of moles of gas on both sides,
00:10:03.060 --> 00:10:08.060
has no effect on the composition
of the equilibrium mixture.
00:10:09.000 --> 00:10:10.980
Let's go back to the
reaction for the synthesis
00:10:10.980 --> 00:10:14.470
of ammonia gas from nitrogen
gas and hydrogen gas.
00:10:14.470 --> 00:10:17.050
And let's say this
reaction is at equilibrium.
00:10:17.050 --> 00:10:19.170
And we add in some helium gas
00:10:19.170 --> 00:10:22.010
to the reaction mixture at equilibrium.
00:10:22.010 --> 00:10:25.340
Helium is an inert gas,
which means it doesn't react
00:10:25.340 --> 00:10:27.770
with any of the gases
that we have present.
00:10:27.770 --> 00:10:28.740
It's tempting to say,
00:10:28.740 --> 00:10:32.720
adding this inert gas would
increase the total pressure
00:10:32.720 --> 00:10:36.430
and therefore the net reaction
would shift to the right
00:10:36.430 --> 00:10:39.100
to get rid of that increased pressure.
00:10:39.100 --> 00:10:42.250
However, notice that helium is
not a part of the expression
00:10:42.250 --> 00:10:45.500
for Qc and therefore after you add it,
00:10:45.500 --> 00:10:48.630
you're not actually changing
any of these concentrations.
00:10:48.630 --> 00:10:53.630
And so Qc is still equal to Kc
after the addition of helium.
00:10:53.890 --> 00:10:55.700
And since Qc is equal to Kc,
00:10:55.700 --> 00:10:57.820
the reaction is still at equilibrium
00:10:57.820 --> 00:11:00.450
and there's no shift either direction.
00:11:00.450 --> 00:11:03.220
Therefore adding an
inert gas to a reaction,
00:11:03.220 --> 00:11:05.780
make sure at equilibrium, has no effect
00:11:05.780 --> 00:11:08.753
on the composition of
the reaction mixture.
|
Le Chȃtelier’s principle: Changing concentration | https://www.youtube.com/watch?v=jjmAGbcKEZY | vtt | https://www.youtube.com/api/timedtext?v=jjmAGbcKEZY&ei=3VWUZcGsL56ip-oPiIu62A0&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245325&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=65B99DF7CF813D7AC5E8C6243E6600B5CEC65EF5.BDEBFBC4BDFFBDD8A9C993A49B885A69F0D77AA9&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.930 --> 00:00:02.710
- [Instructor] Le
Chatelier's principle says,
00:00:02.710 --> 00:00:06.420
if a stress is applied to a
reaction mixture at equilibrium,
00:00:06.420 --> 00:00:08.770
the net reaction goes in the direction
00:00:08.770 --> 00:00:10.920
that relieves the stress.
00:00:10.920 --> 00:00:13.770
Change in the concentration
of a reactant or product
00:00:13.770 --> 00:00:18.010
is one way to place a stress
on a reaction at equilibrium.
00:00:18.010 --> 00:00:21.220
For example, let's consider
the hypothetical reaction
00:00:21.220 --> 00:00:24.770
where gas A turns into gas B.
00:00:24.770 --> 00:00:27.760
And let's say the reaction
is at equilibrium.
00:00:27.760 --> 00:00:29.590
And we suddenly introduce a stress
00:00:29.590 --> 00:00:34.590
such as we increase the
concentration of reactant A.
00:00:34.800 --> 00:00:37.083
According to Le Chatelier's principle,
00:00:38.200 --> 00:00:40.180
the net reaction is
gonna go in the direction
00:00:40.180 --> 00:00:41.520
that relieves the stress.
00:00:41.520 --> 00:00:44.390
And since we increase
the concentration of A,
00:00:44.390 --> 00:00:46.970
the net reaction is gonna go to the right
00:00:46.970 --> 00:00:50.190
to decrease the concentration of A.
00:00:50.190 --> 00:00:51.680
Let's use some particular diagrams
00:00:51.680 --> 00:00:53.060
so we can get into the details
00:00:53.060 --> 00:00:55.440
of how the reaction goes to the right.
00:00:55.440 --> 00:00:58.330
So we're gonna symbolize
gas A by red particles
00:00:58.330 --> 00:01:00.970
and gas B by blue particles.
00:01:00.970 --> 00:01:02.980
And for this hypothetical reaction,
00:01:02.980 --> 00:01:05.740
the equilibrium constant is equal to three
00:01:05.740 --> 00:01:09.070
at 25 degrees Celsius.
00:01:09.070 --> 00:01:11.480
Let's start by writing
the reaction quotient.
00:01:11.480 --> 00:01:16.480
Qc is equal to, and we get that
from our balanced equation.
00:01:16.490 --> 00:01:20.200
That would be the concentration
of B to the first power
00:01:20.200 --> 00:01:25.200
divided by the concentration
of A, also to the first power.
00:01:28.050 --> 00:01:30.520
Let's calculate the
concentrations of B and A
00:01:30.520 --> 00:01:33.010
from our first particular diagram.
00:01:33.010 --> 00:01:35.670
So B is represented by the blue spheres
00:01:35.670 --> 00:01:37.650
and there are three blue spheres.
00:01:37.650 --> 00:01:40.960
If each particle represents
0.1 moles of a substance,
00:01:40.960 --> 00:01:44.310
and the volume of the
container is one litter,
00:01:44.310 --> 00:01:46.040
since we have three particles,
00:01:46.040 --> 00:01:49.630
that'd be three times
0.1, which is 0.3 moles
00:01:49.630 --> 00:01:53.260
divided by a volume of
one litter is 0.3 molar..
00:01:53.260 --> 00:01:57.590
So the concentration of B is 0.3 molar.
00:01:57.590 --> 00:02:00.430
For A, we have one
particles, that's 0.1 mole
00:02:00.430 --> 00:02:03.530
divided by one litter, which is 0.1 molar.
00:02:03.530 --> 00:02:07.128
So the concentration of A is 0.1 molar.
00:02:07.128 --> 00:02:09.810
And 0.3 divided by 0.1 is equal to three.
00:02:09.810 --> 00:02:14.400
So Qc at this moment in
time is equal to three.
00:02:14.400 --> 00:02:16.490
Notice we could have just
counted our particles,
00:02:16.490 --> 00:02:20.590
three blues and one red
and said three over one.
00:02:20.590 --> 00:02:22.810
That would have been a little bit faster.
00:02:22.810 --> 00:02:27.780
So Qc is equal to three and
Kc is also equal to three.
00:02:27.780 --> 00:02:29.351
So I should have written a C in here.
00:02:29.351 --> 00:02:34.160
So when Qc is equal to Kc, the
reaction is at equilibrium.
00:02:34.160 --> 00:02:36.730
So in this first particular diagram here
00:02:36.730 --> 00:02:41.730
where Qc is equal to Kc, the
reactions are at equilibrium.
00:02:41.890 --> 00:02:43.480
Next, we're gonna introduce a stress
00:02:43.480 --> 00:02:45.500
to our reaction at equilibrium.
00:02:45.500 --> 00:02:48.930
We're going to increase
the concentration of A.
00:02:48.930 --> 00:02:51.790
So here, we're gonna
add four particles of A
00:02:51.790 --> 00:02:55.810
to the reaction mixture at equilibrium.
00:02:55.810 --> 00:02:58.540
The second particulate diagram
shows what the reaction
00:02:58.540 --> 00:03:02.010
looks like right after we
add those four red particles.
00:03:02.010 --> 00:03:05.100
So we started with one red
particle and we added four.
00:03:05.100 --> 00:03:07.610
So now there's a total
of five red particles.
00:03:07.610 --> 00:03:10.910
And we still have the
same three blue particles
00:03:10.910 --> 00:03:13.710
that we had in the first
particular diagram.
00:03:13.710 --> 00:03:17.200
Let's calculate Qc at this moment in time.
00:03:17.200 --> 00:03:20.300
So just after we introduced the stress.
00:03:20.300 --> 00:03:23.250
Since there are three blue
particles and five red particles,
00:03:23.250 --> 00:03:27.633
Qc is equal to three divided
by five, which is equal to 0.6.
00:03:29.470 --> 00:03:33.690
Since Qc is equal to 0.6,
and Kc is equal to three,
00:03:33.690 --> 00:03:38.241
at this moment in time,
Qc is less than Kc.
00:03:38.241 --> 00:03:41.810
So there are too many reactants
and not enough products.
00:03:41.810 --> 00:03:46.080
Therefore, the net reaction
is going to go to the right
00:03:46.080 --> 00:03:49.100
and we're going to decrease
in the amount of A,
00:03:49.100 --> 00:03:52.870
and we're gonna increase
in the amount of B.
00:03:52.870 --> 00:03:54.749
The third particular
diagram shows what happens
00:03:54.749 --> 00:03:58.120
after the net reaction moves to the right.
00:03:58.120 --> 00:04:00.250
So we said, we're gonna
decrease the amount of A
00:04:00.250 --> 00:04:02.880
and increase in the amount of B.
00:04:02.880 --> 00:04:04.910
We're going from three blues
00:04:04.910 --> 00:04:08.957
in the second particular diagram
to six blues in the third.
00:04:08.957 --> 00:04:13.957
And we're going from five
reds to only two reds.
00:04:14.940 --> 00:04:19.940
Therefore, three reds must
have turned into blues
00:04:20.110 --> 00:04:23.000
to get the third particular
diagram on the right.
00:04:23.000 --> 00:04:27.540
And if we calculate Qc for
our third particular diagram,
00:04:27.540 --> 00:04:30.980
it'd be equal to six divided by two,
00:04:30.980 --> 00:04:33.280
which is equal to three.
00:04:33.280 --> 00:04:37.780
So at this moment in
time, Qc is equal to Kc.
00:04:37.780 --> 00:04:39.090
They're both equal to three.
00:04:39.090 --> 00:04:41.827
So equilibrium has been reestablished
00:04:41.827 --> 00:04:44.940
in the third particular diagram.
00:04:44.940 --> 00:04:47.640
It isn't always necessary
to calculate Q values
00:04:47.640 --> 00:04:51.730
when doing a Le Chatelier's
changing concentration problem.
00:04:51.730 --> 00:04:54.040
However, for this hypothetical reaction,
00:04:54.040 --> 00:04:57.440
it's useful to calculate
Q values to understand
00:04:57.440 --> 00:04:59.760
that we're starting at equilibrium
00:04:59.760 --> 00:05:01.520
and then a stress is introduced
00:05:01.520 --> 00:05:04.080
such as changing the concentration
of a reaction or product.
00:05:04.080 --> 00:05:08.400
And that means the reaction
is no longer at equilibrium.
00:05:08.400 --> 00:05:10.460
Le Chatelier's principle
allows us to predict
00:05:10.460 --> 00:05:14.130
which direction the net reaction will go
00:05:14.130 --> 00:05:16.320
or we could also use Q to predict
00:05:16.320 --> 00:05:18.150
the direction of the net reaction.
00:05:18.150 --> 00:05:21.850
The net reaction will continue
going in that new direction
00:05:21.850 --> 00:05:23.970
until Q is equal to K again
00:05:23.970 --> 00:05:27.220
and equilibrium has been reestablished,
00:05:27.220 --> 00:05:28.530
let's look at another reaction.
00:05:28.530 --> 00:05:30.570
This is the synthesis of ammonia
00:05:30.570 --> 00:05:34.060
from nitrogen gas and hydrogen gas.
00:05:34.060 --> 00:05:36.800
And let's see the reaction
is at equilibrium.
00:05:36.800 --> 00:05:38.810
So let's also look at this on a graph
00:05:38.810 --> 00:05:41.320
of concentration versus time.
00:05:41.320 --> 00:05:44.580
At equilibrium, the concentrations
of reactants and products
00:05:44.580 --> 00:05:48.040
are constant, which is why we
see these straight lines here
00:05:48.040 --> 00:05:51.983
for the concentration of
hydrogen, ammonia, and nitrogen.
00:05:52.830 --> 00:05:56.480
And let's introduce a stress
to the system at equilibrium.
00:05:56.480 --> 00:05:58.710
So right now we are at equilibrium
00:05:58.710 --> 00:06:00.980
and all the concentrations are constant.
00:06:00.980 --> 00:06:05.160
And let's increase the
concentration of hydrogen.
00:06:05.160 --> 00:06:08.020
So we can see that on our graph.
00:06:08.020 --> 00:06:10.530
So right here, there's a sudden increase
00:06:10.530 --> 00:06:13.670
in the concentration of hydrogen.
00:06:13.670 --> 00:06:16.870
Adding hydrogen means that
Q is no longer equal to K
00:06:16.870 --> 00:06:19.870
and therefore the reaction
is not at equilibrium.
00:06:19.870 --> 00:06:21.880
So let's go ahead and write over here,
00:06:21.880 --> 00:06:24.173
Now we're not at equilibrium.
00:06:25.050 --> 00:06:27.600
And Le Chatelier's principle
allows us to predict
00:06:27.600 --> 00:06:30.560
which direction the
net reaction will move.
00:06:30.560 --> 00:06:33.130
So since we added a stress,
00:06:33.130 --> 00:06:36.600
the stress being increased
concentration of hydrogen,
00:06:36.600 --> 00:06:38.860
the net reaction is
gonna move to the right
00:06:38.860 --> 00:06:42.670
to get rid of some of that
hydrogen that was added.
00:06:42.670 --> 00:06:44.460
And when the reaction goes to the right,
00:06:44.460 --> 00:06:46.850
the amount of ammonia will increase.
00:06:46.850 --> 00:06:49.620
And that's what we can see right
here on this red line here,
00:06:49.620 --> 00:06:52.170
the amount of ammonia is increasing.
00:06:52.170 --> 00:06:54.340
And the amount of ammonia increases
00:06:54.340 --> 00:06:57.760
because nitrogen and hydrogen
are reacting to form ammonia.
00:06:57.760 --> 00:06:59.900
Therefore, the amount
of nitrogen and hydrogen
00:06:59.900 --> 00:07:00.851
will decrease.
00:07:00.851 --> 00:07:03.560
Here we can see the amount
of hydrogen is decreasing.
00:07:03.560 --> 00:07:05.711
And down here, we can see
the amount of nitrogen
00:07:05.711 --> 00:07:07.800
is decreasing.
00:07:07.800 --> 00:07:09.710
The reaction will continue
to go to the right
00:07:09.710 --> 00:07:12.060
until equilibrium is reestablished.
00:07:12.060 --> 00:07:14.330
And that happens at the
second dotted line here.
00:07:14.330 --> 00:07:16.250
And we know that because we can see
00:07:16.250 --> 00:07:19.830
all of these concentrations
are now constant.
00:07:19.830 --> 00:07:23.870
So the reaction has reached equilibrium.
00:07:23.870 --> 00:07:26.720
So far we've only talked about
change in the concentration
00:07:26.720 --> 00:07:28.600
of a reactant so for example,
00:07:28.600 --> 00:07:31.632
if we increase the
concentration of hydrogen,
00:07:31.632 --> 00:07:34.260
the net reaction goes to the right.
00:07:34.260 --> 00:07:36.360
We could also say shifts to the right.
00:07:36.360 --> 00:07:38.530
So for a reaction at equilibrium,
00:07:38.530 --> 00:07:40.730
if you increase the
concentration of reactants,
00:07:40.730 --> 00:07:42.520
such as the concentration of hydrogen
00:07:42.520 --> 00:07:45.750
or the concentration of nitrogen,
00:07:45.750 --> 00:07:49.070
the reaction will shift to the right
00:07:49.070 --> 00:07:52.970
to decrease the amount of
one of those reactants.
00:07:52.970 --> 00:07:54.840
And if our reaction is at equilibrium
00:07:54.840 --> 00:07:57.700
and we were to increase
the amount of our product,
00:07:57.700 --> 00:07:59.348
increase the amount of ammonia,
00:07:59.348 --> 00:08:00.940
so this time the stress place
00:08:00.940 --> 00:08:03.130
is increased concentration of a product,
00:08:03.130 --> 00:08:05.310
Le Chatelier's principle
says the net reaction
00:08:05.310 --> 00:08:08.560
is going to move in the direction
that decreases the stress.
00:08:08.560 --> 00:08:11.640
So in this case, the net
reaction would go to the left
00:08:11.640 --> 00:08:13.833
to decrease the amount of ammonia.
00:08:14.730 --> 00:08:16.460
And if our reaction is at equilibrium
00:08:16.460 --> 00:08:21.460
and we were to decrease the
concentration of our product,
00:08:21.490 --> 00:08:24.520
the net reaction would shift to the right
00:08:24.520 --> 00:08:27.110
to make more of the product.
00:08:27.110 --> 00:08:29.930
Or if we decrease the concentration
of one of our reactants,
00:08:29.930 --> 00:08:32.240
let's say of nitrogen,
00:08:32.240 --> 00:08:34.600
in this case the reaction
will shift to the left
00:08:34.600 --> 00:08:36.493
to make more of our reactant.
|
Worked example: Using the reaction quotient to find equilibrium partial pressures | https://www.youtube.com/watch?v=U7U3e0r_8y8 | vtt | https://www.youtube.com/api/timedtext?v=U7U3e0r_8y8&ei=3VWUZYHWL-zumLAP_beT6Ac&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245325&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=8A0B4814259B356932423B813BB71225EE03F258.E15C78EFB141418255A9F2DE79BBA200FF049910&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.568 --> 00:00:02.932
- [Tutor] For the
reaction of iron two oxide
00:00:02.932 --> 00:00:07.463
plus carbon monoxide goes to
solid iron and carbon dioxide.
00:00:07.463 --> 00:00:12.463
The equilibrium constant Kp is
equal to 0.26 at 1000 Kelvin.
00:00:12.818 --> 00:00:15.929
Our goal is to find the
equilibrium partial pressures
00:00:15.929 --> 00:00:19.531
of our two gasses, carbon
monoxide and carbon dioxide.
00:00:19.531 --> 00:00:21.232
If the initial partial pressures
00:00:21.232 --> 00:00:24.210
are 0.80 atmospheres for carbon monoxide
00:00:24.210 --> 00:00:28.140
and 0.40 atmospheres for carbon dioxide,
00:00:28.140 --> 00:00:30.131
we can use the reaction quotient Q,
00:00:30.131 --> 00:00:32.833
to predict which direction
that reaction will go
00:00:32.833 --> 00:00:34.819
to reach equilibrium.
00:00:34.819 --> 00:00:36.569
So let's calculate Qp
00:00:37.648 --> 00:00:39.221
and Qp
00:00:39.221 --> 00:00:40.370
is equal to,
00:00:40.370 --> 00:00:42.139
first we think about our products
00:00:42.139 --> 00:00:44.885
and we leave solids out of
equilibrium expressions,
00:00:44.885 --> 00:00:47.787
and therefore we also leave it
out of our expression for Qp.
00:00:47.787 --> 00:00:49.381
So we're gonna leave out iron.
00:00:49.381 --> 00:00:52.818
We're going to include carbon
dioxide since it's a gas.
00:00:52.818 --> 00:00:56.115
So we're gonna write the partial
pressure of carbon dioxide,
00:00:56.115 --> 00:00:57.830
and since we have a coefficient of one
00:00:57.830 --> 00:00:59.229
in front of carbon dioxide,
00:00:59.229 --> 00:01:01.685
it's the partial pressure
raise to the first power
00:01:01.685 --> 00:01:04.140
divided by, next we look at our reactants,
00:01:04.140 --> 00:01:06.709
and we have a solid, so
we're gonna leave that out.
00:01:06.709 --> 00:01:09.231
So we have another gas, carbon monoxide.
00:01:09.231 --> 00:01:12.090
So this will be the partial
pressure of carbon monoxide
00:01:12.090 --> 00:01:13.460
raised to the first power,
00:01:13.460 --> 00:01:15.878
since there's also a coefficient of one.
00:01:15.878 --> 00:01:17.749
Next, we plug in our partial pressures
00:01:17.749 --> 00:01:19.218
at this moment in time.
00:01:19.218 --> 00:01:21.593
The partial pressure of carbon dioxide
00:01:21.593 --> 00:01:22.467
is
00:01:22.467 --> 00:01:23.300
0.40,
00:01:24.158 --> 00:01:26.631
and the partial pressure
of carbon monoxide
00:01:26.631 --> 00:01:27.464
is
00:01:27.464 --> 00:01:28.297
0.80
00:01:28.297 --> 00:01:29.635
atmospheres.
00:01:29.635 --> 00:01:32.146
So we plug those into
our expression for Qp
00:01:32.146 --> 00:01:33.108
and 0.40
00:01:33.108 --> 00:01:34.679
divided by 0.80
00:01:34.679 --> 00:01:36.236
is equal to
00:01:36.236 --> 00:01:37.750
0.50.
00:01:37.750 --> 00:01:39.390
So Qp
00:01:39.390 --> 00:01:43.210
at this moment in time is equal to 0.50.
00:01:43.210 --> 00:01:46.730
Since QP is not equal to
Kp at this moment in time,
00:01:46.730 --> 00:01:49.569
the reaction is not at equilibrium.
00:01:49.569 --> 00:01:54.120
So Qp is equal to 0.50
and Kp is equal to 0.26.
00:01:54.120 --> 00:01:54.953
So Qp
00:01:55.850 --> 00:01:57.199
is greater
00:01:57.199 --> 00:01:58.548
than Kp.
00:01:58.548 --> 00:02:00.986
And when Qp is greater than Kp,
00:02:00.986 --> 00:02:04.655
there are too many products
and not enough reactants.
00:02:04.655 --> 00:02:09.467
Therefore the net reaction
is going to move to the left.
00:02:09.467 --> 00:02:12.373
Next let's fill out our I.C.E
table for this reaction.
00:02:12.373 --> 00:02:15.679
I stands for the initial
partial pressure in atmospheres.
00:02:15.679 --> 00:02:18.369
And so the initial partial
pressure of carbon monoxide
00:02:18.369 --> 00:02:20.276
was 0.80 atmospheres.
00:02:20.276 --> 00:02:22.717
And the initial partial
pressure of carbon dioxide
00:02:22.717 --> 00:02:25.068
is 0.40 atmospheres.
00:02:25.068 --> 00:02:26.656
C stands for change.
00:02:26.656 --> 00:02:30.017
And E stands for the
equilibrium partial pressure.
00:02:30.017 --> 00:02:32.609
Calculating Qp allowed us to realize
00:02:32.609 --> 00:02:35.306
that the net reaction moves to the left.
00:02:35.306 --> 00:02:37.416
And if the net reaction moves to the left,
00:02:37.416 --> 00:02:39.999
we're going to lose some carbon dioxide
00:02:39.999 --> 00:02:43.569
and we're going to gain
some carbon monoxide.
00:02:43.569 --> 00:02:46.506
So first let's think about carbon dioxide.
00:02:46.506 --> 00:02:47.695
We're gonna lose some of it,
00:02:47.695 --> 00:02:50.146
but we don't know how much and therefore
00:02:50.146 --> 00:02:52.169
that's gonna be represented by X.
00:02:52.169 --> 00:02:55.767
So we're gonna write minus
X here for carbon dioxide.
00:02:55.767 --> 00:02:57.689
And since the coefficient is a one
00:02:57.689 --> 00:02:59.457
in front of carbon dioxide,
00:02:59.457 --> 00:03:02.177
and it's also one in
front of carbon monoxide,
00:03:02.177 --> 00:03:04.536
if we lose X for carbon dioxide,
00:03:04.536 --> 00:03:08.376
we're going to gain X for carbon monoxide.
00:03:08.376 --> 00:03:10.745
Therefore the equilibrium partial pressure
00:03:10.745 --> 00:03:12.619
for carbon monoxide
00:03:12.619 --> 00:03:13.452
would be
00:03:13.452 --> 00:03:14.926
0.80
00:03:14.926 --> 00:03:15.759
plus X.
00:03:16.629 --> 00:03:19.956
And the equilibrium partial
pressure for carbon dioxide
00:03:19.956 --> 00:03:20.789
would be
00:03:20.789 --> 00:03:21.622
0.40
00:03:22.646 --> 00:03:23.479
minus X.
00:03:24.417 --> 00:03:27.725
Our next step is to write an
equilibrium constant expression
00:03:27.725 --> 00:03:29.235
for this reaction.
00:03:29.235 --> 00:03:34.235
So Kp is equal to the partial
pressure of carbon dioxide
00:03:34.543 --> 00:03:38.845
divided by the partial
pressure of carbon monoxide.
00:03:38.845 --> 00:03:41.965
So the expressions for
Kp and Qp look the same,
00:03:41.965 --> 00:03:43.994
but the difference is for Kp,
00:03:43.994 --> 00:03:46.954
it would be the equilibrium
partial pressures only.
00:03:46.954 --> 00:03:48.185
Whereas for Qp,
00:03:48.185 --> 00:03:51.373
it's the partial pressures
at any moment in time.
00:03:51.373 --> 00:03:52.434
And since for Kp,
00:03:52.434 --> 00:03:55.535
we're talking about the
equilibrium partial pressures,
00:03:55.535 --> 00:03:58.591
we can take those directly
from our I.C.E table
00:03:58.591 --> 00:03:59.754
and plug them in.
00:03:59.754 --> 00:04:03.496
So we can plug in the equilibrium
partial pressure of CO2
00:04:03.496 --> 00:04:08.496
and the equilibrium partial
pressure of carbon monoxide.
00:04:08.833 --> 00:04:12.046
Here we can see our two
equilibrium partial pressures
00:04:12.046 --> 00:04:14.622
plugged into our Kp expression
00:04:14.622 --> 00:04:17.114
and also the equilibrium constant Kp
00:04:17.114 --> 00:04:19.634
is equal to 0.26 for this reaction,
00:04:19.634 --> 00:04:21.625
so that's plugged in as well.
00:04:21.625 --> 00:04:23.697
Our next step is to solve for X.
00:04:23.697 --> 00:04:27.736
So we multiply both sides by 0.80 plus X,
00:04:27.736 --> 00:04:31.115
and we get this and then
we do some more algebra
00:04:31.115 --> 00:04:35.536
and we get down to 1.26
X is equal to 0.192.
00:04:35.536 --> 00:04:36.369
So
00:04:36.369 --> 00:04:37.202
0.192
00:04:37.202 --> 00:04:38.035
divided by
00:04:38.035 --> 00:04:39.502
1.26
00:04:39.502 --> 00:04:40.335
is equal to
00:04:40.335 --> 00:04:41.470
0.15.
00:04:41.470 --> 00:04:42.303
So X
00:04:42.303 --> 00:04:43.564
is equal to
00:04:43.564 --> 00:04:44.397
0.
00:04:44.397 --> 00:04:45.230
1
00:04:45.230 --> 00:04:46.776
5.
00:04:46.776 --> 00:04:49.189
Now that we know that X is equal to 0.15,
00:04:49.189 --> 00:04:50.879
we can go back to our I.C.E table
00:04:50.879 --> 00:04:54.028
and solve for the equilibrium
partial pressures.
00:04:54.028 --> 00:04:55.720
So for carbon monoxide,
00:04:55.720 --> 00:04:59.760
the equilibrium partial
pressure is 0.80 plus X.
00:04:59.760 --> 00:05:01.240
So that's equal to
00:05:01.240 --> 00:05:02.348
0.80
00:05:02.348 --> 00:05:03.480
plus
00:05:03.480 --> 00:05:04.313
0.
00:05:04.313 --> 00:05:05.146
1
00:05:05.146 --> 00:05:05.979
5,
00:05:05.979 --> 00:05:07.185
which is equal to
00:05:07.185 --> 00:05:08.018
0.
00:05:08.018 --> 00:05:08.851
9
00:05:08.851 --> 00:05:09.684
5
00:05:09.684 --> 00:05:10.517
atmospheres.
00:05:10.517 --> 00:05:12.325
So that's the equilibrium partial pressure
00:05:12.325 --> 00:05:14.313
of carbon monoxide.
00:05:14.313 --> 00:05:15.733
For carbon dioxide,
00:05:15.733 --> 00:05:19.730
the equilibrium partial
pressure is 0.40 minus X.
00:05:19.730 --> 00:05:20.563
So
00:05:20.563 --> 00:05:21.529
0.40
00:05:21.529 --> 00:05:22.809
minus
00:05:22.809 --> 00:05:23.642
0.15
00:05:24.499 --> 00:05:25.796
is equal to
00:05:25.796 --> 00:05:26.629
0.
00:05:26.629 --> 00:05:27.462
2
00:05:27.462 --> 00:05:28.295
5
00:05:28.295 --> 00:05:29.128
atmospheres.
00:05:29.128 --> 00:05:31.135
So that's the equilibrium partial pressure
00:05:31.135 --> 00:05:33.394
for carbon dioxide.
00:05:33.394 --> 00:05:34.227
Finally,
00:05:34.227 --> 00:05:36.223
we can use the reaction quotient Qp
00:05:36.223 --> 00:05:38.183
to make sure that these two answers,
00:05:38.183 --> 00:05:41.393
for equilibrium partial
pressures are correct.
00:05:41.393 --> 00:05:44.539
So we can write that Qp is equal to
00:05:44.539 --> 00:05:47.363
the partial pressure of CO2
00:05:47.363 --> 00:05:50.753
divided by the partial pressure of CO.
00:05:50.753 --> 00:05:52.144
And we can plug in those,
00:05:52.144 --> 00:05:54.335
those equilibrium partial pressures.
00:05:54.335 --> 00:05:55.603
So this would be
00:05:55.603 --> 00:05:57.561
0.25 atmospheres,
00:05:57.561 --> 00:06:01.133
was the equilibrium partial
pressure of carbon dioxide
00:06:01.133 --> 00:06:04.334
and 0.95 was the
equilibrium partial pressure
00:06:04.334 --> 00:06:05.913
of carbon monoxide.
00:06:05.913 --> 00:06:07.913
And 0.25 divided by 0.95
00:06:08.807 --> 00:06:09.987
is equal to
00:06:09.987 --> 00:06:10.820
0.
00:06:10.820 --> 00:06:11.653
2
00:06:11.653 --> 00:06:12.928
6.
00:06:12.928 --> 00:06:13.761
And
00:06:13.761 --> 00:06:14.797
since Kp
00:06:14.797 --> 00:06:16.770
is also equal to
00:06:16.770 --> 00:06:17.603
0.26
00:06:18.487 --> 00:06:19.991
at this moment in time,
00:06:19.991 --> 00:06:20.985
Qp
00:06:20.985 --> 00:06:22.010
is equal
00:06:22.010 --> 00:06:23.075
to Kp
00:06:23.075 --> 00:06:25.963
and the reaction is at equilibrium.
00:06:25.963 --> 00:06:28.076
Therefore we know we have the correct
00:06:28.076 --> 00:06:30.300
equilibrium partial pressures.
|
Using the reaction quotient | https://www.youtube.com/watch?v=JDUNQMj9Yk0 | vtt | https://www.youtube.com/api/timedtext?v=JDUNQMj9Yk0&ei=3VWUZb6OL-H7vdIPr9ixKA&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245325&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=2790DDE62B6918ED3C0C88D6B2F46F80AC06D370.545E9B7B2A4493DC7794EE054FFDC746CEF2436F&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.250 --> 00:00:01.240
- [Instructor] The reaction quotient
00:00:01.240 --> 00:00:03.800
is symbolized by the capital letter Q.
00:00:03.800 --> 00:00:07.840
And it tells us whether a
reaction is at equilibrium or not.
00:00:07.840 --> 00:00:09.900
If the reaction is not at equilibrium,
00:00:09.900 --> 00:00:11.730
it also allows us to predict
00:00:11.730 --> 00:00:14.160
which direction the net reaction will go
00:00:14.160 --> 00:00:15.900
to reach equilibrium.
00:00:15.900 --> 00:00:17.770
For example, let's look
at the hypothetical
00:00:17.770 --> 00:00:21.700
reaction where A gas turns into gas B.
00:00:21.700 --> 00:00:25.200
Gas A will be represented by
red circles or red spheres,
00:00:25.200 --> 00:00:28.580
and gas B will be
represented by blue spheres.
00:00:28.580 --> 00:00:31.320
The equilibrium constant for
this hypothetical reaction
00:00:31.320 --> 00:00:35.280
is equal to 3 at 25 degrees Celsius.
00:00:35.280 --> 00:00:36.880
Let's start by writing out the expression
00:00:36.880 --> 00:00:38.400
for the reaction quotient.
00:00:38.400 --> 00:00:41.450
So we would write out here QC is equal to,
00:00:41.450 --> 00:00:42.840
and this has the same form
00:00:42.840 --> 00:00:45.600
as the equilibrium constant expression.
00:00:45.600 --> 00:00:49.460
So we would put concentration
of B to the first power,
00:00:49.460 --> 00:00:54.273
divided by the concentration
of A, also to the first power.
00:00:55.640 --> 00:00:58.080
Let's look at our first
particulate diagram here,
00:00:58.080 --> 00:00:59.600
and let's think about each particle
00:00:59.600 --> 00:01:02.720
representing 0.1 moles of a substance.
00:01:02.720 --> 00:01:06.960
And the volume of the
container is one liter.
00:01:06.960 --> 00:01:10.220
So let's first find the concentration of B
00:01:10.220 --> 00:01:12.980
so we can plug it into
our expression for Q.
00:01:12.980 --> 00:01:14.550
B are the blue spheres.
00:01:14.550 --> 00:01:18.370
So we count up one,
two, three blue spheres.
00:01:18.370 --> 00:01:21.260
Each sphere or each particle
represents 0.1 moles.
00:01:21.260 --> 00:01:24.340
So three times 0.1 is 0.3.
00:01:24.340 --> 00:01:26.390
And then we divide that by the volume
00:01:26.390 --> 00:01:30.380
of one liter to get a
concentration of 0.3 moles.
00:01:30.380 --> 00:01:33.370
So we can go ahead and plug in 0.3 mole
00:01:33.370 --> 00:01:35.800
for the concentration of B.
00:01:35.800 --> 00:01:38.660
Next, we divide that by
the concentration of A,
00:01:38.660 --> 00:01:41.950
and since there are five red particles,
00:01:41.950 --> 00:01:44.310
and each particle represents 0.1 moles,
00:01:44.310 --> 00:01:47.650
five times 0.1 is 0.5 moles of A
00:01:47.650 --> 00:01:49.490
divided by a volume of one liter,
00:01:49.490 --> 00:01:54.080
it gives a concentration
of 0.5 mole for A.
00:01:54.080 --> 00:01:55.610
Notice that we could have just counted
00:01:55.610 --> 00:01:58.820
the number of particles,
three blues and five reds,
00:01:58.820 --> 00:02:00.930
and just done three divided by five
00:02:00.930 --> 00:02:05.010
and get the same value for
the reaction quotient Q.
00:02:05.010 --> 00:02:08.500
So QC is equal to three fists or 0.6.
00:02:08.500 --> 00:02:11.860
And KC remember was equal to three.
00:02:11.860 --> 00:02:14.360
So Q is not equal to K.
00:02:14.360 --> 00:02:18.180
In this case, QC is less than KC.
00:02:18.180 --> 00:02:21.480
Since Q is not equal to K,
at this moment and time,
00:02:21.480 --> 00:02:24.420
the reaction is not at equilibrium.
00:02:24.420 --> 00:02:26.860
In order for this reaction
to reach equilibrium,
00:02:26.860 --> 00:02:29.360
Q needs to be equal to K.
00:02:29.360 --> 00:02:32.560
And since Q is a lot smaller than K,
00:02:32.560 --> 00:02:33.440
if you think about it,
00:02:33.440 --> 00:02:36.130
we need to increase the numerator
00:02:36.130 --> 00:02:38.620
and decrease the denominator.
00:02:38.620 --> 00:02:41.650
So that means, we have too many reactants
00:02:41.650 --> 00:02:43.220
and not enough products.
00:02:43.220 --> 00:02:46.970
And so the net reaction,
if go back up here
00:02:46.970 --> 00:02:48.480
to the equation here,
00:02:48.480 --> 00:02:51.490
the net reaction is going
to move to the right
00:02:51.490 --> 00:02:53.460
to make more products.
00:02:53.460 --> 00:02:55.810
So the net reaction moves to the right
00:02:55.810 --> 00:02:57.920
to make more blue particles
00:02:57.920 --> 00:03:00.650
and therefore the number of
red particles would decrease.
00:03:00.650 --> 00:03:02.080
We can see that comparing these
00:03:02.080 --> 00:03:04.020
first two particulate diagrams here.
00:03:04.020 --> 00:03:06.530
So let's compare the
first particular diagram
00:03:06.530 --> 00:03:08.670
to the second particular diagram.
00:03:08.670 --> 00:03:10.190
And the first particulate diagram,
00:03:10.190 --> 00:03:12.920
we had three blues and five reds.
00:03:12.920 --> 00:03:15.220
And the second particulate diagram,
00:03:15.220 --> 00:03:19.210
we have five blues and only three reds.
00:03:19.210 --> 00:03:21.460
So that shows the reaction
has moved to the right
00:03:21.460 --> 00:03:23.010
to increase the amount of products
00:03:23.010 --> 00:03:25.590
and to decrease the amount of reactants.
00:03:25.590 --> 00:03:28.490
Let's calculate QC at this moment and time
00:03:28.490 --> 00:03:30.310
for our second particular diagram
00:03:30.310 --> 00:03:32.860
to see if we've reached equilibrium yet.
00:03:32.860 --> 00:03:36.230
Well, we have five blue
particles and only three reds.
00:03:36.230 --> 00:03:40.890
So QC would be equal to five
over three or five thirds.
00:03:40.890 --> 00:03:43.980
Remember that the equilibrium constant KC,
00:03:43.980 --> 00:03:45.690
is equal to three.
00:03:45.690 --> 00:03:49.750
Therefore, QC is still not equal to KC.
00:03:49.750 --> 00:03:53.050
And therefore the reaction
is not at equilibrium.
00:03:53.050 --> 00:03:56.300
And Q is actually still less than K.
00:03:56.300 --> 00:03:57.850
Therefore the net reaction
00:03:57.850 --> 00:04:00.290
is going to move to the right again
00:04:00.290 --> 00:04:01.930
to increase the amount of products
00:04:01.930 --> 00:04:04.700
and to decrease the amount of reactants.
00:04:04.700 --> 00:04:06.990
Let's compare our second
particulate diagram
00:04:06.990 --> 00:04:09.110
to our third particulate diagram.
00:04:09.110 --> 00:04:10.820
And the second particulate diagram,
00:04:10.820 --> 00:04:12.750
we had five blues and three reds.
00:04:12.750 --> 00:04:14.150
And then the third one here,
00:04:14.150 --> 00:04:18.070
we have one, two, three,
four, five, six blues,
00:04:18.070 --> 00:04:19.460
and two reds.
00:04:19.460 --> 00:04:21.890
So we've increased in the amount of blue
00:04:21.890 --> 00:04:24.480
and we've decreased in the amount of red.
00:04:24.480 --> 00:04:27.510
Let's calculate QC for the moment of time
00:04:27.510 --> 00:04:30.450
represented by our third
particulate diagram.
00:04:30.450 --> 00:04:33.610
Well, there are six
blues and only two reds.
00:04:33.610 --> 00:04:36.080
So QC is equal to six divided by two,
00:04:36.080 --> 00:04:38.283
which is equal to three.
00:04:39.490 --> 00:04:41.840
So QC is equal to three
00:04:41.840 --> 00:04:44.570
and remember K is also equal to three.
00:04:44.570 --> 00:04:49.330
So QC is equal to KC and
therefore this reaction
00:04:49.330 --> 00:04:51.520
is now at equilibrium.
00:04:51.520 --> 00:04:52.750
And at equilibrium,
00:04:52.750 --> 00:04:54.520
the reactions turn into the products
00:04:54.520 --> 00:04:57.890
at the same rate the products
turn back into the reactants.
00:04:57.890 --> 00:05:00.420
And therefore the
concentration of both reactants
00:05:00.420 --> 00:05:03.580
and products remained
constant at equilibrium.
00:05:03.580 --> 00:05:05.300
So when Q is less than K,
00:05:05.300 --> 00:05:07.710
the reaction is not at equilibrium.
00:05:07.710 --> 00:05:10.620
There are too many reactants
and not enough products.
00:05:10.620 --> 00:05:13.230
Therefore the net
reaction goes to the right
00:05:13.230 --> 00:05:15.870
to increase the amount of products.
00:05:15.870 --> 00:05:18.120
The net reaction continues
to go to the right
00:05:18.120 --> 00:05:20.790
until Q is equal to K and the reaction
00:05:20.790 --> 00:05:22.600
has reached equilibrium.
00:05:22.600 --> 00:05:25.180
At that point, the concentrations
of reactants and products
00:05:25.180 --> 00:05:27.720
stop changing and they remain constant.
00:05:27.720 --> 00:05:31.140
It's also possible for
Q to be greater than K.
00:05:31.140 --> 00:05:34.400
And if that's true, the
reaction is not at equilibrium,
00:05:34.400 --> 00:05:36.590
but in this case you
have too many products
00:05:36.590 --> 00:05:38.450
and not enough reactants.
00:05:38.450 --> 00:05:41.610
Therefore the net
reaction goes to the left
00:05:41.610 --> 00:05:43.970
to increase the amount of reactants
00:05:43.970 --> 00:05:46.140
and to decrease the amount of products.
00:05:46.140 --> 00:05:48.540
The net reaction will
continue to go to the left
00:05:48.540 --> 00:05:53.170
until Q is equal to K and the
reaction reaches equilibrium.
00:05:53.170 --> 00:05:54.420
Let's look at another reaction,
00:05:54.420 --> 00:05:56.800
which is the decomposition of phosgene
00:05:56.800 --> 00:06:00.250
to form carbon monoxide and chlorine gas.
00:06:00.250 --> 00:06:03.300
KC for this reaction is equal to 2.2 times
00:06:03.300 --> 00:06:06.850
10 to the negative 10th
at 100 degrees Celsius.
00:06:06.850 --> 00:06:08.820
And let's say we're given concentrations
00:06:08.820 --> 00:06:11.730
of phosgene carbon monoxide and chlorine
00:06:11.730 --> 00:06:12.760
at a moment in time,
00:06:12.760 --> 00:06:16.050
and asked if the reaction
is at equilibrium or not.
00:06:16.050 --> 00:06:18.170
And if the reaction's not at equilibrium,
00:06:18.170 --> 00:06:21.440
we need to predict which
direction the net reaction will go
00:06:21.440 --> 00:06:23.470
to reach equilibrium.
00:06:23.470 --> 00:06:26.070
Our approach is gonna be to calculate QC
00:06:26.070 --> 00:06:30.410
at that moment in time,
and then compare QC to KC.
00:06:30.410 --> 00:06:34.180
So first we need to
write our QC expression,
00:06:34.180 --> 00:06:38.720
and this is equal to the
concentration of carbon monoxide
00:06:38.720 --> 00:06:40.140
raised to the first power
00:06:40.140 --> 00:06:43.030
times the concentration of chlorine
00:06:43.030 --> 00:06:45.070
raised to the first power
00:06:45.070 --> 00:06:49.070
and that's divided by the
concentration of phosgene.
00:06:49.070 --> 00:06:52.283
So the concentration of COCL2.
00:06:53.170 --> 00:06:54.310
So at this moment of time,
00:06:54.310 --> 00:06:57.210
the concentration of carbon
monoxide is 3.4 times
00:06:57.210 --> 00:06:58.950
10 to the negative six mole.
00:06:58.950 --> 00:07:01.470
The concentration of
chlorine is 6.0 times,
00:07:01.470 --> 00:07:03.150
times 10 to the negative six mole,
00:07:03.150 --> 00:07:04.590
and the concentration of phosgene
00:07:04.590 --> 00:07:08.160
is equal to 2.0 times 10
to the negative third mole.
00:07:08.160 --> 00:07:11.150
When we plug all those into
our Q expression and solve,
00:07:11.150 --> 00:07:13.570
we get that QC is equal to 1.0
00:07:13.570 --> 00:07:15.483
times 10 to the negative eighth.
00:07:16.530 --> 00:07:21.460
So in this case, QC is greater than KC
00:07:21.460 --> 00:07:24.790
because QC is equal to 1.0
times 10 to the negative eight
00:07:24.790 --> 00:07:28.610
and KC is equal to 2.2 times
10 to the negative 10th.
00:07:28.610 --> 00:07:30.950
And when QC is greater than KC,
00:07:30.950 --> 00:07:33.870
we have too many products
and not enough reactants.
00:07:33.870 --> 00:07:37.270
Therefore the net reaction
is going to go to the left
00:07:37.270 --> 00:07:39.150
and there's going to be an increase
00:07:39.150 --> 00:07:41.200
in the amount of phosgene.
00:07:41.200 --> 00:07:43.850
The reaction will
continue to go to the left
00:07:43.850 --> 00:07:48.850
until Q is equal to K, and the
reaction reaches equilibrium.
|
Worked example: Calculating equilibrium concentrations from initial concentrations | https://www.youtube.com/watch?v=l81swfmUaek | vtt | https://www.youtube.com/api/timedtext?v=l81swfmUaek&ei=3VWUZZvyL7ycp-oPtcqEuA0&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245325&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=C0EA0A80378C295E57F9EAD41180D281437CE455.7A6BF688FC1BAD666AED89F4370BB74D208110F1&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.700 --> 00:00:02.400
- [Instructor] For the
reaction bromine gas
00:00:02.400 --> 00:00:05.670
plus chlorine gas goes to BrCl,
00:00:05.670 --> 00:00:10.290
Kc is equal to 7.0 at 400 Kelvin.
00:00:10.290 --> 00:00:13.840
If the initial concentration
of bromine is 0.60 molar
00:00:13.840 --> 00:00:15.740
and the initial concentration of chlorine
00:00:15.740 --> 00:00:19.140
is also 0.60 molar, our
goal is to calculate
00:00:19.140 --> 00:00:24.140
the equilibrium concentrations
of Br2, Cl2 and BrCl.
00:00:25.970 --> 00:00:28.220
To help us find the
equilibrium concentrations,
00:00:28.220 --> 00:00:30.030
we're gonna use an ICE table,
00:00:30.030 --> 00:00:33.280
where I stands for the
initial concentration,
00:00:33.280 --> 00:00:35.740
C stands for the change in concentration
00:00:35.740 --> 00:00:39.750
and E stands for
equilibrium concentration.
00:00:39.750 --> 00:00:41.380
For the initial concentrations,
00:00:41.380 --> 00:00:43.423
we have 0.60 molar for bromine,
00:00:43.423 --> 00:00:46.700
0.60 molar for chlorine, and if we assume
00:00:46.700 --> 00:00:48.440
the reaction hasn't started yet,
00:00:48.440 --> 00:00:52.600
then we're gonna put a zero
in here for our product, BrCl.
00:00:52.600 --> 00:00:57.040
Next, we think about Br2
reacting with Cl2 to form BrCl.
00:00:58.200 --> 00:01:00.300
Some of the bromine is going to react,
00:01:00.300 --> 00:01:01.930
but we don't know how much,
00:01:01.930 --> 00:01:04.650
so we're gonna call that amount x,
00:01:04.650 --> 00:01:06.760
and we're gonna lose some of that bromine
00:01:06.760 --> 00:01:10.340
when we form our product,
so we're gonna write minus x
00:01:10.340 --> 00:01:13.090
under bromine in our ICE table.
00:01:13.090 --> 00:01:14.980
Next, we think about mole ratios.
00:01:14.980 --> 00:01:18.490
In the balanced equation,
it's a one to one mole ratio
00:01:18.490 --> 00:01:20.360
of bromine to chlorine.
00:01:20.360 --> 00:01:22.790
Therefore, if we're losing x for bromine,
00:01:22.790 --> 00:01:25.290
we're also going to lose x for chlorine.
00:01:25.290 --> 00:01:29.730
So I can write here minus x
under chlorine in the ICE table.
00:01:29.730 --> 00:01:33.640
When Br2 and Cl2 react
together, we lose our reactants,
00:01:33.640 --> 00:01:36.630
and that means we're gonna
gain some of our products.
00:01:36.630 --> 00:01:39.800
To figure out how much, we
need to look at mole ratios.
00:01:39.800 --> 00:01:44.730
So the mole ratio of bromine
to BrCl is one to two,
00:01:44.730 --> 00:01:48.270
therefore if we're losing x for Br2,
00:01:48.270 --> 00:01:52.050
we must be gaining two x for BrCl.
00:01:52.050 --> 00:01:55.800
So I can go ahead and write
plus two x under BrCl.
00:01:55.800 --> 00:01:58.870
Next, let's think about
equilibrium concentrations.
00:01:58.870 --> 00:02:01.450
If the initial concentration
of bromine is 0.6
00:02:01.450 --> 00:02:04.780
and we're losing x, the
equilibrium concentration
00:02:04.780 --> 00:02:08.870
must be 0.60 minus x.
00:02:08.870 --> 00:02:10.340
And the same thing for chlorine.
00:02:10.340 --> 00:02:14.640
It would be 0.60 minus x.
00:02:14.640 --> 00:02:19.430
For BrCl, we start off with
zero, and we gained two x.
00:02:19.430 --> 00:02:22.840
Therefore at equilibrium,
the equilibrium concentration
00:02:22.840 --> 00:02:25.730
would be equal to just two x.
00:02:25.730 --> 00:02:27.730
The next step is to use
the balanced equation
00:02:27.730 --> 00:02:31.150
to write an equilibrium
constant expression.
00:02:31.150 --> 00:02:33.920
So we would write Kc is equal to,
00:02:33.920 --> 00:02:35.690
and then we look at our balanced equation,
00:02:35.690 --> 00:02:38.410
and for our product we have BrCl
00:02:38.410 --> 00:02:39.900
with a two as a coefficient,
00:02:39.900 --> 00:02:44.807
so Kc would be equal to the
concentration of BrCl squared,
00:02:46.530 --> 00:02:49.200
and we're gonna divide
that by the concentration
00:02:49.200 --> 00:02:51.570
of our reactants, which would be Br2,
00:02:51.570 --> 00:02:55.980
so the concentration of Br2
raised to the first power,
00:02:55.980 --> 00:02:57.550
because the coefficient of one,
00:02:57.550 --> 00:03:00.370
times the concentration of Cl2
00:03:00.370 --> 00:03:03.970
also raised to the first power.
00:03:03.970 --> 00:03:06.960
The concentrations in an
equilibrium constant expression
00:03:06.960 --> 00:03:10.560
are equilibrium concentrations,
therefore we can plug in
00:03:10.560 --> 00:03:13.720
the equilibrium concentrations
from our ICE table.
00:03:13.720 --> 00:03:18.560
So the equilibrium concentration
for BrCl was two x,
00:03:18.560 --> 00:03:23.560
the equilibrium concentration
for Br2 was 0.60 minus x,
00:03:23.600 --> 00:03:27.830
and the same for chlorine, so
we can plug that in as well.
00:03:27.830 --> 00:03:30.130
Here we have our
equilibrium concentrations
00:03:30.130 --> 00:03:33.080
plugged into our equilibrium
constant expression,
00:03:33.080 --> 00:03:37.830
and also Kc was equal to 7.0
for this reaction at 400 Kelvin
00:03:37.830 --> 00:03:41.220
so 7.0 is plugged in for Kc.
00:03:41.220 --> 00:03:45.460
Our goal is to solve for x, and
I've re-written it down here
00:03:45.460 --> 00:03:49.730
because 0.60 minus x times 0.60 minus x
00:03:49.730 --> 00:03:52.970
is equal to 0.60 minus x squared.
00:03:52.970 --> 00:03:56.048
And if you write it this
way, it's a little bit easier
00:03:56.048 --> 00:03:57.430
to see that we can solve for x
00:03:57.430 --> 00:04:00.930
by taking the square root of both sides.
00:04:00.930 --> 00:04:04.260
So let's go ahead and take
the square root of both sides
00:04:04.260 --> 00:04:06.390
and solve for x.
00:04:06.390 --> 00:04:07.850
Taking the square root of both sides
00:04:07.850 --> 00:04:12.850
gives us 2.65 is equal to
two x over 0.60 minus x.
00:04:12.940 --> 00:04:15.190
To solve for x, we would
then multiply both sides
00:04:15.190 --> 00:04:18.760
by 0.60 minus x to give us this,
00:04:18.760 --> 00:04:20.520
and then after a little more algebra,
00:04:20.520 --> 00:04:24.317
we get 1.59 is equal to 4.65x.
00:04:24.317 --> 00:04:27.853
So x is equal to 1.59 divided by 4.65,
00:04:28.870 --> 00:04:30.880
which is equal to 0.34.
00:04:33.920 --> 00:04:36.260
Now that we know that x is equal to 0.34,
00:04:36.260 --> 00:04:38.830
we can plug that into our ICE table
00:04:38.830 --> 00:04:42.070
and solve for our
equilibrium concentrations.
00:04:42.070 --> 00:04:44.890
So for the equilibrium
concentration of Br2,
00:04:44.890 --> 00:04:49.513
it's 0.60 minus x, so
that's 0.60 minus 0.34,
00:04:52.400 --> 00:04:56.620
which is equal to 0.26 molar.
00:04:56.620 --> 00:05:00.980
So 0.26 molar is the equilibrium
concentration for bromine.
00:05:00.980 --> 00:05:02.970
For chlorine, it would
be the same calculation,
00:05:02.970 --> 00:05:07.350
0.60 minus x would be 0.60 minus 0.34,
00:05:07.350 --> 00:05:09.520
so the equilibrium
concentration of chlorine
00:05:09.520 --> 00:05:12.330
is also 0.26 molar.
00:05:12.330 --> 00:05:16.990
For BrCl, it's two times x
so that's two times 0.34,
00:05:19.030 --> 00:05:23.020
which is equal to 0.68 molar.
00:05:23.020 --> 00:05:27.733
So 0.68 molar is the equilibrium
concentration for BrCl.
|
Worked example: Calculating an equilibrium constant from initial and equilibrium pressures | https://www.youtube.com/watch?v=MKt3X0SGrtw | vtt | https://www.youtube.com/api/timedtext?v=MKt3X0SGrtw&ei=3VWUZZqTL8SDmLAP-fmR8Ag&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245325&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=3D10A60099B6A304BE8874F828A536285DB12E41.58C61D884494B217736A59B60F8FCF8828340B9E&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.760 --> 00:00:02.370
- [Instructor] Let's say
we have a pure sample
00:00:02.370 --> 00:00:04.540
of phosphorus pentachloride,
00:00:04.540 --> 00:00:08.284
and we add the PCl5 to a
previously evacuated flask
00:00:08.284 --> 00:00:11.410
at 500 Kelvin.
00:00:11.410 --> 00:00:13.620
And let's say the initial
pressure of the PCl5
00:00:13.620 --> 00:00:18.200
is 1.66 atmospheres.
00:00:18.200 --> 00:00:23.159
Some of the PCl5 is going
to turn into PCl3 and Cl2.
00:00:23.159 --> 00:00:26.370
Once equilibrium is
reached, the total pressure,
00:00:26.370 --> 00:00:30.332
let's say, is measured
to be 2.35 atmospheres.
00:00:30.332 --> 00:00:33.930
Our goal is to calculate the
equilibrium partial pressures
00:00:33.930 --> 00:00:38.930
of these three substances,
so PCl5, PCl3 and Cl2.
00:00:39.250 --> 00:00:41.500
And from those equilibrium
partial pressures,
00:00:41.500 --> 00:00:44.140
we can also calculate the Kp value
00:00:44.140 --> 00:00:47.120
for this reaction at 500 Kelvin.
00:00:47.120 --> 00:00:49.430
To help us find the
equilibrium partial pressures,
00:00:49.430 --> 00:00:51.650
we're gonna use an ICE
table where I stands
00:00:51.650 --> 00:00:54.298
for the initial partial
pressure in atmospheres,
00:00:54.298 --> 00:00:56.770
C is the change in partial pressure,
00:00:56.770 --> 00:01:00.620
and E stands for the
equilibrium partial pressure.
00:01:00.620 --> 00:01:01.470
We already know we're starting
00:01:01.470 --> 00:01:06.340
with a partial pressure of
1.66 atmospheres for PCl5.
00:01:06.340 --> 00:01:08.960
And if we assume that the
reaction hasn't started yet,
00:01:08.960 --> 00:01:11.820
we're starting with zero
for our partial pressures
00:01:11.820 --> 00:01:14.473
of PCl3 and Cl2.
00:01:15.570 --> 00:01:18.690
Some of the PCl5 is going to decompose.
00:01:18.690 --> 00:01:20.380
And since we don't know how much,
00:01:20.380 --> 00:01:22.370
we're gonna call that amount x.
00:01:22.370 --> 00:01:24.630
So, we're gonna write minus x here,
00:01:24.630 --> 00:01:27.320
since we're gonna lose some PCl5.
00:01:27.320 --> 00:01:29.350
Next, we need to look at mole ratios.
00:01:29.350 --> 00:01:34.125
So, the mole ratio of PCl5
to PCl3 is one to one.
00:01:34.125 --> 00:01:37.070
So, for losing x for PCl5,
00:01:37.070 --> 00:01:40.755
we must be gaining x for PCl3.
00:01:40.755 --> 00:01:43.040
The same idea with Cl2,
00:01:43.040 --> 00:01:45.460
the coefficient in the
balanced equation is a one.
00:01:45.460 --> 00:01:48.280
So, if we're losing x for PCl5,
00:01:48.280 --> 00:01:52.220
that means we're gaining x for Cl2.
00:01:52.220 --> 00:01:55.161
Therefore, the equilibrium
partial pressure for PCl5
00:01:55.161 --> 00:01:58.900
would be 1.66 minus x.
00:01:58.900 --> 00:02:01.700
The equilibrium partial pressure for PCl3
00:02:01.700 --> 00:02:04.210
would be zero plus x, which is just x.
00:02:04.210 --> 00:02:06.446
And the equilibrium
partial pressure for Cl2
00:02:06.446 --> 00:02:09.780
would be zero plus x, which is also x.
00:02:09.780 --> 00:02:13.050
To figure out what x is, we're
going to use Dalton's law.
00:02:13.050 --> 00:02:15.700
And Dalton's law says
that the total pressure
00:02:15.700 --> 00:02:18.430
of a mixture of gases is equal to the sum
00:02:18.430 --> 00:02:20.560
of the individual partial pressures
00:02:20.560 --> 00:02:22.850
of the gases in the mixture.
00:02:22.850 --> 00:02:24.360
So, we said that the total pressure
00:02:24.360 --> 00:02:26.856
of all the gases at equilibrium
00:02:26.856 --> 00:02:30.870
is equal to 2.35 atmospheres.
00:02:30.870 --> 00:02:33.600
So, we can plug that into Dalton's law.
00:02:33.600 --> 00:02:36.290
And then, we can take the
equilibrium partial pressures
00:02:36.290 --> 00:02:40.800
from our ICE table and plug
those into Dalton's law as well.
00:02:40.800 --> 00:02:43.220
So, we're gonna plug in 1.66 minus x
00:02:43.220 --> 00:02:46.154
for the equilibrium
partial pressure of PCl5,
00:02:46.154 --> 00:02:49.962
x for the equilibrium
partial pressure of PCl3,
00:02:49.962 --> 00:02:53.370
and x for the equilibrium
partial pressure of PCl2.
00:02:54.560 --> 00:02:59.110
So, let's plug in 1.66 minus x.
00:02:59.110 --> 00:03:03.340
And then, we have plus x and plus x.
00:03:03.340 --> 00:03:04.450
And let's solve for x.
00:03:04.450 --> 00:03:07.110
Notice how we have a minus x and a plus x.
00:03:07.110 --> 00:03:08.630
So, that cancels out.
00:03:08.630 --> 00:03:13.490
So, we simply subtract 1.66 from 2.35
00:03:13.490 --> 00:03:16.880
and we find that x is equal to .69.
00:03:16.880 --> 00:03:20.220
So, if x is equal to .69,
00:03:20.220 --> 00:03:25.220
the equilibrium partial pressure
of Cl2 is .69 atmospheres.
00:03:25.733 --> 00:03:29.061
And the equilibrium partial pressure PCl3
00:03:29.061 --> 00:03:31.061
is also .69 atmospheres.
00:03:32.854 --> 00:03:35.104
And 1.66 minus .69 gives us
00:03:36.162 --> 00:03:39.335
the equilibrium partial pressure of PCl5
00:03:39.335 --> 00:03:42.335
and that's equal to .97 atmospheres.
00:03:44.860 --> 00:03:47.180
Now that we have our
equilibrium partial pressures
00:03:47.180 --> 00:03:48.680
for all three gases,
00:03:48.680 --> 00:03:51.930
we can calculate the value
for the equilibrium constant
00:03:51.930 --> 00:03:54.470
for this reaction at 500 Kelvin.
00:03:54.470 --> 00:03:57.170
First, we need to write an
equilibrium constant expression.
00:03:57.170 --> 00:04:01.630
So, we would write Kp is equal
to, and for our products,
00:04:01.630 --> 00:04:05.847
we have PCl3, so this would be
the partial pressure of PCl3
00:04:07.446 --> 00:04:10.930
times the partial pressure
of our other product,
00:04:10.930 --> 00:04:12.720
which is Cl2, so let's put in there
00:04:12.720 --> 00:04:15.130
the partial pressure of Cl2.
00:04:15.130 --> 00:04:20.130
And all of that is divided by
the partial pressure of PCl5.
00:04:21.210 --> 00:04:24.423
So, this would be the
partial pressure of PCl5.
00:04:25.890 --> 00:04:28.730
Next, we plug in our
equilibrium partial pressures.
00:04:28.730 --> 00:04:33.730
So, the equilibrium partial
pressure of PCl3 is .69.
00:04:33.790 --> 00:04:38.220
The equilibrium partial
pressure of Cl2 is also .69.
00:04:38.220 --> 00:04:42.664
And the equilibrium partial
pressure of PCl5 is .97.
00:04:42.664 --> 00:04:45.090
Once we plug our numbers in and we solve,
00:04:45.090 --> 00:04:50.090
we get that Kp is equal
to .49 at 500 Kelvin.
|
Properties of the equilibrium constant | https://www.youtube.com/watch?v=U39OqCEMjto | vtt | https://www.youtube.com/api/timedtext?v=U39OqCEMjto&ei=3VWUZa6rL-avp-oPh_W2uAw&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245325&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=82DFB84EC38814A237DF6D65FC2161A0B3395848.61EDC992F558673E8683EB268869850F86ACE1B7&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.400 --> 00:00:02.900
- [Instructor] An equilibrium
constant has one value
00:00:02.900 --> 00:00:05.990
for a particular reaction
at a certain temperature.
00:00:05.990 --> 00:00:07.640
For example, for this reaction,
00:00:07.640 --> 00:00:11.940
we have oxalic acid turning
into two H plus ions
00:00:11.940 --> 00:00:14.320
and the oxalate anion.
00:00:14.320 --> 00:00:17.740
The equilibrium constant,
K C, for this reaction
00:00:17.740 --> 00:00:20.490
is equal to 3.8 times
10 to the negative six
00:00:20.490 --> 00:00:22.910
at 25 degrees Celsius.
00:00:22.910 --> 00:00:25.830
However, the value of the
equilibrium constant changes
00:00:25.830 --> 00:00:28.300
if we change how we write
the balanced equation.
00:00:28.300 --> 00:00:30.250
For example, let's reverse everything.
00:00:30.250 --> 00:00:34.100
So, instead of having oxalic
acid on the reactant side,
00:00:34.100 --> 00:00:35.810
let's have it on the product side.
00:00:35.810 --> 00:00:38.970
And instead of having H plus
ions in the product side
00:00:38.970 --> 00:00:40.760
and oxalate on the product side,
00:00:40.760 --> 00:00:43.800
let's put them on the reactant side.
00:00:43.800 --> 00:00:46.050
Since we've reversed the reaction,
00:00:46.050 --> 00:00:48.270
there's a new equilibrium constant.
00:00:48.270 --> 00:00:51.570
So we're going to write K
C for the reverse reaction,
00:00:51.570 --> 00:00:52.403
is equal to,
00:00:52.403 --> 00:00:54.100
and to figure out the value
00:00:54.100 --> 00:00:56.180
for the new equilibrium constant,
00:00:56.180 --> 00:00:57.600
since we reversed everything,
00:00:57.600 --> 00:01:01.630
we take the inverse of the
original equilibrium constant.
00:01:01.630 --> 00:01:03.250
So to find the new K C value,
00:01:03.250 --> 00:01:06.790
we take one over the
original equilibrium constant
00:01:06.790 --> 00:01:11.790
of 3.8 times 10 to the negative six.
00:01:13.400 --> 00:01:18.400
And this is equal to 2.6
times 10 to the fifth,
00:01:20.360 --> 00:01:23.490
also at 25 degrees Celsius.
00:01:23.490 --> 00:01:24.980
Let's look at another example of how
00:01:24.980 --> 00:01:26.700
changing how we write the equation
00:01:26.700 --> 00:01:29.600
changes the value for
the equilibrium constant.
00:01:29.600 --> 00:01:31.330
And we start by looking at
00:01:31.330 --> 00:01:33.560
the ionization of hydrofluoric acid,
00:01:33.560 --> 00:01:37.350
turning into an H plus
ion and a fluoride anion.
00:01:37.350 --> 00:01:39.450
The K C value for this
reaction is equal to
00:01:39.450 --> 00:01:41.700
6.8 times 10 to the negative fourth
00:01:41.700 --> 00:01:44.570
at 25 degrees Celsius.
00:01:44.570 --> 00:01:46.410
This time we're going to
multiply everything through
00:01:46.410 --> 00:01:47.800
by a factor of two.
00:01:47.800 --> 00:01:50.120
So it would be two H F
00:01:50.120 --> 00:01:54.790
turning into two H plus, plus two F minus.
00:01:54.790 --> 00:01:56.210
Our goal is to find the value
00:01:56.210 --> 00:01:58.920
for the new equilibrium constant K C.
00:01:58.920 --> 00:02:01.609
And since we multiplied everything through
00:02:01.609 --> 00:02:02.830
by a factor of two,
00:02:02.830 --> 00:02:05.070
we're going to take the
old equilibrium constant
00:02:05.070 --> 00:02:08.220
and we're going to raise
it to the second power.
00:02:08.220 --> 00:02:10.120
So this is K C is equal to
00:02:10.120 --> 00:02:15.050
6.8 times 10 to the negative fourth.
00:02:15.050 --> 00:02:16.893
And we're going to square that.
00:02:18.010 --> 00:02:23.010
So this is equal to 4.6 times
10 to the negative seventh
00:02:24.140 --> 00:02:27.010
at 25 degrees Celsius.
00:02:27.010 --> 00:02:30.050
So since we multiplied
through by a factor of two,
00:02:30.050 --> 00:02:32.940
we raised the equilibrium
constant to the second power.
00:02:32.940 --> 00:02:35.490
If we had multiplied through
by a factor of three,
00:02:35.490 --> 00:02:37.820
we would have raised the
old equilibrium constant
00:02:37.820 --> 00:02:39.602
to the third power.
00:02:39.602 --> 00:02:42.800
Let's use the two reactions
we've just looked at here.
00:02:42.800 --> 00:02:46.640
So we have oxalic acid turning
into H plus and oxalate.
00:02:46.640 --> 00:02:50.010
And the other one we looked
at was hydrofluoric acid
00:02:50.010 --> 00:02:52.830
ionizing to turn into H plus and F minus.
00:02:52.830 --> 00:02:54.270
Let's use those two reactions
00:02:54.270 --> 00:02:56.610
to calculate the equilibrium constant
00:02:56.610 --> 00:02:58.470
for a third reaction.
00:02:58.470 --> 00:03:00.450
And this third reaction shows oxalate
00:03:00.450 --> 00:03:02.550
reacting with hydrofluoric acid
00:03:02.550 --> 00:03:06.800
to form oxalic acid
and the fluoride anion.
00:03:06.800 --> 00:03:09.260
Our first step is to get
these first two reactions
00:03:09.260 --> 00:03:11.360
to look more like the third reaction.
00:03:11.360 --> 00:03:15.051
For example, we have oxalic
acid on the reactant side,
00:03:15.051 --> 00:03:17.120
in the first reaction here,
00:03:17.120 --> 00:03:19.500
and oxalic acid is on the product side
00:03:19.500 --> 00:03:21.230
for the third reaction.
00:03:21.230 --> 00:03:23.240
Also notice, oxalate
is on the product side
00:03:23.240 --> 00:03:25.170
for the first and over here for the third,
00:03:25.170 --> 00:03:26.860
it's on the reactant side.
00:03:26.860 --> 00:03:29.610
So we need to reverse the first reaction
00:03:29.610 --> 00:03:32.060
to make it look more like the third one.
00:03:32.060 --> 00:03:34.060
Here we have that reaction reversed.
00:03:34.060 --> 00:03:37.136
And since we reversed the
reaction, we would have to take
00:03:37.136 --> 00:03:40.210
the inverse of the equilibrium constant,
00:03:40.210 --> 00:03:42.610
which we did in the earlier example.
00:03:42.610 --> 00:03:45.530
So let's go ahead and cross
out this first one here,
00:03:45.530 --> 00:03:48.215
because we're not going
to need it anymore.
00:03:48.215 --> 00:03:50.700
And let's move on to our next reaction
00:03:50.700 --> 00:03:53.510
and try to make it look
more like the third one.
00:03:53.510 --> 00:03:55.100
So here we have hydrofluoric acid
00:03:55.100 --> 00:03:58.210
turning into H plus and F minus.
00:03:58.210 --> 00:04:00.140
And for our third reaction,
00:04:00.140 --> 00:04:02.650
we have hydrofluoric acid
on the reactant side,
00:04:02.650 --> 00:04:05.040
but notice there is a coefficient of two
00:04:05.040 --> 00:04:06.400
in the balanced equation,
00:04:06.400 --> 00:04:09.970
and we have only a one in
how we have it written.
00:04:09.970 --> 00:04:12.720
So we need to multiply everything through
00:04:12.720 --> 00:04:14.609
by a factor of two
00:04:14.609 --> 00:04:19.609
to give us two H F and two
H plus and two F minus.
00:04:21.630 --> 00:04:23.270
And since we multiplied everything through
00:04:23.270 --> 00:04:25.040
by a factor of two,
00:04:25.040 --> 00:04:27.760
we would need to square
the equilibrium constant
00:04:27.760 --> 00:04:29.310
for the original reaction.
00:04:29.310 --> 00:04:32.670
And once again, this is
from our previous example.
00:04:32.670 --> 00:04:35.583
So we already know that
equilibrium constant value.
00:04:36.430 --> 00:04:38.970
Next, let's add these
two reactions together
00:04:38.970 --> 00:04:43.140
and make sure they give
us the third reaction.
00:04:43.140 --> 00:04:46.726
So we have all of our
reactants on one side
00:04:46.726 --> 00:04:51.726
and we have all of our products
on the other side here.
00:04:52.000 --> 00:04:53.830
And we look for things that are the same
00:04:53.830 --> 00:04:56.050
on both the reactants
and the products side.
00:04:56.050 --> 00:04:58.170
Well, there's two H plus on the left
00:04:58.170 --> 00:05:00.050
and there's two H plus on the right,
00:05:00.050 --> 00:05:01.700
so that would cancel out.
00:05:01.700 --> 00:05:04.640
And now, notice that we would have
00:05:04.640 --> 00:05:09.640
oxalate plus two H F going to
oxalic acid plus two F minus.
00:05:13.620 --> 00:05:15.610
So adding our two reactions together
00:05:15.610 --> 00:05:18.800
does give us our third reaction.
00:05:18.800 --> 00:05:21.980
Once we've confirmed that adding
our two reactions together
00:05:21.980 --> 00:05:24.350
gives us our third reaction,
00:05:24.350 --> 00:05:26.240
we can use the equilibrium constants
00:05:26.240 --> 00:05:27.670
for the first two reactions
00:05:27.670 --> 00:05:30.950
to figure out the equilibrium
constant for the third.
00:05:30.950 --> 00:05:32.370
So the equilibrium constant
00:05:32.370 --> 00:05:34.960
for this first reaction
we're gonna call K one,
00:05:34.960 --> 00:05:37.720
for the second reaction
we're gonna call K two,
00:05:37.720 --> 00:05:39.090
and the equilibrium constant
00:05:39.090 --> 00:05:41.260
that we're trying to find
for the third reaction
00:05:41.260 --> 00:05:42.653
we'll call K C.
00:05:43.530 --> 00:05:47.150
To find the equilibrium constant
for the third reaction K C,
00:05:47.150 --> 00:05:49.530
we need to multiply the
equilibrium constants
00:05:49.530 --> 00:05:51.720
for the first two reactions together.
00:05:51.720 --> 00:05:56.720
So K C is equal to K one times K two.
00:05:58.040 --> 00:06:00.240
We've already calculated
the value for our K one
00:06:00.240 --> 00:06:02.298
from an earlier example,
00:06:02.298 --> 00:06:03.650
it was 2.6 times 10 to the fifth,
00:06:03.650 --> 00:06:05.880
and we also calculated K two,
00:06:05.880 --> 00:06:09.830
and it was 4.6 times 10
to the negative seven.
00:06:09.830 --> 00:06:10.870
So to find K C,
00:06:10.870 --> 00:06:12.980
the equilibrium constant
for the third reaction,
00:06:12.980 --> 00:06:15.230
we simply multiply those two together
00:06:15.230 --> 00:06:20.130
and we get that K C is
equal to point one two
00:06:20.130 --> 00:06:23.410
at 25 degrees Celsius.
00:06:23.410 --> 00:06:25.350
So whenever you add reactions together
00:06:25.350 --> 00:06:26.930
to get a new reaction,
00:06:26.930 --> 00:06:29.280
to find the equilibrium
constant for the new reaction,
00:06:29.280 --> 00:06:32.206
you simply need to multiply
the equilibrium constants
00:06:32.206 --> 00:06:34.853
of the reactions that you added together.
|
Magnitude of the equilibrium constant | https://www.youtube.com/watch?v=CoRawW0_Kns | vtt | https://www.youtube.com/api/timedtext?v=CoRawW0_Kns&ei=3lWUZebrOuHfmLAP36SQiAk&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245327&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=1A750087AD6A5ECEC0CC4995D5AB2C8EEB7DF5E0.22F56A9A9415E66422B17517303E07C80DBD6950&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.080 --> 00:00:02.070
- [Instructor] The magnitude
of the equilibrium constant
00:00:02.070 --> 00:00:04.480
tells us the relative amounts of products
00:00:04.480 --> 00:00:06.840
and reactants at equilibrium.
00:00:06.840 --> 00:00:09.270
For example, let's look
at a hypothetical reaction
00:00:09.270 --> 00:00:13.110
where gas A turns into gas B.
00:00:13.110 --> 00:00:14.350
And for the first example,
00:00:14.350 --> 00:00:17.640
let's say that gas A is
represented by a red sphere
00:00:17.640 --> 00:00:20.740
and gas B is represented by a blue sphere.
00:00:20.740 --> 00:00:22.900
And down here, we have
a particulate diagram
00:00:22.900 --> 00:00:26.910
showing an equilibrium mixture
of our hypothetical reaction.
00:00:26.910 --> 00:00:29.160
Let's write the equilibrium
constant expression
00:00:29.160 --> 00:00:31.440
for this hypothetical reaction.
00:00:31.440 --> 00:00:34.310
So we're gonna write Kc is equal to,
00:00:34.310 --> 00:00:36.820
and we think products over reactants.
00:00:36.820 --> 00:00:38.600
So our product is B.
00:00:38.600 --> 00:00:41.520
So this can be the concentration of B.
00:00:41.520 --> 00:00:44.200
And since the coefficient is a
one in the balanced equation,
00:00:44.200 --> 00:00:47.000
it's the concentration of
B raised to the first power
00:00:47.000 --> 00:00:50.530
divided by the concentration
of our reactant, which is A.
00:00:50.530 --> 00:00:52.540
And A in the balanced equation
00:00:52.540 --> 00:00:54.070
also has a coefficient of one.
00:00:54.070 --> 00:00:57.160
So this is the concentration
of A raised to the first power.
00:00:57.160 --> 00:01:00.910
If we assume that each particle
in our particulate diagram
00:01:00.910 --> 00:01:04.510
represents 0.1 moles of a substance,
00:01:04.510 --> 00:01:08.610
and the volume is one liter,
00:01:08.610 --> 00:01:13.160
we can calculate the
concentration of both A and B.
00:01:13.160 --> 00:01:16.950
For example, for B, there
are five blue spheres.
00:01:16.950 --> 00:01:21.360
So that'll be five times
0.1 moles or 0.5 moles.
00:01:21.360 --> 00:01:23.510
So for the concentration of B,
00:01:23.510 --> 00:01:28.510
we have 0.5 moles divided
by a volume of one liter.
00:01:28.650 --> 00:01:32.670
So 0.5 divided by one is 0.5 molar.
00:01:32.670 --> 00:01:34.060
So we can go ahead and plug that in
00:01:34.060 --> 00:01:36.120
for our concentration of B.
00:01:36.120 --> 00:01:38.730
It's 0.5 molar.
00:01:38.730 --> 00:01:41.440
Next, we can do the same thing for A.
00:01:41.440 --> 00:01:44.430
There are also five red spheres.
00:01:44.430 --> 00:01:48.270
And so therefore the concentration
of A is also 0.5 molar.
00:01:48.270 --> 00:01:49.180
So we can plug that
00:01:49.180 --> 00:01:52.240
into our equilibrium constant expression.
00:01:52.240 --> 00:01:54.410
0.5 divided by 0.5 is equal to one.
00:01:54.410 --> 00:01:57.080
So therefore, Kc, the equilibrium constant
00:01:57.080 --> 00:02:00.060
is equal to one at whatever
temperature we have
00:02:00.060 --> 00:02:02.130
for our hypothetical reaction.
00:02:02.130 --> 00:02:05.130
So our equilibrium constant
Kc is equal to one.
00:02:05.130 --> 00:02:08.800
And we saw in our particulate
diagram at equilibrium,
00:02:08.800 --> 00:02:12.170
we have equal amounts of
reactants and products.
00:02:12.170 --> 00:02:13.720
Therefore just by knowing the value
00:02:13.720 --> 00:02:15.530
for the equilibrium constant,
00:02:15.530 --> 00:02:17.757
we know about the relative
amounts of reactants
00:02:17.757 --> 00:02:20.620
and products at equilibrium.
00:02:20.620 --> 00:02:22.680
Let's look at another
hypothetical reaction,
00:02:22.680 --> 00:02:25.990
which also has gas A turning into gas B.
00:02:25.990 --> 00:02:30.310
However, this time gas A
is green and gas B is red.
00:02:30.310 --> 00:02:33.250
And let's calculate the
equilibrium constant Kc
00:02:33.250 --> 00:02:34.570
for this reaction.
00:02:34.570 --> 00:02:36.620
And once again, our particulate diagram
00:02:36.620 --> 00:02:38.970
shows an equilibrium mixture.
00:02:38.970 --> 00:02:40.960
So Kc is equal to the concentration of B
00:02:40.960 --> 00:02:42.917
over the concentration of A.
00:02:42.917 --> 00:02:46.540
And it's a lot faster to
simply count our particles.
00:02:46.540 --> 00:02:50.420
So for B, B is red, we
have one red particle here,
00:02:50.420 --> 00:02:53.400
so we can go ahead and put in one.
00:02:53.400 --> 00:02:57.740
And then for gas A, we
have one, two, three, four,
00:02:57.740 --> 00:03:01.260
five, six, seven, eight,
nine, 10 particles.
00:03:01.260 --> 00:03:04.700
So one divided by 10 is equal to 0.1.
00:03:04.700 --> 00:03:08.530
So Kc is equal to 0.1 for
this hypothetical reaction
00:03:08.530 --> 00:03:10.100
at a certain temperature.
00:03:10.100 --> 00:03:13.120
So the magnitude of the
equilibrium constant tells us
00:03:13.120 --> 00:03:16.840
about the reaction mixture at equilibrium.
00:03:16.840 --> 00:03:19.950
For this reaction, Kc is equal to 0.1.
00:03:19.950 --> 00:03:22.660
So K is less than one.
00:03:22.660 --> 00:03:24.930
And if we think about what that means,
00:03:24.930 --> 00:03:27.320
K is equal to products over reactants.
00:03:27.320 --> 00:03:28.910
So if K is less than one,
00:03:28.910 --> 00:03:32.120
that means we have a smaller
number in the numerator
00:03:32.120 --> 00:03:34.080
and a larger number in the denominator,
00:03:34.080 --> 00:03:37.610
which means there are more
reactants than products
00:03:37.610 --> 00:03:39.530
at equilibrium.
00:03:39.530 --> 00:03:41.520
Let's look at another
hypothetical reaction
00:03:41.520 --> 00:03:43.750
where gas A turns into gas B.
00:03:43.750 --> 00:03:47.370
This time gas A is
yellow and gas B is blue.
00:03:47.370 --> 00:03:49.360
If we look at our particulate diagram,
00:03:49.360 --> 00:03:52.100
showing our reaction
mixture at equilibrium,
00:03:52.100 --> 00:03:57.100
there are 10 blue particles
and only one yellow particle.
00:03:58.240 --> 00:04:02.070
So when plug into our
equilibrium constant expression,
00:04:02.070 --> 00:04:04.980
this time it's going to be 10 over one.
00:04:04.980 --> 00:04:09.460
Therefore the equilibrium
constant Kc is equal to 10
00:04:09.460 --> 00:04:12.920
for this particular reaction
at a certain temperature.
00:04:12.920 --> 00:04:15.410
Once again, the magnitude
of the equilibrium constant
00:04:15.410 --> 00:04:18.270
tells us something about
the reaction mixture
00:04:18.270 --> 00:04:19.730
at equilibrium.
00:04:19.730 --> 00:04:23.260
For this hypothetical
reaction, Kc is equal to 10.
00:04:23.260 --> 00:04:25.830
So K is greater than one.
00:04:25.830 --> 00:04:27.480
And when K is greater than one,
00:04:27.480 --> 00:04:29.720
once again, we have
products over reactants.
00:04:29.720 --> 00:04:33.520
So the numerator must be
larger than the denominator,
00:04:33.520 --> 00:04:35.410
which means we have a lot more products
00:04:35.410 --> 00:04:38.190
than reactants at equilibrium.
00:04:38.190 --> 00:04:40.610
Let's look at the reaction
of carbon monoxide
00:04:40.610 --> 00:04:44.030
and chlorine gas to form phosgene.
00:04:44.030 --> 00:04:46.530
At 100 degrees Celsius,
the equilibrium constant
00:04:46.530 --> 00:04:50.653
for this reaction is 4.56
times 10 to the ninth.
00:04:51.830 --> 00:04:55.460
Since the equilibrium constant
K is greater than one,
00:04:55.460 --> 00:04:57.870
we know there are more
products than reactants
00:04:57.870 --> 00:04:59.310
at equilibrium.
00:04:59.310 --> 00:05:01.410
And with the extremely large value for K,
00:05:01.410 --> 00:05:02.800
like 10 to the ninth,
00:05:02.800 --> 00:05:04.300
we could even assume this reaction
00:05:04.300 --> 00:05:06.610
essentially goes to completion.
00:05:06.610 --> 00:05:09.240
For the reaction of
hydrogen gas and iodine gas
00:05:09.240 --> 00:05:13.010
to form hydrogen iodine,
the equilibrium constant Kc
00:05:13.010 --> 00:05:17.120
is equal to 51 at 448 degrees Celsius.
00:05:17.120 --> 00:05:20.540
Since the equilibrium constant
is relatively close to one.
00:05:20.540 --> 00:05:21.850
This means at equilibrium,
00:05:21.850 --> 00:05:24.920
we have appreciable amounts
of both our reactants
00:05:24.920 --> 00:05:27.010
and our products.
00:05:27.010 --> 00:05:30.010
Let's look at the reaction of
nitrogen gas plus oxygen gas
00:05:30.010 --> 00:05:32.700
plus bromine gas to form NOBr.
00:05:32.700 --> 00:05:36.370
At 298 Kelvin, the equilibrium
constant for this reaction
00:05:36.370 --> 00:05:40.490
is 9.5 times 10 to the negative 31st.
00:05:40.490 --> 00:05:43.960
Since the equilibrium
constant K is less than one,
00:05:43.960 --> 00:05:45.260
we know at equilibrium,
00:05:45.260 --> 00:05:48.200
there are more reactants
than there are products.
00:05:48.200 --> 00:05:50.360
And with an extremely small K value,
00:05:50.360 --> 00:05:53.518
like 9.5 times 10 to the negative 31st,
00:05:53.518 --> 00:05:56.720
this reaction barely proceeds at all.
00:05:56.720 --> 00:05:58.080
So at equilibrium, you're gonna have
00:05:58.080 --> 00:06:00.770
almost all nitrogen, oxygen and bromine
00:06:00.770 --> 00:06:02.833
and very little NOBr.
|
Worked examples: Calculating equilibrium constants | https://www.youtube.com/watch?v=5HZbCNg9mIw | vtt | https://www.youtube.com/api/timedtext?v=5HZbCNg9mIw&ei=31WUZZDdJZKMp-oP4f2aqAE&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245327&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=DE9078EAE7CEBB2691661A8BA48C38A5FAE24381.9D0EB8EBA3AFA45FC0A1B5E48A32FEC34DBD62A4&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.220 --> 00:00:03.200
- [Instructor] An equilibrium
constant can be calculated
00:00:03.200 --> 00:00:06.130
from experimentally
measured concentrations
00:00:06.130 --> 00:00:08.930
or partial pressures of
reactants and products
00:00:08.930 --> 00:00:09.963
at equilibrium.
00:00:10.800 --> 00:00:12.700
As an example, let's look at the reaction
00:00:12.700 --> 00:00:16.040
where N2O4 in the gaseous
state turns into 2NO2
00:00:16.930 --> 00:00:18.820
also in the gaseous state.
00:00:18.820 --> 00:00:20.490
And let's say we do an experiment
00:00:20.490 --> 00:00:23.920
and we allow this reaction
to come to equilibrium
00:00:23.920 --> 00:00:26.888
and the temperature is
100 degrees Celsius.
00:00:26.888 --> 00:00:28.650
And at equilibrium,
00:00:28.650 --> 00:00:33.650
the concentration of NO2 0.017 molar
00:00:33.710 --> 00:00:38.710
and the concentration of
N2O4 is 0.00140 molar.
00:00:40.350 --> 00:00:43.590
To calculate the equilibrium
constant for this reaction
00:00:43.590 --> 00:00:46.210
at 100 degrees Celsius,
we first need to write
00:00:46.210 --> 00:00:48.950
the equilibrium constant expression.
00:00:48.950 --> 00:00:51.170
We can write the equilibrium
constant expression
00:00:51.170 --> 00:00:53.170
by using the balanced equation.
00:00:53.170 --> 00:00:55.410
We start by writing the
equilibrium constant,
00:00:55.410 --> 00:00:57.110
which is symbolized by K.
00:00:57.110 --> 00:00:58.950
And since we're dealing
with concentrations,
00:00:58.950 --> 00:01:00.760
we're calculating Kc.
00:01:00.760 --> 00:01:04.690
And Kc is equal to, we do
products over reactants.
00:01:04.690 --> 00:01:08.740
So this would be the concentration of NO2.
00:01:08.740 --> 00:01:12.490
And since there is a coefficient
of two in front of NO2,
00:01:12.490 --> 00:01:15.994
this is the concentration of
NO2 raised to the second power
00:01:15.994 --> 00:01:19.823
divided by the concentration
of our reactant, N2O4.
00:01:21.650 --> 00:01:24.630
And since there's an implied
one in front of N2O4,
00:01:24.630 --> 00:01:28.530
this is the concentration of
N2O4 raised to the first power.
00:01:28.530 --> 00:01:31.470
Next, we plug in our
equilibrium concentrations.
00:01:31.470 --> 00:01:36.470
So the equilibrium
concentration of NO2 is 0.0172.
00:01:36.770 --> 00:01:38.130
So let's plug that in.
00:01:38.130 --> 00:01:42.463
So this is equal to 0.0172 squared
00:01:45.084 --> 00:01:48.643
divided by the equilibrium
concentration of N2O4,
00:01:49.780 --> 00:01:51.553
which was 0.00140.
00:01:52.750 --> 00:01:54.920
So we plug that in as well.
00:01:54.920 --> 00:01:59.480
So 0.00140.
00:01:59.480 --> 00:02:03.033
When we solve this, we get
that Kc is equal to 0.211,
00:02:05.460 --> 00:02:08.660
and this is at 100 degrees Celsius.
00:02:08.660 --> 00:02:10.960
It's important to always
give the temperature
00:02:10.960 --> 00:02:13.960
when you're giving a value
for an equilibrium constant,
00:02:13.960 --> 00:02:17.110
because an equilibrium
constant is only constant
00:02:17.110 --> 00:02:20.930
for a particular reaction
at a particular temperature.
00:02:20.930 --> 00:02:22.470
And it's also important to note
00:02:22.470 --> 00:02:26.090
that the equilibrium constant
doesn't have any units.
00:02:26.090 --> 00:02:29.850
So we would just say
that Kc is equal to 0.211
00:02:29.850 --> 00:02:34.100
at 100 degrees Celsius for
this particular reaction.
00:02:34.100 --> 00:02:36.080
Let's calculate the equilibrium constant
00:02:36.080 --> 00:02:37.720
for another reaction.
00:02:37.720 --> 00:02:42.000
In this reaction, carbon
dioxide reacts with hydrogen gas
00:02:42.000 --> 00:02:45.410
to produce carbon monoxide and H2O.
00:02:45.410 --> 00:02:47.920
And since everything is
in the gaseous state,
00:02:47.920 --> 00:02:50.960
experimentally, it's easier
to work with partial pressures
00:02:50.960 --> 00:02:53.150
than it is to work with concentrations.
00:02:53.150 --> 00:02:55.490
So instead of calculating Kc,
00:02:55.490 --> 00:02:59.110
we're gonna calculate Kp or
the p stands for pressure.
00:02:59.110 --> 00:03:03.840
So we're trying to find Kp at
500 Kelvin for this reaction.
00:03:03.840 --> 00:03:07.080
To help us find Kp, we're
going to use an ICE table
00:03:07.080 --> 00:03:10.150
where I stands for the
initial partial pressure
00:03:10.150 --> 00:03:12.070
in atmospheres, C stands for the
00:03:12.070 --> 00:03:15.020
change in the partial
pressure, also in atmospheres
00:03:15.020 --> 00:03:18.070
and E is the equilibrium partial pressure.
00:03:18.070 --> 00:03:20.640
Let's say that a mixture
of carbon dioxide,
00:03:20.640 --> 00:03:22.940
hydrogen gas and H2O are placed
00:03:22.940 --> 00:03:25.150
in a previously evacuated flask
00:03:25.150 --> 00:03:29.320
and allowed to come to
equilibrium at 500 Kelvin.
00:03:29.320 --> 00:03:32.510
And let's say the initial
measured partial pressures
00:03:32.510 --> 00:03:36.540
are 4.10 atmospheres for carbon dioxide,
00:03:36.540 --> 00:03:40.160
1.80 atmospheres for hydrogen gas
00:03:40.160 --> 00:03:44.090
and 3.20 atmospheres for H2O.
00:03:44.090 --> 00:03:46.420
And since we didn't
add any carbon monoxide
00:03:46.420 --> 00:03:48.320
in the beginning, the
initial partial pressure
00:03:48.320 --> 00:03:49.888
of that would be zero.
00:03:49.888 --> 00:03:52.850
And after the reaction
comes to equilibrium,
00:03:52.850 --> 00:03:55.440
we measure the partial pressure of H2O
00:03:55.440 --> 00:03:58.440
to be 3.40 atmospheres.
00:03:58.440 --> 00:04:01.885
So that's why we have 3.40
in the equilibrium parts
00:04:01.885 --> 00:04:04.780
on the ICE table under H2O.
00:04:04.780 --> 00:04:09.150
So the initial partial pressure
of H2O is 3.20 atmospheres
00:04:09.150 --> 00:04:13.370
and the equilibrium
partial pressure is 3.40.
00:04:13.370 --> 00:04:16.790
So H2O has increased in partial pressure.
00:04:16.790 --> 00:04:19.080
We can go ahead in here and write plus X
00:04:19.080 --> 00:04:21.750
for an increase in the
partial pressure of H2O
00:04:21.750 --> 00:04:26.750
and 3.20 plus X must be equal to 3.40.
00:04:28.920 --> 00:04:33.080
So X is equal to 0.20.
00:04:33.080 --> 00:04:37.050
So the partial pressure of
water increased by 0.20.
00:04:37.050 --> 00:04:40.115
And we could either write plus
X in here on our ICE table,
00:04:40.115 --> 00:04:43.193
or we could just write plus 0.20.
00:04:45.290 --> 00:04:47.710
Now that we know that change
in the partial pressure
00:04:47.710 --> 00:04:50.900
for H2O, we can use this information
00:04:50.900 --> 00:04:53.350
to fill out the rest of our ICE table.
00:04:53.350 --> 00:04:56.270
For example, the mole
ratio of carbon monoxide
00:04:56.270 --> 00:04:58.970
to H2O is 1:1.
00:04:58.970 --> 00:05:02.810
So if we gained plus 0.20 for H2O,
00:05:02.810 --> 00:05:07.810
we're also gonna gain plus
0.20 for carbon monoxide.
00:05:08.010 --> 00:05:10.120
And if we're gaining for
our two products here,
00:05:10.120 --> 00:05:12.410
the net reaction is moving to the right
00:05:12.410 --> 00:05:14.270
to increase the amount of products,
00:05:14.270 --> 00:05:16.990
which means we're losing reactants.
00:05:16.990 --> 00:05:19.460
And we can figure out
by how much by looking
00:05:19.460 --> 00:05:21.340
at the mole ratios again.
00:05:21.340 --> 00:05:22.900
So for both of our reactants,
00:05:22.900 --> 00:05:26.460
we have ones as coefficients
in the balanced equation.
00:05:26.460 --> 00:05:29.310
So if it's plus X for
both of our products,
00:05:29.310 --> 00:05:32.400
it must be minus X for
both of our reactants.
00:05:32.400 --> 00:05:36.877
And since X is 0.20, it'd be minus 0.20
00:05:38.000 --> 00:05:39.960
for the change in the partial pressure
00:05:39.960 --> 00:05:42.143
for both of our reactants.
00:05:43.250 --> 00:05:46.830
Therefore the equilibrium partial
pressure of carbon dioxide
00:05:46.830 --> 00:05:51.670
would be 4.10 minus 0.20, which is 3.90
00:05:53.720 --> 00:05:58.720
and for H2, it'd be 1.80
minus 0.20, which is 1.60.
00:06:00.750 --> 00:06:03.650
And for carbon monoxide,
we started off with zero
00:06:03.650 --> 00:06:06.260
and we gained positive 0.20.
00:06:06.260 --> 00:06:11.020
Therefore the equilibrium
partial pressure is 0.20.
00:06:11.020 --> 00:06:13.900
So as the net reaction moved to the right,
00:06:13.900 --> 00:06:16.140
we lost some of our reactants
00:06:16.140 --> 00:06:18.300
and we gained some of our products
00:06:18.300 --> 00:06:20.870
until the reaction reached equilibrium
00:06:20.870 --> 00:06:23.920
and we got our equilibrium
partial pressures.
00:06:23.920 --> 00:06:27.310
In our equilibrium, the
rate of the forward reaction
00:06:28.410 --> 00:06:30.300
is equal to the rate
of the reverse reaction
00:06:30.300 --> 00:06:33.040
and therefore these
equilibrium partial pressures
00:06:33.040 --> 00:06:35.130
remain constant.
00:06:35.130 --> 00:06:37.470
Now that we know our
equilibrium partial pressures,
00:06:37.470 --> 00:06:41.040
we're ready to calculate
the equilibrium constant Kp.
00:06:41.040 --> 00:06:43.900
So we need to write an
equilibrium constant expression.
00:06:43.900 --> 00:06:48.460
So Kp is equal to, we think
about products over reactants.
00:06:48.460 --> 00:06:49.820
And for our products,
00:06:49.820 --> 00:06:53.270
we would have the partial
pressure of carbon monoxide.
00:06:53.270 --> 00:06:56.100
And since the coefficient is a one
00:06:56.100 --> 00:06:59.010
in front of carbon monoxide
in the balanced equation,
00:06:59.010 --> 00:07:01.410
it would be the partial
pressure of carbon monoxide
00:07:01.410 --> 00:07:04.530
raised to the first power
times the partial pressure
00:07:04.530 --> 00:07:07.440
of our other product, which is H2O.
00:07:07.440 --> 00:07:09.830
And once again, the coefficient is a one.
00:07:09.830 --> 00:07:13.300
So that's the partial pressure
raised to the first power.
00:07:13.300 --> 00:07:15.470
All of this is divided by,
00:07:15.470 --> 00:07:17.300
we think about our reactants next,
00:07:17.300 --> 00:07:19.270
and they both have coefficients of one
00:07:19.270 --> 00:07:20.770
in the balanced equation.
00:07:20.770 --> 00:07:24.940
So it would be the partial
pressure of carbon dioxide
00:07:24.940 --> 00:07:29.940
times the partial
pressure of hydrogen gas.
00:07:30.780 --> 00:07:34.090
The partial pressures in our
equilibrium constant expression
00:07:34.090 --> 00:07:36.370
are the equilibrium partial pressures,
00:07:36.370 --> 00:07:38.266
which we can get from the ICE table.
00:07:38.266 --> 00:07:41.590
So the equilibrium partial
pressure of carbon monoxide
00:07:41.590 --> 00:07:46.590
is 0.20, the equilibrium
partial pressure of H2O is 3.40.
00:07:48.070 --> 00:07:50.270
We can plug in the
equilibrium partial pressures
00:07:50.270 --> 00:07:53.369
for carbon dioxide and the
equilibrium partial pressure
00:07:53.369 --> 00:07:56.030
for hydrogen gas as well.
00:07:56.030 --> 00:07:58.240
And here we have the
equilibrium partial pressures
00:07:58.240 --> 00:08:01.230
plugged into our equilibrium
constant expression.
00:08:01.230 --> 00:08:02.600
And when we solve this,
00:08:02.600 --> 00:08:06.767
we get that Kp is equal
to 0.11 at 500 Kelvin.
|
Writing equilibrium constant and reaction quotient expressions | https://www.youtube.com/watch?v=lG8tCeNzEjY | vtt | https://www.youtube.com/api/timedtext?v=lG8tCeNzEjY&ei=31WUZYyNJYfJp-oPqbyDmAY&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245327&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=43C03C9C8D2646EC1415AAD583E00499A68E4DC4.A5FDFE90604ADB32B126029C78DEA716A586B308&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.480 --> 00:00:02.820
- [Instructor] The equilibrium
constant is symbolized
00:00:02.820 --> 00:00:07.410
by the letter K, and
equilibrium constant tells us
00:00:07.410 --> 00:00:10.110
about the relative
concentrations of reactants
00:00:10.110 --> 00:00:12.590
and products at equilibrium.
00:00:12.590 --> 00:00:14.822
Let's say we have a hypothetical reaction
00:00:14.822 --> 00:00:19.822
where reactants A and B
turn into products C and D.
00:00:20.070 --> 00:00:21.510
And in the balanced equation,
00:00:21.510 --> 00:00:23.840
the lowercase letters
are the coefficients.
00:00:23.840 --> 00:00:26.380
So we have a lowercase a, a lowercase b,
00:00:26.380 --> 00:00:29.230
lowercase c and lowercase
d as coefficients
00:00:29.230 --> 00:00:31.020
in our balanced equation.
00:00:31.020 --> 00:00:33.530
If we were to write an
equilibrium constant expression
00:00:33.530 --> 00:00:35.420
for this hypothetical reaction,
00:00:35.420 --> 00:00:37.700
we'd start by writing the
equilibrium constant K
00:00:37.700 --> 00:00:39.760
and then we have a subscript c here
00:00:39.760 --> 00:00:41.670
because we're dealing with concentrations
00:00:41.670 --> 00:00:43.930
in our equilibrium constant expression.
00:00:43.930 --> 00:00:47.330
And the equilibrium
constant Kc is equal to,
00:00:47.330 --> 00:00:51.180
and in the numerator, we
have the concentrations
00:00:51.180 --> 00:00:53.420
of our two products multiplied together.
00:00:53.420 --> 00:00:55.200
And the concentration of each product
00:00:55.200 --> 00:00:58.810
is raised to the power of the coefficient.
00:00:58.810 --> 00:00:59.940
In the denominator,
00:00:59.940 --> 00:01:03.260
we have the concentrations
of the two reactants
00:01:03.260 --> 00:01:06.720
multiplied by each other
and raised to the power,
00:01:06.720 --> 00:01:08.400
each concentration is raised to the power
00:01:08.400 --> 00:01:11.220
of the coefficient in
the balanced equation.
00:01:11.220 --> 00:01:13.351
It's important to emphasize
that the concentrations
00:01:13.351 --> 00:01:14.184
that we're plugging
00:01:14.184 --> 00:01:16.730
into our equilibrium constant expression
00:01:16.730 --> 00:01:19.550
are equilibrium concentrations.
00:01:19.550 --> 00:01:22.020
And when we plug in our
equilibrium concentrations
00:01:22.020 --> 00:01:24.430
into our equilibrium constant expression,
00:01:24.430 --> 00:01:27.800
we get a value for the
equilibrium constant K.
00:01:27.800 --> 00:01:30.960
And K is constant for
a particular reaction
00:01:30.960 --> 00:01:32.940
at a certain temperature.
00:01:32.940 --> 00:01:35.360
Let's write an equilibrium
constant expression
00:01:35.360 --> 00:01:36.890
for the following reaction,
00:01:36.890 --> 00:01:39.450
which shows the synthesis of ammonia
00:01:39.450 --> 00:01:41.910
from nitrogen and hydrogen,
00:01:41.910 --> 00:01:43.940
and everything is in the gaseous state.
00:01:43.940 --> 00:01:46.910
We start by writing the
equilibrium constant Kc,
00:01:46.910 --> 00:01:49.180
c because we're dealing
with concentrations,
00:01:49.180 --> 00:01:51.700
and we start with our
product, which is ammonia.
00:01:51.700 --> 00:01:55.340
So we write the concentration of ammonia
00:01:55.340 --> 00:01:58.490
and we raise the concentration of ammonia
00:01:58.490 --> 00:02:00.370
to the power of the coefficient
00:02:00.370 --> 00:02:02.400
in the balanced equation, which is a two.
00:02:02.400 --> 00:02:06.600
So this is the concentration
of ammonia to the second power.
00:02:06.600 --> 00:02:10.150
Then, in the denominator, we
think about our reactants.
00:02:10.150 --> 00:02:11.730
So we have nitrogen.
00:02:11.730 --> 00:02:14.620
So we write the concentration of nitrogen.
00:02:14.620 --> 00:02:17.620
And since the coefficient is a
one in the balanced equation,
00:02:17.620 --> 00:02:20.700
that'd be the concentration
of nitrogen to the first power
00:02:20.700 --> 00:02:23.540
multiplied by the concentration
of our other reactants,
00:02:23.540 --> 00:02:24.880
which is hydrogens.
00:02:24.880 --> 00:02:26.650
We write in here H2.
00:02:26.650 --> 00:02:28.500
And because there's a coefficient of three
00:02:28.500 --> 00:02:29.910
in the balanced equation,
00:02:29.910 --> 00:02:34.140
we raise the concentration of
hydrogen to the third power.
00:02:34.140 --> 00:02:35.940
For gases, it's often more convenient
00:02:35.940 --> 00:02:37.820
to measure partial pressures
00:02:37.820 --> 00:02:40.340
instead of measuring concentrations.
00:02:40.340 --> 00:02:44.750
So let's say that A, B,
C and D are all gases.
00:02:44.750 --> 00:02:47.780
We could write an equilibrium
constant expression
00:02:47.780 --> 00:02:52.260
using partial pressures
instead of concentrations.
00:02:52.260 --> 00:02:54.720
And if we did that, instead of writing Kc,
00:02:54.720 --> 00:02:58.290
we would write Kp where
p stands for pressure.
00:02:58.290 --> 00:03:03.200
And Kc and Kp usually have
different values from each other.
00:03:03.200 --> 00:03:05.560
So if we go back to our previous reaction
00:03:05.560 --> 00:03:07.580
where everything was in the gaseous state,
00:03:07.580 --> 00:03:10.020
we could write a Kp expression.
00:03:10.020 --> 00:03:13.130
So we would write Kp is equal to,
00:03:13.130 --> 00:03:15.540
we think about products over reactants.
00:03:15.540 --> 00:03:19.020
So this would be the partial
pressure of our product,
00:03:19.020 --> 00:03:23.770
ammonia, raised to the second power
00:03:23.770 --> 00:03:27.600
divided by the partial
pressure of nitrogen
00:03:27.600 --> 00:03:32.000
raised to the first power
times the partial pressure
00:03:32.000 --> 00:03:37.000
of hydrogen raised to the third power.
00:03:37.620 --> 00:03:39.360
For the synthesis of ammonia,
00:03:39.360 --> 00:03:41.650
everything was in the gaseous state.
00:03:41.650 --> 00:03:44.660
And when all substances,
reactants and products
00:03:44.660 --> 00:03:46.390
are in the same phase,
00:03:46.390 --> 00:03:50.460
we call this a homogeneous equilibrium.
00:03:50.460 --> 00:03:52.850
When the substances are
in different phases,
00:03:52.850 --> 00:03:56.630
we call it a heterogeneous equilibrium.
00:03:56.630 --> 00:03:59.860
For example, in the decomposition
of calcium carbonate
00:03:59.860 --> 00:04:03.060
to turn into calcium
oxide and carbon dioxide,
00:04:03.060 --> 00:04:07.450
calcium carbonate is a solid
and calcium oxide is a solid,
00:04:07.450 --> 00:04:09.210
but carbon dioxide is a gas.
00:04:09.210 --> 00:04:12.910
So we have substances in different phases.
00:04:12.910 --> 00:04:15.310
When we write an equilibrium
constant expression
00:04:15.310 --> 00:04:18.090
for a heterogeneous equilibrium,
00:04:18.090 --> 00:04:20.980
we leave pure solids and pure liquids
00:04:20.980 --> 00:04:23.740
out of the equilibrium
constant expression.
00:04:23.740 --> 00:04:26.160
So if we write an equilibrium
constant expression
00:04:26.160 --> 00:04:28.850
for the decomposition
of calcium carbonate,
00:04:28.850 --> 00:04:31.350
let's write a Kc expression first here.
00:04:31.350 --> 00:04:33.620
So we write Kc is equal to,
00:04:33.620 --> 00:04:36.850
and we think about
products over reactants.
00:04:36.850 --> 00:04:40.030
For products, we have carbon
dioxide in the gaseous state.
00:04:40.030 --> 00:04:41.670
So it's okay to include that
00:04:41.670 --> 00:04:43.710
in our equilibrium constant expression.
00:04:43.710 --> 00:04:46.880
So we write the concentration of CO2.
00:04:46.880 --> 00:04:49.560
And since the coefficient is a
one in the balanced equation,
00:04:49.560 --> 00:04:51.400
this would be the concentration of CO2
00:04:51.400 --> 00:04:53.280
raised to the first power.
00:04:53.280 --> 00:04:55.090
Our other products is a solid.
00:04:55.090 --> 00:04:56.150
So we're gonna leave that
00:04:56.150 --> 00:04:59.450
out of our equilibrium
constant expression.
00:04:59.450 --> 00:05:03.510
And for our reactant calcium
carbonate, that's also a solid,
00:05:03.510 --> 00:05:06.600
so that's also left out of our expression.
00:05:06.600 --> 00:05:09.670
If we were to write a Kp expression here,
00:05:09.670 --> 00:05:12.640
we would include the
partial pressure of our gas,
00:05:12.640 --> 00:05:14.180
which is carbon dioxide.
00:05:14.180 --> 00:05:16.470
So this would be the partial
pressure of carbon dioxide
00:05:16.470 --> 00:05:17.720
to the first power.
00:05:17.720 --> 00:05:19.920
And once again, we would
leave the two solids
00:05:19.920 --> 00:05:23.600
out of our equilibrium
constant expression.
00:05:23.600 --> 00:05:25.200
The reason why we leave pure solids
00:05:25.200 --> 00:05:28.150
and pure liquids out of
equilibrium constant expressions
00:05:28.150 --> 00:05:31.690
for heterogeneous equilibria
is because the concentration
00:05:31.690 --> 00:05:35.930
of a pure solid or a pure liquid
remains constant over time.
00:05:35.930 --> 00:05:38.120
So it doesn't help us to include it
00:05:38.120 --> 00:05:40.530
in our equilibrium expression.
00:05:40.530 --> 00:05:43.420
Finally, let's talk about
the reaction quotient,
00:05:43.420 --> 00:05:46.680
which is symbolized by the letter Q.
00:05:46.680 --> 00:05:48.560
A Q expression has the same form
00:05:48.560 --> 00:05:50.800
as an equilibrium constant expression.
00:05:50.800 --> 00:05:54.120
And Q tells us the relative
concentrations of reactants
00:05:54.120 --> 00:05:57.950
and products at any moment in time.
00:05:57.950 --> 00:06:02.290
And just like we could write
a Kc or a Kp expression,
00:06:02.290 --> 00:06:05.960
we could write a Qc or a Qp expression.
00:06:05.960 --> 00:06:09.940
Let's go back to our reaction
for the synthesis of ammonia
00:06:09.940 --> 00:06:12.880
from nitrogen gas and hydrogen gas.
00:06:12.880 --> 00:06:16.410
Notice how the Qc
expression has the same form
00:06:16.410 --> 00:06:18.660
as the Kc expression.
00:06:18.660 --> 00:06:21.560
The difference is, for the Kc expression,
00:06:21.560 --> 00:06:25.430
all of our concentrations are
equilibrium concentrations.
00:06:25.430 --> 00:06:27.500
So I could put an eq here
00:06:27.500 --> 00:06:32.233
for the concentrations of
ammonia, nitrogen, and hydrogen.
00:06:33.170 --> 00:06:34.780
So for the Kc expression,
00:06:34.780 --> 00:06:37.240
it's only equilibrium concentrations,
00:06:37.240 --> 00:06:39.430
but for the Qc expression,
00:06:39.430 --> 00:06:42.850
it's the concentrations
at any moment in time.
00:06:42.850 --> 00:06:46.150
So that moment in time
might be at equilibrium
00:06:46.150 --> 00:06:49.630
or it might not be at equilibrium.
00:06:49.630 --> 00:06:54.450
If Qc is equal to KC, the
reaction is at equilibrium,
00:06:54.450 --> 00:06:59.450
but if Qc is greater than
Kc, or if Qc is less than Kc,
00:06:59.600 --> 00:07:02.233
the reaction is not at equilibrium.
|
Direction of reversible reactions | https://www.youtube.com/watch?v=9u914ckHlUI | vtt | https://www.youtube.com/api/timedtext?v=9u914ckHlUI&ei=31WUZffzJPeEp-oPs7yGsAc&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245327&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=5B1E85FBBFCBCCC900633569A33CA8E30A97E713.E3D9CF988F838BC91986ECBD7535B51945F38134&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.190 --> 00:00:02.660
- [Instructor] As an example
of a reversible reaction,
00:00:02.660 --> 00:00:04.900
let's look at the hypothetical reaction
00:00:04.900 --> 00:00:09.900
where diatomic gas X2 turns
into its individual atoms X,
00:00:10.050 --> 00:00:11.340
and it would turn into two of them.
00:00:11.340 --> 00:00:13.650
So X2 goes to 2X.
00:00:13.650 --> 00:00:18.160
The forward reaction
is X2 turning into 2X.
00:00:18.160 --> 00:00:23.160
And the reverse reaction
is 2X combining to form X2.
00:00:23.210 --> 00:00:26.930
And let's say the X2
is a reddish brown gas.
00:00:26.930 --> 00:00:30.850
If we assume that both the
forward and the reverse reactions
00:00:30.850 --> 00:00:32.690
are elementary reactions,
00:00:32.690 --> 00:00:34.570
we can actually write the rate law
00:00:34.570 --> 00:00:36.350
from the balanced equation.
00:00:36.350 --> 00:00:38.330
So for the forward reaction,
00:00:38.330 --> 00:00:41.680
let's go ahead and write the
rate of the forward reaction
00:00:41.680 --> 00:00:45.320
is equal to the rate constant
for the forward reaction,
00:00:45.320 --> 00:00:49.340
which we will symbolize
as K with the subscript F,
00:00:49.340 --> 00:00:51.560
times the concentration of,
00:00:51.560 --> 00:00:53.880
if we're going in the forward direction,
00:00:53.880 --> 00:00:56.190
the reactants would be X2.
00:00:56.190 --> 00:00:59.490
So times the concentration of X2.
00:00:59.490 --> 00:01:02.930
And since we have a coefficient
of 1 in front of X2,
00:01:02.930 --> 00:01:04.313
for this elementary reaction,
00:01:04.313 --> 00:01:07.083
this would be raised to the first power.
00:01:07.940 --> 00:01:11.090
Next we can write the rate
law for the reverse reaction.
00:01:11.090 --> 00:01:13.320
So the rate of the reverse reaction
00:01:13.320 --> 00:01:15.040
is equal to the rate constant,
00:01:15.040 --> 00:01:17.300
and we'll put in a subscript R here.
00:01:17.300 --> 00:01:19.840
So that's the rate constant
for the reverse reaction.
00:01:19.840 --> 00:01:24.710
And in the reverse reaction,
2X combines to form X2.
00:01:24.710 --> 00:01:28.190
So this would be times
the concentration of X.
00:01:28.190 --> 00:01:30.870
And since we have a
two as our coefficient,
00:01:30.870 --> 00:01:34.743
we need to raise the concentration
of X to the second power.
00:01:35.980 --> 00:01:38.130
Next, let's look at these
particulate diagrams
00:01:38.130 --> 00:01:41.520
and think about what happens
for the forward reaction.
00:01:41.520 --> 00:01:43.210
So we start at time is equal to zero,
00:01:43.210 --> 00:01:45.060
and we start with only X2.
00:01:45.060 --> 00:01:47.680
So here are five particles of X2.
00:01:47.680 --> 00:01:49.130
If we wait 10 seconds,
00:01:49.130 --> 00:01:51.260
now we've gone from five particles of X2
00:01:51.260 --> 00:01:54.120
to only three particles of X2.
00:01:54.120 --> 00:01:57.010
So overall, two of those particles of X2
00:01:57.010 --> 00:01:58.720
have turned into X.
00:01:58.720 --> 00:02:01.180
And so there are four particles of X
00:02:01.180 --> 00:02:03.480
in this second particular diagram.
00:02:03.480 --> 00:02:04.990
We wait another 10 seconds
00:02:04.990 --> 00:02:07.120
for a total of time is
equal to 20 seconds.
00:02:07.120 --> 00:02:09.980
And we've gone from three particles of X2
00:02:09.980 --> 00:02:13.240
to only two particles of X2,
00:02:13.240 --> 00:02:16.050
and we've increased in the particles of X.
00:02:16.050 --> 00:02:19.650
So now we're up to six particles of X.
00:02:19.650 --> 00:02:22.650
So the concentration of X2 has decreased.
00:02:22.650 --> 00:02:27.650
We went from five particles
of X2 to three particles of X2
00:02:28.220 --> 00:02:30.530
to only two particles of X2.
00:02:30.530 --> 00:02:34.240
And if we look at the rate
law for the forward reaction,
00:02:34.240 --> 00:02:37.500
the rate of the forward
reaction is proportional
00:02:37.500 --> 00:02:40.470
to the concentration of X2.
00:02:40.470 --> 00:02:43.760
So if the concentration of X2 decreases,
00:02:43.760 --> 00:02:48.450
the rate of the forward
reaction also decreases.
00:02:48.450 --> 00:02:49.810
We can see the same concept
00:02:49.810 --> 00:02:53.560
if we look at a graph of rate versus time.
00:02:53.560 --> 00:02:56.100
So if we look at this line right here,
00:02:56.100 --> 00:02:59.250
we're starting on a certain
rate for the forward reaction.
00:02:59.250 --> 00:03:01.730
And as the concentration of X2 decreases,
00:03:01.730 --> 00:03:04.760
we can see the rate of
the reaction decrease.
00:03:04.760 --> 00:03:07.130
So the rate of the
reaction stops decreasing
00:03:07.130 --> 00:03:10.430
when we get to time is
equal to 20 seconds.
00:03:10.430 --> 00:03:13.960
Next, let's think about the
rate of the reverse reaction.
00:03:13.960 --> 00:03:15.850
Well, when time is equal to zero,
00:03:15.850 --> 00:03:18.450
the rate of the reverse reaction is zero.
00:03:18.450 --> 00:03:21.410
And that's because when we
start out, we have only X2,
00:03:21.410 --> 00:03:23.330
we don't have any X present.
00:03:23.330 --> 00:03:25.760
So the reverse reaction doesn't happen.
00:03:25.760 --> 00:03:28.430
But as soon as some of
that X2 turns into X,
00:03:28.430 --> 00:03:31.400
it's possible for the
reverse reaction to happen.
00:03:31.400 --> 00:03:34.310
And as we increase in the amount of X,
00:03:34.310 --> 00:03:37.444
and we look at our rate law
here for the reverse reaction,
00:03:37.444 --> 00:03:40.590
as we increase in the concentration of X,
00:03:40.590 --> 00:03:44.530
the rate of the reverse reaction
should increase as well.
00:03:44.530 --> 00:03:46.120
And so that's why we see,
00:03:46.120 --> 00:03:49.550
that's why we see the rate of
the reverse reaction increase
00:03:49.550 --> 00:03:52.220
as time increases.
00:03:52.220 --> 00:03:54.760
So as the forward reaction is happening,
00:03:54.760 --> 00:03:59.490
the reverse reaction is also
occurring at the same time.
00:03:59.490 --> 00:04:00.820
However, we don't really see that
00:04:00.820 --> 00:04:03.120
when we look at our particular diagram.
00:04:03.120 --> 00:04:04.410
In our particular diagrams,
00:04:04.410 --> 00:04:07.520
we see a net conversion of X2 into 2X,
00:04:07.520 --> 00:04:10.030
for example, looking from
the first particular diagram
00:04:10.030 --> 00:04:11.410
to the second,
00:04:11.410 --> 00:04:13.950
we see that two particles of X2
00:04:13.950 --> 00:04:17.130
have turned into four particles of X.
00:04:17.130 --> 00:04:20.600
And going from the second
diagram to the third diagram,
00:04:20.600 --> 00:04:23.170
we see that another particle of X2
00:04:23.170 --> 00:04:24.700
has turned into 2X.
00:04:24.700 --> 00:04:27.860
And therefore we have six particles of X
00:04:27.860 --> 00:04:30.780
at time is equal to 20 seconds.
00:04:30.780 --> 00:04:34.050
So since we see a net conversion
of reactants to products
00:04:34.050 --> 00:04:35.770
in our particular diagram,
00:04:35.770 --> 00:04:38.840
the rate of the forward
reaction must be greater
00:04:38.840 --> 00:04:41.250
than the rate of the reverse reaction.
00:04:41.250 --> 00:04:42.490
And we can see that.
00:04:42.490 --> 00:04:46.460
So before time is equal
to 20 seconds here,
00:04:46.460 --> 00:04:48.720
if we look at our rates, let's just pick,
00:04:48.720 --> 00:04:51.391
for example, time is equal to 10 seconds,
00:04:51.391 --> 00:04:53.140
for the forward reaction,
00:04:53.140 --> 00:04:57.473
there's a higher rate than
for the reverse reaction.
00:04:58.683 --> 00:05:00.428
So at times equal to 20 seconds,
00:05:00.428 --> 00:05:03.030
the rate of the forward reaction
00:05:03.030 --> 00:05:06.480
becomes equal to the rate
of the reverse reaction.
00:05:06.480 --> 00:05:09.070
So here's the line on our graph,
00:05:09.070 --> 00:05:11.010
where the rates become equal,
00:05:11.010 --> 00:05:14.480
and also notice the rates
become constant at this point.
00:05:14.480 --> 00:05:16.520
And when the rate of the forward reaction
00:05:16.520 --> 00:05:19.070
is equal to the rate of
the reverse reaction,
00:05:19.070 --> 00:05:21.220
the reaction has reached equilibrium.
00:05:21.220 --> 00:05:23.330
So to the right of the dotted line,
00:05:23.330 --> 00:05:25.830
the reaction is at equilibrium.
00:05:25.830 --> 00:05:27.780
And to the left of the dotted line,
00:05:27.780 --> 00:05:31.573
the reaction is not at equilibrium.
00:05:34.210 --> 00:05:36.550
And since the rate of the forward reaction
00:05:36.550 --> 00:05:39.983
is equal to the rate of the
reverse reaction at equilibrium,
00:05:39.983 --> 00:05:41.900
X2 is turning into 2X
00:05:41.900 --> 00:05:45.180
at the same rate that 2X
is turning back into X2.
00:05:45.180 --> 00:05:47.690
Therefore, the concentrations of X2
00:05:47.690 --> 00:05:50.480
and X at equilibrium remain constant.
00:05:50.480 --> 00:05:53.260
And we can see that when we
look at the particular diagrams
00:05:53.260 --> 00:05:54.710
where time is equal to 20 seconds,
00:05:54.710 --> 00:05:56.780
and time is equal to 30 seconds.
00:05:56.780 --> 00:06:01.780
So both of these particular
diagrams have two X2 particles
00:06:01.960 --> 00:06:05.733
and six X particles.
00:06:06.660 --> 00:06:09.530
Let's look at a summary of
what the rates of the forward
00:06:09.530 --> 00:06:11.110
and reverse reaction mean
00:06:11.110 --> 00:06:13.590
in terms of reactants and products.
00:06:13.590 --> 00:06:16.280
If the rate of the forward reaction
00:06:16.280 --> 00:06:19.450
is greater than the rate
of the reverse reaction,
00:06:19.450 --> 00:06:21.290
that means there's a net conversion
00:06:21.290 --> 00:06:23.170
of reactants to products.
00:06:23.170 --> 00:06:25.070
So therefore over time,
00:06:25.070 --> 00:06:26.970
the amount of reactants would decrease
00:06:26.970 --> 00:06:29.193
and the amount of products would increase.
00:06:30.040 --> 00:06:32.880
Eventually, the rate
of the forward reaction
00:06:32.880 --> 00:06:36.200
becomes equal to the rate
of the reverse reaction.
00:06:36.200 --> 00:06:38.860
And that means the
reaction is at equilibrium
00:06:38.860 --> 00:06:40.430
and there's no net change
00:06:40.430 --> 00:06:42.820
in the amounts of reactants or products.
00:06:42.820 --> 00:06:45.640
So reactants are turning into
products at the same rate
00:06:45.640 --> 00:06:48.850
the products are turning
back into reactants.
00:06:48.850 --> 00:06:51.610
And then finally, if the
rate of the reverse reaction
00:06:51.610 --> 00:06:54.710
is greater than the rate
of the forward reaction,
00:06:54.710 --> 00:06:57.430
there's a net conversion
of products to reactants.
00:06:57.430 --> 00:07:00.890
So products are turning into reactants
00:07:00.890 --> 00:07:04.150
faster than reactants are
turning into products.
00:07:04.150 --> 00:07:06.240
And the example that we looked at,
00:07:06.240 --> 00:07:08.270
the rate of the forward reaction
00:07:08.270 --> 00:07:10.910
was greater than the rate
of the reverse reaction.
00:07:10.910 --> 00:07:12.770
And eventually the rates became equal
00:07:12.770 --> 00:07:15.100
and the reaction reached equilibrium.
00:07:15.100 --> 00:07:17.750
If we had looked at an example
of this third case here
00:07:17.750 --> 00:07:19.920
where the rate of the
reverse reaction is greater
00:07:19.920 --> 00:07:22.300
than the rate of the forward reaction,
00:07:22.300 --> 00:07:24.530
eventually the two
rates would become equal
00:07:24.530 --> 00:07:27.393
and this reaction would
reach equilibrium too.
|
Dynamic equilibrium | https://www.youtube.com/watch?v=zaHM74k9Z1w | vtt | https://www.youtube.com/api/timedtext?v=zaHM74k9Z1w&ei=31WUZeaEJb6KvdIPt8CEiAU&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245327&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=3CCB73775B4EF75DDFE273229F68300FBC509DF2.98CE9C9AA92D30DC1644D3E2C76AB3A3E3A1ECAA&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.650 --> 00:00:02.940
- [Instructor] To illustrate
the concept of equilibrium,
00:00:02.940 --> 00:00:04.970
let's say that we have a beaker
00:00:04.970 --> 00:00:08.840
and we put some water into our beaker.
00:00:08.840 --> 00:00:13.840
And also we make sure that
our beaker has a lid on it.
00:00:14.220 --> 00:00:17.210
Some of those water molecules
are going to evaporate
00:00:17.210 --> 00:00:19.160
and turn into a gas.
00:00:19.160 --> 00:00:22.050
And eventually once we
have enough gaseous water,
00:00:22.050 --> 00:00:24.650
some of the gaseous water
is going to condense
00:00:24.650 --> 00:00:27.610
and turn back into liquid water.
00:00:27.610 --> 00:00:29.250
To represent these two processes,
00:00:29.250 --> 00:00:31.120
we can show liquid water on the left
00:00:31.120 --> 00:00:33.370
and gaseous water on the right.
00:00:33.370 --> 00:00:35.220
So in the forward process,
00:00:35.220 --> 00:00:37.630
liquid water turns into gaseous water.
00:00:37.630 --> 00:00:39.460
And this forward arrow here
00:00:39.460 --> 00:00:42.490
represents the process of vaporization.
00:00:42.490 --> 00:00:45.490
And when gaseous water turns
back into liquid water,
00:00:45.490 --> 00:00:47.930
that's represented by this
arrow here on the bottom,
00:00:47.930 --> 00:00:51.240
and so that's the process of condensation.
00:00:51.240 --> 00:00:53.430
Since we start with liquid water,
00:00:53.430 --> 00:00:55.960
at first, the rate of vaporization
00:00:55.960 --> 00:00:59.100
is greater than the rate of condensation.
00:00:59.100 --> 00:01:01.860
But eventually we reach
a point where the rate of
00:01:01.860 --> 00:01:05.800
vaporization is equal to
the rate of condensation.
00:01:05.800 --> 00:01:09.340
And when that happens, if
you're turning liquid water
00:01:09.340 --> 00:01:11.470
into gaseous water at the same rate,
00:01:11.470 --> 00:01:14.890
you're turning gaseous water
back into liquid water,
00:01:14.890 --> 00:01:18.330
the number of water molecules
in a liquid and gaseous state
00:01:18.330 --> 00:01:20.420
would remain constant.
00:01:20.420 --> 00:01:23.570
So when the rate of vaporization
is equal to the rate of
00:01:23.570 --> 00:01:27.700
condensation, we've reached
a state of equilibrium.
00:01:27.700 --> 00:01:31.720
And this is a dynamic equilibrium
because if we zoom in and
00:01:31.720 --> 00:01:35.170
we look at this, water
molecules are being converted
00:01:35.170 --> 00:01:38.220
from the liquid state to the
gaseous state all the time
00:01:38.220 --> 00:01:40.970
and molecules are going from
the gaseous state back to the
00:01:40.970 --> 00:01:42.190
liquid state all the time.
00:01:42.190 --> 00:01:44.890
However, since the rates are equal,
00:01:44.890 --> 00:01:46.670
the number of molecules in the liquid
00:01:46.670 --> 00:01:48.660
and gaseous state remained constant.
00:01:48.660 --> 00:01:51.340
And if we look at it from a
macroscopic point of view,
00:01:51.340 --> 00:01:54.640
the level of water wouldn't change at all.
00:01:54.640 --> 00:01:57.660
Now let's apply this concept
of dynamic equilibrium
00:01:57.660 --> 00:02:00.440
to a hypothetical chemical reaction.
00:02:00.440 --> 00:02:04.140
In our hypothetical reaction
X2 which is a reddish brown
00:02:04.140 --> 00:02:09.140
gas, decomposes into its
individual atoms to form 2X
00:02:09.740 --> 00:02:12.610
and individual atoms are colorless.
00:02:12.610 --> 00:02:17.610
So in the forward reaction,
we're going from X2 to 2X.
00:02:18.414 --> 00:02:20.960
So X2 is decomposing to 2X.
00:02:20.960 --> 00:02:25.140
And in the reverse
reaction, the two atoms of X
00:02:25.140 --> 00:02:28.870
are combining together to form X2.
00:02:28.870 --> 00:02:32.040
When we have a forward
reaction and a reverse reaction
00:02:32.040 --> 00:02:35.190
by convention, we say,
what's on the left side,
00:02:35.190 --> 00:02:39.760
are the reactants, and
what's on the right side,
00:02:39.760 --> 00:02:41.150
are the products.
00:02:41.150 --> 00:02:45.023
And by using these terms,
we can avoid confusion.
00:02:46.000 --> 00:02:48.990
Let's say that we start our
reaction with only reactants.
00:02:48.990 --> 00:02:53.040
So only X2 is present in
this first container here.
00:02:53.040 --> 00:02:57.250
And there are five particles of X2.
00:02:57.250 --> 00:03:01.060
If every particle represents 0.1 moles,
00:03:01.060 --> 00:03:03.580
since we have five particles of X2,
00:03:03.580 --> 00:03:07.230
we have 0.5 moles of X2.
00:03:07.230 --> 00:03:10.325
And let's say, this is
a one liter container.
00:03:10.325 --> 00:03:14.290
0.5 divided by one would be 0.5 molar.
00:03:14.290 --> 00:03:19.290
So the initial concentration
of gas, X2 is 0.5 molar.
00:03:21.290 --> 00:03:24.250
And since we don't have any of the X,
00:03:24.250 --> 00:03:27.220
there are no white dots
in this box, right?
00:03:27.220 --> 00:03:30.723
The initial concentration
of X would be zero molar.
00:03:32.170 --> 00:03:34.748
So let me just write that in here, 0M.
00:03:34.748 --> 00:03:36.330
Next we wait 10 seconds.
00:03:36.330 --> 00:03:38.077
So we start off at time's
equal to zero seconds,
00:03:38.077 --> 00:03:40.650
and now we're at time's
equal to 10 seconds.
00:03:40.650 --> 00:03:41.860
And now we can see, there are
00:03:41.860 --> 00:03:46.400
three particles of X2 in our box.
00:03:46.400 --> 00:03:49.260
And so that would be 0.3M,
00:03:49.260 --> 00:03:51.940
so let's go ahead and write 0.3M in
00:03:51.940 --> 00:03:53.490
for our concentration.
00:03:53.490 --> 00:03:56.370
And now we have some particles of X.
00:03:56.370 --> 00:04:00.230
There are one, two, three, four particles.
00:04:00.230 --> 00:04:04.060
And once again, if each
particle represents 0.1 moles
00:04:04.060 --> 00:04:08.133
that's 0.4 moles of X
divided by one or 0.4M.
00:04:11.930 --> 00:04:13.310
We wait another 10 seconds,
00:04:13.310 --> 00:04:15.940
so when time is equal to 20 seconds,
00:04:15.940 --> 00:04:19.130
now there are two particles of X2
00:04:19.130 --> 00:04:23.820
and one, two, three, four,
five, six particles of X.
00:04:23.820 --> 00:04:28.820
So now the concentrations are
0.2M for X2 and 0.6M for X.
00:04:33.640 --> 00:04:36.900
We wait another 10 seconds
for a total of 30 seconds.
00:04:36.900 --> 00:04:40.330
And there are still two particles of X2
00:04:40.330 --> 00:04:43.170
and six particles of X.
00:04:43.170 --> 00:04:46.000
And so the concentrations
after 30 seconds,
00:04:46.000 --> 00:04:49.160
the concentration of X2
is 0.2M and of X is 0.6M.
00:04:54.350 --> 00:04:57.728
Notice how the concentration
of X2 went from 0.5M
00:04:57.728 --> 00:05:02.728
to 0.3M to 0.2, and then it
was also 0.2 after 30 seconds.
00:05:03.430 --> 00:05:07.860
So it became constant when
time is equal to 20 seconds.
00:05:07.860 --> 00:05:10.410
The concentration of X went
from zero to 0.4 to 0.6
00:05:11.760 --> 00:05:15.560
and then it was also 0.6 after 30 seconds.
00:05:15.560 --> 00:05:18.650
So the concentrations became
constant when time is equal to
00:05:18.650 --> 00:05:22.440
20 seconds, which means the
reaction reached equilibrium
00:05:22.440 --> 00:05:24.160
after 20 seconds.
00:05:24.160 --> 00:05:26.770
So at time is equal to zero
was not at equilibrium.
00:05:26.770 --> 00:05:29.900
When time is equal to 10 seconds,
it was not at equilibrium.
00:05:29.900 --> 00:05:32.220
Only when time was equal to 20 seconds,
00:05:32.220 --> 00:05:33.700
did it reach equilibrium.
00:05:33.700 --> 00:05:37.470
And that equilibrium, the
rate of the forward reaction
00:05:37.470 --> 00:05:40.530
is equal to the rate of
the reverse reaction.
00:05:40.530 --> 00:05:44.440
And if that's true, then
X2 is being turned into 2X
00:05:44.440 --> 00:05:49.080
at the same rate that 2X is
being turned back into X2.
00:05:49.080 --> 00:05:53.490
And if those rates are equal,
the concentrations of X2
00:05:53.490 --> 00:05:56.893
and X at equilibrium
would remain constant.
00:05:57.800 --> 00:05:59.280
We can see the same concept,
00:05:59.280 --> 00:06:03.440
if you look at a graph of
concentration versus time.
00:06:03.440 --> 00:06:06.840
Concentration of X2 starts
at 0.5M when time is
00:06:06.840 --> 00:06:10.270
equal to zero seconds,
and then drops to 0.3M
00:06:10.270 --> 00:06:11.400
after 10 seconds.
00:06:11.400 --> 00:06:14.220
And after 20 seconds, it's at 0.2M
00:06:14.220 --> 00:06:16.480
and then stays constant after that.
00:06:16.480 --> 00:06:19.650
For the concentration of
X, we start out at 0M,
00:06:19.650 --> 00:06:22.560
we increase 2.4 after 10 seconds,
00:06:22.560 --> 00:06:25.640
then we're at 0.6 and
then we are constant.
00:06:25.640 --> 00:06:27.660
So if you think about a line,
00:06:27.660 --> 00:06:31.280
if we just draw a dash
line here at 20 seconds.
00:06:31.280 --> 00:06:34.014
That's the dividing line
between on the left,
00:06:34.014 --> 00:06:36.750
where we're not at equilibrium.
00:06:36.750 --> 00:06:40.000
And so the concentrations
are always changing.
00:06:40.000 --> 00:06:42.290
And then to the right of that dotted line,
00:06:42.290 --> 00:06:44.260
we are at equilibrium where
00:06:44.260 --> 00:06:47.000
the concentrations remain constant.
00:06:47.000 --> 00:06:51.873
So the equilibrium concentration
of X2 gas is equal to
00:06:51.873 --> 00:06:56.220
0.2M and the equilibrium concentration
00:06:56.220 --> 00:07:00.470
of X gas is equal to 0.6M.
00:07:00.470 --> 00:07:02.850
Finally, let's use these
particular diagrams
00:07:02.850 --> 00:07:04.450
to think about what we would see
00:07:04.450 --> 00:07:06.630
at a macroscopic level as the
00:07:06.630 --> 00:07:08.980
reaction proceeds to equilibrium.
00:07:08.980 --> 00:07:10.520
And the first particulate diagram
00:07:10.520 --> 00:07:12.752
we see only red particles.
00:07:12.752 --> 00:07:17.752
So only our reactants X2 are
present in the beginning.
00:07:18.010 --> 00:07:20.097
However, as time goes on,
the number of red particles
00:07:20.097 --> 00:07:23.620
decreases from five in the
first particular diagram
00:07:23.620 --> 00:07:26.650
to three in the second to two
00:07:26.650 --> 00:07:30.140
and then the number stays at
two because remember we reach
00:07:30.140 --> 00:07:33.500
equilibrium after 20 seconds.
00:07:33.500 --> 00:07:36.360
So what we would see from a
macroscopic point of view,
00:07:36.360 --> 00:07:40.223
is we'd start out with a
reaction vessel that is a darker
00:07:40.223 --> 00:07:44.340
brown red, and then it would
be a lighter brown red.
00:07:44.340 --> 00:07:46.670
And then finally, when
we reach equilibrium
00:07:46.670 --> 00:07:48.180
and even lighter brown red,
00:07:48.180 --> 00:07:51.680
and it would stay that
same light brown red,
00:07:51.680 --> 00:07:54.207
because we've reached equilibrium
and the concentrations
00:07:54.207 --> 00:07:58.400
of reactants and products
remain constant at equilibrium.
00:07:58.400 --> 00:08:02.520
Even though our reactants are
turning into our products.
00:08:02.520 --> 00:08:05.360
Our products are turning back
into our reactants at the same
00:08:05.360 --> 00:08:07.440
rate and therefore the concentrations
00:08:07.440 --> 00:08:10.143
of both reactants and
products are constant.
|
Biodiversity | https://www.youtube.com/watch?v=TZ-S9sc6HYM | vtt | https://www.youtube.com/api/timedtext?v=TZ-S9sc6HYM&ei=4FWUZe2EIu6vp-oPwrOK8AE&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245328&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=19E2DA9F56C34BED0A3073000EF3C57937860204.0D24B7AFCD53BA3C16D017CBF3769D4026C5470D&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.170 --> 00:00:01.280
- [Instructor] Today, we're going to talk
00:00:01.280 --> 00:00:02.990
about biodiversity.
00:00:02.990 --> 00:00:05.270
So biodiversity as you might've guessed
00:00:05.270 --> 00:00:09.310
comes from two words,
biological and diversity.
00:00:09.310 --> 00:00:11.460
And essentially, it's the variations
00:00:11.460 --> 00:00:15.060
or the diversity present
between living things.
00:00:15.060 --> 00:00:18.020
Now, I grew up in the
sunny state of Arizona.
00:00:18.020 --> 00:00:19.170
And at first glance,
00:00:19.170 --> 00:00:21.060
there doesn't seem to be much variety
00:00:21.060 --> 00:00:22.720
in such a hot and dry place.
00:00:22.720 --> 00:00:24.970
I mean, it's the desert, right?
00:00:24.970 --> 00:00:26.210
But if we take a closer look
00:00:26.210 --> 00:00:28.530
at a place such as the Sonoran Desert,
00:00:28.530 --> 00:00:30.090
and here's a picture,
00:00:30.090 --> 00:00:32.790
we would find all kinds
of different living things
00:00:32.790 --> 00:00:37.750
like saguaro cacti,
jackrabbits, tarantulas,
00:00:37.750 --> 00:00:39.710
silver-haired bats and the roadrunner,
00:00:39.710 --> 00:00:41.830
which is my personal favorite.
00:00:41.830 --> 00:00:45.910
So we can say that the desert
is actually quite biodiverse.
00:00:45.910 --> 00:00:47.340
So in other words,
00:00:47.340 --> 00:00:52.150
it's home to a large
variety of living things.
00:00:52.150 --> 00:00:54.940
Since there are both big
and small differences
00:00:54.940 --> 00:00:56.580
between different living things,
00:00:56.580 --> 00:01:00.350
we can think of biodiversity
on three different levels.
00:01:00.350 --> 00:01:02.530
So the first and smallest scale level
00:01:02.530 --> 00:01:04.750
is going to be genetic biodiversity,
00:01:04.750 --> 00:01:07.310
which is just the genetic variation
00:01:07.310 --> 00:01:09.170
within a group of organisms.
00:01:09.170 --> 00:01:12.700
And a really great example
of this kind of biodiversity
00:01:12.700 --> 00:01:14.650
is the rock pocket mouse.
00:01:14.650 --> 00:01:16.450
And I know, that's a
mouthful of words to say.
00:01:16.450 --> 00:01:17.860
But it's really cute.
00:01:17.860 --> 00:01:19.540
I mean, look at this picture.
00:01:19.540 --> 00:01:22.230
So this is a species that can
actually be found right here
00:01:22.230 --> 00:01:23.270
in the Sonoran Desert.
00:01:23.270 --> 00:01:26.070
And the cool thing
about this mouse species
00:01:26.070 --> 00:01:28.180
is that there exists both tan
00:01:28.180 --> 00:01:30.380
and black-colored rock pocket mice.
00:01:30.380 --> 00:01:32.240
So even though both colored rodents
00:01:32.240 --> 00:01:34.100
come from the same species,
00:01:34.100 --> 00:01:35.580
there are genetic biodiversity
00:01:35.580 --> 00:01:38.590
creates mice with
completely different traits.
00:01:38.590 --> 00:01:39.910
And what's even more awesome
00:01:39.910 --> 00:01:42.530
is the fact that these
colors, tan and black,
00:01:42.530 --> 00:01:45.660
have come about due to natural selection.
00:01:45.660 --> 00:01:46.840
So scientists have found
00:01:46.840 --> 00:01:49.450
that there are more
black-colored rock pocket mice
00:01:49.450 --> 00:01:53.280
in places with dark black-ish lava rock.
00:01:53.280 --> 00:01:55.680
While there are more
tan-colored rock pocket mice
00:01:55.680 --> 00:01:57.570
in lighter colored sands.
00:01:57.570 --> 00:02:00.150
And this makes sense because
if you think about it,
00:02:00.150 --> 00:02:04.090
the mice are hunted from
above by predators like birds.
00:02:04.090 --> 00:02:07.860
So having a coat color that
blends into their surroundings
00:02:07.860 --> 00:02:10.810
would increase their chances of survival.
00:02:10.810 --> 00:02:14.650
So having this kind of genetic
biodiversity is really great,
00:02:14.650 --> 00:02:16.060
because the rock pocket mice
00:02:16.060 --> 00:02:19.570
can use many different colored
landscapes as habitats.
00:02:19.570 --> 00:02:23.110
And if let's say the
landscape color were to change
00:02:23.110 --> 00:02:26.710
and suddenly become
dominated by dark lava rock,
00:02:26.710 --> 00:02:28.700
then this population of mice
00:02:28.700 --> 00:02:30.450
would have the genetic diversity
00:02:30.450 --> 00:02:33.550
that it needs to adapt to this change.
00:02:33.550 --> 00:02:36.550
So the second level is
species biodiversity,
00:02:36.550 --> 00:02:41.140
which is the variety of
species in a particular area.
00:02:41.140 --> 00:02:43.160
So going back to the Sonoran Desert,
00:02:43.160 --> 00:02:46.560
there are all kinds of mammals and birds,
00:02:46.560 --> 00:02:48.060
plants, and insects.
00:02:48.060 --> 00:02:50.960
But what I think is
even more mind boggling
00:02:50.960 --> 00:02:53.670
is the sheer number of
bat species there are.
00:02:53.670 --> 00:02:57.040
I mean, we have silver-haired
bats, as I mentioned earlier.
00:02:57.040 --> 00:03:01.470
But also bats like spotted
bats, Western red bats,
00:03:01.470 --> 00:03:05.180
and even this kind of bat
called Peter's ghost-faced bat,
00:03:05.180 --> 00:03:07.880
which I think is a really awesome name.
00:03:07.880 --> 00:03:09.540
And you're probably thinking, okay, Abby,
00:03:09.540 --> 00:03:10.860
this is really interesting.
00:03:10.860 --> 00:03:12.440
But so what?
00:03:12.440 --> 00:03:14.320
Well, like genetic biodiversity,
00:03:14.320 --> 00:03:17.780
species biodiversity is
super duper important.
00:03:17.780 --> 00:03:20.520
Because having a lot of different species
00:03:20.520 --> 00:03:23.730
means that more roles can
be filled in an ecosystem,
00:03:23.730 --> 00:03:26.170
which makes the ecosystem healthier.
00:03:26.170 --> 00:03:27.760
So moving on to the final level,
00:03:27.760 --> 00:03:30.000
we have ecosystem biodiversity.
00:03:30.000 --> 00:03:34.150
And this is just the variety
of ecosystems on the planet.
00:03:34.150 --> 00:03:36.620
Now we've been talking a lot
about the Sonoran Desert.
00:03:36.620 --> 00:03:39.910
And a desert is actually a
type of ecosystem on earth.
00:03:39.910 --> 00:03:40.830
And if you recall,
00:03:40.830 --> 00:03:43.960
ecosystems are made up
of both living things
00:03:43.960 --> 00:03:45.760
and their physical environment.
00:03:45.760 --> 00:03:48.990
So in this case, living
things in the desert ecosystem
00:03:48.990 --> 00:03:52.280
could include things like
rattlesnakes, scorpions,
00:03:52.280 --> 00:03:53.690
and cacti.
00:03:53.690 --> 00:03:57.470
Well, non-living things
could include rock formations
00:03:57.470 --> 00:03:58.890
or a sand dunes.
00:03:58.890 --> 00:04:01.240
And in addition to desert ecosystems,
00:04:01.240 --> 00:04:05.250
earth has forest ecosystems,
coral reef ecosystems,
00:04:05.250 --> 00:04:07.790
all kinds of different ecosystems.
00:04:07.790 --> 00:04:10.310
And having all these
different kinds of ecosystems
00:04:10.310 --> 00:04:13.490
is extremely critical for our survival.
00:04:13.490 --> 00:04:16.770
Because the diversity
of ecosystems on earth
00:04:16.770 --> 00:04:21.180
provide us humans with important
resources and services.
00:04:21.180 --> 00:04:23.630
So without ecosystem biodiversity,
00:04:23.630 --> 00:04:24.730
our quality of life,
00:04:24.730 --> 00:04:28.860
and in fact, our very
survival could be at risk.
00:04:28.860 --> 00:04:32.120
So as you can tell, every
level of biodiversity
00:04:32.120 --> 00:04:35.323
is incredibly important
for unique reasons.
00:04:36.160 --> 00:04:38.640
Now, biodiversity doesn't remain constant.
00:04:38.640 --> 00:04:40.490
So we can think of biodiversity
00:04:40.490 --> 00:04:43.010
as something that can change over time.
00:04:43.010 --> 00:04:44.690
Now, the important thing to remember
00:04:44.690 --> 00:04:47.970
is that speciation increases biodiversity
00:04:47.970 --> 00:04:51.260
while extinction decreases biodiversity.
00:04:51.260 --> 00:04:53.630
So let's talk about speciation first.
00:04:53.630 --> 00:04:57.640
So speciation happens when
one species evolves into two
00:04:57.640 --> 00:05:00.210
or more species over time.
00:05:00.210 --> 00:05:01.170
And you might have heard
00:05:01.170 --> 00:05:03.420
or seen something that looks like this.
00:05:03.420 --> 00:05:05.870
And I'll draw it out
right here to the right.
00:05:05.870 --> 00:05:09.050
And this is just a very
simple speciation model
00:05:09.050 --> 00:05:11.170
or a phylogenetic tree.
00:05:11.170 --> 00:05:13.350
So we have here a common ancestor
00:05:13.350 --> 00:05:17.130
that branches off into
different species over time.
00:05:17.130 --> 00:05:20.620
This arrow representing
time or T for short.
00:05:20.620 --> 00:05:22.910
And it's speciation events like these
00:05:22.910 --> 00:05:25.170
that have led to the biodiversity
00:05:25.170 --> 00:05:27.590
that we see on earth today.
00:05:27.590 --> 00:05:29.690
On the flip side, we have extinction
00:05:29.690 --> 00:05:32.240
which causes biodiversity to decrease.
00:05:32.240 --> 00:05:36.490
And what we mean by this word
extinction is that a species
00:05:36.490 --> 00:05:40.100
or population of living
things dies off completely.
00:05:40.100 --> 00:05:42.750
So notice that it can happen
on different levels too.
00:05:42.750 --> 00:05:45.400
For example, if a population goes extinct,
00:05:45.400 --> 00:05:48.500
then we no longer have the
genetic variants in the gene pool
00:05:48.500 --> 00:05:52.460
or the set of genes for
a particular species.
00:05:52.460 --> 00:05:55.400
But if a species went extinct entirely,
00:05:55.400 --> 00:05:57.180
then that species is no longer there
00:05:57.180 --> 00:06:01.590
to fulfill its unique role
or its ecological niche.
00:06:01.590 --> 00:06:03.230
So you might've heard of the dodo bird,
00:06:03.230 --> 00:06:05.510
which is a species that
actually went extinct
00:06:05.510 --> 00:06:08.340
way back in the 1600s.
00:06:08.340 --> 00:06:09.850
So, some of the major causes
00:06:09.850 --> 00:06:11.500
behind the dodo birds extinction
00:06:11.500 --> 00:06:14.860
include over hunting, habitat loss
00:06:14.860 --> 00:06:18.240
and competition with some
newly introduced species.
00:06:18.240 --> 00:06:20.480
And unfortunately, the last dodo bird
00:06:20.480 --> 00:06:24.260
was reportedly killed in 1681.
00:06:24.260 --> 00:06:25.910
And even though we can't enjoy
00:06:25.910 --> 00:06:28.010
the presence of dodo birds anymore,
00:06:28.010 --> 00:06:29.440
learning about this extinct bird
00:06:29.440 --> 00:06:32.150
actually brings up a really good question.
00:06:32.150 --> 00:06:34.690
That is, what effect do humans have
00:06:34.690 --> 00:06:36.760
on biodiversity right now?
00:06:36.760 --> 00:06:38.040
Well, it's sad to say,
00:06:38.040 --> 00:06:41.850
but humans are actually causing
biodiversity to decrease.
00:06:41.850 --> 00:06:45.710
Things like climate change,
habitat destruction,
00:06:45.710 --> 00:06:47.810
and overexploiting resources
00:06:47.810 --> 00:06:51.160
have caused a huge loss of biodiversity.
00:06:51.160 --> 00:06:53.190
And if you remember having biodiversity
00:06:53.190 --> 00:06:55.320
is really critical to our survival,
00:06:55.320 --> 00:06:57.720
which is a big, oh, oh.
00:06:57.720 --> 00:06:59.370
In fact, species extinction
00:06:59.370 --> 00:07:03.840
is now occurring at a rate
of 100 to 1000 times faster
00:07:03.840 --> 00:07:07.040
than the background rate
detected in fossil records.
00:07:07.040 --> 00:07:08.680
And because the extinction rate
00:07:08.680 --> 00:07:11.400
is much bigger than the speciation rate,
00:07:11.400 --> 00:07:16.400
the result is an overall loss
or decrease in biodiversity.
00:07:16.680 --> 00:07:18.850
So today we learned about biodiversity,
00:07:18.850 --> 00:07:21.800
which is the variety of
life present on earth.
00:07:21.800 --> 00:07:25.170
We talked about three different
levels of biodiversity
00:07:25.170 --> 00:07:28.270
moving from genetic
biodiversity to species
00:07:28.270 --> 00:07:30.660
and then ecosystem biodiversity.
00:07:30.660 --> 00:07:33.720
And we also talked about how
biodiversity isn't stagnant
00:07:33.720 --> 00:07:35.040
or fixed in place.
00:07:35.040 --> 00:07:38.270
We have speciation events
that can increase biodiversity
00:07:38.270 --> 00:07:41.770
and extinctions that
decrease biodiversity.
00:07:41.770 --> 00:07:43.940
And finally, we learned that human actions
00:07:43.940 --> 00:07:45.800
are threatening biodiversity,
00:07:45.800 --> 00:07:48.640
as we currently have a
greater extinction rate
00:07:48.640 --> 00:07:50.603
than speciation rate.
|
Formation of biomolecules | https://www.youtube.com/watch?v=9RUSMa-UIcQ | vtt | https://www.youtube.com/api/timedtext?v=9RUSMa-UIcQ&ei=4VWUZfm7NYCrp-oPqtKyOA&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245329&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=B6BDCED3842D06224A263AE4AE535DA2B163224E.B084F087499E5AF069E75D98319547792075B4F2&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.320 --> 00:00:04.740
- [Sal] So all organisms
need food to survive.
00:00:04.740 --> 00:00:07.820
Now, for some of you, this
might be pretty obvious.
00:00:07.820 --> 00:00:10.080
You realize what might happen to your body
00:00:10.080 --> 00:00:11.940
if you don't get food.
00:00:11.940 --> 00:00:16.380
You might realize that you
need that food for both energy
00:00:17.240 --> 00:00:22.090
and you need that to actually
build up your actual body.
00:00:22.090 --> 00:00:26.270
So you need it for matter as well.
00:00:26.270 --> 00:00:27.810
But some of you might be thinking,
00:00:27.810 --> 00:00:29.240
all right, I have a mouth.
00:00:29.240 --> 00:00:31.670
I understand where the food goes.
00:00:31.670 --> 00:00:33.270
I also understand what's left over
00:00:33.270 --> 00:00:34.530
when I'm done with the food.
00:00:34.530 --> 00:00:38.070
And so I must have extracted
some energy and matter from it,
00:00:38.070 --> 00:00:40.430
but you just said all organisms, Sal,
00:00:40.430 --> 00:00:42.230
and I'm looking outside of a window
00:00:42.230 --> 00:00:45.500
and I see a tree and a
tree does not have a mouth.
00:00:45.500 --> 00:00:46.750
A tree is an organism.
00:00:46.750 --> 00:00:48.700
How does it get its food?
00:00:48.700 --> 00:00:51.130
And the answer you might already realize
00:00:51.130 --> 00:00:51.963
is that the tree
00:00:51.963 --> 00:00:55.970
can make its own food
through photosynthesis.
00:00:55.970 --> 00:00:58.360
We've seen this in other videos.
00:00:58.360 --> 00:01:03.360
You have carbon dioxide in
the air and you have water.
00:01:04.030 --> 00:01:07.840
And the presence of energy
in the form of sunlight,
00:01:07.840 --> 00:01:12.840
through the process of
photosynthesis, would produce glucose
00:01:14.150 --> 00:01:17.270
and molecular oxygen as a byproduct.
00:01:17.270 --> 00:01:19.700
And you can count the various carbons
00:01:19.700 --> 00:01:21.610
that are in this dark gray color.
00:01:21.610 --> 00:01:24.350
Oxygen's in this red
color and hydrogen's here.
00:01:24.350 --> 00:01:27.050
And you can see that
everything all adds up.
00:01:27.050 --> 00:01:30.790
You have one, two, three,
four, five six carbons here
00:01:30.790 --> 00:01:33.200
in the six carbon dioxide molecules.
00:01:33.200 --> 00:01:34.570
And then you could see in this glucose,
00:01:34.570 --> 00:01:38.330
you have one, two, three,
four, five, six carbons.
00:01:38.330 --> 00:01:39.730
I encourage you to pause the video
00:01:39.730 --> 00:01:41.980
and make sure that the
oxygens are all accounted for
00:01:41.980 --> 00:01:45.500
between the glucose molecule
and this molecular oxygen,
00:01:45.500 --> 00:01:48.250
and that the hydrogens
are all accounted for.
00:01:48.250 --> 00:01:51.330
And so a plant can produce its own food,
00:01:51.330 --> 00:01:52.400
and then when they need it,
00:01:52.400 --> 00:01:54.840
they can metabolize that food
00:01:54.840 --> 00:01:57.760
through a process of respiration.
00:01:57.760 --> 00:01:59.910
It's really important to realize
00:01:59.910 --> 00:02:03.170
that respiration does
not just occur in your
00:02:03.170 --> 00:02:04.280
and my bodies.
00:02:04.280 --> 00:02:07.450
Even organisms like plants
need to break down the food
00:02:07.450 --> 00:02:11.180
that they produced if they
wanna use it for energy.
00:02:11.180 --> 00:02:12.580
Now, the question you might have is,
00:02:12.580 --> 00:02:14.090
where is the energy here?
00:02:14.090 --> 00:02:16.600
Just as it takes energy
to rearrange these atoms
00:02:16.600 --> 00:02:20.290
and molecules into glucose,
under the right conditions,
00:02:20.290 --> 00:02:22.320
through a metabolic pathway,
00:02:22.320 --> 00:02:24.050
you can go the other way around.
00:02:24.050 --> 00:02:27.810
And chemically, that will release
energy, which even a plant
00:02:27.810 --> 00:02:30.530
which isn't running around,
it isn't doing jumping jacks,
00:02:30.530 --> 00:02:31.710
it isn't talking.
00:02:31.710 --> 00:02:34.310
It needs energy just to be alive.
00:02:34.310 --> 00:02:37.980
All living things need
energy in order to exist,
00:02:37.980 --> 00:02:41.420
in order to maintain their
cells, in order to reproduce.
00:02:41.420 --> 00:02:43.901
So many of you all have
probably heard the term
00:02:43.901 --> 00:02:46.970
carbohydrate when we're
thinking about food
00:02:46.970 --> 00:02:49.650
or when we're thinking
about an energy context.
00:02:49.650 --> 00:02:52.690
And it's important to note
that this glucose molecule here
00:02:52.690 --> 00:02:55.080
is an example of a carbohydrate.
00:02:55.080 --> 00:02:57.210
It's not the only example of it,
00:02:57.210 --> 00:02:58.960
but one question might be,
00:02:58.960 --> 00:03:01.088
why is it even called a carbohydrate?
00:03:01.088 --> 00:03:03.430
Well, when you break
down the different parts,
00:03:03.430 --> 00:03:05.860
it seems like it would involve carbon.
00:03:05.860 --> 00:03:07.720
Right over here, you have the carbo part.
00:03:07.720 --> 00:03:09.370
And it seems like it's somehow
00:03:09.370 --> 00:03:11.910
involving water: carbohydrate.
00:03:11.910 --> 00:03:13.690
And that's because early chemists,
00:03:13.690 --> 00:03:15.970
they didn't actually
understand the structure
00:03:15.970 --> 00:03:18.320
of a carbohydrate the way that we do now.
00:03:18.320 --> 00:03:21.000
All they saw was the
ratio between the carbons,
00:03:21.000 --> 00:03:22.800
the hydrogens and the oxygens.
00:03:22.800 --> 00:03:23.890
That for every carbon.
00:03:23.890 --> 00:03:25.820
So let's say there are N carbons,
00:03:25.820 --> 00:03:28.800
there's going to be
twice as many hydrogens,
00:03:28.800 --> 00:03:31.870
and N oxygens as well.
00:03:31.870 --> 00:03:33.400
So one thing, one way to think about it,
00:03:33.400 --> 00:03:36.470
for every single carbon, you have an H2O.
00:03:36.470 --> 00:03:38.220
So every carbon, you have a water.
00:03:38.220 --> 00:03:40.050
So that's why early chemists,
00:03:40.050 --> 00:03:43.350
when they saw this ratio,
they called it carbohydrates.
00:03:43.350 --> 00:03:45.420
Glucose is a very simple carbohydrate,
00:03:45.420 --> 00:03:48.350
but you can make up chains
of things like glucose
00:03:48.350 --> 00:03:51.380
to build up more complex carbohydrates.
00:03:51.380 --> 00:03:52.920
Now it's important to realize
00:03:52.920 --> 00:03:56.600
that these types of molecules
aren't just used for energy.
00:03:56.600 --> 00:03:59.480
They can also be used for matter.
00:03:59.480 --> 00:04:01.620
The more that you study biochemistry,
00:04:01.620 --> 00:04:03.780
you're going to see a lot
of different molecules
00:04:03.780 --> 00:04:05.430
that are made up of these building blocks
00:04:05.430 --> 00:04:07.740
of carbons, oxygens, and hydrogens.
00:04:07.740 --> 00:04:10.130
And sometimes you might
even recognize structures
00:04:10.130 --> 00:04:11.710
that look a little bit like glucose,
00:04:11.710 --> 00:04:13.900
or look like things that
have been put together
00:04:13.900 --> 00:04:16.160
from some of these basic building blocks.
00:04:16.160 --> 00:04:19.320
For example, this molecule right over here
00:04:19.320 --> 00:04:22.450
is known as thymidine monophosphate,
00:04:22.450 --> 00:04:23.870
and it's a fancy name.
00:04:23.870 --> 00:04:25.850
But you can look at the
building blocks here.
00:04:25.850 --> 00:04:28.940
The monophosphate, you
have a phosphate group
00:04:28.940 --> 00:04:30.290
right over here.
00:04:30.290 --> 00:04:33.880
Thymidine comes from this
part of the molecule.
00:04:33.880 --> 00:04:36.610
It's sometimes known as a nitrogenous base
00:04:36.610 --> 00:04:39.600
because it has nitrogen that
you see in blue over here.
00:04:39.600 --> 00:04:42.430
And then right over here,
connecting the pieces,
00:04:42.430 --> 00:04:46.730
you have a five carbon sugar: Ribose.
00:04:46.730 --> 00:04:48.670
Now glucose is a six carbon sugar,
00:04:48.670 --> 00:04:50.650
Ribose is a five carbon sugar,
00:04:50.650 --> 00:04:52.280
but there are metabolic pathways
00:04:52.280 --> 00:04:53.960
where you can go from five carbon sugars
00:04:53.960 --> 00:04:56.280
to six carbon sugars, and back and forth.
00:04:56.280 --> 00:04:57.210
And what's interesting
00:04:57.210 --> 00:04:59.894
about things like thymidine monophosphate
00:04:59.894 --> 00:05:02.760
is it is a building block for something
00:05:02.760 --> 00:05:06.420
that is very, very, very important: DNA.
00:05:06.420 --> 00:05:08.510
Thymidine monophosphate is a nucleotide
00:05:08.510 --> 00:05:10.390
with a nitrogenous base thymine.
00:05:10.390 --> 00:05:12.610
You put a bunch of these
nucleotides together,
00:05:12.610 --> 00:05:16.130
not all of them have a
nitrogenous base of thymine here,
00:05:16.130 --> 00:05:19.290
but they form this double
helix structure that we study
00:05:19.290 --> 00:05:21.720
in a lot of depth in
many, many other videos.
00:05:21.720 --> 00:05:24.270
And you might already realize that DNA
00:05:24.270 --> 00:05:26.360
is the molecular basis of inheritance.
00:05:26.360 --> 00:05:31.000
We could not be who we are
without these types of molecules.
00:05:31.000 --> 00:05:32.890
Now, what's also
interesting is how do these
00:05:32.890 --> 00:05:35.740
different constituent
molecules rearrange themselves,
00:05:35.740 --> 00:05:39.130
even in the presence of energy,
to make other molecules?
00:05:39.130 --> 00:05:42.259
Or to get energy, how do
they re-rearrange themselves
00:05:42.259 --> 00:05:44.040
to release that energy?
00:05:44.040 --> 00:05:47.700
And all of these metabolic
pathways are facilitated
00:05:47.700 --> 00:05:50.220
by what are known as enzymes.
00:05:50.220 --> 00:05:53.370
And just to give an example of an enzyme
00:05:53.370 --> 00:05:56.470
this big thing here is commonly known
00:05:56.470 --> 00:05:58.210
as the Rubisco enzyme.
00:05:58.210 --> 00:05:59.430
Now you don't have to know its name
00:05:59.430 --> 00:06:01.140
at this point in your careers,
00:06:01.140 --> 00:06:03.870
but this is one of the enzymes
in the metabolic pathways
00:06:03.870 --> 00:06:06.650
that's able to take carbon dioxide
00:06:06.650 --> 00:06:08.530
and attach it to another molecule
00:06:08.530 --> 00:06:12.840
that eventually can get us to
forming a glucose molecule.
00:06:12.840 --> 00:06:15.450
And what happens here is
the various constituents
00:06:15.450 --> 00:06:18.170
attach to different
parts of these enzymes.
00:06:18.170 --> 00:06:20.590
And these enzymes change
their shape as they attach
00:06:20.590 --> 00:06:23.330
to certain things and they
can jam things together.
00:06:23.330 --> 00:06:25.170
They can synthesize other molecules
00:06:25.170 --> 00:06:27.840
or they can even help to break them apart.
00:06:27.840 --> 00:06:29.510
And it all comes full circle
00:06:29.510 --> 00:06:32.690
because the enzymes
themselves, these are proteins.
00:06:32.690 --> 00:06:34.830
These are made up of amino acids,
00:06:34.830 --> 00:06:36.728
which themselves are made up
00:06:36.728 --> 00:06:39.610
of a lot of these building block molecules
00:06:39.610 --> 00:06:41.981
that contain your carbons, your oxygens,
00:06:41.981 --> 00:06:44.300
and your hydrogens in them.
00:06:44.300 --> 00:06:46.050
I'll let you go now.
00:06:46.050 --> 00:06:47.440
But the important thing is to realize
00:06:47.440 --> 00:06:49.600
is that we have whole universes occurring
00:06:49.600 --> 00:06:51.800
in our cells, and that
all of these molecules
00:06:51.800 --> 00:06:54.850
and biological systems are
connected in different ways.
00:06:54.850 --> 00:06:56.150
And you have a whole series
00:06:56.150 --> 00:06:58.370
of metabolic pathways that are facilitated
00:06:58.370 --> 00:07:03.150
by enzymes that take one set
of things and step-by-step,
00:07:03.150 --> 00:07:06.798
put them together or break them apart
00:07:06.798 --> 00:07:11.410
in order to do all of the
different biological functions
00:07:11.410 --> 00:07:14.163
that we know are necessary for life.
|
Photosynthesis | https://www.youtube.com/watch?v=Yxm-WMYEpHg | vtt | https://www.youtube.com/api/timedtext?v=Yxm-WMYEpHg&ei=4FWUZee7ItuhhcIPnJqfmAY&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245328&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=7981BA537DF70D18857525DC3570BFC31E94ABA1.182B3B7796F5ED7B7A85850957A8255B974581ED&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.740 --> 00:00:02.530
- Hey everybody, Dr. Sammy here,
00:00:02.530 --> 00:00:04.460
your friendly neighborhood entomologist.
00:00:04.460 --> 00:00:08.173
And today, we're gonna
talk about photosynthesis.
00:00:09.420 --> 00:00:10.990
There's very little life on this planet
00:00:10.990 --> 00:00:13.570
that could exist without photosynthesis.
00:00:13.570 --> 00:00:15.430
It is the prerequisite for pretty much
00:00:15.430 --> 00:00:17.190
everything you see around you.
00:00:17.190 --> 00:00:20.020
It's how you get from the
intangible light of the sun
00:00:20.020 --> 00:00:22.860
to physical bodies like
those of humans are
00:00:22.860 --> 00:00:25.180
hungry, hungry caterpillars.
00:00:25.180 --> 00:00:27.963
But what does photosynthesis
actually mean?
00:00:28.860 --> 00:00:31.340
I hear people say all the
time, that photosynthesis
00:00:31.340 --> 00:00:36.340
is the process by which
plants make sugar from light.
00:00:38.260 --> 00:00:39.950
And it almost seems like magic.
00:00:39.950 --> 00:00:42.110
Light is not a substance.
00:00:42.110 --> 00:00:44.500
It is not made up of the
molecular building blocks
00:00:44.500 --> 00:00:45.940
that compose all matter.
00:00:45.940 --> 00:00:47.920
And thus, it doesn't have mass.
00:00:47.920 --> 00:00:51.320
You can fill a room with light
and never run out of space.
00:00:51.320 --> 00:00:55.100
So how could you possibly make
something physical out of it?
00:00:55.100 --> 00:00:57.170
Well, you can't.
00:00:57.170 --> 00:01:01.930
So, instead light is a form of energy,
00:01:01.930 --> 00:01:04.313
energy being the capacity to do work.
00:01:06.940 --> 00:01:09.430
So, this is where it's
helpful to know word origin.
00:01:09.430 --> 00:01:13.800
The word photosynthesis is
made up of two Greek words.
00:01:13.800 --> 00:01:18.800
It literally means light and
to put together, that's right.
00:01:19.030 --> 00:01:20.750
In addition to being an entomologist,
00:01:20.750 --> 00:01:22.870
a double a little bit in
etymology, just to make sure
00:01:22.870 --> 00:01:25.090
I'm maximally confusing to people.
00:01:25.090 --> 00:01:28.880
Anyway, you're literally
using light to drive reactions
00:01:28.880 --> 00:01:32.890
that combine ingredients into
new products, a form of work.
00:01:32.890 --> 00:01:37.060
So you're not turning light
itself into material sugar.
00:01:37.060 --> 00:01:41.360
You're taking matter that
already exists in the form of
00:01:41.360 --> 00:01:43.700
six molecules of carbon dioxide,
00:01:43.700 --> 00:01:45.780
six molecules of liquid water,
00:01:45.780 --> 00:01:49.800
and using the energy of
the sun to power a reaction
00:01:49.800 --> 00:01:52.400
that combines them into a new substance
00:01:52.400 --> 00:01:55.203
with molecular oxygen as a byproduct.
00:01:56.310 --> 00:01:57.610
Think of it this way.
00:01:57.610 --> 00:02:01.360
When you bake a cake, you
don't say that you made cake
00:02:01.360 --> 00:02:02.680
from heat.
00:02:02.680 --> 00:02:04.680
It would be more accurate to say
00:02:04.680 --> 00:02:09.680
that you took flour,
eggs, sugar, and butter
00:02:10.150 --> 00:02:13.123
and used heat to combine
them into something new.
00:02:14.790 --> 00:02:16.370
So sticking with our analogy,
00:02:16.370 --> 00:02:19.700
the ingredients for photosynthesis
are just carbon dioxide
00:02:19.700 --> 00:02:22.453
from the atmosphere and
water from the ground,
00:02:23.690 --> 00:02:26.580
with light to do the heavy lifting.
00:02:26.580 --> 00:02:30.960
Carbon dioxide and water are put together
00:02:30.960 --> 00:02:34.030
to produce a carbohydrate
which literally means
00:02:34.030 --> 00:02:35.143
water and carbon.
00:02:36.000 --> 00:02:39.150
As you can see with this
typical carbohydrate molecule,
00:02:39.150 --> 00:02:43.130
glucose, your carbon is
attached to the same atoms
00:02:43.130 --> 00:02:46.320
that compose water, two
hydrogens and oxygen.
00:02:46.320 --> 00:02:49.820
This carbohydrate has more chemical energy
00:02:49.820 --> 00:02:54.350
or bond energy than the molecules
of water or carbon dioxide
00:02:54.350 --> 00:02:56.200
that served as ingredients.
00:02:56.200 --> 00:02:59.930
Thus, the energy at the end
of the process is much greater
00:02:59.930 --> 00:03:03.170
than the energy that the
ingredients had at the outset.
00:03:03.170 --> 00:03:06.790
This means that photosynthesis
is a sort of useful reaction
00:03:06.790 --> 00:03:10.630
that stores energy like a
big biochemical solar cell.
00:03:10.630 --> 00:03:13.820
We call these endergonic reactions.
00:03:13.820 --> 00:03:15.250
And you might be able to see already
00:03:15.250 --> 00:03:18.040
why they will be so valuable
in biological systems.
00:03:18.040 --> 00:03:20.790
You take molecules that
don't have much energy
00:03:20.790 --> 00:03:23.640
and use them to produce
something that can do work.
00:03:23.640 --> 00:03:25.500
And the kitchen where
all this work happens
00:03:25.500 --> 00:03:26.770
is the chloroplast.
00:03:26.770 --> 00:03:29.201
Literally, the green maker.
00:03:29.201 --> 00:03:32.040
The chloroplast is a
little organ or organelle
00:03:32.040 --> 00:03:33.920
present in some plant cells.
00:03:33.920 --> 00:03:37.890
And it's what makes plant cells
and ultimately plants green.
00:03:37.890 --> 00:03:41.720
And this is because the
chloroplasts bear the green pigment
00:03:41.720 --> 00:03:42.553
chlorophyll.
00:03:44.080 --> 00:03:46.490
Now the same way that
the word photosynthesis
00:03:46.490 --> 00:03:49.410
can be broken down neatly
into its two base words.
00:03:49.410 --> 00:03:52.200
The process itself can
be separated into two
00:03:52.200 --> 00:03:53.590
neat little segments.
00:03:53.590 --> 00:03:55.910
I like to think of them
as a charging step,
00:03:55.910 --> 00:03:59.260
where energy from light is
converted into chemical energy
00:03:59.260 --> 00:04:02.270
and synthesis step where the
energy is used to do the work
00:04:02.270 --> 00:04:04.540
of actually synthesizing the end product,
00:04:04.540 --> 00:04:06.113
typically a carbohydrate.
00:04:07.160 --> 00:04:09.610
So the first segment requires
the direct input of light
00:04:09.610 --> 00:04:13.590
and as such is referred to as
the light dependent reactions.
00:04:13.590 --> 00:04:15.800
These happened in a
section of the chloroplast
00:04:15.800 --> 00:04:17.280
called the thylakoids.
00:04:17.280 --> 00:04:18.960
They form these neat little pouches.
00:04:18.960 --> 00:04:21.780
The inside of which is called
the lumen and the outside
00:04:21.780 --> 00:04:23.060
called the stroma.
00:04:23.060 --> 00:04:25.210
When a photon of light ends
it's eight minute journey
00:04:25.210 --> 00:04:27.670
from the surface of the sun
to the surface of a leaf
00:04:27.670 --> 00:04:29.590
its energy is absorbed by the chlorophyll
00:04:29.590 --> 00:04:31.810
embedded in the thylakoid membrane.
00:04:31.810 --> 00:04:35.600
This energy powers a pump which
literally charges the inside
00:04:35.600 --> 00:04:39.183
of the thylakoids like a battery
by moving the ions inside.
00:04:40.150 --> 00:04:43.760
As the charge builds up, the
energy can be used to do work.
00:04:43.760 --> 00:04:47.040
But the next segment of
this process happens outside
00:04:47.040 --> 00:04:49.760
of the thylakoids in the stroma.
00:04:49.760 --> 00:04:51.580
So they get that energy where it's needed.
00:04:51.580 --> 00:04:53.480
The thylakoids transfers the energy
00:04:53.480 --> 00:04:57.700
to a molecule called ADP,
adenosine diphosphate.
00:04:57.700 --> 00:04:59.350
By adding another phosphate bond
00:04:59.350 --> 00:05:02.443
and making it ATP, adenosine triphosphate.
00:05:03.320 --> 00:05:04.912
Now you might've heard of this one.
00:05:04.912 --> 00:05:08.052
It's often called the
energy currency of the cell.
00:05:08.052 --> 00:05:10.960
Pretty much wherever energy
is needed for cell to do work
00:05:10.960 --> 00:05:12.209
ATP is involved.
00:05:12.209 --> 00:05:16.160
You might have also heard that
the energy is stored inside
00:05:16.160 --> 00:05:20.230
of the phosphate bonds,
and that breaking them
00:05:20.230 --> 00:05:22.500
releases the energy.
00:05:22.500 --> 00:05:25.710
But try to remember that these
bonds depicted by the lines
00:05:25.710 --> 00:05:28.410
in these diagrams are just a convention.
00:05:28.410 --> 00:05:30.960
It represents an adherence
of these atoms together
00:05:30.960 --> 00:05:34.290
via attraction, and it
shows you where they adhere.
00:05:34.290 --> 00:05:36.983
But the energy isn't actually in the bond,
00:05:38.060 --> 00:05:41.550
the attraction between the
atoms builds up potential energy
00:05:41.550 --> 00:05:45.120
like a rubber band that's
being pulled really tightly.
00:05:45.120 --> 00:05:48.680
When you let it go, it
could hit a paper cup
00:05:48.680 --> 00:05:51.240
and do the work of displacing that cup.
00:05:51.240 --> 00:05:53.070
The rubber band then falls to the ground
00:05:53.070 --> 00:05:56.820
in a low energy state because
it's energy has been released.
00:05:56.820 --> 00:05:59.120
So when you put the energy into a system
00:05:59.120 --> 00:06:02.020
great enough to overcome the
attraction between the atoms
00:06:02.020 --> 00:06:05.270
and force them apart,
thereby breaking the bonds,
00:06:05.270 --> 00:06:08.480
atoms or in this case
a whole phosphate group
00:06:08.480 --> 00:06:11.150
can go spiraling off taking what was
00:06:11.150 --> 00:06:12.710
potential energy with it.
00:06:12.710 --> 00:06:14.593
If it hits something that it can bond with
00:06:14.593 --> 00:06:17.300
that energy is released
as the bond is formed
00:06:17.300 --> 00:06:21.050
and can be used to do work
such as the magic of ATP
00:06:21.050 --> 00:06:23.860
is described as energetic
because it's easy
00:06:23.860 --> 00:06:27.160
to break the bond between it
and the last phosphate group.
00:06:27.160 --> 00:06:29.820
Meaning you don't have
to put much energy in
00:06:29.820 --> 00:06:31.843
but you get a ton of energy out.
00:06:33.450 --> 00:06:35.130
So back to the thylakoids.
00:06:35.130 --> 00:06:37.250
Those photons of light were able to net us
00:06:37.250 --> 00:06:40.300
a highly energetic ATP molecule.
00:06:40.300 --> 00:06:42.310
But the next segment of photosynthesis
00:06:42.310 --> 00:06:44.210
is gonna need some electrons too.
00:06:44.210 --> 00:06:45.990
That light energy is used to do the work
00:06:45.990 --> 00:06:48.650
of loading up a mobile
electron carrier with electrons
00:06:48.650 --> 00:06:50.200
and a proton.
00:06:50.200 --> 00:06:52.740
This carrier is called NADP plus.
00:06:52.740 --> 00:06:54.710
And when it's got a full
load to take to the next
00:06:54.710 --> 00:06:57.313
set of reactions, it's called NADPH,
00:06:58.810 --> 00:07:01.100
and that's pretty much the
light dependent reactions
00:07:01.100 --> 00:07:02.160
in a nutshell.
00:07:02.160 --> 00:07:06.210
The only other thing you should
probably remember is that,
00:07:06.210 --> 00:07:09.430
well, this is where all the
oxygen in your lungs comes from.
00:07:09.430 --> 00:07:11.870
So, you know, no big deal.
00:07:11.870 --> 00:07:14.940
When chlorophyll gets excited
by that photon of light
00:07:15.890 --> 00:07:17.980
it turns into a real bully.
00:07:17.980 --> 00:07:20.260
The work it's doing
creates such a powerful
00:07:20.260 --> 00:07:22.890
electro-chemical imbalance
and the chlorophyll
00:07:22.890 --> 00:07:25.560
balances the equation by
just stealing an electron
00:07:25.560 --> 00:07:26.610
from water.
00:07:26.610 --> 00:07:29.550
This causes water to fall
apart releasing its oxygen
00:07:29.550 --> 00:07:31.583
which the plant just lets go of.
00:07:32.580 --> 00:07:34.350
So now that we've taken
care of the section
00:07:34.350 --> 00:07:37.430
that's dependent on light,
let's discuss the section
00:07:37.430 --> 00:07:38.263
that isn't.
00:07:39.750 --> 00:07:43.420
The light independent
reactions or the Calvin cycle
00:07:43.420 --> 00:07:45.770
occur in the stroma of the chloroplast.
00:07:45.770 --> 00:07:48.000
And this is where the earth shattering
00:07:48.000 --> 00:07:51.140
chemical reaction occurs
that allows for all life
00:07:51.140 --> 00:07:52.060
on this planet.
00:07:52.060 --> 00:07:55.660
The fixation of gaseous
carbon or inorganic carbon
00:07:55.660 --> 00:07:58.193
into carbon chains, organic carbon.
00:07:59.120 --> 00:08:01.330
And this is so important because fixation
00:08:01.330 --> 00:08:03.053
doesn't just happen on its own.
00:08:03.980 --> 00:08:07.370
CO2 in the atmosphere doesn't
form organic chains or sugars.
00:08:07.370 --> 00:08:10.010
When it bumps into more
CO2 in the atmosphere
00:08:10.010 --> 00:08:13.390
it requires the help of
enzymes and energetic molecules
00:08:13.390 --> 00:08:15.140
made by living organisms.
00:08:15.140 --> 00:08:17.780
It's why when we first
landed a rover on Mars
00:08:17.780 --> 00:08:19.870
we immediately started
looking for the evidence
00:08:19.870 --> 00:08:21.320
of organic molecules.
00:08:21.320 --> 00:08:25.660
It will be evidence that
something is or was living there.
00:08:25.660 --> 00:08:28.680
In the light independent
reactions a plant enzyme
00:08:28.680 --> 00:08:33.020
fixes carbon dioxide from the
air into a chain of carbon.
00:08:33.020 --> 00:08:35.750
So ATP and NADPH which were produced
00:08:35.750 --> 00:08:38.720
in the light dependent
reactions, provide the energy
00:08:38.720 --> 00:08:42.490
and the electrons to create two
energetic reactive molecules
00:08:42.490 --> 00:08:44.120
that can be combined to make glucose
00:08:44.120 --> 00:08:46.443
or other useful molecules.
00:08:47.360 --> 00:08:49.770
And the beauty of it
is that the byproducts
00:08:49.770 --> 00:08:54.770
of the light independent
reactions, ADP and NADP plus
00:08:55.270 --> 00:08:58.540
are shuttled off from the
stroma back to the thylakoids
00:08:58.540 --> 00:09:00.920
for more light dependent reactions
00:09:00.920 --> 00:09:03.140
where they can be recharged and recycled
00:09:03.140 --> 00:09:04.343
for use again later.
00:09:05.350 --> 00:09:09.300
And, wow, photosynthesis.
00:09:09.300 --> 00:09:11.710
The takeaway here is that photosynthesis
00:09:11.710 --> 00:09:16.020
allows you to go from the
intangible energy of the sun
00:09:16.020 --> 00:09:17.930
to the stored chemical energy
00:09:17.930 --> 00:09:20.780
that life on this planet is based on.
00:09:20.780 --> 00:09:23.510
The sun's energy is converted
to the chemical energy
00:09:23.510 --> 00:09:26.500
of a carbohydrate molecule
in the chloroplast.
00:09:26.500 --> 00:09:28.680
That molecule can later be broken down
00:09:28.680 --> 00:09:31.610
in most of that energy
reclaimed either by the plant
00:09:31.610 --> 00:09:33.410
or by creatures that eat that plant.
00:09:34.300 --> 00:09:37.810
All life on earth is carbon-based.
00:09:37.810 --> 00:09:40.780
And every single molecule of that carbon
00:09:40.780 --> 00:09:44.230
once existed in the
atmosphere in gaseous form
00:09:44.230 --> 00:09:47.660
as carbon dioxide until
some enterprising plant
00:09:47.660 --> 00:09:52.090
or microorganism synthesized
it into something you can use.
00:09:52.090 --> 00:09:54.910
And while they were added many
of them filled the atmosphere
00:09:54.910 --> 00:09:57.470
with the oxygen that
we all need to breathe.
00:09:57.470 --> 00:10:00.000
So the next time you see a plant,
00:10:00.000 --> 00:10:01.967
shake its leaf and say thank you.
|
Organization of multicellular organisms | https://www.youtube.com/watch?v=8pWMifyG5bU | vtt | https://www.youtube.com/api/timedtext?v=8pWMifyG5bU&ei=5VWUZcnXBsG-mLAP65eU4Ag&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=71C792F3A6FBD24E9A2F07127EEB0CF97B2929A4.B46C05655E38887530A60304B40C4CDFF481B814&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.310 --> 00:00:01.143
- [Instructor] In this video,
00:00:01.143 --> 00:00:03.180
we're gonna take a journey in life
00:00:03.180 --> 00:00:07.150
and we're gonna start with
the smallest scale of life
00:00:07.150 --> 00:00:11.210
that is indisputably life,
and that is the cell.
00:00:11.210 --> 00:00:13.390
Now, the reason why I
qualified that a little bit
00:00:13.390 --> 00:00:16.940
is some people debate whether
viruses are living or not,
00:00:16.940 --> 00:00:18.580
'cause they have certain aspects.
00:00:18.580 --> 00:00:22.430
Viruses can reproduce, they
do have genetic information
00:00:22.430 --> 00:00:25.070
but they need other
living forms to reproduce,
00:00:25.070 --> 00:00:27.660
in particular they need other cells.
00:00:27.660 --> 00:00:29.352
But even though we imagined cells
00:00:29.352 --> 00:00:34.060
to be these very small microscopic things,
00:00:34.060 --> 00:00:37.406
they are in and of themselves
almost an entire world,
00:00:37.406 --> 00:00:39.821
and we go into depth into
that into other videos
00:00:39.821 --> 00:00:41.410
in Khan Academy.
00:00:41.410 --> 00:00:43.057
But the fact that every cell in your body,
00:00:43.057 --> 00:00:45.770
except for a few like red blood cells
00:00:45.770 --> 00:00:48.960
have all of your genetic
information in there.
00:00:48.960 --> 00:00:52.246
All of those 3 billion base pairs of DNA
00:00:52.246 --> 00:00:55.630
that make you a human being
00:00:55.630 --> 00:00:58.349
in and of itself is mind-boggling.
00:00:58.349 --> 00:01:01.460
But then the fact that
the cell specializes
00:01:01.460 --> 00:01:02.863
so that not all cells are the same
00:01:02.863 --> 00:01:05.027
even though they have that
same genetic information,
00:01:05.027 --> 00:01:08.210
they somehow know what type of cell to be
00:01:08.210 --> 00:01:10.570
that's even more interesting.
00:01:10.570 --> 00:01:13.705
So we could start at the
most basic building block
00:01:13.705 --> 00:01:16.079
in your body or really any organism's body
00:01:16.079 --> 00:01:18.860
and that's specialized cells.
00:01:18.860 --> 00:01:21.533
So what you're seeing here
is a big cluster of neurons
00:01:21.533 --> 00:01:24.190
which are dyed here in the red,
00:01:24.190 --> 00:01:27.758
and I believe these blues
show their actual nuclei
00:01:27.758 --> 00:01:30.300
where they have their genetic information.
00:01:30.300 --> 00:01:32.880
And then dyed in green,
you have what are called
00:01:32.880 --> 00:01:35.807
neuroglia cells which
are other types of cells
00:01:35.807 --> 00:01:39.870
that are inside the human brain
mainly to support neurons.
00:01:39.870 --> 00:01:42.520
Most of what we believe is thought
00:01:42.520 --> 00:01:45.170
occurs through triggering neurons,
00:01:45.170 --> 00:01:46.870
which then trigger other neurons
00:01:46.870 --> 00:01:50.290
and form cascades of these
electro-chemical signals
00:01:50.290 --> 00:01:53.400
which we're just starting to understand.
00:01:53.400 --> 00:01:57.520
But this is just one little
small fraction of a human brain.
00:01:57.520 --> 00:01:59.680
A human brain, for example we'll have
00:01:59.680 --> 00:02:04.130
on the order of 80 to 90 billion neurons.
00:02:04.130 --> 00:02:05.625
And for every one of those neurons
00:02:05.625 --> 00:02:08.740
depending on what part of the
brain you're talking about,
00:02:08.740 --> 00:02:11.870
you're talking about five
to 10 neuroglia cells.
00:02:11.870 --> 00:02:14.810
So you're talking about many
hundreds of billions of cells
00:02:14.810 --> 00:02:17.960
just in one human brain.
00:02:17.960 --> 00:02:19.990
But then if we were to
zoom out a little bit
00:02:19.990 --> 00:02:21.837
and you take a bunch of
these specialized cells
00:02:21.837 --> 00:02:25.120
working together or at
least near each other,
00:02:25.120 --> 00:02:26.623
you have tissue.
00:02:27.600 --> 00:02:31.280
And so as I said before,
this is a zoomed in view
00:02:31.280 --> 00:02:35.060
of neural tissue in
particular of brain tissue.
00:02:35.060 --> 00:02:37.710
And then if you zoom
out a little bit more,
00:02:37.710 --> 00:02:41.400
the tissue makes up organs.
00:02:41.400 --> 00:02:44.770
And if we're thinking about
neural tissue like this,
00:02:44.770 --> 00:02:47.680
we can imagine that it makes up the brain
00:02:47.680 --> 00:02:49.660
which is an organ.
00:02:49.660 --> 00:02:53.930
And then organs build up to systems.
00:02:53.930 --> 00:02:56.410
And right over here, you have a picture
00:02:56.410 --> 00:02:59.620
of the nervous system of
which the brain is apart.
00:02:59.620 --> 00:03:00.453
You also have the spinal cord,
00:03:00.453 --> 00:03:01.936
and then you also have all of the nerves
00:03:01.936 --> 00:03:03.660
that go throughout the body.
00:03:03.660 --> 00:03:05.713
So we have a system.
00:03:06.580 --> 00:03:09.170
And then you put all
of the systems together
00:03:09.170 --> 00:03:13.060
and you get the actual organism,
00:03:13.060 --> 00:03:16.470
which of course you can somewhat
visualize right over here
00:03:16.470 --> 00:03:18.290
where you can see all of
these different organs
00:03:18.290 --> 00:03:22.150
and organ systems put
together to create who we are.
00:03:22.150 --> 00:03:24.796
And just to connect to the
organism with the cells,
00:03:24.796 --> 00:03:27.460
that basic building block of life.
00:03:27.460 --> 00:03:30.210
If you are a average size human being,
00:03:30.210 --> 00:03:35.210
you likely have 30 to 40
trillion cells in your body.
00:03:35.910 --> 00:03:37.570
And if that isn't mind blowing enough
00:03:37.570 --> 00:03:38.910
and it is just an estimate,
00:03:38.910 --> 00:03:40.460
it's estimated that there's as many
00:03:40.460 --> 00:03:45.190
as 100 trillion bacteria in your body.
00:03:45.190 --> 00:03:49.500
And so even though you think
you are just "an individual"
00:03:49.500 --> 00:03:51.532
you are a universe of living things
00:03:51.532 --> 00:03:53.430
in these complex systems.
00:03:53.430 --> 00:03:55.560
And it's an interesting question of why
00:03:55.560 --> 00:03:56.930
and right over here.
00:03:56.930 --> 00:03:59.410
We know that organisms
interact with each other.
00:03:59.410 --> 00:04:01.810
We know that they interact
with their environment
00:04:01.810 --> 00:04:04.211
just as each of our nerve
cells might not appreciate
00:04:04.211 --> 00:04:08.350
that they are one of 86
billion in dissension mind,
00:04:08.350 --> 00:04:11.710
maybe we ourselves as
organisms don't appreciate
00:04:11.710 --> 00:04:13.620
that we too are building blocks
00:04:13.620 --> 00:04:15.553
of maybe something even larger.
|
Genes, proteins, and cells | https://www.youtube.com/watch?v=_iVu3g_S05I | vtt | https://www.youtube.com/api/timedtext?v=_iVu3g_S05I&ei=4VWUZargAu-sxN8P28aG6AM&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245329&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=18AA64D4F2B0C7FA39B4AA2E86430D9C25BFE651.78F80CC2275635517302C67D5C0F6ADC275070&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.500 --> 00:00:02.010
- [Instructor] So when I was younger,
00:00:02.010 --> 00:00:03.550
around seven or eight years old,
00:00:03.550 --> 00:00:06.450
I used to have a beta fish named Bob,
00:00:06.450 --> 00:00:09.670
and he happened to be a blue-colored fish.
00:00:09.670 --> 00:00:12.670
Now, I've always wondered
how he got his color.
00:00:12.670 --> 00:00:15.940
So for example, were
his parents also blue?
00:00:15.940 --> 00:00:18.440
Does he have any siblings that were blue?
00:00:18.440 --> 00:00:21.530
So today, let's try to
answer in simple terms
00:00:21.530 --> 00:00:24.430
how Bob gets his blue color.
00:00:24.430 --> 00:00:27.030
And we'll start by defining genes.
00:00:27.030 --> 00:00:30.040
Genes. What are genes?
00:00:30.040 --> 00:00:33.140
Well, genes are basic hereditary units
00:00:33.140 --> 00:00:34.620
that are well, first of all,
00:00:34.620 --> 00:00:37.110
they are passed down
from parent to offspring.
00:00:37.110 --> 00:00:41.530
So I'll write passed
down parent to offspring.
00:00:41.530 --> 00:00:43.690
And they also contain information
00:00:43.690 --> 00:00:46.220
about an organism's traits.
00:00:46.220 --> 00:00:51.220
Contain info about an organism's traits.
00:00:51.310 --> 00:00:53.810
So it would only make sense that since Bob
00:00:53.810 --> 00:00:57.260
is a blue-colored fish,
that he must have a parent
00:00:57.260 --> 00:01:00.300
or ancestor who is also blue-colored.
00:01:00.300 --> 00:01:03.920
Now, a single kind of gene can
have many different versions,
00:01:03.920 --> 00:01:07.030
and we call these versions alleles.
00:01:07.030 --> 00:01:08.420
Alleles.
00:01:08.420 --> 00:01:11.823
And these are just different
variations of a single gene.
00:01:12.720 --> 00:01:14.460
So for example, there may be a gene
00:01:14.460 --> 00:01:17.930
that provides information
about beta fish coloration.
00:01:17.930 --> 00:01:22.930
So let me draw an arrow from
Bob to, we'll say, color gene.
00:01:23.500 --> 00:01:28.500
And one allele of this gene may
lead to a blue-colored fish.
00:01:29.110 --> 00:01:32.910
So I'll write here blue color.
00:01:32.910 --> 00:01:36.950
And another allele may
lead to green coloration.
00:01:36.950 --> 00:01:41.530
And I'll write here, next
to blue color, green color.
00:01:41.530 --> 00:01:44.790
But physically, what are genes, exactly?
00:01:44.790 --> 00:01:49.410
Well, genes are part of DNA
or deoxyribonucleic acid.
00:01:49.410 --> 00:01:51.110
And I know, it's a really big word.
00:01:51.110 --> 00:01:53.060
So let me write it out for us.
00:01:53.060 --> 00:01:57.120
DNA. Deoxyribonucleic acid.
00:01:57.120 --> 00:01:57.953
DNA.
00:01:59.550 --> 00:02:02.220
So DNA is a macromolecule,
00:02:02.220 --> 00:02:05.980
or a really big and complex molecule.
00:02:05.980 --> 00:02:10.760
So when you hear macro, just
think big or complex molecule.
00:02:10.760 --> 00:02:14.530
And you can also think of
DNA like a giant cookbook
00:02:14.530 --> 00:02:17.890
of genetic information,
because that's what it is.
00:02:17.890 --> 00:02:21.473
It is a cookbook of genetic information.
00:02:23.230 --> 00:02:25.890
So here is a close-up sketch of DNA.
00:02:25.890 --> 00:02:29.220
And what I'm showing
here is that DNA consists
00:02:29.220 --> 00:02:32.530
of subunits called nucleotides.
00:02:32.530 --> 00:02:33.930
Nucleotides.
00:02:33.930 --> 00:02:38.930
And these are represented
by As, Ts, Cs, and Gs.
00:02:40.860 --> 00:02:43.810
Now genes are like the individual recipes.
00:02:43.810 --> 00:02:46.390
You can think of them as the recipes found
00:02:46.390 --> 00:02:48.700
inside your DNA cookbook.
00:02:48.700 --> 00:02:51.420
So they are specific
segments of nucleotides
00:02:51.420 --> 00:02:54.090
within the long DNA molecule.
00:02:54.090 --> 00:02:57.350
So a gene could be from here to here.
00:02:57.350 --> 00:03:00.970
And we think of this as a recipe.
00:03:00.970 --> 00:03:03.920
But what do these gene
recipes make anyways?
00:03:03.920 --> 00:03:06.690
Well, many genes encode proteins,
00:03:06.690 --> 00:03:09.330
which are made of long sequences
00:03:09.330 --> 00:03:11.710
or chains of amino acids.
00:03:11.710 --> 00:03:13.520
So, I'll write here under proteins
00:03:13.520 --> 00:03:17.620
that proteins are made
of amino acid chains.
00:03:17.620 --> 00:03:19.430
And genes provide instructions
00:03:19.430 --> 00:03:21.370
for how to create these chains.
00:03:21.370 --> 00:03:24.770
So thinking back to how
genes are like recipes
00:03:24.770 --> 00:03:27.030
because each gene has a different set
00:03:27.030 --> 00:03:30.440
of quote-unquote,
"ingredients", or in this case,
00:03:30.440 --> 00:03:32.450
a different nucleotide sequence,
00:03:32.450 --> 00:03:36.500
different genes would therefore
encode different proteins.
00:03:36.500 --> 00:03:38.050
So proteins in this example,
00:03:38.050 --> 00:03:40.630
if you want to continue
on with this analogy,
00:03:40.630 --> 00:03:42.650
proteins would be like
the finished products
00:03:42.650 --> 00:03:44.030
of your recipes.
00:03:44.030 --> 00:03:46.410
Remember how I mentioned that alleles
00:03:46.410 --> 00:03:49.500
are different versions of a specific gene?
00:03:49.500 --> 00:03:53.020
Well, different alleles have
different nucleotide sequences
00:03:53.020 --> 00:03:57.740
and are therefore likely to
also encode different proteins.
00:03:57.740 --> 00:03:59.980
So I'll write under
here, different alleles,
00:03:59.980 --> 00:04:02.820
and draw an arrow to different proteins.
00:04:02.820 --> 00:04:05.300
So different genes and different alleles
00:04:05.300 --> 00:04:07.680
can give us different proteins.
00:04:07.680 --> 00:04:11.370
So of blue fish like Bob,
likely has a distinct allele
00:04:11.370 --> 00:04:15.460
that encodes proteins, which
give him his natural blue color
00:04:15.460 --> 00:04:17.260
or his natural blue shade.
00:04:17.260 --> 00:04:20.230
Now, an organism has many different genes,
00:04:20.230 --> 00:04:23.010
which means an organism has the capacity
00:04:23.010 --> 00:04:25.920
to produce many different
kinds of proteins.
00:04:25.920 --> 00:04:28.800
And proteins serve all kinds of functions,
00:04:28.800 --> 00:04:33.600
some of which include
growth, sending messages,
00:04:33.600 --> 00:04:36.210
oh, also catalyzing chemical reactions,
00:04:36.210 --> 00:04:38.440
if you have heard of enzymes before.
00:04:38.440 --> 00:04:41.640
So, I'll write catalyzing
chemical reactions
00:04:42.650 --> 00:04:44.303
and providing structure.
00:04:45.430 --> 00:04:47.270
Ultimately, it's the activity
00:04:47.270 --> 00:04:49.440
of these different kinds of proteins
00:04:49.440 --> 00:04:52.320
that help determine an
organism's physical traits,
00:04:52.320 --> 00:04:54.680
just like how proteins can determine
00:04:54.680 --> 00:04:56.883
the color of Bob the beta fish.
00:04:57.810 --> 00:04:59.190
Now, you might be wondering too,
00:04:59.190 --> 00:05:01.760
what genes do in the big picture.
00:05:01.760 --> 00:05:04.930
For example, not all of the
cells in Bob the beta fish
00:05:04.930 --> 00:05:06.670
function in the same way, right?
00:05:06.670 --> 00:05:08.660
You could say that there
are different types
00:05:08.660 --> 00:05:11.600
of cells that perform specific functions.
00:05:11.600 --> 00:05:14.830
And this is known as cell specialization.
00:05:14.830 --> 00:05:18.560
So cell specialization is when
different cells specialize
00:05:18.560 --> 00:05:20.290
in different functions.
00:05:20.290 --> 00:05:22.160
And each type of specialized cell
00:05:22.160 --> 00:05:25.430
contains a unique combination of proteins
00:05:25.430 --> 00:05:27.910
that give the cell its
specialized function
00:05:27.910 --> 00:05:29.140
within an organism.
00:05:29.140 --> 00:05:31.930
So I'll write here that
cell specialization
00:05:31.930 --> 00:05:35.260
comes from unique combos of proteins.
00:05:35.260 --> 00:05:36.640
And it's important to note
00:05:36.640 --> 00:05:40.640
that every cell in an organism
contains the same genes.
00:05:40.640 --> 00:05:41.970
So going back to Bob here,
00:05:41.970 --> 00:05:44.530
we can say that all his cells contain
00:05:44.530 --> 00:05:47.210
the same DNA and genetic information,
00:05:47.210 --> 00:05:50.740
whether it's on his tail or in his eye,
00:05:50.740 --> 00:05:52.470
but what makes their functions different
00:05:52.470 --> 00:05:55.350
is which subset of genes are expressed
00:05:55.350 --> 00:05:59.460
or used to build proteins
in the different cell types.
00:05:59.460 --> 00:06:03.360
So, I'll write here, all of
the cells in Bob the beta fish
00:06:03.360 --> 00:06:06.280
have the same DNA and genes,
00:06:06.280 --> 00:06:09.163
just different protein combinations.
00:06:10.070 --> 00:06:13.100
So today, we learned about
genes which are passed down
00:06:13.100 --> 00:06:14.440
from parent to offspring,
00:06:14.440 --> 00:06:18.230
just like how Bob the blue
beta fish got his color,
00:06:18.230 --> 00:06:21.950
and they contain information
about organisms' traits.
00:06:21.950 --> 00:06:24.890
So genes are parts of longer DNA molecules
00:06:24.890 --> 00:06:28.980
and they consist of specific
segments of nucleotide bases.
00:06:28.980 --> 00:06:33.520
So thinking back to our cookbook
and recipe analogy, right?
00:06:33.520 --> 00:06:36.780
Genes can encode all kinds
of different proteins.
00:06:36.780 --> 00:06:39.150
And it's this unique set of proteins
00:06:39.150 --> 00:06:42.370
within each cell that gives
the cell its specific function
00:06:42.370 --> 00:06:43.500
within the organism.
00:06:43.500 --> 00:06:46.490
As we talked about with Bob the beta fish,
00:06:46.490 --> 00:06:50.330
and all of the cells in Bob
having the same DNA and genes,
00:06:50.330 --> 00:06:51.873
just different proteins.
|
Greenhouse effect and greenhouse gases | https://www.youtube.com/watch?v=YpfxiDktSoI | vtt | https://www.youtube.com/api/timedtext?v=YpfxiDktSoI&ei=41WUZeLoPOD5vdIPg_yQuAE&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245332&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=6FD0810A390C65E0EFAE027A26DD9D6284C588F0.62E609846918608F50F275A384CC1D24C8808572&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.370 --> 00:00:01.203
- [Instructor] In this video,
00:00:01.203 --> 00:00:04.400
we're gonna talk about
the greenhouse effect
00:00:04.400 --> 00:00:06.790
and also the greenhouse gases,
00:00:06.790 --> 00:00:09.680
which cause the greenhouse effect.
00:00:09.680 --> 00:00:12.070
Now let's just start with a basic idea.
00:00:12.070 --> 00:00:15.880
Imagine if earth had no
atmosphere, what would happen?
00:00:15.880 --> 00:00:16.880
Well, you have the sun,
00:00:16.880 --> 00:00:20.130
which is on average,
93 million miles away.
00:00:20.130 --> 00:00:22.700
It's sending electromagnetic radiation
00:00:22.700 --> 00:00:24.750
our way to the surface of the earth.
00:00:24.750 --> 00:00:27.080
We're actually getting a
very, very small fraction
00:00:27.080 --> 00:00:30.570
of the total electromagnetic
radiation of the sun.
00:00:30.570 --> 00:00:33.570
And then that would heat up
the surface of the earth.
00:00:33.570 --> 00:00:36.330
Now, what I have always found mind-blowing
00:00:36.330 --> 00:00:38.330
is anything with temperature
00:00:38.330 --> 00:00:40.850
will emit electromagnetic radiation.
00:00:40.850 --> 00:00:42.950
And so it's emitting some of that energy,
00:00:42.950 --> 00:00:44.930
it's losing some of that energy
00:00:44.930 --> 00:00:47.320
to electromagnetic radiation.
00:00:47.320 --> 00:00:50.750
So the surface would be releasing that
00:00:50.750 --> 00:00:53.950
and it would go out into space.
00:00:53.950 --> 00:00:57.450
But now let's introduce
the idea of an atmosphere.
00:00:57.450 --> 00:00:58.930
And in particular, we're gonna think
00:00:58.930 --> 00:01:00.403
about our lower atmosphere,
00:01:00.403 --> 00:01:02.760
which starts at the surface and goes up
00:01:02.760 --> 00:01:05.160
to about five to nine miles in altitude,
00:01:05.160 --> 00:01:07.282
often known as the troposphere.
00:01:07.282 --> 00:01:10.840
Now the troposphere has molecules in it,
00:01:10.840 --> 00:01:14.030
has gases in it like carbon dioxide,
00:01:14.030 --> 00:01:17.140
like water vapor, like methane.
00:01:17.140 --> 00:01:21.320
Others include nitrous oxide
and chlorofluorocarbons.
00:01:21.320 --> 00:01:22.990
You don't have to know
the chemical formula
00:01:22.990 --> 00:01:24.240
of all of these things,
00:01:24.240 --> 00:01:27.310
but what's interesting about these gases
00:01:27.310 --> 00:01:31.230
that are in the lower atmosphere
is that they can absorb
00:01:31.230 --> 00:01:33.410
some of those electromagnetic waves
00:01:33.410 --> 00:01:35.680
that the surface of the earth is emitting.
00:01:35.680 --> 00:01:38.130
So some of that energy
will make it out to space,
00:01:38.130 --> 00:01:40.740
but some of that energy
will then be absorbed
00:01:40.740 --> 00:01:43.020
by these molecules, by these gases,
00:01:43.020 --> 00:01:45.850
and then they will emit
some of that back to earth.
00:01:45.850 --> 00:01:48.150
And so that's why it's
called a greenhouse effect
00:01:48.150 --> 00:01:49.550
because of all of that energy
00:01:49.550 --> 00:01:51.510
that might have been sent out to space
00:01:51.510 --> 00:01:54.590
if you didn't have an
atmosphere, not all of it is.
00:01:54.590 --> 00:01:57.080
Some of it is reabsorbed
by the atmosphere,
00:01:57.080 --> 00:01:59.610
which then sends it
back down to the surface
00:01:59.610 --> 00:02:01.750
and that process can go on and on and on.
00:02:01.750 --> 00:02:05.930
You can imagine that it's
trapping some of the energy.
00:02:05.930 --> 00:02:09.280
Now, the greenhouse effect
and greenhouse gases,
00:02:09.280 --> 00:02:12.088
the ones that I just listed,
they're oftentimes associated
00:02:12.088 --> 00:02:15.550
with man-made climate
change and global warming.
00:02:15.550 --> 00:02:17.720
And they are, for good reason,
00:02:17.720 --> 00:02:18.920
but it's important to realize
00:02:18.920 --> 00:02:22.570
that we actually need some
base level greenhouse effect
00:02:22.570 --> 00:02:25.870
just for earth to be habitable
in the way that it is.
00:02:25.870 --> 00:02:29.080
Without greenhouse gases, earth's surface
00:02:29.080 --> 00:02:32.730
would be about negative
18 degrees Celsius,
00:02:32.730 --> 00:02:35.326
which is the same as
zero degrees Fahrenheit,
00:02:35.326 --> 00:02:37.225
which I think most of
y'all would recognize
00:02:37.225 --> 00:02:39.920
is very, very, very cold
00:02:39.920 --> 00:02:42.940
relative to what the actual averages are,
00:02:42.940 --> 00:02:47.940
which are 15 degrees Celsius
or 59 degrees Fahrenheit.
00:02:48.920 --> 00:02:50.570
And of course, these are
average temperatures,
00:02:50.570 --> 00:02:53.291
but 59 is a nice refreshing brisk day,
00:02:53.291 --> 00:02:56.870
not a frigid day like
zero degrees Fahrenheit.
00:02:56.870 --> 00:02:57.930
And of course, these are averages.
00:02:57.930 --> 00:03:01.920
It fluctuates around this on
time of year and where you are.
00:03:01.920 --> 00:03:02.900
But this has makes it clear
00:03:02.900 --> 00:03:05.270
that we do need these greenhouse gases
00:03:05.270 --> 00:03:07.920
to keep the earth reasonably warm.
00:03:07.920 --> 00:03:09.020
Now, the problem is,
00:03:09.020 --> 00:03:11.660
is if the concentration
of these greenhouse gases
00:03:11.660 --> 00:03:15.490
go out of equilibrium,
become unusually high,
00:03:15.490 --> 00:03:18.860
and it does look like
that is indeed happening.
00:03:18.860 --> 00:03:20.639
This right over here is a chart,
00:03:20.639 --> 00:03:22.750
and the way that we're
able to figure that out
00:03:22.750 --> 00:03:25.340
is by taking ice samples and rock samples
00:03:25.340 --> 00:03:27.980
and looking into our past
or the geologic record
00:03:27.980 --> 00:03:30.020
of how much carbon dioxide there has been
00:03:30.020 --> 00:03:31.990
over the last 800,000 years.
00:03:31.990 --> 00:03:35.210
And 800,000 years is a
very long time period.
00:03:35.210 --> 00:03:37.100
Modern human beings have only been around
00:03:37.100 --> 00:03:40.090
for 200,000 or 300,000 years.
00:03:40.090 --> 00:03:43.370
And what you can see is the
concentration of carbon dioxide
00:03:43.370 --> 00:03:46.870
has roughly fluctuated between
about 200 parts per million
00:03:46.870 --> 00:03:48.880
and about 300 parts per million,
00:03:48.880 --> 00:03:51.290
at least over the duration of this chart.
00:03:51.290 --> 00:03:54.240
But in recent times, we've
gone well beyond that.
00:03:54.240 --> 00:03:57.810
We've almost gone double
that average right over here.
00:03:57.810 --> 00:03:59.319
And this is actually the highest levels
00:03:59.319 --> 00:04:03.430
we've seen in three million years.
00:04:03.430 --> 00:04:05.920
That's important to
realize that carbon dioxide
00:04:05.920 --> 00:04:08.760
makes up a small percentage
of our atmosphere.
00:04:08.760 --> 00:04:10.220
In fact, all of these greenhouse gases
00:04:10.220 --> 00:04:12.090
make up a small percentage.
00:04:12.090 --> 00:04:16.510
78% of the troposphere is
in nitrogen, 21% is oxygen.
00:04:16.510 --> 00:04:19.740
The last 1% is things like argon,
00:04:19.740 --> 00:04:23.130
water vapor, carbon dioxide, methane.
00:04:23.130 --> 00:04:25.050
So even this small amount,
00:04:25.050 --> 00:04:27.540
when the concentration
increases dramatically
00:04:27.540 --> 00:04:29.300
can have a huge effect.
00:04:29.300 --> 00:04:31.630
Now you might say, "Hey,
we were at these levels
00:04:31.630 --> 00:04:34.120
three million years ago roughly,
00:04:34.120 --> 00:04:36.696
maybe this is just some type of cycle
00:04:36.696 --> 00:04:38.780
that we're seeing on earth."
00:04:38.780 --> 00:04:41.720
And to recognize it,
this is indeed manmade,
00:04:41.720 --> 00:04:44.170
we just have to look at a chart like this.
00:04:44.170 --> 00:04:45.940
This tells us two things.
00:04:45.940 --> 00:04:48.850
This tells us annual
emissions in this blue line,
00:04:48.850 --> 00:04:51.660
this blue curve, and
then the total emission
00:04:51.660 --> 00:04:53.920
or the total concentration
in the atmosphere,
00:04:53.920 --> 00:04:56.870
because about one of the
things about greenhouse gas
00:04:56.870 --> 00:04:58.780
like carbon dioxide, when it's emitted,
00:04:58.780 --> 00:05:00.360
it doesn't just disappear.
00:05:00.360 --> 00:05:02.907
And we can see if we go to
the pre-industrial revolution
00:05:02.907 --> 00:05:05.910
or the early stages of
the industrial revolution,
00:05:05.910 --> 00:05:09.770
CO2 emissions were pretty
low, pretty close to zero,
00:05:09.770 --> 00:05:11.660
at least on this scale right over here.
00:05:11.660 --> 00:05:14.030
There might've been some
basic CO2 emissions,
00:05:14.030 --> 00:05:16.750
people had fires and stoves
and things like that.
00:05:16.750 --> 00:05:19.070
But then as the industrial
revolution came into play
00:05:19.070 --> 00:05:21.440
and we started using
fossil fuels more and more
00:05:21.440 --> 00:05:24.610
to fuel transportation and
factories and other things,
00:05:24.610 --> 00:05:26.460
our emissions have gone up dramatically.
00:05:26.460 --> 00:05:28.870
And this coincides with
the total concentration
00:05:28.870 --> 00:05:33.180
going well above that
800,000 year average.
00:05:33.180 --> 00:05:35.900
So it's important to keep in
mind, the greenhouse effect
00:05:35.900 --> 00:05:38.870
is needed to some degree,
but the problem is,
00:05:38.870 --> 00:05:41.130
is when the concentration
of greenhouse gases
00:05:41.130 --> 00:05:44.950
like carbon dioxide go well
beyond their historic averages,
00:05:44.950 --> 00:05:46.880
which can over time warm the earth
00:05:46.880 --> 00:05:50.230
and even a few degrees
centigrade of warming the earth
00:05:50.230 --> 00:05:52.940
can have huge consequences
on our environment
00:05:52.940 --> 00:05:54.400
and on our weather.
00:05:54.400 --> 00:05:56.830
I'll throw out one last
idea just for kicks
00:05:56.830 --> 00:05:59.180
because even though it's
called the greenhouse effect,
00:05:59.180 --> 00:06:01.990
it's actually not how
actual greenhouses work.
00:06:01.990 --> 00:06:04.400
The greenhouse effect,
as we just described it,
00:06:04.400 --> 00:06:07.526
is really based on this idea that things
00:06:07.526 --> 00:06:09.950
are getting the infrared radiation.
00:06:09.950 --> 00:06:12.610
The electromagnetic radiation
is getting reabsorbed,
00:06:12.610 --> 00:06:15.440
which then gets reemitted
back to the surface
00:06:15.440 --> 00:06:16.630
and vice right versa.
00:06:16.630 --> 00:06:17.640
In a real greenhouse,
00:06:17.640 --> 00:06:20.640
you can imagine that it
is made out of glass.
00:06:20.640 --> 00:06:24.030
What's happening is the
sunlight can come in
00:06:24.030 --> 00:06:25.720
and it's warming the surface
00:06:25.720 --> 00:06:29.260
and it's warming the air
inside the greenhouse,
00:06:29.260 --> 00:06:32.180
and then that air is not
allowed to circulate.
00:06:32.180 --> 00:06:34.880
So if the greenhouse had a little hole
00:06:34.880 --> 00:06:36.070
at the top right over here,
00:06:36.070 --> 00:06:38.040
that hot air would be allowed to go out
00:06:38.040 --> 00:06:40.530
and circulate with the cool air up here,
00:06:40.530 --> 00:06:42.420
but the air isn't allowed to mix,
00:06:42.420 --> 00:06:44.920
and so the air gets hotter
and hotter and hotter.
00:06:44.920 --> 00:06:46.590
It actually turns out that the glass
00:06:46.590 --> 00:06:49.220
can let the electromagnetic radiation out
00:06:49.220 --> 00:06:51.470
unlike greenhouse gases.
00:06:51.470 --> 00:06:54.890
So it is a different
actual physical process,
00:06:54.890 --> 00:06:57.793
but you can see where people
try to create the metaphor.
|
Cell specialization | https://www.youtube.com/watch?v=TdZr_ucEhgo | vtt | https://www.youtube.com/api/timedtext?v=TdZr_ucEhgo&ei=4VWUZf6qL9iNp-oP3eGVsA0&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245329&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=6B0FE1682530C8457163B91D5EAD74E3484AA8D5.937C62C4FFE368D7DB9BFC3CF188107DDBD6B0D9&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:02.040 --> 00:00:04.080
- [Instructor] Ah, the
basic building blocks
00:00:04.080 --> 00:00:06.823
of all living things, cells.
00:00:09.620 --> 00:00:12.040
These incredible packages of organelles
00:00:12.040 --> 00:00:13.940
and subcellular components
00:00:13.940 --> 00:00:17.030
carry out a variety of
functions in the body,
00:00:17.030 --> 00:00:19.003
like taking in nutrients,
00:00:20.950 --> 00:00:22.823
converting them into energy,
00:00:24.540 --> 00:00:27.040
and working with other
cells to produce things
00:00:27.040 --> 00:00:28.223
that the body needs.
00:00:29.550 --> 00:00:33.253
Each cell is essentially like
its own little mini factory,
00:00:34.270 --> 00:00:36.860
with complex processes
occurring within the cell
00:00:36.860 --> 00:00:38.623
to carry out specific functions.
00:00:39.790 --> 00:00:43.170
Okay, so when we zoom into
the cell to figure out
00:00:43.170 --> 00:00:46.690
how exactly these cell
processes are carried out,
00:00:46.690 --> 00:00:48.260
one of the star players
00:00:48.260 --> 00:00:53.133
is a class of biological
macromolecules known as proteins.
00:00:57.910 --> 00:00:58.810
Proteins carry out
00:00:58.810 --> 00:01:01.660
many incredibly important
tasks in the cell,
00:01:01.660 --> 00:01:05.110
such as providing structural support,
00:01:05.110 --> 00:01:07.490
aiding in chemical reactions
00:01:10.730 --> 00:01:13.283
and even building or repairing the cell.
00:01:16.020 --> 00:01:20.600
We can imagine proteins
as a chain of amino acids,
00:01:20.600 --> 00:01:23.800
kind of think of them as
like beads on a bracelet
00:01:24.870 --> 00:01:29.870
that fold and twist into distinct
three-dimensional shapes.
00:01:31.370 --> 00:01:33.490
The structure of a protein
00:01:34.610 --> 00:01:38.670
along with the chemical
properties of its amino acid,
00:01:38.670 --> 00:01:40.623
evidently, determine its function.
00:01:45.290 --> 00:01:47.950
Does it form a round, globular sphere
00:01:47.950 --> 00:01:51.080
that can attach and interact
with other compounds?
00:01:51.080 --> 00:01:54.320
Or does it twist into
long and narrow strands
00:01:54.320 --> 00:01:56.343
that can provide structural support?
00:01:57.230 --> 00:01:59.600
The huge variety of structures
00:01:59.600 --> 00:02:01.450
that proteins can take on
00:02:01.450 --> 00:02:03.850
leads to the wide range
of cellular functions
00:02:03.850 --> 00:02:05.050
that they can carry out.
00:02:06.330 --> 00:02:09.050
Okay, so now that we've
talked about proteins,
00:02:09.050 --> 00:02:10.640
let's zoom back out
00:02:10.640 --> 00:02:13.780
to analyze how different
types of cells come together
00:02:13.780 --> 00:02:17.013
to carry out a variety of
functions in an organism.
00:02:18.420 --> 00:02:21.903
This is where cell
specialization comes into play,
00:02:25.290 --> 00:02:28.700
which is the process by
which a cell takes on
00:02:28.700 --> 00:02:31.620
a specific structure and function.
00:02:31.620 --> 00:02:34.610
So to better help understand this concept,
00:02:34.610 --> 00:02:37.730
let's consider a movie theater analogy
00:02:37.730 --> 00:02:40.900
where the movie theater is your body.
00:02:40.900 --> 00:02:44.870
There is the cashier that
handles all the money,
00:02:44.870 --> 00:02:49.870
the snack vendor who handles
out popcorn and snacks
00:02:49.950 --> 00:02:51.870
and even the ticket operator
00:02:51.870 --> 00:02:54.590
who directs you to the proper screenings.
00:02:54.590 --> 00:02:55.870
In this analogy,
00:02:55.870 --> 00:02:59.370
each person has their
own distinct functions
00:02:59.370 --> 00:03:00.400
in what they handle,
00:03:00.400 --> 00:03:03.660
like money or popcorn or tickets.
00:03:03.660 --> 00:03:04.890
In a similar way,
00:03:04.890 --> 00:03:07.860
the body is also composed
of specialized cells
00:03:07.860 --> 00:03:09.023
with unique roles,
00:03:10.530 --> 00:03:14.823
such as red blood cells that
carry oxygen in the blood,
00:03:16.330 --> 00:03:20.230
muscle cells that contract and relax
00:03:20.230 --> 00:03:24.130
or even nerve cells that
carry signaling messages
00:03:24.130 --> 00:03:25.130
throughout the body.
00:03:26.170 --> 00:03:29.863
Now, remember how I told
you about proteins before?
00:03:30.810 --> 00:03:33.630
Well, cell specialization is largely based
00:03:33.630 --> 00:03:38.630
on which proteins are present
or absent in the cell.
00:03:40.410 --> 00:03:44.350
It is a cell's unique
combination of proteins
00:03:46.250 --> 00:03:48.750
that determine which
functions can be carried out.
00:03:52.900 --> 00:03:54.930
But no cell works alone,
00:03:54.930 --> 00:03:57.363
because teamwork makes the dream work.
00:03:58.470 --> 00:04:00.740
Groups of specialized cells
00:04:02.660 --> 00:04:05.820
that carry out specific
functions for the organism
00:04:05.820 --> 00:04:08.053
are organized into tissues.
00:04:11.890 --> 00:04:15.220
Looking back at our movie theater analogy,
00:04:15.220 --> 00:04:18.360
there are multiple people
within each department
00:04:18.360 --> 00:04:21.713
that work together to help the
theater function efficiently.
00:04:22.990 --> 00:04:26.020
Similarly, our specialized
cells work together
00:04:26.020 --> 00:04:28.903
as tissues to help the organism function.
00:04:29.810 --> 00:04:32.733
The red blood cells make up the blood,
00:04:33.930 --> 00:04:34.930
a connective tissue
00:04:34.930 --> 00:04:37.770
that moves important
substances throughout the body.
00:04:37.770 --> 00:04:40.750
The muscle cells help
make up muscle tissue
00:04:43.180 --> 00:04:44.790
which helps the body move
00:04:44.790 --> 00:04:48.440
and neurons or nerve cells
make up nervous tissue
00:04:50.220 --> 00:04:52.653
that helps the organism
process information.
00:04:53.610 --> 00:04:57.910
So what are the key takeaways
about cell specialization?
00:04:57.910 --> 00:05:02.010
Number one, cells are the
fundamental unit of life.
00:05:02.010 --> 00:05:03.520
They're the smallest structural
00:05:03.520 --> 00:05:06.370
and functional unit of an organism.
00:05:06.370 --> 00:05:11.170
Number two, proteins help
carry out cell processes.
00:05:11.170 --> 00:05:13.810
Number three, specialized cells carry out
00:05:13.810 --> 00:05:16.160
specific functions in an organism.
00:05:16.160 --> 00:05:18.020
Think of the movie theater analogy
00:05:18.020 --> 00:05:21.490
where each person has
its own specific role.
00:05:21.490 --> 00:05:24.270
And number four, groups
of specialized cells
00:05:24.270 --> 00:05:25.900
come together as tissues
00:05:25.900 --> 00:05:28.120
to carry out one or
more specific functions
00:05:28.120 --> 00:05:29.083
for the organism.
|
Taking and visualizing powers of a complex number | https://www.youtube.com/watch?v=VZmnLQ3CMbE | vtt | https://www.youtube.com/api/timedtext?v=VZmnLQ3CMbE&ei=5VWUZYf-CqT6mLAPppCGoAc&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=915C3F1C3B0C6C4268860B518300D60D2CE7BE4E.A771B351AA43F23963EAA4AAB6256E4DC1A73BBF&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.450 --> 00:00:02.940
- We're told to consider the
complex number z is equal
00:00:02.940 --> 00:00:05.950
to -1 plus i times the square root of 3.
00:00:05.950 --> 00:00:09.500
Find z to the fourth in
polar and rectangular form.
00:00:09.500 --> 00:00:12.250
So pause this video and see
if you can figure that out.
00:00:13.090 --> 00:00:14.910
All right, now let's work
through this together.
00:00:14.910 --> 00:00:19.320
So first let's just think
about what the modulus of z is.
00:00:19.320 --> 00:00:22.240
We know that the modulus
is going to be equal to the
00:00:22.240 --> 00:00:25.480
square root of the real part squared
00:00:25.480 --> 00:00:28.940
plus the square root of 3, plus
the imaginary part squared.
00:00:28.940 --> 00:00:33.040
So it is going to be -1 squared
00:00:33.040 --> 00:00:36.800
plus square root of 3 squared,
00:00:36.800 --> 00:00:39.400
which is going to be equal to 1 plus 3.
00:00:39.400 --> 00:00:43.300
So principal root of
4, which is equal to 2.
00:00:43.300 --> 00:00:44.910
Now the next interesting question is,
00:00:44.910 --> 00:00:47.540
what is the argument of z?
00:00:47.540 --> 00:00:49.300
And the reason why I'm
even going through this is
00:00:49.300 --> 00:00:50.850
once we put it into polar form,
00:00:50.850 --> 00:00:53.720
it's going to be a lot
easier to both visualize
00:00:53.720 --> 00:00:56.640
what it means to take the
various exponents of it.
00:00:56.640 --> 00:00:59.850
And then we can convert
back into rectangular form.
00:00:59.850 --> 00:01:04.850
And so let us, let me draw
another complex plane here.
00:01:05.790 --> 00:01:07.130
Imaginary axis.
00:01:07.130 --> 00:01:10.410
That is my real axis.
00:01:10.410 --> 00:01:14.100
And if I were to plot z, it
would look something like this.
00:01:14.100 --> 00:01:16.160
We have -1 in the real direction.
00:01:16.160 --> 00:01:18.530
So that might be -1 there.
00:01:18.530 --> 00:01:22.940
And we have square root of 3
in the imaginary direction,
00:01:22.940 --> 00:01:24.120
square root of 3.
00:01:24.120 --> 00:01:27.950
So our point z is right over here
00:01:27.950 --> 00:01:32.090
and we know the distance
from the origin, the modulus,
00:01:32.090 --> 00:01:35.630
we know that this distance
right over here is 2.
00:01:35.630 --> 00:01:38.050
We know that this distance right over here
00:01:38.050 --> 00:01:40.000
is square root of 3.
00:01:40.000 --> 00:01:44.540
And we know that this
distance right over here is 1.
00:01:44.540 --> 00:01:46.650
And so you might
immediately recognize this
00:01:46.650 --> 00:01:50.470
as a 30-60-90 triangle because
in a 30-60-90 triangle,
00:01:50.470 --> 00:01:53.680
the short side is half of the hypotenuse,
00:01:53.680 --> 00:01:55.840
and the long side is the square root of 3
00:01:55.840 --> 00:01:57.400
times the short side.
00:01:57.400 --> 00:02:00.450
So we know that this is a 60-degree angle.
00:02:00.450 --> 00:02:02.820
We know that this is a 30-degree angle.
00:02:02.820 --> 00:02:04.460
And the reason why that helps us,
00:02:04.460 --> 00:02:06.340
sorry, it's hard to see that 30 degree.
00:02:06.340 --> 00:02:07.830
The reason why that helps us is
00:02:07.830 --> 00:02:09.540
if this is 60 degrees,
00:02:09.540 --> 00:02:14.540
we know that the argument
here must be 120 degrees.
00:02:14.970 --> 00:02:19.610
So the arg of z, the argument
of z, is 120 degrees.
00:02:19.610 --> 00:02:20.880
And so just like that
00:02:20.880 --> 00:02:24.210
we can now think about z in polar form.
00:02:24.210 --> 00:02:26.360
So let me write it right over here.
00:02:26.360 --> 00:02:31.360
We can write that z is
equal to its modulus, 2,
00:02:31.370 --> 00:02:34.153
times the cosine of 120 degrees,
00:02:36.486 --> 00:02:39.569
plus i times the sine of 120 degrees.
00:02:41.660 --> 00:02:44.990
And we could also
visualize z now over here.
00:02:44.990 --> 00:02:48.030
So its modulus is 2.
00:02:48.030 --> 00:02:53.030
So that's halfway to 4, and
its argument is 120 degrees.
00:02:53.820 --> 00:02:56.450
So it would put us right over here.
00:02:56.450 --> 00:03:00.140
This is where z is.
00:03:00.140 --> 00:03:02.933
Now, what would z squared be?
00:03:03.830 --> 00:03:05.700
Well, when you multiply complex numbers
00:03:05.700 --> 00:03:08.740
and you've represented them in polar form,
00:03:08.740 --> 00:03:11.570
we know that you would
multiply the moduli,
00:03:11.570 --> 00:03:13.690
so it would then be 2 squared.
00:03:13.690 --> 00:03:15.500
So it'd be 4 right over here.
00:03:15.500 --> 00:03:18.220
And then you would add the arguments.
00:03:18.220 --> 00:03:21.560
So you would essentially
rotate z by another 120 degrees
00:03:21.560 --> 00:03:23.000
'cause you're multiplying it by z.
00:03:23.000 --> 00:03:26.680
So it's going to be cosine of 240 degrees
00:03:26.680 --> 00:03:31.680
plus i sine of 240 degrees.
00:03:31.800 --> 00:03:34.440
Once again, 2 times 2 is equal to 4.
00:03:34.440 --> 00:03:38.290
120 degrees plus another
120 degrees is 240 degrees.
00:03:38.290 --> 00:03:41.240
And so now where would z squared sit?
00:03:41.240 --> 00:03:46.140
Well, its argument is 240
degrees and its modulus is 4.
00:03:46.140 --> 00:03:50.000
So now it is twice as far from the origin.
00:03:50.000 --> 00:03:51.930
And now let's think about what,
00:03:51.930 --> 00:03:53.520
I'll do this in a new color,
00:03:53.520 --> 00:03:56.563
what z to the third power
is going to be equal to.
00:03:57.420 --> 00:04:00.180
Well, that's going to be
z squared times z again.
00:04:00.180 --> 00:04:03.350
So we're gonna multiply
2 times this modulus.
00:04:03.350 --> 00:04:06.130
So that's going to be equal to 8 times,
00:04:06.130 --> 00:04:09.330
and then we're going to rotate
z squared by 120 degrees.
00:04:09.330 --> 00:04:14.330
So cosine of 360 degrees
00:04:14.870 --> 00:04:19.113
plus i sine of 360 degrees.
00:04:20.900 --> 00:04:25.270
And so that's going to put
us at 8 for our modulus.
00:04:25.270 --> 00:04:27.670
And 360 degrees is the
same thing as zero degrees.
00:04:27.670 --> 00:04:29.190
So we are right over here.
00:04:29.190 --> 00:04:32.260
So this is z to the third power.
00:04:32.260 --> 00:04:34.520
And I think, you know where this is going.
00:04:34.520 --> 00:04:37.480
What is z to the fourth power going to be?
00:04:37.480 --> 00:04:39.410
Let me move my screen down a little bit
00:04:39.410 --> 00:04:41.490
so I have a little more real estate.
00:04:41.490 --> 00:04:43.060
z to the 4th.
00:04:43.060 --> 00:04:45.260
Well, I'm just gonna
take this modulus here
00:04:45.260 --> 00:04:47.684
since I'm going to multiply
z to the third times z,
00:04:47.684 --> 00:04:51.810
I'm gonna multiply that
modulus times 2 to get to 16.
00:04:51.810 --> 00:04:55.370
And then I'm going to
add another 120 degrees.
00:04:55.370 --> 00:04:58.800
Well, I could write cosine of 480 degrees,
00:04:58.800 --> 00:05:01.760
or 360 degrees is the same
thing as zero degrees.
00:05:01.760 --> 00:05:05.710
So this I could say is zero
degrees. This is zero degrees.
00:05:05.710 --> 00:05:09.473
So if I add 120 to that, I
get cosine of 120 degrees.
00:05:11.504 --> 00:05:13.754
Plus i sine of 120 degrees.
00:05:15.910 --> 00:05:19.580
So my argument is back
to being at 120 degrees,
00:05:19.580 --> 00:05:21.790
but now my modulus is 16.
00:05:21.790 --> 00:05:23.740
So there's 4, 8, 12, 16,
00:05:23.740 --> 00:05:25.840
this outer circle right over here.
00:05:25.840 --> 00:05:29.910
I am right over there
with z to the fourth.
00:05:29.910 --> 00:05:30.910
So we're almost done.
00:05:30.910 --> 00:05:34.450
We've just represented z to
the fourth in polar form.
00:05:34.450 --> 00:05:37.780
Now we just have to think
about it in rectangular form.
00:05:37.780 --> 00:05:39.570
Now, lucky for us,
00:05:39.570 --> 00:05:42.020
we already know what
cosine of 120 degrees is
00:05:42.020 --> 00:05:45.430
and sine of 120 degrees is.
00:05:45.430 --> 00:05:48.160
It is, we can construct if we want
00:05:48.160 --> 00:05:52.410
another 30-60-90 triangle right over here.
00:05:52.410 --> 00:05:56.930
So the hypotenuse here has length 16.
00:05:56.930 --> 00:05:59.000
The short side is going to be 1/2 of that.
00:05:59.000 --> 00:06:00.320
So it has length 8.
00:06:00.320 --> 00:06:02.620
And then the long side is
gonna be square root of 3
00:06:02.620 --> 00:06:03.680
times the short side.
00:06:03.680 --> 00:06:06.170
So it's going to be 8 square roots of 3.
00:06:06.170 --> 00:06:08.180
So if we wanted to write z to the fourth
00:06:08.180 --> 00:06:10.690
in rectangular form,
00:06:10.690 --> 00:06:13.223
it would be the real part is -8.
00:06:14.270 --> 00:06:19.270
Plus i times 8 square
roots of 3, and we're done.
|
Indoor air pollutants | https://www.youtube.com/watch?v=nqRPRwO79kg | vtt | https://www.youtube.com/api/timedtext?v=nqRPRwO79kg&ei=5VWUZcqeD9WNmLAP6pCFoAg&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=4874ECE50FEA59FBB7974C172687C417175BE284.7CEE2769DE496242B3A660010DFBAC81A67600F3&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.530 --> 00:00:03.260
- [Instructor] Let's talk
about indoor air pollution.
00:00:03.260 --> 00:00:05.950
I remember when I first heard
about indoor air pollution
00:00:05.950 --> 00:00:08.320
in my AP environmental science class,
00:00:08.320 --> 00:00:10.370
I was a little confused.
00:00:10.370 --> 00:00:12.280
When I used to think of pollution,
00:00:12.280 --> 00:00:14.420
I would think of images like this
00:00:14.420 --> 00:00:15.850
or this.
00:00:15.850 --> 00:00:18.380
But pollution is often invisible,
00:00:18.380 --> 00:00:21.540
and it isn't just
restricted to the outdoors.
00:00:21.540 --> 00:00:25.170
Indoor air pollutants can lead
to serious health conditions
00:00:25.170 --> 00:00:26.930
and even death.
00:00:26.930 --> 00:00:29.030
But there are ways to identify
00:00:29.030 --> 00:00:31.400
and prevent indoor air pollution.
00:00:31.400 --> 00:00:33.360
Let's take a look at an example.
00:00:33.360 --> 00:00:34.730
This is Ava.
00:00:34.730 --> 00:00:37.560
And let's say Ava, like many
other people in the world,
00:00:37.560 --> 00:00:40.210
spends the majority of her time indoors.
00:00:40.210 --> 00:00:44.350
She works, sleeps, cooks,
and eats in her home.
00:00:44.350 --> 00:00:46.950
And lately, she's been
experiencing headaches
00:00:46.950 --> 00:00:48.630
and she's been coughing.
00:00:48.630 --> 00:00:51.620
A possible culprit is
indoor air pollution.
00:00:51.620 --> 00:00:54.730
So, where could the indoor
air pollution be coming from?
00:00:54.730 --> 00:00:57.010
Let's take a look at Ava's house.
00:00:57.010 --> 00:00:58.640
Indoor air pollution can come from
00:00:58.640 --> 00:01:00.610
many different kinds of sources,
00:01:00.610 --> 00:01:03.550
both human-made and natural.
00:01:03.550 --> 00:01:05.650
Ava's furniture, paneling, and carpets
00:01:05.650 --> 00:01:08.300
could be releasing
volatile organic compounds,
00:01:08.300 --> 00:01:11.130
which are often written down as VOCs,
00:01:11.130 --> 00:01:12.960
and they basically include substances
00:01:12.960 --> 00:01:17.080
that form gases at room
temperature, like formaldehyde.
00:01:17.080 --> 00:01:19.030
Formaldehyde is used as an adhesive
00:01:19.030 --> 00:01:21.110
in building materials and upholstery,
00:01:21.110 --> 00:01:22.990
and it can get into the air.
00:01:22.990 --> 00:01:25.560
This is the same stuff
that is used to embalm
00:01:25.560 --> 00:01:27.620
and preserve dead bodies.
00:01:27.620 --> 00:01:30.700
In other words, it's not
pleasant to breathe in.
00:01:30.700 --> 00:01:33.210
The United States
Environmental Protection Agency
00:01:33.210 --> 00:01:35.140
says that formaldehyde is one of the four
00:01:35.140 --> 00:01:38.320
most dangerous air
pollutants in the country.
00:01:38.320 --> 00:01:41.630
Formaldehyde can make
you dizzy and nauseated.
00:01:41.630 --> 00:01:45.610
And if you're exposed to
enough of it, it can kill you.
00:01:45.610 --> 00:01:48.880
Indoor air pollutants can also
come from Ava's house itself
00:01:48.880 --> 00:01:53.080
in the form of particulates,
which are teeny-tiny particles
00:01:53.080 --> 00:01:56.120
so small that they can
stay suspended in the air.
00:01:56.120 --> 00:01:58.320
And they can be really dangerous
00:01:58.320 --> 00:02:00.650
because they can travel
deep into the lungs
00:02:00.650 --> 00:02:02.480
and damage cells.
00:02:02.480 --> 00:02:05.460
One such particulate is asbestos.
00:02:05.460 --> 00:02:09.260
It's actually, in my opinion,
a really cool substance.
00:02:09.260 --> 00:02:11.060
It's an electrical insulator,
00:02:11.060 --> 00:02:14.210
and it's fireproof and it's acid-proof.
00:02:14.210 --> 00:02:16.880
And there was a time when
many houses were being built
00:02:16.880 --> 00:02:19.150
with asbestos in its building insulation,
00:02:19.150 --> 00:02:20.830
flooring, and roofing.
00:02:20.830 --> 00:02:24.060
It's actually a natural
material that's mined,
00:02:24.060 --> 00:02:27.630
and it has light fluffy fibers
that can be woven into cloth.
00:02:27.630 --> 00:02:30.460
To me, it always looked like unicorn hair.
00:02:30.460 --> 00:02:33.400
But really, it's more
like evil unicorn hair.
00:02:33.400 --> 00:02:36.080
Each fiber can break
into microscopic pieces
00:02:36.080 --> 00:02:37.580
that could scar your lungs
00:02:37.580 --> 00:02:41.050
and lead to lung cancer
and other lung diseases.
00:02:41.050 --> 00:02:42.640
Particulates in Ava's house
00:02:42.640 --> 00:02:44.650
could also be coming from the paint.
00:02:44.650 --> 00:02:47.920
Lead paint in Ava's house
could begin to chip away
00:02:47.920 --> 00:02:50.920
and could suspend small
particles in the air.
00:02:50.920 --> 00:02:53.320
These particles could
cause lead poisoning,
00:02:53.320 --> 00:02:56.730
which can cause headaches
and nerve and brain damage.
00:02:56.730 --> 00:02:59.430
The use of lead and
asbestos has been restricted
00:02:59.430 --> 00:03:01.400
by many governments around the world,
00:03:01.400 --> 00:03:04.363
but these materials can still
be found in older buildings.
00:03:05.480 --> 00:03:08.050
Another way inside air can become polluted
00:03:08.050 --> 00:03:11.393
is through combustion, which
is to say burning stuff.
00:03:12.240 --> 00:03:14.910
Combustion can cause a
wide variety of pollutants
00:03:14.910 --> 00:03:18.670
that can irritate lungs,
including carbon monoxide,
00:03:18.670 --> 00:03:22.823
nitrogen oxides, sulfur
dioxide, and particulates.
00:03:24.520 --> 00:03:27.900
One way that carbon monoxide
can build up inside a building
00:03:27.900 --> 00:03:30.370
is from a poorly-maintained furnace.
00:03:30.370 --> 00:03:33.440
Carbon monoxide molecules
have a secret weapon.
00:03:33.440 --> 00:03:35.760
They can trick the proteins in your blood
00:03:35.760 --> 00:03:37.740
into thinking they're oxygen.
00:03:37.740 --> 00:03:39.743
This can cause asphyxiation,
00:03:40.840 --> 00:03:43.520
which is when the body
cannot get enough oxygen,
00:03:43.520 --> 00:03:45.470
and it can be deadly.
00:03:45.470 --> 00:03:48.270
Ava should make sure that her
furnace is well maintained
00:03:48.270 --> 00:03:50.110
and serviced regularly.
00:03:50.110 --> 00:03:51.860
Combustion-related air pollution
00:03:51.860 --> 00:03:53.950
doesn't just come from furnaces, though.
00:03:53.950 --> 00:03:56.350
In less economically-developed countries,
00:03:56.350 --> 00:03:59.860
families sometimes use open
fires for heating and cooking.
00:03:59.860 --> 00:04:04.360
People often burn wood, peat,
and even coal inside homes
00:04:04.360 --> 00:04:06.690
without the necessary
ventilation to circulate
00:04:06.690 --> 00:04:08.970
and dilute the pollutants in the air.
00:04:08.970 --> 00:04:10.630
Combustion-related air pollution
00:04:10.630 --> 00:04:13.570
can also come from poorly
ventilated fireplaces
00:04:13.570 --> 00:04:14.923
and tobacco smoke.
00:04:16.150 --> 00:04:17.910
So, what could Eva do to reduce
00:04:17.910 --> 00:04:19.960
combustion-related air pollution?
00:04:19.960 --> 00:04:22.580
Well, she could open the windows
00:04:22.580 --> 00:04:24.760
and she could use fans to mix the smoke
00:04:24.760 --> 00:04:27.000
and pollution with outside air.
00:04:27.000 --> 00:04:30.030
Ava should also install a
carbon monoxide detector
00:04:30.030 --> 00:04:32.130
to make sure that the air is safe.
00:04:32.130 --> 00:04:34.750
A carbon monoxide detector
could also detect leaks
00:04:34.750 --> 00:04:36.993
from natural gas stoves or heaters.
00:04:37.930 --> 00:04:41.220
It's also possible that Ava's
house has natural pollutants,
00:04:41.220 --> 00:04:44.550
like mold, dust, or even radon.
00:04:44.550 --> 00:04:47.140
Mold is a type of microscopic fungus
00:04:47.140 --> 00:04:49.420
that's always floating around in the air,
00:04:49.420 --> 00:04:52.950
and breathing it in can cause
itchy eyes, runny noses,
00:04:52.950 --> 00:04:55.440
and it can trigger asthma attacks.
00:04:55.440 --> 00:04:58.200
And mold loves moisture.
00:04:58.200 --> 00:05:00.100
So, when the air is really humid,
00:05:00.100 --> 00:05:03.520
there will be more mold spores,
which is good for the molds,
00:05:03.520 --> 00:05:05.400
but bad for us.
00:05:05.400 --> 00:05:08.240
And what areas of the house
tend to have the most moisture?
00:05:08.240 --> 00:05:10.190
The bathrooms and the kitchen,
00:05:10.190 --> 00:05:12.980
so these areas especially
need to have windows
00:05:12.980 --> 00:05:15.960
that can be opened or air
fans that can draw moisture
00:05:15.960 --> 00:05:18.530
and the molds outta the house.
00:05:18.530 --> 00:05:22.300
Another kind of natural
indoor air pollutant is radon,
00:05:22.300 --> 00:05:25.360
which is a radioactive noble gas.
00:05:25.360 --> 00:05:27.110
It's produced by the natural decay
00:05:27.110 --> 00:05:29.443
of radioactive rocks in the ground.
00:05:30.550 --> 00:05:33.380
Let's say that Ava's
basement has some cracks
00:05:33.380 --> 00:05:35.530
in the foundation and the walls.
00:05:35.530 --> 00:05:37.550
That would mean that
when radon seeps upward
00:05:37.550 --> 00:05:40.210
through the soil, it
could enter these cracks
00:05:40.210 --> 00:05:42.920
and be stuck inside Ava's house.
00:05:42.920 --> 00:05:45.730
Breathing in too much radon
could damage lung tissue
00:05:45.730 --> 00:05:47.930
and even lead to lung cancer,
00:05:47.930 --> 00:05:50.000
depending on where the house is built.
00:05:50.000 --> 00:05:52.150
Some places, like Ava's house,
00:05:52.150 --> 00:05:54.940
are more likely to have radon than others.
00:05:54.940 --> 00:05:57.970
Ava can prevent radon exposure
by sealing up the cracks
00:05:57.970 --> 00:05:59.890
in the foundation of her house
00:05:59.890 --> 00:06:02.460
and by ventilating her basement.
00:06:02.460 --> 00:06:06.050
Some indoor air pollution
requires professional remediation.
00:06:06.050 --> 00:06:08.330
To get rid of asbestos, for example,
00:06:08.330 --> 00:06:11.030
an accredited asbestos
abatement specialist
00:06:11.030 --> 00:06:14.300
basically shows up in a
biohazard suit like this.
00:06:14.300 --> 00:06:16.500
That's how dangerous it is.
00:06:16.500 --> 00:06:18.000
For other situations,
00:06:18.000 --> 00:06:21.810
there's a simple solution to
Ava's problem: ventilation.
00:06:21.810 --> 00:06:23.050
Ava could open windows
00:06:23.050 --> 00:06:26.200
on the opposing sides of
her home just a crack.
00:06:26.200 --> 00:06:28.000
The outdoor air would flow in,
00:06:28.000 --> 00:06:30.090
dilute the indoor air pollutants,
00:06:30.090 --> 00:06:32.080
and carry them outta the house.
00:06:32.080 --> 00:06:35.260
This natural ventilation
allows the air to circulate
00:06:35.260 --> 00:06:38.400
and reduces the buildup
of indoor air pollutants.
00:06:38.400 --> 00:06:40.850
There are a lot of ways
that indoor air pollutants
00:06:40.850 --> 00:06:43.650
could sneak into Ava's house, from nature,
00:06:43.650 --> 00:06:47.050
from combustion, and
from human-made items.
00:06:47.050 --> 00:06:48.820
Being aware of these sources can help Ava
00:06:48.820 --> 00:06:50.490
make sure that the air inside her house
00:06:50.490 --> 00:06:52.653
is fresh, clean, and healthy.
|
Human impact on aquatic environments | https://www.youtube.com/watch?v=nZjMRq9tev8 | vtt | https://www.youtube.com/api/timedtext?v=nZjMRq9tev8&ei=5VWUZeTtFL-ShcIPp9KnoAo&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=C0391BCA17FC11E1913FE3D9918AB5CFD554E795.618164E9D693CF972420124505BF39369A6861CD&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.230 --> 00:00:01.200
- [Narrator] When you go to the beach
00:00:01.200 --> 00:00:04.630
and you look at the ocean, it
oftentimes might look fine.
00:00:04.630 --> 00:00:05.910
But as we'll see in this video,
00:00:05.910 --> 00:00:09.210
we, human beings have been
stressing aquatic environments.
00:00:09.210 --> 00:00:12.850
And if we're not careful, we
might completely ruin them.
00:00:12.850 --> 00:00:17.850
For example, this is what a
healthy coral reef looks like.
00:00:18.160 --> 00:00:21.500
And coral are fascinating organisms.
00:00:21.500 --> 00:00:25.050
You can view them as little
animals that are fixed in place
00:00:25.050 --> 00:00:28.280
because they're releasing
this calcium carbonate
00:00:28.280 --> 00:00:30.430
the same things that eggshells are made of
00:00:30.430 --> 00:00:31.680
that they're fixed too
00:00:31.680 --> 00:00:34.550
and then that builds the coral reef.
00:00:34.550 --> 00:00:37.640
But they can exist, they
have their homeostasis
00:00:37.640 --> 00:00:39.900
in a particular temperature range
00:00:39.900 --> 00:00:43.140
and a given amount of various chemicals
00:00:43.140 --> 00:00:45.150
that are in the water.
00:00:45.150 --> 00:00:47.270
Now we know that human beings
00:00:47.270 --> 00:00:49.300
were causing the climate to warm,
00:00:49.300 --> 00:00:52.570
and that's all also causing
ocean temperatures to warm
00:00:52.570 --> 00:00:54.640
and as ocean temperatures warm,
00:00:54.640 --> 00:00:59.320
many of our coral reefs are
not able to be as sustainable.
00:00:59.320 --> 00:01:03.410
For example, this is a
less healthy coral reef.
00:01:03.410 --> 00:01:07.020
Some of the coral is still
alive and seemingly doing okay,
00:01:07.020 --> 00:01:10.790
but in other places, you see
what is known as bleaching,
00:01:10.790 --> 00:01:12.830
where the reef is now white
00:01:12.830 --> 00:01:15.030
and that's because in those situations,
00:01:15.030 --> 00:01:17.380
the coral is essentially dying off.
00:01:17.380 --> 00:01:19.010
Now you might say, well,
this is unfortunate
00:01:19.010 --> 00:01:21.490
because coral reefs are very beautiful
00:01:21.490 --> 00:01:23.760
and now it is less beautiful.
00:01:23.760 --> 00:01:25.550
But what are the other impacts?
00:01:25.550 --> 00:01:28.240
Well, all sorts of organisms and animals
00:01:28.240 --> 00:01:31.000
live in coral reefs,
get their food from it,
00:01:31.000 --> 00:01:32.150
get their shelter from it
00:01:32.150 --> 00:01:33.780
and if the coral reef start to die off,
00:01:33.780 --> 00:01:35.630
then the animals are going to die off.
00:01:35.630 --> 00:01:37.490
On top of that, these coral reefs
00:01:37.490 --> 00:01:40.700
that the coral are essentially
building as they live,
00:01:40.700 --> 00:01:43.200
they prevent erosion on the coastlines.
00:01:43.200 --> 00:01:45.580
So one change that affects one organism
00:01:45.580 --> 00:01:47.180
or one part of an ecosystem
00:01:47.180 --> 00:01:49.260
can have a lot of follow on effects
00:01:49.260 --> 00:01:52.080
on other parts of the ecosystem.
00:01:52.080 --> 00:01:54.130
Another perhaps more obvious way
00:01:54.130 --> 00:01:57.580
that we've been not being
nice to aquatic environments
00:01:57.580 --> 00:01:59.820
is things like oil spills.
00:01:59.820 --> 00:02:01.650
And you've probably seen this on the news
00:02:01.650 --> 00:02:03.220
when you have major oil spills,
00:02:03.220 --> 00:02:05.350
they tend to be pretty disturbing images,
00:02:05.350 --> 00:02:07.820
but this right here is a
bird that is covered in oil.
00:02:07.820 --> 00:02:10.420
And you can imagine when
a bird is covered in oil,
00:02:10.420 --> 00:02:12.250
it's not going to be able to fly,
00:02:12.250 --> 00:02:13.760
it's not going to be able to swim,
00:02:13.760 --> 00:02:15.450
it's not going to be able to have food
00:02:15.450 --> 00:02:18.110
and in a lot of cases,
it is likely to die.
00:02:18.110 --> 00:02:20.350
And just as we described
at the coral reef,
00:02:20.350 --> 00:02:22.030
this doesn't just affect the bird,
00:02:22.030 --> 00:02:25.610
it affects the entire ecosystem,
including human beings.
00:02:25.610 --> 00:02:27.500
And this is just the effect on a bird,
00:02:27.500 --> 00:02:28.630
it has affects on the fish,
00:02:28.630 --> 00:02:31.770
it has effects on the just natural balance
00:02:31.770 --> 00:02:33.833
that occurs in that aquatic environment.
00:02:34.670 --> 00:02:38.380
Now, another idea that
is less talked about
00:02:38.380 --> 00:02:42.240
is this notion of oceanic dead zones.
00:02:42.240 --> 00:02:46.210
And this right over here is
a picture of the gulf coast
00:02:46.210 --> 00:02:48.010
right off the coast of Louisiana,
00:02:48.010 --> 00:02:51.420
I was actually born right around there.
00:02:51.420 --> 00:02:55.300
And what it shows is every
year, this hypoxic zone,
00:02:55.300 --> 00:02:59.210
which is a zone of low oxygen
levels in the water form
00:02:59.210 --> 00:03:01.350
off the coast, and this
shows how bad it is.
00:03:01.350 --> 00:03:04.890
The red areas are the
really bad, very low oxygen.
00:03:04.890 --> 00:03:06.990
Sometimes you might forget,
and you might say, okay,
00:03:06.990 --> 00:03:10.080
for all of us who live in
the land or live on the land
00:03:10.080 --> 00:03:12.140
or in the air, we breathe oxygen,
00:03:12.140 --> 00:03:15.010
but organisms in the
water need oxygen as well.
00:03:15.010 --> 00:03:17.270
Oxygen that has been
dissolved in the water.
00:03:17.270 --> 00:03:19.430
And what's interesting is why this forms,
00:03:19.430 --> 00:03:21.720
it's actually a little
bit counter-intuitive.
00:03:21.720 --> 00:03:24.640
It turns out that chemicals
from human runoff,
00:03:24.640 --> 00:03:25.710
especially fertilizer.
00:03:25.710 --> 00:03:27.230
So you might not realize it,
00:03:27.230 --> 00:03:29.460
but this is the Delta of
the Mississippi river.
00:03:29.460 --> 00:03:31.860
And that has run off farm runoff
00:03:31.860 --> 00:03:35.650
from as far north as Minnesota
and Chicago and sewage
00:03:35.650 --> 00:03:39.010
and that farm runoff and that
fertilizer and that sewage,
00:03:39.010 --> 00:03:41.350
as it comes into the Gulf,
00:03:41.350 --> 00:03:44.180
it actually promotes algae formation.
00:03:44.180 --> 00:03:45.470
And you might say, well, that's good.
00:03:45.470 --> 00:03:48.890
Some more life is growing,
but so much algae gets formed
00:03:48.890 --> 00:03:52.570
and when that algae finally
dies and it gets decomposed,
00:03:52.570 --> 00:03:55.110
the decomposers actually use the oxygen.
00:03:55.110 --> 00:03:58.130
Remember, when you are actually
trying to metabolize things,
00:03:58.130 --> 00:04:01.180
you're using oxygen in order
to extract that energy.
00:04:01.180 --> 00:04:04.710
And so the oxygen in the ocean
in that area gets depleted,
00:04:04.710 --> 00:04:06.180
and then you have a situation
00:04:06.180 --> 00:04:08.460
where almost nothing can live
00:04:08.460 --> 00:04:10.480
in these zones right over here.
00:04:10.480 --> 00:04:12.450
And this is just a sample of the things
00:04:12.450 --> 00:04:14.270
that we are doing to
our aquatic environment.
00:04:14.270 --> 00:04:15.460
And there's other things,
00:04:15.460 --> 00:04:17.760
there's elemental sources of mercury
00:04:17.760 --> 00:04:19.460
that we throw into aquatic environments,
00:04:19.460 --> 00:04:21.660
and it makes the water highly toxic.
00:04:21.660 --> 00:04:24.670
There's obviously other
forms of trash, pollution,
00:04:24.670 --> 00:04:25.840
that we've put into the water
00:04:25.840 --> 00:04:27.210
but this is just to give you a sense
00:04:27.210 --> 00:04:29.210
and to start giving you an appreciation
00:04:29.210 --> 00:04:31.410
about how imbalanced everything is
00:04:31.410 --> 00:04:35.270
and how in one part of
the country say in Chicago
00:04:35.270 --> 00:04:37.870
waste that's going into
the Mississippi River
00:04:37.870 --> 00:04:41.113
can affect aquatic environments,
thousands of miles away.
|
Dividing complex numbers in polar form | https://www.youtube.com/watch?v=lyWaNZ1ERMw | vtt | https://www.youtube.com/api/timedtext?v=lyWaNZ1ERMw&ei=5VWUZby6HOW4mLAP6sWjqAg&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=17EF6E7759197FFC78B04BF48BF799729DDA5E5F.1AE623BBC8E6CA6533EB7DDF18002A5BB8A284FC&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.330 --> 00:00:02.620
- [Narrator] So we are given
these two complex numbers
00:00:02.620 --> 00:00:03.453
and we want to know
00:00:03.453 --> 00:00:07.010
what W sub one divided by W sub two is.
00:00:07.010 --> 00:00:09.760
So pause this video and see
if you can figure that out.
00:00:10.620 --> 00:00:13.760
All right, now let's work
through this together.
00:00:13.760 --> 00:00:15.760
So the form that they've written this in
00:00:15.760 --> 00:00:18.080
it actually makes it
pretty straightforward
00:00:18.080 --> 00:00:20.270
to spot the modulus
00:00:20.270 --> 00:00:23.670
and the argument of each
of these complex numbers.
00:00:23.670 --> 00:00:25.920
The modulus of W sub one
00:00:25.920 --> 00:00:28.780
we can see out here is equal to eight.
00:00:28.780 --> 00:00:30.180
And the argument
00:00:30.180 --> 00:00:31.870
of W sub one
00:00:31.870 --> 00:00:32.703
we can see
00:00:32.703 --> 00:00:34.960
is four Pi over three
00:00:34.960 --> 00:00:36.760
if we're thinking in terms of radians.
00:00:36.760 --> 00:00:41.360
So four Pi over three
radians, and then similarly
00:00:41.360 --> 00:00:43.620
for W sub two
00:00:43.620 --> 00:00:45.060
its modulus
00:00:45.060 --> 00:00:46.570
is equal to
00:00:46.570 --> 00:00:47.403
two
00:00:47.403 --> 00:00:49.620
and its argument
00:00:49.620 --> 00:00:50.810
is equal to
00:00:50.810 --> 00:00:53.163
seven Pi over six.
00:00:54.230 --> 00:00:55.800
Seven
00:00:55.800 --> 00:00:56.633
Pi
00:00:57.590 --> 00:00:59.250
over six.
00:00:59.250 --> 00:01:00.730
Now, in many videos
00:01:00.730 --> 00:01:02.320
we have talked about when you multiply
00:01:02.320 --> 00:01:04.220
one complex number by another
00:01:04.220 --> 00:01:05.780
you're essentially transforming it.
00:01:05.780 --> 00:01:08.680
So you are going to
scale the modulus of one
00:01:08.680 --> 00:01:10.030
by the modulus of the other.
00:01:10.030 --> 00:01:12.500
And you're going to
rotate the argument of one
00:01:12.500 --> 00:01:14.780
by the argument of the
other, I guess you could say
00:01:14.780 --> 00:01:16.930
you're going to add the angles.
00:01:16.930 --> 00:01:18.840
So another way to think about it is
00:01:18.840 --> 00:01:23.840
if you have the modulus of W
sub one divided by W sub two.
00:01:23.840 --> 00:01:26.810
Well then you're just going
to divide these moduli here.
00:01:26.810 --> 00:01:29.550
So this is just going to be eight over two
00:01:29.550 --> 00:01:31.380
which is equal to four.
00:01:31.380 --> 00:01:33.340
And then the argument
00:01:33.340 --> 00:01:34.610
of
00:01:34.610 --> 00:01:35.460
W
00:01:35.460 --> 00:01:36.660
sub one
00:01:36.660 --> 00:01:38.900
over W sub two.
00:01:38.900 --> 00:01:42.360
This is, you could imagine
you're starting at W sub one
00:01:42.360 --> 00:01:46.260
and then you are going
to rotate it clockwise
00:01:46.260 --> 00:01:48.540
by W sub two's argument.
00:01:48.540 --> 00:01:51.330
And so this is going to be four Pi
00:01:51.330 --> 00:01:52.310
over three
00:01:52.310 --> 00:01:53.300
minus
00:01:53.300 --> 00:01:54.970
seven Pi
00:01:54.970 --> 00:01:55.920
over six.
00:01:55.920 --> 00:01:57.230
And let's see what this is going to be.
00:01:57.230 --> 00:02:00.440
If we have a common
denominator four Pi over three
00:02:00.440 --> 00:02:04.010
is the same thing as eight Pi over six
00:02:04.010 --> 00:02:06.080
minus seven Pi
00:02:06.080 --> 00:02:07.260
over six
00:02:07.260 --> 00:02:10.550
which is going to be equal to Pi over six.
00:02:10.550 --> 00:02:12.340
And so we could write this,
00:02:12.340 --> 00:02:13.410
the
00:02:13.410 --> 00:02:14.560
quotient
00:02:14.560 --> 00:02:17.110
W one divided by W two
00:02:17.110 --> 00:02:18.260
is going to be equal to
00:02:18.260 --> 00:02:19.700
if we wanted to write it in this form
00:02:19.700 --> 00:02:22.140
its modulus is equal to four.
00:02:22.140 --> 00:02:23.720
It's going to be four times
00:02:23.720 --> 00:02:24.930
cosine
00:02:24.930 --> 00:02:26.870
of Pi over six
00:02:26.870 --> 00:02:27.890
plus
00:02:27.890 --> 00:02:28.740
i
00:02:28.740 --> 00:02:30.330
times sine
00:02:30.330 --> 00:02:32.090
of Pi
00:02:32.090 --> 00:02:33.960
over six.
00:02:33.960 --> 00:02:36.950
Now cosine of Pi over
six, we can figure out
00:02:36.950 --> 00:02:40.280
Pi over six is the same
thing as a 30 degree angle.
00:02:40.280 --> 00:02:42.270
And so the cosine of that
00:02:42.270 --> 00:02:44.160
is square root of three over two
00:02:44.160 --> 00:02:46.060
square root three over two.
00:02:46.060 --> 00:02:48.930
And the sine of Pi over six
00:02:48.930 --> 00:02:52.120
we know from our 30, 60, 90 triangles
00:02:52.120 --> 00:02:53.720
is going to be one half.
00:02:53.720 --> 00:02:55.380
So this is one half.
00:02:55.380 --> 00:02:56.980
And so if you distribute this four
00:02:56.980 --> 00:02:57.990
this is going to be equal to
00:02:57.990 --> 00:02:59.960
four times square root of three over two
00:02:59.960 --> 00:03:02.290
is two square roots of three
00:03:02.290 --> 00:03:04.520
and then four times one half is two.
00:03:04.520 --> 00:03:05.890
So plus
00:03:05.890 --> 00:03:06.980
two
00:03:06.980 --> 00:03:07.900
i
00:03:07.900 --> 00:03:09.453
and we are done.
|
Multiplying complex numbers in polar form | https://www.youtube.com/watch?v=VkdXztTFsvM | vtt | https://www.youtube.com/api/timedtext?v=VkdXztTFsvM&ei=5VWUZY7_G8Gyp-oP_ZOw4Aw&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=2DC465D35C8D145F8DF600FAB74837F4DF3BDBCB.4E9F3038030B5A55460C1DAA0081E45538E44091&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.420 --> 00:00:02.480
- [Instructor] We're given
two different complex numbers
00:00:02.480 --> 00:00:05.310
here, and we want to figure
out what is the product?
00:00:05.310 --> 00:00:08.610
Pause this video and see
if you can figure that out.
00:00:08.610 --> 00:00:11.910
All right, now let's
work on this together.
00:00:11.910 --> 00:00:14.550
So we know from the form
that it's written here
00:00:14.550 --> 00:00:18.810
that the modulus of w sub
one is equal to three.
00:00:18.810 --> 00:00:20.620
And we know that the argument
00:00:20.620 --> 00:00:24.683
of w sub one is equal to 330 degrees.
00:00:25.700 --> 00:00:27.830
And by the same line of reasoning, we know
00:00:27.830 --> 00:00:31.610
that the modulus of w
sub two is equal to two.
00:00:31.610 --> 00:00:35.650
And that the argument of w sub two
00:00:35.650 --> 00:00:37.720
is going to be equal to,
00:00:37.720 --> 00:00:42.300
we can see that right
over here, 120 degrees.
00:00:42.300 --> 00:00:44.250
Now, when you multiply complex numbers
00:00:44.250 --> 00:00:46.930
you could view as one
transforming the other.
00:00:46.930 --> 00:00:49.150
We've seen this in multiple examples.
00:00:49.150 --> 00:00:52.600
So let's imagine that we
are transforming w two
00:00:52.600 --> 00:00:55.200
by multiplying it by w one.
00:00:55.200 --> 00:00:56.740
So what is going to happen?
00:00:56.740 --> 00:00:58.200
Well, let me write it here.
00:00:58.200 --> 00:01:03.200
So what's the resulting
modulus of w one times w two?
00:01:03.230 --> 00:01:05.620
Well, we're just going to
scale up w two's modulus
00:01:05.620 --> 00:01:07.410
by w one's modulus.
00:01:07.410 --> 00:01:09.320
Or essentially we're just
going to multiply the two.
00:01:09.320 --> 00:01:12.850
So this is going to be equal
to six, three times two.
00:01:12.850 --> 00:01:17.850
And then the argument of
w sub one times w sub two,
00:01:18.210 --> 00:01:21.800
if we start at w sub two's
argument, 120 degrees
00:01:21.800 --> 00:01:25.120
and then we rotate it
by w sub one's argument,
00:01:25.120 --> 00:01:27.270
well then you're going
to add these two angles,
00:01:27.270 --> 00:01:30.350
that gets you to 450 degrees.
00:01:30.350 --> 00:01:32.380
So this is equal to 450 degrees,
00:01:32.380 --> 00:01:34.320
which is more than a complete rotation.
00:01:34.320 --> 00:01:36.130
And so if we wanted to give it an angle
00:01:36.130 --> 00:01:38.860
between zero and 360 degrees,
00:01:38.860 --> 00:01:41.260
if we just subtract 360 from that,
00:01:41.260 --> 00:01:45.140
that is going to be equal to 90 degrees.
00:01:45.140 --> 00:01:48.060
And so we can rewrite this here,
00:01:48.060 --> 00:01:49.890
or we can rewrite the product
00:01:49.890 --> 00:01:54.200
as w sub one times w sub two is equal
00:01:54.200 --> 00:01:59.200
to its modulus six times cosine
of its argument, 90 degrees.
00:02:01.170 --> 00:02:05.980
Plus i times sine of its argument.
00:02:05.980 --> 00:02:10.210
Now we know what the cosine
and sine of 90 degrees is.
00:02:10.210 --> 00:02:13.830
Cosine of 90 degrees is equal to zero
00:02:13.830 --> 00:02:16.700
and sine of 90 degrees is equal to one.
00:02:16.700 --> 00:02:18.590
So all of the simplifies quite nicely.
00:02:18.590 --> 00:02:21.430
All you're left with is a six times I.
00:02:21.430 --> 00:02:26.123
So this is equal to
six i, and we are done.
|
Multiplying complex numbers graphically example: -1-i | https://www.youtube.com/watch?v=ebEwF4kb6pI | vtt | https://www.youtube.com/api/timedtext?v=ebEwF4kb6pI&ei=5VWUZbHlGuKAp-oP3dKD4Ao&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=A769F761C0C6C55CBB7C49DD6D43028F4CE4528D.59D81FE9228481530F3DD5C980A7487A56E0F904&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.150 --> 00:00:02.420
- [Instructor] We are
told, suppose we multiply
00:00:02.420 --> 00:00:06.380
a complex number Z by -1-i.
00:00:07.460 --> 00:00:09.440
So this is Z right over here.
00:00:09.440 --> 00:00:13.740
Which point represents
the product of Z and -1-I?
00:00:16.550 --> 00:00:19.150
Pause this video and see
if you can figure that out.
00:00:20.320 --> 00:00:23.350
All right, now let's work
through this together.
00:00:23.350 --> 00:00:26.490
So the way I think about this is,
00:00:26.490 --> 00:00:30.660
when you multiply by a complex number,
00:00:30.660 --> 00:00:33.680
you are going to rotate by the argument
00:00:33.680 --> 00:00:35.260
of that complex number.
00:00:35.260 --> 00:00:38.640
And you're going to scale the modulus of Z
00:00:38.640 --> 00:00:42.070
by the modulus of this complex number.
00:00:42.070 --> 00:00:44.160
Now, let me just think
about that a little bit.
00:00:44.160 --> 00:00:47.163
So I'm gonna draw another
complex plane here.
00:00:48.240 --> 00:00:50.770
And so this is my real axis,
00:00:50.770 --> 00:00:55.053
this is my imaginary
axis, right over here.
00:00:56.740 --> 00:00:58.790
And -1-I, so that's -1 and then minus 1i.
00:01:03.580 --> 00:01:05.480
So it would go right over there.
00:01:05.480 --> 00:01:07.870
It would be that right over here.
00:01:07.870 --> 00:01:10.390
And so let's think about two things.
00:01:10.390 --> 00:01:12.710
Let's think about what its argument is,
00:01:12.710 --> 00:01:16.090
and let's think about
what it's modulus is.
00:01:16.090 --> 00:01:20.810
So its argument is going to
be this angle right over here.
00:01:20.810 --> 00:01:23.090
And you might already recognize
00:01:23.090 --> 00:01:26.190
that if this has a length of one,
00:01:26.190 --> 00:01:28.340
if this has a length of one,
00:01:28.340 --> 00:01:29.360
or another way of thinking about,
00:01:29.360 --> 00:01:34.360
this has a length of one,
this is a 45, 45, 90 triangle.
00:01:35.290 --> 00:01:37.340
So this is 45 degrees
00:01:37.340 --> 00:01:40.400
but then of course you
have this 180 before that.
00:01:40.400 --> 00:01:45.400
So that's going to be 180 plus
45, is a 225 degree argument.
00:01:47.260 --> 00:01:52.260
So the argument here is going
to be equal to 225 degrees.
00:01:53.740 --> 00:01:55.230
So when you multiply by this,
00:01:55.230 --> 00:01:58.740
you are going to rotate by 225 degrees.
00:01:58.740 --> 00:02:02.380
So let's see this is going
to be rotating by 180 degrees
00:02:02.380 --> 00:02:04.370
and then another 45.
00:02:04.370 --> 00:02:06.467
So if you just rotate it by that,
00:02:06.467 --> 00:02:08.743
you would end up right over here.
00:02:09.890 --> 00:02:12.740
Now we also are going
to scale the modulus.
00:02:12.740 --> 00:02:16.350
And you can see two choices
that scale that modulus.
00:02:16.350 --> 00:02:19.090
And so we know it's going
to be choice A or choice B
00:02:19.090 --> 00:02:22.300
because choices C or D
you'd have to rotate more
00:02:22.300 --> 00:02:23.630
to get over there.
00:02:23.630 --> 00:02:24.960
And so to think about that,
00:02:24.960 --> 00:02:27.270
we have to just think about the modulus
00:02:27.270 --> 00:02:31.040
of -1-i, this point right over here
00:02:31.040 --> 00:02:35.130
and then just scale up this
modulus by that same amount.
00:02:35.130 --> 00:02:36.910
Well, the modulus is just the distance
00:02:36.910 --> 00:02:39.000
from zero in the complex plane.
00:02:39.000 --> 00:02:41.380
So it's going to be this
distance right over here.
00:02:41.380 --> 00:02:43.130
And you could use the Pythagorean theorem
00:02:43.130 --> 00:02:46.370
to know that this squared,
if you call this C,
00:02:46.370 --> 00:02:49.750
C squared is equal to one
squared plus one squared
00:02:49.750 --> 00:02:51.630
or C squared is equal to two
00:02:51.630 --> 00:02:54.540
or C is equal to the square root of two.
00:02:54.540 --> 00:02:56.840
So that's the modulus right over here.
00:02:56.840 --> 00:03:00.670
Modulus is equal to square root of two
00:03:00.670 --> 00:03:03.550
which is approximately, it's
a little bit more than 1.4.
00:03:03.550 --> 00:03:05.550
So let's just call it approximately 1.4.
00:03:06.950 --> 00:03:10.720
So not only going to
rotate by 225 degrees,
00:03:10.720 --> 00:03:12.640
we're going to scale the modulus,
00:03:12.640 --> 00:03:14.440
the distance from the origin by 1.4.
00:03:15.347 --> 00:03:18.630
So it looks like it's three units
00:03:18.630 --> 00:03:20.550
from the origin right over here.
00:03:20.550 --> 00:03:22.480
If you multiply that by 1.4,
00:03:22.480 --> 00:03:27.120
three times 1.4 is about
four, or it is exactly 4.2.
00:03:27.120 --> 00:03:31.030
So 4.2 of these units is
one, two, three, four,
00:03:31.030 --> 00:03:34.000
a little bit further,
you get right over here
00:03:34.000 --> 00:03:36.273
to choice B and we're done.
|
Multiplying complex numbers graphically example: -3i | https://www.youtube.com/watch?v=fqwR6RNPJgc | vtt | https://www.youtube.com/api/timedtext?v=fqwR6RNPJgc&ei=5VWUZZKyJp--mLAPruG14A4&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=D01D652FD535E234BE2FB7E89777F8CBF0EFF1E0.53DE2F99A551DE2AEB725AF2C7D9EC187739F336&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.000 --> 00:00:02.460
- [Instructor] Suppose we
multiply a complex number Z
00:00:02.460 --> 00:00:04.130
by negative three i,
00:00:04.130 --> 00:00:06.600
and there shows Z right over here
00:00:06.600 --> 00:00:09.540
Plot the point that
represents the product of Z
00:00:09.540 --> 00:00:11.563
and negative three i.
00:00:11.563 --> 00:00:15.308
I so pause this video and see
if you can work through that.
00:00:15.308 --> 00:00:17.800
All right, now let's do it step-by-step.
00:00:17.800 --> 00:00:20.290
First I wanna think about what would,
00:00:20.290 --> 00:00:22.123
where would three Z be?
00:00:23.340 --> 00:00:28.050
Well, three Z would have
the same angle as Z,
00:00:28.050 --> 00:00:30.010
but it's absolute value
00:00:30.010 --> 00:00:32.920
or it's modulus would
be three times larger.
00:00:32.920 --> 00:00:34.440
So you'd be going in this direction
00:00:34.440 --> 00:00:35.610
but it'd be three times further.
00:00:35.610 --> 00:00:37.860
So that's one times it's modulus.
00:00:37.860 --> 00:00:38.802
That's two times it's modulus.
00:00:38.802 --> 00:00:40.580
That's three times it's modulus
00:00:40.580 --> 00:00:42.800
or it's three times it's absolute value.
00:00:42.800 --> 00:00:45.820
So three Z would be right over here.
00:00:45.820 --> 00:00:50.060
Now what about negative three Z?
00:00:50.060 --> 00:00:51.917
Well, if you multiply it by a negative,
00:00:51.917 --> 00:00:53.385
it's just going to flip it around.
00:00:53.385 --> 00:00:56.920
You can think about it as
flipping it at 180 degrees
00:00:56.920 --> 00:00:59.730
but it's going to have the same modulus.
00:00:59.730 --> 00:01:01.400
So instead of being right over here,
00:01:01.400 --> 00:01:02.540
at three in this direction,
00:01:02.540 --> 00:01:05.190
it's going to be one, two,
three in this direction,
00:01:05.190 --> 00:01:06.023
right over here.
00:01:06.023 --> 00:01:08.860
So that is negative three Z.
00:01:08.860 --> 00:01:11.100
And now perhaps most interestingly,
00:01:11.100 --> 00:01:13.830
what happens when you multiply it by i?
00:01:13.830 --> 00:01:17.940
So if we have negative three i times Z,
00:01:17.940 --> 00:01:21.010
now which is exactly what
they want us to figure out.
00:01:21.010 --> 00:01:23.000
Well, let's think about
what happens if you had one
00:01:23.000 --> 00:01:24.830
and if you multiply that by i.
00:01:24.830 --> 00:01:26.900
So one times i becomes one i.
00:01:26.900 --> 00:01:28.930
So it goes over there.
00:01:28.930 --> 00:01:32.060
What if you then took one
i and multiplied it by i?
00:01:32.060 --> 00:01:33.750
Well, then you have negative one.
00:01:33.750 --> 00:01:35.625
What if you took negative one
and you multiplied it by i?
00:01:35.625 --> 00:01:40.360
Well, then now you have negative one i.
00:01:40.360 --> 00:01:42.790
So notice every time we multiply by i,
00:01:42.790 --> 00:01:45.550
we are rotating by 90 degrees.
00:01:45.550 --> 00:01:47.669
So over here, if we take negative three Z
00:01:47.669 --> 00:01:52.390
and multiply it by i, you're
just going to rotate 90 degrees
00:01:52.390 --> 00:01:55.040
and you're going to get right over there.
00:01:55.040 --> 00:01:58.930
So this is negative three i times Z,
00:01:58.930 --> 00:02:01.373
which is exactly what we were looking for.
|
Converting a complex number from polar to rectangular form | https://www.youtube.com/watch?v=auywa7dydAk | vtt | https://www.youtube.com/api/timedtext?v=auywa7dydAk&ei=5VWUZb6BGZW_mLAPvdaRiAM&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=A3A13967EBACB54465068E022D6C9A0E9CF52185.7213822DA24E78875E7F30E8D5169291862D0580&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.200 --> 00:00:03.840
- [Instructor] We are told,
consider the complex number Z,
00:00:03.840 --> 00:00:06.900
which is equal to the square root of 17
00:00:06.900 --> 00:00:11.900
times cosine of 346 degrees
plus I sine of 346 degrees.
00:00:13.530 --> 00:00:17.290
And they ask us to plot Z
in the complex plane below.
00:00:17.290 --> 00:00:20.520
If necessary round the points coordinates
00:00:20.520 --> 00:00:22.290
to the nearest integer.
00:00:22.290 --> 00:00:23.830
So, I encourage you to pause this video
00:00:23.830 --> 00:00:24.663
and at least think about
00:00:24.663 --> 00:00:29.130
where we would likely
plot this complex number.
00:00:29.130 --> 00:00:29.963
All right.
00:00:29.963 --> 00:00:31.410
Now let's work through it together.
00:00:31.410 --> 00:00:32.900
So when you look at it like this,
00:00:32.900 --> 00:00:34.910
you can see that what's being attempted
00:00:34.910 --> 00:00:39.910
is a conversion from polar
form to rectangular form.
00:00:40.240 --> 00:00:42.820
And if we're thinking about polar form,
00:00:42.820 --> 00:00:47.100
we can think about the angle
of this complex number,
00:00:47.100 --> 00:00:49.840
which is clearly 346 degrees.
00:00:49.840 --> 00:00:51.870
And so, 346 degrees
00:00:52.850 --> 00:00:57.180
is about 14 degrees
short of a full circle.
00:00:57.180 --> 00:01:01.880
So, it would get us probably
something around there.
00:01:01.880 --> 00:01:06.580
And then we also see what the magnitude
00:01:06.580 --> 00:01:09.500
or the modulus of the complex
number is right over here.
00:01:09.500 --> 00:01:11.000
Square root of 17.
00:01:11.000 --> 00:01:14.470
Square root of 17 is a
little bit more than four
00:01:14.470 --> 00:01:16.250
'cause four squared is 16.
00:01:16.250 --> 00:01:17.630
So if we go in this direction,
00:01:17.630 --> 00:01:22.043
let's see, that's gonna be
about one, two, three, four.
00:01:23.060 --> 00:01:24.630
We're gonna go right about there.
00:01:24.630 --> 00:01:26.880
So, if I were to just guess
00:01:26.880 --> 00:01:28.580
where this is going to put us,
00:01:28.580 --> 00:01:30.920
it's going to put us right around here,
00:01:30.920 --> 00:01:34.450
right around four minus one I.
00:01:34.450 --> 00:01:36.040
But let's actually (indistinct)
get a calculator out
00:01:36.040 --> 00:01:40.830
and see if this evaluates
to roughly four minus one I.
00:01:40.830 --> 00:01:45.830
So for the real part,
let's go 346 degrees.
00:01:46.250 --> 00:01:49.200
And we're gonna take the cosine of it.
00:01:49.200 --> 00:01:50.650
And then we're gonna multiply that
00:01:50.650 --> 00:01:52.940
times the square root of 17.
00:01:52.940 --> 00:01:57.940
So times 17 square root,
a little over four,
00:01:58.020 --> 00:01:59.340
which is equal to that.
00:01:59.340 --> 00:02:00.173
Actually, yes.
00:02:00.173 --> 00:02:02.390
The real part does look
almost exactly four.
00:02:02.390 --> 00:02:05.050
Especially, if we are rounding
to the nearest integer.
00:02:05.050 --> 00:02:06.620
It's a little bit more than four.
00:02:06.620 --> 00:02:09.200
And now let's do the imaginary part.
00:02:09.200 --> 00:02:13.100
So we have 346 degrees.
00:02:13.100 --> 00:02:15.400
And we're gonna take the sine of it.
00:02:15.400 --> 00:02:18.800
And we're going to multiply
that times the square root of 17
00:02:18.800 --> 00:02:23.800
times 17 square root,
which is equal to, yep.
00:02:24.090 --> 00:02:25.840
If we were round to the nearest integer,
00:02:25.840 --> 00:02:27.960
it's about negative one.
00:02:27.960 --> 00:02:30.820
So, we get to this point right over here,
00:02:30.820 --> 00:02:35.820
which is approximately four minus I.
00:02:36.330 --> 00:02:37.963
And we are done.
|
Energy Conservation | https://www.youtube.com/watch?v=GSc5zo4WjJs | vtt | https://www.youtube.com/api/timedtext?v=GSc5zo4WjJs&ei=5VWUZdLqIpeLp-oP7a6K2Ak&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=42BD6B04F78B56AE6DF747DC2ED5DD8F897D0D5F.D09DFA72D26C0E881DF49BDC9E70A8DA464FDC57&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.290 --> 00:00:01.123
- [Narrator] In this video,
00:00:01.123 --> 00:00:04.360
we're going to talk
about energy conservation
00:00:04.360 --> 00:00:09.310
or trying to save or lower the
amount of energy that we use.
00:00:09.310 --> 00:00:11.350
Now, a lot of y'all might
already have a sense
00:00:11.350 --> 00:00:12.320
that that is a good thing
00:00:12.320 --> 00:00:13.950
while others of you might say,
00:00:13.950 --> 00:00:17.710
hey why can't I just use
as much energy as possible?
00:00:17.710 --> 00:00:20.060
Why should I try to use less energy?
00:00:20.060 --> 00:00:22.690
And there's several
answers to that question.
00:00:22.690 --> 00:00:26.410
The number one reason is
energy has a huge impact
00:00:26.410 --> 00:00:27.730
on the environment.
00:00:27.730 --> 00:00:29.510
Most of the energy we produce.
00:00:29.510 --> 00:00:31.270
And we'll talk about that in a little bit
00:00:31.270 --> 00:00:35.270
has the by-product of
emitting greenhouse gases
00:00:35.270 --> 00:00:38.270
which are contributing to global warming.
00:00:38.270 --> 00:00:41.300
And then on top of that, it
has implications to society
00:00:41.300 --> 00:00:43.140
the infrastructure around us.
00:00:43.140 --> 00:00:45.380
And it has frankly impacts on your
00:00:45.380 --> 00:00:48.760
and your family's pocketbooks
because energy costs money.
00:00:48.760 --> 00:00:51.830
So let's first think about the household.
00:00:51.830 --> 00:00:53.600
So this chart right over here,
00:00:53.600 --> 00:00:57.600
which is from the U.S. Energy
Information Administration
00:00:57.600 --> 00:01:02.230
says residential site electricity
consumption by end use.
00:01:02.230 --> 00:01:03.780
And I want to stress that it says
00:01:03.780 --> 00:01:06.710
electricity consumption
because electricity consumption
00:01:06.710 --> 00:01:10.870
is not the only energy
consumption in a household.
00:01:10.870 --> 00:01:12.880
Depending on where you
are it might be around
00:01:12.880 --> 00:01:15.330
50 or 60% of consumption
00:01:15.330 --> 00:01:18.190
but natural gas is another major source.
00:01:18.190 --> 00:01:20.400
And in some cases even petroleum.
00:01:20.400 --> 00:01:21.620
But when you look over here,
00:01:21.620 --> 00:01:26.220
the major uses of energy in a
household are air conditioning
00:01:26.220 --> 00:01:27.980
and that's going to be
especially pronounced
00:01:27.980 --> 00:01:31.290
if you live in a hot and
humid part of the country
00:01:31.290 --> 00:01:32.650
or part of the world.
00:01:32.650 --> 00:01:33.730
You have space heating
00:01:33.730 --> 00:01:35.970
which is what most of us
associate with heaters.
00:01:35.970 --> 00:01:37.460
And then you have water heating.
00:01:37.460 --> 00:01:39.200
Many of y'all probably don't appreciate
00:01:39.200 --> 00:01:42.080
when you take those long hot showers
00:01:42.080 --> 00:01:44.810
that it took energy to warm up that water.
00:01:44.810 --> 00:01:45.880
And then you have lighting.
00:01:45.880 --> 00:01:48.300
You have appliances after that.
00:01:48.300 --> 00:01:51.430
So as you as an individual
wanted to conserve energy
00:01:51.430 --> 00:01:55.920
it makes a lot of sense to
look at things like this.
00:01:55.920 --> 00:01:58.210
And so if you wanna
conserve energy at home
00:01:58.210 --> 00:02:01.070
use less air conditioning if you can.
00:02:01.070 --> 00:02:03.560
Use less heating if you can.
00:02:03.560 --> 00:02:06.720
Take shorter showers or
maybe not as hot showers.
00:02:06.720 --> 00:02:09.550
And showers not only have
the energy consumption
00:02:09.550 --> 00:02:10.970
from heating the water
00:02:10.970 --> 00:02:12.990
but it also has the energy
consumption that's happening
00:02:12.990 --> 00:02:15.740
at the water treatment
plant to clean your water
00:02:15.740 --> 00:02:18.150
and to process your water
that also takes energy.
00:02:18.150 --> 00:02:20.480
And right over here is a refrigerator.
00:02:20.480 --> 00:02:22.680
And if you have an older refrigerator
00:02:22.680 --> 00:02:24.600
or a less efficient refrigerator
00:02:24.600 --> 00:02:27.410
that's going to use a lot more
energy to do the same work.
00:02:27.410 --> 00:02:29.880
And once again, it's not
just impact on the climate.
00:02:29.880 --> 00:02:32.140
It's going to save you
and your family money
00:02:32.140 --> 00:02:34.460
by using less energy.
00:02:34.460 --> 00:02:35.780
But as we'll see,
00:02:35.780 --> 00:02:38.066
energy consumption is
not just a phenomenon
00:02:38.066 --> 00:02:40.270
inside of the house.
00:02:40.270 --> 00:02:43.360
What we see here is
U.S. energy consumption
00:02:43.360 --> 00:02:46.570
by source and sector in 2020.
00:02:46.570 --> 00:02:49.100
And this is a little
bit of a complex diagram
00:02:49.100 --> 00:02:51.690
but it's telling us a lot of information
00:02:51.690 --> 00:02:55.040
Here on the left it tells
us our sources of energy.
00:02:55.040 --> 00:02:59.100
So 35% of the energy in the United States
00:02:59.100 --> 00:03:00.720
comes from petroleum.
00:03:00.720 --> 00:03:03.800
Then 34% from natural gas.
00:03:03.800 --> 00:03:05.720
Then 12% from renewable energy.
00:03:05.720 --> 00:03:08.780
That'd be things like
wind power or solar power.
00:03:08.780 --> 00:03:13.130
Then you have 10% from
coal and 9% from nuclear.
00:03:13.130 --> 00:03:14.880
And then not only does this tell us where
00:03:14.880 --> 00:03:16.340
the energy is coming from
00:03:16.340 --> 00:03:18.800
it's telling us how it is being used.
00:03:18.800 --> 00:03:21.670
So we could see 36% in
the industrial sector.
00:03:21.670 --> 00:03:23.180
So that's all of the factories
00:03:23.180 --> 00:03:25.550
the manufacturing that
produces all of the goods
00:03:25.550 --> 00:03:28.910
and services and raw materials
that we have in society.
00:03:28.910 --> 00:03:32.100
35% of our energy in the
United States is used
00:03:32.100 --> 00:03:34.350
for transportation, moving things around.
00:03:34.350 --> 00:03:37.770
Moving ourselves around, but
also moving stuff around.
00:03:37.770 --> 00:03:40.410
And then 17% is residential.
00:03:40.410 --> 00:03:41.740
12% is commercial.
00:03:41.740 --> 00:03:43.420
So this would be things like
00:03:43.420 --> 00:03:45.570
the energy that the
shopping mall all is using
00:03:45.570 --> 00:03:48.630
or the energy that's being
used in an office building.
00:03:48.630 --> 00:03:51.370
This little gray and black
box down here is interesting
00:03:51.370 --> 00:03:54.520
because it shows the role of electricity
00:03:54.520 --> 00:03:56.180
in this whole scheme.
00:03:56.180 --> 00:03:58.050
Sometimes something like petroleum
00:03:58.050 --> 00:04:02.490
might be directly used by
say an industrial user,
00:04:02.490 --> 00:04:04.529
but sometimes that petroleum is then used
00:04:04.529 --> 00:04:07.350
for electricity generation
00:04:07.350 --> 00:04:09.550
which can then be used
by these various sectors.
00:04:09.550 --> 00:04:13.570
Similarly, something like
coal could be used directly
00:04:13.570 --> 00:04:16.360
or it could be used to
produce electricity.
00:04:16.360 --> 00:04:18.770
Now one of the eye-popping
things that I didn't appreciate
00:04:18.770 --> 00:04:20.550
until I saw this diagram
00:04:20.550 --> 00:04:23.740
are the electrical system energy losses,
00:04:23.740 --> 00:04:27.090
roughly 65% of the energy is lost.
00:04:27.090 --> 00:04:29.440
If you have a more
efficient electrical grid
00:04:29.440 --> 00:04:31.550
or we know when to
produce the electricity.
00:04:31.550 --> 00:04:34.030
So it more matches up with the demand.
00:04:34.030 --> 00:04:37.350
Then we can once again
conserve energy as a society.
00:04:37.350 --> 00:04:39.030
And so that's why it's
important to realize
00:04:39.030 --> 00:04:42.010
some people think, hey,
if I'm using electricity
00:04:42.010 --> 00:04:43.860
or if I'm using an electric car
00:04:43.860 --> 00:04:46.770
that maybe has less
impact on the environment.
00:04:46.770 --> 00:04:49.170
Well it depends where that
electricity is coming from.
00:04:49.170 --> 00:04:51.400
An electric car actually
gives us the option
00:04:51.400 --> 00:04:53.660
of not necessarily using petroleum.
00:04:53.660 --> 00:04:56.304
It gives us the option of
potentially using renewable energy
00:04:56.304 --> 00:04:58.100
or nuclear energy.
00:04:58.100 --> 00:04:59.391
But that electricity could be coming from
00:04:59.391 --> 00:05:02.810
things that significantly
impact the environment.
00:05:02.810 --> 00:05:04.490
But when you generally look at this,
00:05:04.490 --> 00:05:06.560
it tells us that as a society
00:05:06.560 --> 00:05:09.020
we have to think about things like
00:05:09.020 --> 00:05:10.912
investing in public transportation
00:05:10.912 --> 00:05:13.600
so that we conserve energy there.
00:05:13.600 --> 00:05:15.690
This right over here is a cement plant.
00:05:15.690 --> 00:05:17.470
Are there ways to produce these things
00:05:17.470 --> 00:05:20.190
that are more efficient
that use less energy.
00:05:20.190 --> 00:05:22.750
And then there's regulations that might
00:05:22.750 --> 00:05:25.100
motivate us as individuals to
00:05:25.100 --> 00:05:27.970
say carpool or drive electric cars
00:05:27.970 --> 00:05:30.820
which once again, aren't
necessarily going to be clean.
00:05:30.820 --> 00:05:33.000
It depends where that
electricity comes from.
00:05:33.000 --> 00:05:36.740
But it gives us the option
of using renewable sources.
00:05:36.740 --> 00:05:37.840
So I'll leave you there.
00:05:37.840 --> 00:05:40.480
Energy conservation is a complex topic
00:05:40.480 --> 00:05:42.420
but a very very very important one.
00:05:42.420 --> 00:05:43.938
But hopefully this gives you a start
00:05:43.938 --> 00:05:47.460
on how you can look at how
energy is being used in the world
00:05:47.460 --> 00:05:50.110
where it comes from and
how you can make a change
00:05:50.110 --> 00:05:53.030
both at the personal
level, right over here.
00:05:53.030 --> 00:05:56.670
And as a member of our
democracy at the societal level
|
Reduction of Air Pollutants | https://www.youtube.com/watch?v=s4OcGrPQqJ0 | vtt | https://www.youtube.com/api/timedtext?v=s4OcGrPQqJ0&ei=5VWUZYK9KafxvdIP1cyokAo&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=AA0207AD52BB65D9A07372186A808B32E7ED03F6.1E1C5CEDE99E73BA5B7F9883749D379493CD47&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.820 --> 00:00:01.950
- [Instructor] Hey there, friends.
00:00:01.950 --> 00:00:03.960
Today, we're gonna learn
about air pollution.
00:00:03.960 --> 00:00:06.340
And to start off, we're going back in time
00:00:06.340 --> 00:00:08.990
to the small town of Donora, Pennsylvania,
00:00:08.990 --> 00:00:11.447
in October of 1948.
00:00:11.447 --> 00:00:13.930
(pensive harp music)
00:00:13.930 --> 00:00:16.480
Walking into this small industrial town,
00:00:16.480 --> 00:00:19.800
you can immediately sense
that something is wrong.
00:00:19.800 --> 00:00:20.900
It's the middle of the day,
00:00:20.900 --> 00:00:24.130
but there's a thick
yellowish smog everywhere,
00:00:24.130 --> 00:00:27.350
enveloping everything and
even blocking out the sun.
00:00:27.350 --> 00:00:31.400
It's so dark that streetlights
are on during the daytime.
00:00:31.400 --> 00:00:35.820
It stings your eyes and it's
hard, even painful to breathe.
00:00:35.820 --> 00:00:38.890
What we're experiencing
is the Donora Death Fog,
00:00:38.890 --> 00:00:41.100
one of the worst air pollution disasters
00:00:41.100 --> 00:00:42.860
in the United States.
00:00:42.860 --> 00:00:47.300
Donora was an industrial town
full of steel plants and mills
00:00:47.300 --> 00:00:49.000
which released toxic emissions,
00:00:49.000 --> 00:00:52.010
such as hydrogen fluoride
and sulfur dioxide
00:00:52.010 --> 00:00:54.850
when processing steel and other metals.
00:00:54.850 --> 00:00:56.700
Normally, these poisonous gases
00:00:56.700 --> 00:00:58.960
would disperse into the atmosphere.
00:00:58.960 --> 00:01:02.250
But this time, there was
a temperature inversion,
00:01:02.250 --> 00:01:03.940
which caused a blanket of warm air
00:01:03.940 --> 00:01:06.700
to cover a layer of colder
air near the surface
00:01:06.700 --> 00:01:08.453
and ride over Donora.
00:01:09.630 --> 00:01:11.400
Consequently, the toxic emissions
00:01:11.400 --> 00:01:14.400
were essentially trapped
under the warm air.
00:01:14.400 --> 00:01:15.870
Over the course of several days
00:01:15.870 --> 00:01:19.360
from October 26th to October 31st,
00:01:19.360 --> 00:01:22.210
these toxic emissions
had accumulated so much
00:01:22.210 --> 00:01:25.760
that half of the 14,000
people living in Donora
00:01:25.760 --> 00:01:29.490
suffered from respiratory
problems and 20 people died.
00:01:29.490 --> 00:01:32.320
Relief only came when the
steel mills were shut down
00:01:32.320 --> 00:01:34.683
and a rainstorm alleviated the smog.
00:01:36.230 --> 00:01:38.950
But following the deadly Donora smog,
00:01:38.950 --> 00:01:41.360
the public began to
realize just how dangerous
00:01:41.360 --> 00:01:43.770
and life-threatening
air pollution could be,
00:01:43.770 --> 00:01:46.380
and citizens demanded change.
00:01:46.380 --> 00:01:48.850
Donora became a turning
point in US history
00:01:48.850 --> 00:01:51.780
and was a start of the clean air movement.
00:01:51.780 --> 00:01:54.810
The Air Pollution Control Act of 1955
00:01:54.810 --> 00:01:57.940
was the first piece of
US federal legislation
00:01:57.940 --> 00:02:00.790
involving air pollution and provided funds
00:02:00.790 --> 00:02:03.810
for research about air pollution.
00:02:03.810 --> 00:02:07.640
Then, in 1963, the Clean
Air Act was passed,
00:02:07.640 --> 00:02:11.240
the first federal legislation
to control air pollution,
00:02:11.240 --> 00:02:15.440
and later expanded in 1970,
which resulted in the creation
00:02:15.440 --> 00:02:19.300
of the US Environmental
Protection Agency, the EPA,
00:02:19.300 --> 00:02:21.160
to develop and enforce regulations
00:02:21.160 --> 00:02:22.780
to protect the general public
00:02:22.780 --> 00:02:25.810
from exposure to major
outdoor air pollutants.
00:02:25.810 --> 00:02:30.810
The Clean Air Act was expanded
in 1977 and again in 1990.
00:02:30.890 --> 00:02:33.550
And throughout its nearly-60-year history,
00:02:33.550 --> 00:02:36.570
our air quality has drastically improved
00:02:36.570 --> 00:02:38.743
and pollutants have dropped sharply.
00:02:39.950 --> 00:02:44.300
Since 1990, major air pollutants
such as carbon monoxide,
00:02:44.300 --> 00:02:47.240
nitrogen oxides, sulfur dioxide,
00:02:47.240 --> 00:02:50.360
and volatile organic compounds
have greatly decreased,
00:02:50.360 --> 00:02:52.700
and that's just since 1990.
00:02:52.700 --> 00:02:55.550
These four main air
pollutants that I highlighted
00:02:55.550 --> 00:02:59.160
are largely released as emissions
from burning fossil fuels,
00:02:59.160 --> 00:03:01.220
which comes from driving vehicles
00:03:01.220 --> 00:03:03.400
and operating coal-fired power plants
00:03:03.400 --> 00:03:05.590
and other industrial facilities.
00:03:05.590 --> 00:03:09.020
So, as we've started to
drive more efficient vehicles
00:03:09.020 --> 00:03:12.670
and obtain more energy from
clean renewable sources,
00:03:12.670 --> 00:03:15.560
we've decreased the amount
of fossil fuels that we use.
00:03:15.560 --> 00:03:18.090
And in turn, we've reduced emissions
00:03:18.090 --> 00:03:21.263
from fossil fuels and
associated air pollutants.
00:03:22.670 --> 00:03:25.710
But how does the Clean
Air Act work exactly?
00:03:25.710 --> 00:03:27.140
How do we clean the air
00:03:27.140 --> 00:03:30.310
and limit emissions of harmful pollutants?
00:03:30.310 --> 00:03:33.190
Clean Air Act regulations
implemented by the EPA
00:03:33.190 --> 00:03:36.140
have led to new technologies
that help to limit emissions
00:03:36.140 --> 00:03:38.290
and remove pollutants from the air.
00:03:38.290 --> 00:03:40.240
In particular, many of these technologies
00:03:40.240 --> 00:03:41.620
help to reduce air pollution
00:03:41.620 --> 00:03:45.020
from coal-burning power
plants and vehicles.
00:03:45.020 --> 00:03:47.250
Each of these
pollution-control technologies
00:03:47.250 --> 00:03:50.260
functions to remove harmful
components out of emissions
00:03:50.260 --> 00:03:53.000
and release a less harmful substance.
00:03:53.000 --> 00:03:55.870
In the last decade or so,
you've also probably noticed
00:03:55.870 --> 00:03:59.120
more and more electric
vehicles on the road.
00:03:59.120 --> 00:04:01.100
Improving the fuel economy of vehicles
00:04:01.100 --> 00:04:04.010
and even using battery-powered
electric vehicles
00:04:04.010 --> 00:04:06.670
can reduce the need to
burn as much gasoline,
00:04:06.670 --> 00:04:10.010
thereby reducing emissions
and giving us cleaner air.
00:04:10.010 --> 00:04:11.950
A good example is the growing demand
00:04:11.950 --> 00:04:14.730
for hybrid and purely electric vehicles.
00:04:14.730 --> 00:04:16.390
Here we have a simplified figure
00:04:16.390 --> 00:04:18.280
that explains the sources of energy
00:04:18.280 --> 00:04:19.890
for different types of vehicles
00:04:19.890 --> 00:04:21.800
and their respective emissions.
00:04:21.800 --> 00:04:24.220
On the left, we have
conventional vehicles,
00:04:24.220 --> 00:04:27.680
which rely on fossil fuels
such as gasoline or diesel
00:04:27.680 --> 00:04:30.030
and, when driven,
produce lots of emissions
00:04:30.030 --> 00:04:33.080
like carbon dioxide and air pollutants.
00:04:33.080 --> 00:04:35.240
Hybrid and plug-in hybrid vehicles
00:04:35.240 --> 00:04:37.930
are similar to conventional vehicles
00:04:37.930 --> 00:04:40.500
in that they have an
internal combustion engine,
00:04:40.500 --> 00:04:42.670
but they also have an electric motor
00:04:42.670 --> 00:04:45.080
which uses energy stored in batteries.
00:04:45.080 --> 00:04:48.410
These batteries can be charged
by regenerative braking
00:04:48.410 --> 00:04:50.580
or, in the case of plug-in hybrids,
00:04:50.580 --> 00:04:53.940
just by using a wall outlet
or other charging equipment.
00:04:53.940 --> 00:04:56.110
In turn, because these hybrid cars
00:04:56.110 --> 00:04:58.240
are partially fueled by batteries,
00:04:58.240 --> 00:05:01.620
they produce fewer emissions
than a conventional car.
00:05:01.620 --> 00:05:04.780
Finally, vehicles that
rely solely on electricity,
00:05:04.780 --> 00:05:08.510
known as battery electric
vehicles or BEVs,
00:05:08.510 --> 00:05:10.530
can use an alternative electricity source
00:05:10.530 --> 00:05:12.050
so that there's no emissions
00:05:12.050 --> 00:05:14.530
at the source of the electricity.
00:05:14.530 --> 00:05:17.090
What else can we do to ensure cleaner air?
00:05:17.090 --> 00:05:19.360
We can reduce our reliance on fossil fuels
00:05:19.360 --> 00:05:22.220
and instead invest in
cleaner renewable resources
00:05:22.220 --> 00:05:26.890
to generate electricity such
as geothermal, wind, and solar.
00:05:26.890 --> 00:05:29.440
And we can make decisions
in our day-to-day lives
00:05:29.440 --> 00:05:31.160
to reduce or prevent air pollution
00:05:31.160 --> 00:05:34.460
by using less energy
and alternative fuels.
00:05:34.460 --> 00:05:37.880
For example, walking, biking,
or using mass transportation
00:05:37.880 --> 00:05:40.550
can reduce the need to burn fossil fuels.
00:05:40.550 --> 00:05:42.190
And there are plenty of other ways
00:05:42.190 --> 00:05:44.010
to reduce our electrical needs;
00:05:44.010 --> 00:05:47.540
in particular, using more
energy-efficient appliances.
00:05:47.540 --> 00:05:49.830
For example, think of the LED bulb,
00:05:49.830 --> 00:05:53.870
which uses 75% less energy
than incandescent lighting.
00:05:53.870 --> 00:05:55.750
So, even switching out bulbs
00:05:55.750 --> 00:05:57.560
in the lights around
your house or apartment
00:05:57.560 --> 00:05:59.363
can make a huge difference.
00:06:01.070 --> 00:06:04.790
But there's still many other
places out there like Donora,
00:06:04.790 --> 00:06:07.040
and oftentimes folks living in cities
00:06:07.040 --> 00:06:10.810
with heavy air pollution
literally can't afford to leave.
00:06:10.810 --> 00:06:13.120
There's still much work to be done.
00:06:13.120 --> 00:06:16.010
In Donora, though, there's
the Donora Smog Museum,
00:06:16.010 --> 00:06:19.640
which has the tagline
"Clean air started here."
00:06:19.640 --> 00:06:22.160
The terrible incident
suffered by Donora's community
00:06:22.160 --> 00:06:24.290
played a huge and pivotal role
00:06:24.290 --> 00:06:25.860
in opening the eyes of Americans
00:06:25.860 --> 00:06:29.100
to the hazards of air pollution
and spurred political action
00:06:29.100 --> 00:06:31.090
that's carried forth through today
00:06:31.090 --> 00:06:33.650
and will continue into the future.
00:06:33.650 --> 00:06:36.373
Let's all take a deep breath
and be glad that we can.
|
Nuclear Power Generation | https://www.youtube.com/watch?v=E7UIonbL4FU | vtt | https://www.youtube.com/api/timedtext?v=E7UIonbL4FU&ei=5VWUZcLsFKuMvdIPmtazwAw&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=4497E3BE9FEBBE27042D3D4C87F2930ADCF079E0.C3297E82ECE384FC23474831D683E0C420CC6165&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:01.300 --> 00:00:02.610
- [Professor] Hey there, friends.
00:00:02.610 --> 00:00:05.520
Today, we're going to
learn about nuclear power,
00:00:05.520 --> 00:00:08.800
and to do so, we're gonna
visit my home state.
00:00:08.800 --> 00:00:10.710
Idaho? That's right.
00:00:10.710 --> 00:00:14.390
Land of the potatoes
and also nuclear power?
00:00:14.390 --> 00:00:15.860
If you've driven through Idaho,
00:00:15.860 --> 00:00:17.350
there's a good chance that you passed
00:00:17.350 --> 00:00:19.960
by a quaint small town called Arco
00:00:19.960 --> 00:00:22.260
where you'll find the
restaurant Pickle's Place,
00:00:22.260 --> 00:00:24.520
home to the Atomic Burger.
00:00:24.520 --> 00:00:29.520
Wait, a radioactive burger?
Sounds a little disturbing.
00:00:30.320 --> 00:00:32.610
Actually, Arco became the
first city in the world
00:00:32.610 --> 00:00:35.090
to be powered by nuclear energy.
00:00:35.090 --> 00:00:37.430
And of course, Arco became the first city
00:00:37.430 --> 00:00:40.620
to serve Atomic Burgers,
grilled and seared
00:00:40.620 --> 00:00:43.053
to perfection using nuclear energy.
00:00:43.890 --> 00:00:46.470
But what's going on under that grill?
00:00:46.470 --> 00:00:48.440
Are they using glowing green rocks
00:00:48.440 --> 00:00:50.880
to make those delicious Atomic Burgers?
00:00:50.880 --> 00:00:51.913
Let's find out.
00:00:54.270 --> 00:00:56.750
Nuclear power plants often look ominous
00:00:56.750 --> 00:00:58.470
and a little bit scary,
00:00:58.470 --> 00:01:00.330
but they produce power the same way
00:01:00.330 --> 00:01:02.550
most other power plants do.
00:01:02.550 --> 00:01:05.720
Simply put, they boil
water to create steam,
00:01:05.720 --> 00:01:08.710
which spins turbines to produce energy.
00:01:08.710 --> 00:01:12.100
Most nuclear power plants
use light water reactors
00:01:12.100 --> 00:01:13.930
to generate electricity,
00:01:13.930 --> 00:01:16.513
which are made up of five basic parts.
00:01:17.480 --> 00:01:20.120
First off, we have the core of the reactor
00:01:20.120 --> 00:01:22.650
where fuel rods are inserted.
00:01:22.650 --> 00:01:24.780
Next up, we have the containment shell
00:01:24.780 --> 00:01:28.610
that encases the reactor
and the spent fuel rods.
00:01:28.610 --> 00:01:30.670
Within there, we have supply of water,
00:01:30.670 --> 00:01:32.900
which is boiled to reduce steam.
00:01:32.900 --> 00:01:35.720
That steam then rotates a turbine attached
00:01:35.720 --> 00:01:38.890
to a generator which produces electricity.
00:01:38.890 --> 00:01:41.480
This act of turning an electric generator
00:01:41.480 --> 00:01:45.060
is actually the same process
that's used for coal,
00:01:45.060 --> 00:01:49.030
gas, geothermal, hydro
power, and wind power.
00:01:49.030 --> 00:01:52.170
No matter how complex the
electricity generation system,
00:01:52.170 --> 00:01:54.660
that all boils down to the same idea,
00:01:54.660 --> 00:01:56.410
basically turning a wheel,
00:01:56.410 --> 00:02:00.120
one of the oldest
agricultural-era human inventions,
00:02:00.120 --> 00:02:02.500
and that's what makes electricity.
00:02:02.500 --> 00:02:06.090
Finally, we have excess
steam or water vapor,
00:02:06.090 --> 00:02:07.510
which is the only direct emission
00:02:07.510 --> 00:02:09.470
from nuclear power generation.
00:02:09.470 --> 00:02:13.393
Easy as pie, right? Well,
it's actually pretty complex.
00:02:14.650 --> 00:02:18.050
So how is the water heated exactly?
00:02:18.050 --> 00:02:21.140
Nuclear energy isn't as
easy as lighting up a grill,
00:02:21.140 --> 00:02:23.120
and it requires us to go down
00:02:23.120 --> 00:02:26.490
to the smallest unit of matter, the atom.
00:02:26.490 --> 00:02:28.960
Here, we get our energy
at the atomic level,
00:02:28.960 --> 00:02:31.360
but it's not from the atom alone.
00:02:31.360 --> 00:02:34.720
No, to gain energy, we
need to split the atom.
00:02:34.720 --> 00:02:37.130
This process is called
fission, which occurs
00:02:37.130 --> 00:02:39.680
when neutrons are fired at an atom,
00:02:39.680 --> 00:02:41.560
causing it to split into separate atoms
00:02:41.560 --> 00:02:43.610
of other smaller elements.
00:02:43.610 --> 00:02:46.230
This split produces a
huge amount of energy,
00:02:46.230 --> 00:02:48.400
which is largely converted to heat,
00:02:48.400 --> 00:02:51.310
which boils the water and produces steam.
00:02:51.310 --> 00:02:53.160
However, we need a special kind
00:02:53.160 --> 00:02:55.160
of atom for fission to happen,
00:02:55.160 --> 00:02:58.623
and most nuclear reactors use uranium-235.
00:03:00.290 --> 00:03:03.200
Wait, why uranium-235 though?
00:03:03.200 --> 00:03:06.470
Well, first, uranium-235 is big,
00:03:06.470 --> 00:03:10.770
not a triple 1/4 pounder big
but big on the atomic scale.
00:03:10.770 --> 00:03:13.830
In the atomic world, this
is known as being heavy.
00:03:13.830 --> 00:03:18.600
Secondly, uranium-235 is unstable
because it's not only big,
00:03:18.600 --> 00:03:21.700
but it's also an isotope,
meaning it has a different number
00:03:21.700 --> 00:03:24.620
of neutrons than the more
common form of uranium,
00:03:24.620 --> 00:03:28.710
which is uranium-238, which
has three more neutrons.
00:03:28.710 --> 00:03:33.530
This makes uranium-235 unstable
or fissile like fission,
00:03:33.530 --> 00:03:36.120
which means it can be split by a neutron,
00:03:36.120 --> 00:03:40.350
thereby producing other elements,
energy, and more neutrons.
00:03:40.350 --> 00:03:44.140
Those produced neutrons
crash into other U-235 atoms,
00:03:44.140 --> 00:03:47.060
splitting them and
causing a chain reaction,
00:03:47.060 --> 00:03:49.163
which is what makes nuclear energy work.
00:03:50.070 --> 00:03:52.850
This chain reaction is
really important to note
00:03:52.850 --> 00:03:56.010
because it's what makes a
nuclear power plant so different
00:03:56.010 --> 00:04:00.240
from its, well, more destructive
cousin, the atomic bomb.
00:04:00.240 --> 00:04:04.380
In atomic bombs, the same process
of nuclear fission is used
00:04:04.380 --> 00:04:07.450
except that it's a fast
destructive, runaway,
00:04:07.450 --> 00:04:09.490
and uncontrolled reaction that results
00:04:09.490 --> 00:04:11.910
in massively powerful explosions,
00:04:11.910 --> 00:04:13.510
not something that we would want
00:04:13.510 --> 00:04:15.523
to happen in a nuclear power plant.
00:04:16.490 --> 00:04:18.330
Now a little goes a long way
00:04:18.330 --> 00:04:20.400
when it comes to nuclear fission.
00:04:20.400 --> 00:04:23.400
The fuel is actually
composed of tiny pellets
00:04:23.400 --> 00:04:28.070
of uranium-235, each the
size of a pencil eraser,
00:04:28.070 --> 00:04:32.160
but each also has the equivalent
energy of a ton of coal.
00:04:32.160 --> 00:04:34.440
Yes, a literal ton.
00:04:34.440 --> 00:04:37.190
These pellets are packed
together to form fuel rods,
00:04:37.190 --> 00:04:39.580
which are bunched into fuel assemblies
00:04:39.580 --> 00:04:42.200
and then placed in the nuclear reactor.
00:04:42.200 --> 00:04:44.810
Nuclear fusion is
therefore really powerful
00:04:44.810 --> 00:04:48.810
and can generate a lot of heat
from very little material.
00:04:48.810 --> 00:04:51.390
But to keep temperatures
from getting too hot,
00:04:51.390 --> 00:04:53.380
which would cause a nuclear meltdown,
00:04:53.380 --> 00:04:57.210
and no, I'm not talking about
melty cheese, unfortunately,
00:04:57.210 --> 00:05:00.320
the reactor is therefore
cooled with water.
00:05:00.320 --> 00:05:03.170
When more heat is generated
by the nuclear reactor
00:05:03.170 --> 00:05:05.410
than can be removed by the cooling system,
00:05:05.410 --> 00:05:08.120
or water in the case of nuclear reactors,
00:05:08.120 --> 00:05:11.340
the fuel rods can get so hot
that they could start to melt
00:05:11.340 --> 00:05:13.090
and fall to the bottom of the reactor
00:05:13.090 --> 00:05:15.100
and potentially melt through and escape
00:05:15.100 --> 00:05:16.940
into the surrounding environment.
00:05:16.940 --> 00:05:18.950
That's called a nuclear meltdown,
00:05:18.950 --> 00:05:21.980
and that's also why in part,
the reactor is surrounded
00:05:21.980 --> 00:05:24.480
by a containment shell of
thick steel and concrete,
00:05:24.480 --> 00:05:27.550
which keeps radioactive
materials from escaping.
00:05:27.550 --> 00:05:29.833
We don't wanna have any
radioactive burgers.
00:05:30.750 --> 00:05:33.550
But fuel rods don't last forever.
00:05:33.550 --> 00:05:35.660
After three to six years in a reactor,
00:05:35.660 --> 00:05:38.730
fuel rods can't sustain the
fission reaction effectively
00:05:38.730 --> 00:05:41.510
anymore and become highly radioactive.
00:05:41.510 --> 00:05:44.450
In turn, they need to be
carefully removed and stored.
00:05:44.450 --> 00:05:46.950
But what to do with nuclear waste?
00:05:46.950 --> 00:05:49.130
The problem with spent nuclear fuel
00:05:49.130 --> 00:05:51.170
is that it's really radioactive.
00:05:51.170 --> 00:05:54.640
These leftover radioactive
materials can persist in the air,
00:05:54.640 --> 00:05:57.930
soil, and water for thousands
and thousands of years
00:05:57.930 --> 00:06:00.140
and damage the DNA of living organisms,
00:06:00.140 --> 00:06:02.990
causing cancer and
other health conditions.
00:06:02.990 --> 00:06:05.550
For a while, actually quite a long time
00:06:05.550 --> 00:06:08.980
from 1946 to 1993, to be exact,
00:06:08.980 --> 00:06:12.290
many countries just dumped
radioactive nuclear waste
00:06:12.290 --> 00:06:13.640
into the ocean.
00:06:13.640 --> 00:06:17.380
This was consequently banned,
and you can imagine why.
00:06:17.380 --> 00:06:20.030
Instead, nuclear waste can be buried,
00:06:20.030 --> 00:06:22.280
but there's problems with that, too.
00:06:22.280 --> 00:06:24.400
Nuclear waste can still leak into soil
00:06:24.400 --> 00:06:27.060
and water if it isn't properly contained.
00:06:27.060 --> 00:06:30.930
So where do we safely bury
it? Well, nowhere really.
00:06:30.930 --> 00:06:33.110
Radioactive spent fuel is stored all
00:06:33.110 --> 00:06:35.600
over the world in various
containment systems,
00:06:35.600 --> 00:06:38.120
but none of them are truly longterm.
00:06:38.120 --> 00:06:41.210
Alternatively, spent fuel
rods can also be recycled
00:06:41.210 --> 00:06:43.810
and reprocessed where unused uranium
00:06:43.810 --> 00:06:46.480
is separated from spent nuclear fuel.
00:06:46.480 --> 00:06:51.110
However, this reprocessing is
quite expensive and dangerous.
00:06:51.110 --> 00:06:53.660
Reprocessing is often much more expensive
00:06:53.660 --> 00:06:56.730
than storing or disposing
of spent nuclear fuel,
00:06:56.730 --> 00:06:59.070
and it still results
in a substantial amount
00:06:59.070 --> 00:07:01.060
of leftover radioactive materials
00:07:01.060 --> 00:07:02.993
that still need to be disposed of.
00:07:04.440 --> 00:07:06.230
There's no perfect solution when it comes
00:07:06.230 --> 00:07:08.050
to energy production, though.
00:07:08.050 --> 00:07:10.030
Any kind of electricity production
00:07:10.030 --> 00:07:12.780
has its own benefits and drawbacks.
00:07:12.780 --> 00:07:16.280
But Pickle Place's Atomic
Burger is quite perfect,
00:07:16.280 --> 00:07:17.743
and I think I'll eat one now.
|
Student tips for using course mastery on Khan Academy | https://www.youtube.com/watch?v=yqdGJ-_0AGg | vtt | https://www.youtube.com/api/timedtext?v=yqdGJ-_0AGg&ei=5VWUZfTYEavjxN8PtLSwgA0&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=2BCDA25DDDFD29DA6E5151AD700478DF8577101D.8FA129B74B295D0848F5B20864A1FFC2A8F3C970&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:03.200 --> 00:00:06.050
- Hi, I'm Shannon from Khan Academy,
00:00:06.050 --> 00:00:08.240
and I want to show you
how to make the most
00:00:08.240 --> 00:00:09.483
of your learning time.
00:00:10.490 --> 00:00:12.570
First, make sure you're logged in
00:00:12.570 --> 00:00:14.410
to your Khan Academy account
00:00:14.410 --> 00:00:17.793
by checking for your name in
the upper right hand corner.
00:00:19.550 --> 00:00:21.410
Now on the left side,
00:00:21.410 --> 00:00:22.860
you should see your classes
00:00:22.860 --> 00:00:25.640
where your teacher has
given you a mastery goal,
00:00:25.640 --> 00:00:27.253
or assignment to work on.
00:00:28.520 --> 00:00:32.150
Click on the tab that says Course mastery
00:00:32.150 --> 00:00:34.543
to view the goal your teacher set for you.
00:00:35.520 --> 00:00:37.450
Now that you're viewing your goal,
00:00:37.450 --> 00:00:40.360
let's talk about the
top five things to know
00:00:40.360 --> 00:00:43.913
about working towards Course
mastery on Khan Academy.
00:00:45.020 --> 00:00:48.180
Number one, your course mastery placement
00:00:48.180 --> 00:00:51.010
is a big goal from your teacher.
00:00:51.010 --> 00:00:52.860
On your learner home page,
00:00:52.860 --> 00:00:55.170
you can see the progress
you've already made
00:00:55.170 --> 00:00:57.110
towards your mastery goal,
00:00:57.110 --> 00:00:59.720
and the due date your teacher set.
00:00:59.720 --> 00:01:01.710
But you can always work ahead,
00:01:01.710 --> 00:01:03.393
or view past goals.
00:01:05.180 --> 00:01:06.670
Click on the mastery goal
00:01:06.670 --> 00:01:09.113
to be taken to the course homepage.
00:01:10.940 --> 00:01:14.010
Here, you'll see the units
that make up the course,
00:01:14.010 --> 00:01:17.453
as well as your progress
towards mastery on each unit.
00:01:18.530 --> 00:01:21.010
As you make progress on each unit,
00:01:21.010 --> 00:01:24.373
you'll see the purple bar
fill from left to right.
00:01:25.940 --> 00:01:28.900
It's helpful to regularly
check your unit progress,
00:01:28.900 --> 00:01:31.350
so you know if you're on
track to meet your goal.
00:01:33.090 --> 00:01:36.280
Click into a unit to view
your current mastery level
00:01:36.280 --> 00:01:39.313
for each skill on the left-hand side.
00:01:40.430 --> 00:01:41.890
With every skill,
00:01:41.890 --> 00:01:43.300
try to get the crown,
00:01:43.300 --> 00:01:46.003
and move your mastery level to Mastered.
00:01:46.890 --> 00:01:51.343
Number two, mastery
takes time and practice.
00:01:52.600 --> 00:01:55.840
As you practice skills
and answer questions,
00:01:55.840 --> 00:01:59.260
your mastery level for
each skill will go up,
00:01:59.260 --> 00:02:01.110
if you answered correctly,
00:02:01.110 --> 00:02:03.453
or down, if you miss questions.
00:02:04.550 --> 00:02:07.040
If you want to make progress more quickly,
00:02:07.040 --> 00:02:08.803
try a Mastery challenge.
00:02:09.660 --> 00:02:12.760
Mastery challenges allow
you to strengthen the skills
00:02:12.760 --> 00:02:16.343
you've already practiced
in just six questions.
00:02:17.650 --> 00:02:20.000
Mastery is not easily earned,
00:02:20.000 --> 00:02:21.870
and that's intentional!
00:02:21.870 --> 00:02:24.710
But putting in the work to achieve mastery
00:02:24.710 --> 00:02:27.323
will prove you've earned and learned it.
00:02:28.400 --> 00:02:31.360
Remember, you can retry an exercise
00:02:31.360 --> 00:02:33.170
as many times as you'd like
00:02:33.170 --> 00:02:35.782
until you earn a score you're happy with.
00:02:35.782 --> 00:02:36.615
(stars twinkling)
00:02:36.615 --> 00:02:39.629
Struggles and mistakes are
what helps your brain grow.
00:02:39.629 --> 00:02:41.920
(congratulatory sound)
00:02:41.920 --> 00:02:45.023
Number three, follow the blue button.
00:02:46.490 --> 00:02:49.590
Your big goal has a lot
of skills you can practice
00:02:49.590 --> 00:02:50.973
at your own pace.
00:02:51.870 --> 00:02:54.250
To make sure you stay on track,
00:02:54.250 --> 00:02:57.053
look for the blue buttons
throughout the course.
00:02:58.140 --> 00:03:00.110
The blue buttons will always guide you
00:03:00.110 --> 00:03:01.993
to what you should work on next.
00:03:03.350 --> 00:03:06.863
Number four, if you're stuck, take a hint.
00:03:08.030 --> 00:03:11.320
It's normal to feel stuck when
you're learning new skills.
00:03:11.320 --> 00:03:13.503
The important thing is you don't give up.
00:03:14.410 --> 00:03:17.600
Take a hint to get
step-by-step instructions
00:03:17.600 --> 00:03:20.680
to the specific question
you're working on.
00:03:20.680 --> 00:03:23.280
And write them down so you
can reference them later.
00:03:24.940 --> 00:03:27.000
You can also try watching a video,
00:03:27.000 --> 00:03:29.133
or reading an article on the skill.
00:03:30.240 --> 00:03:31.410
Once you've done that,
00:03:31.410 --> 00:03:33.743
you're ready to retry the exercise.
00:03:34.970 --> 00:03:36.810
And if you're still stuck,
00:03:36.810 --> 00:03:39.750
reach out to your classmate, a teacher,
00:03:39.750 --> 00:03:41.605
or a family member for support.
00:03:41.605 --> 00:03:43.900
(stars twinkling)
00:03:43.900 --> 00:03:46.813
Number five, the sky's the limit!
00:03:48.000 --> 00:03:51.810
Remember, you have the
potential to succeed.
00:03:51.810 --> 00:03:54.510
Keep trying, keep making mistakes,
00:03:54.510 --> 00:03:57.140
and keep asking for help when you need it.
00:03:57.140 --> 00:03:59.393
There is no limit to what you can learn.
|
Student tips for completing assignments on Khan Academy | https://www.youtube.com/watch?v=dT_-uESRLqw | vtt | https://www.youtube.com/api/timedtext?v=dT_-uESRLqw&ei=5VWUZbaxIu6jmLAP3s-CiA8&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=6B9D2F0617896B6D9AD84BB7E92C8F63D2CEA55F.0F4808307C19BE281A9EE5A9E612530E851A78F8&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:03.200 --> 00:00:06.050
- Hi, I'm Shannon from Khan Academy,
00:00:06.050 --> 00:00:08.240
and I wanna show you how to make the most
00:00:08.240 --> 00:00:10.000
of your learning time.
00:00:10.000 --> 00:00:11.910
First, make sure you're logged into
00:00:11.910 --> 00:00:14.850
your Khan Academy account
by checking for your name
00:00:14.850 --> 00:00:17.500
in the upper right-hand corner.
00:00:17.500 --> 00:00:19.270
If you are not logged in,
00:00:19.270 --> 00:00:21.200
you won't be able to view your assignments
00:00:21.200 --> 00:00:22.500
and any progress you make
00:00:22.500 --> 00:00:24.520
won't be counted towards your classes.
00:00:24.520 --> 00:00:26.440
Now, on the left-hand side,
00:00:26.440 --> 00:00:27.870
you should see your classes
00:00:27.870 --> 00:00:30.700
where your teacher has
given you a mastery goal
00:00:30.700 --> 00:00:32.363
or an assignment to work on.
00:00:33.500 --> 00:00:36.430
Click on the tab that says assignments
00:00:36.430 --> 00:00:38.373
to view assignments from your teacher.
00:00:40.050 --> 00:00:41.730
On the assignments tab,
00:00:41.730 --> 00:00:46.470
you can see all your upcoming
and past due assignments.
00:00:46.470 --> 00:00:48.180
Assignments with the nearest due date
00:00:48.180 --> 00:00:51.121
will appear at the very top of the list.
00:00:51.121 --> 00:00:53.480
Now that you're ready to go,
00:00:53.480 --> 00:00:56.280
let's talk about the
top five things to know
00:00:56.280 --> 00:00:58.720
about assignments on Khan Academy.
00:00:58.720 --> 00:01:01.943
Number one, types of assignments.
00:01:03.180 --> 00:01:05.480
There are two main types of assignments
00:01:05.480 --> 00:01:08.230
you can receive on Khan Academy.
00:01:08.230 --> 00:01:12.163
The first type is practice,
noted with the star symbol.
00:01:13.240 --> 00:01:18.120
Practice can be an exercise,
quiz, or unit test.
00:01:18.120 --> 00:01:20.770
When you complete
practice on Khan Academy,
00:01:20.770 --> 00:01:23.693
you receive instant
feedback after every answer.
00:01:24.730 --> 00:01:27.460
Answer all questions to
complete the assignment
00:01:27.460 --> 00:01:28.593
and receive a score.
00:01:31.330 --> 00:01:36.110
The second type is instruction,
noted with the play symbol
00:01:36.110 --> 00:01:37.483
and the paper symbol.
00:01:38.550 --> 00:01:42.253
Instruction can be in the
form of videos or articles.
00:01:43.300 --> 00:01:46.360
Videos and articles can
help you learn new skills
00:01:46.360 --> 00:01:48.373
or review things you learned in class.
00:01:49.810 --> 00:01:51.590
All videos have subtitles,
00:01:51.590 --> 00:01:54.080
so you can easily follow along.
00:01:54.080 --> 00:01:57.950
Number two, if you're stuck, take a hint.
00:01:57.950 --> 00:02:00.780
It's normal to feel stuck when
you're learning new skills,
00:02:00.780 --> 00:02:03.700
but the important thing
is you don't give up.
00:02:03.700 --> 00:02:06.520
Take a hint to get
step-by-step instructions
00:02:06.520 --> 00:02:08.833
to the specific question
you're working on.
00:02:09.700 --> 00:02:12.060
We recommend that you
write these hints down
00:02:12.060 --> 00:02:13.713
so you can reference them later.
00:02:15.230 --> 00:02:17.180
You can also try watching a video
00:02:17.180 --> 00:02:19.420
or reading an article on this skill,
00:02:19.420 --> 00:02:22.120
even if it hasn't been assigned to you.
00:02:22.120 --> 00:02:24.140
You'll find the videos and articles
00:02:24.140 --> 00:02:26.460
related to each skill you're practicing
00:02:26.460 --> 00:02:30.560
by clicking this stuck or get help link.
00:02:30.560 --> 00:02:31.660
Once you've done that,
00:02:31.660 --> 00:02:34.373
you're ready to retry
the practice exercise.
00:02:35.920 --> 00:02:37.460
And if you're still stuck,
00:02:37.460 --> 00:02:41.080
reach out to a classmate,
teacher, or a family member
00:02:41.080 --> 00:02:41.913
for support.
00:02:44.060 --> 00:02:47.830
Number three, be patient and persistent.
00:02:47.830 --> 00:02:49.710
Not happy with the score you received
00:02:49.710 --> 00:02:51.660
on a practice exercise?
00:02:51.660 --> 00:02:54.070
Trust me, we've all been there.
00:02:54.070 --> 00:02:56.290
But remember, on Khan Academy,
00:02:56.290 --> 00:02:58.200
you can always retry assignments
00:02:58.200 --> 00:03:00.890
until you earn a that you are proud of.
00:03:00.890 --> 00:03:03.103
Click try again to retry.
00:03:08.690 --> 00:03:10.480
You can also return to assignments
00:03:10.480 --> 00:03:11.880
where the due dates have passed
00:03:11.880 --> 00:03:13.433
to try to improve your score.
00:03:14.540 --> 00:03:17.430
Struggles and mistakes are
what helps your brain grow,
00:03:17.430 --> 00:03:18.380
so keep persisting.
00:03:19.860 --> 00:03:23.120
Number four, check your progress.
00:03:23.120 --> 00:03:24.810
On the left-hand side,
00:03:24.810 --> 00:03:28.520
select progress under my account.
00:03:28.520 --> 00:03:30.520
From here, you can review
00:03:30.520 --> 00:03:33.780
all of the activity on Khan Academy.
00:03:33.780 --> 00:03:38.130
This includes exercises you
completed, videos you watched,
00:03:38.130 --> 00:03:39.783
or articles you read.
00:03:41.210 --> 00:03:43.260
Depending on your learning goals,
00:03:43.260 --> 00:03:44.270
you may wanna filter
00:03:44.270 --> 00:03:47.823
to view a certain type
of content or activity.
00:03:49.180 --> 00:03:51.330
And for each practice you completed,
00:03:51.330 --> 00:03:53.960
you can view your current mastery level,
00:03:53.960 --> 00:03:56.910
the number of questions
you answered correctly,
00:03:56.910 --> 00:03:59.533
and how much time you
spent on the activity.
00:04:01.120 --> 00:04:03.620
It's helpful to regularly
check your progress,
00:04:03.620 --> 00:04:06.790
so you know if you're on
track to meet your goals.
00:04:06.790 --> 00:04:11.070
Number five, make Khan Academy your own.
00:04:11.070 --> 00:04:13.640
And finally, adjust Khan Academy
00:04:13.640 --> 00:04:16.630
to work for your unique learning style.
00:04:16.630 --> 00:04:21.190
You can slow down, speed
up, or rewind the videos
00:04:21.190 --> 00:04:22.203
when you need to.
00:04:23.400 --> 00:04:26.930
You can learn in the language
you're most comfortable with.
00:04:26.930 --> 00:04:29.830
Khan Academy is available
in over 50 languages
00:04:29.830 --> 00:04:32.100
and you can easily
switch between languages
00:04:32.100 --> 00:04:33.313
in your settings.
00:04:34.810 --> 00:04:36.160
And if you prefer,
00:04:36.160 --> 00:04:38.870
you can complete
assignments on a smartphone.
00:04:38.870 --> 00:04:43.163
Just download the Khan
Academy app on Android or iOS.
00:04:44.930 --> 00:04:48.870
And remember, you have
the potential to succeed.
00:04:48.870 --> 00:04:51.730
Keep trying, keep making mistakes,
00:04:51.730 --> 00:04:54.320
and keep asking for help when you need it.
00:04:54.320 --> 00:04:56.533
There is no limit to what you can learn.
|
Impacts of Urbanization | https://www.youtube.com/watch?v=2C7F_2OpRT8 | vtt | https://www.youtube.com/api/timedtext?v=2C7F_2OpRT8&ei=5VWUZcXzE86ep-oPirSHqAY&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=25AD3E2C63FB70689A766DD1113D6C333B863DAE.9297CAB37C37F36CDD6E9C6CFC6D0C734128F388&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.150 --> 00:00:01.000
- [Instructor] In this video,
00:00:01.000 --> 00:00:03.160
we're going to talk about cities.
00:00:03.160 --> 00:00:06.410
Today, more than 50% of
the world's population
00:00:06.410 --> 00:00:09.900
lives in a city, and this
percentage grows every year
00:00:09.900 --> 00:00:12.360
because of something called urbanization.
00:00:12.360 --> 00:00:15.460
Urbanization is the creation
and growth of cities,
00:00:15.460 --> 00:00:18.010
human settlements with
higher population densities
00:00:18.010 --> 00:00:19.440
than rural areas.
00:00:19.440 --> 00:00:21.750
The high population density in cities
00:00:21.750 --> 00:00:23.560
has a lot of advantages.
00:00:23.560 --> 00:00:25.320
Because people are closer together,
00:00:25.320 --> 00:00:28.530
it's easier to coordinate
community efforts like recycling,
00:00:28.530 --> 00:00:31.793
public education, and
public transportation.
00:00:33.320 --> 00:00:35.500
Urban residents also tend
to have better access
00:00:35.500 --> 00:00:38.573
to things like medical
care and family planning.
00:00:39.710 --> 00:00:42.450
However, the high
population density of cities
00:00:42.450 --> 00:00:45.530
also can have a negative
impact on the environment.
00:00:45.530 --> 00:00:47.190
You can imagine, with so many people
00:00:47.190 --> 00:00:49.110
living close together in one space,
00:00:49.110 --> 00:00:52.170
it can cause a strain on the
natural resources of the area
00:00:52.170 --> 00:00:54.760
and generate more air and water pollution.
00:00:54.760 --> 00:00:56.520
Cities can use sustainable planning
00:00:56.520 --> 00:00:58.130
to counter these effects.
00:00:58.130 --> 00:01:00.240
Urban planners often talk about the ratio
00:01:00.240 --> 00:01:03.400
between green space and
gray space in a city,
00:01:03.400 --> 00:01:07.570
where the green spaces are
vegetation and the gray spaces
00:01:07.570 --> 00:01:10.790
are things like buildings
and paved surfaces,
00:01:10.790 --> 00:01:13.720
like roads and sidewalks and parking lots.
00:01:13.720 --> 00:01:15.940
These gray spaces may be necessary,
00:01:15.940 --> 00:01:17.900
but cities should be planned thoughtfully
00:01:17.900 --> 00:01:19.730
to add some green spaces too.
00:01:19.730 --> 00:01:23.100
When gray spaces dominate
a cityscape too much,
00:01:23.100 --> 00:01:24.760
the paved surfaces prevent water
00:01:24.760 --> 00:01:27.520
from seeping into the
ground, so when it rains,
00:01:27.520 --> 00:01:29.730
it creates large amounts of runoff.
00:01:29.730 --> 00:01:30.900
Having nowhere to go,
00:01:30.900 --> 00:01:33.690
the water travels across paved surfaces,
00:01:33.690 --> 00:01:35.570
picking up pollutants along the way.
00:01:35.570 --> 00:01:38.220
All this runoff can
lead to flash flooding.
00:01:38.220 --> 00:01:39.420
Adding more green spaces
00:01:39.420 --> 00:01:41.010
can help prevent this from happening
00:01:41.010 --> 00:01:42.960
because plants soak up water.
00:01:42.960 --> 00:01:45.260
There are many creative
ways that urban planners
00:01:45.260 --> 00:01:47.580
can add green spaces to our environment.
00:01:47.580 --> 00:01:50.500
Some buildings in cities
grow plants on their roofs.
00:01:50.500 --> 00:01:52.260
They're called green roofs.
00:01:52.260 --> 00:01:55.960
The plants soak up the rain and
snow melt that hits the roof
00:01:55.960 --> 00:01:58.040
and prevents it from
going into the street.
00:01:58.040 --> 00:02:01.150
Also, plants create shade
and help cool things down,
00:02:01.150 --> 00:02:02.670
so buildings with green roofs
00:02:02.670 --> 00:02:05.340
wouldn't have to spend as much
energy on air conditioning.
00:02:05.340 --> 00:02:07.400
Green spaces can also help the environment
00:02:07.400 --> 00:02:09.730
by allowing for groundwater recharge,
00:02:09.730 --> 00:02:12.580
which is allowing more water
to sink back into the ground
00:02:12.580 --> 00:02:14.710
and replenish the aquifer.
00:02:14.710 --> 00:02:17.300
Some cities do this by
building rain gardens,
00:02:17.300 --> 00:02:19.420
which are gardens specifically designed
00:02:19.420 --> 00:02:21.610
to filter water back into the ground,
00:02:21.610 --> 00:02:23.070
the plants and the rain gardens
00:02:23.070 --> 00:02:24.970
help filter pollutants in the runoff
00:02:24.970 --> 00:02:25.860
and prevent the pollutants
00:02:25.860 --> 00:02:28.230
from contaminating water ecosystems.
00:02:28.230 --> 00:02:30.280
Cities can also help
with groundwater recharge
00:02:30.280 --> 00:02:33.250
by building permeable
surfaces in their cities.
00:02:33.250 --> 00:02:34.970
Parking lots can be constructed
00:02:34.970 --> 00:02:37.920
with permeable paving to reduce runoff.
00:02:37.920 --> 00:02:39.850
Groundwater recharge can
help prevent something
00:02:39.850 --> 00:02:43.223
that happens in coastal cities
called saltwater intrusion.
00:02:44.950 --> 00:02:49.050
Let's say that this city right
here is a city on the coast,
00:02:49.050 --> 00:02:51.300
so it's really close to the ocean.
00:02:51.300 --> 00:02:54.180
And let's say this city decides
to build a pump right here
00:02:54.180 --> 00:02:57.820
to access the freshwater
in the aquifer below it.
00:02:57.820 --> 00:02:59.660
But the city has a lot of people in it
00:02:59.660 --> 00:03:01.000
and it needs a lot of water.
00:03:01.000 --> 00:03:03.820
The city might end up taking
more and more freshwater
00:03:03.820 --> 00:03:05.890
at a rate too fast for the freshwater
00:03:05.890 --> 00:03:07.820
in the aquifer to replenish itself.
00:03:07.820 --> 00:03:09.080
Pulling up so much fresh water
00:03:09.080 --> 00:03:12.580
can create a space for the
saltwater in the nearby ocean
00:03:12.580 --> 00:03:14.230
to come and take its place.
00:03:14.230 --> 00:03:15.600
The saltwater from the ocean
00:03:15.600 --> 00:03:17.730
would contaminate the freshwater supply,
00:03:17.730 --> 00:03:19.540
making it unpotable.
00:03:19.540 --> 00:03:21.710
But if this city decided to increase
00:03:21.710 --> 00:03:24.740
the amount of permeable
surfaces and green spaces,
00:03:24.740 --> 00:03:27.220
then when it rains, the water will be able
00:03:27.220 --> 00:03:29.430
to seep back into the ground
00:03:29.430 --> 00:03:31.130
and it would refill the empty space
00:03:31.130 --> 00:03:33.550
the pump has created with freshwater.
00:03:33.550 --> 00:03:34.760
This would mean that freshwater
00:03:34.760 --> 00:03:36.570
would continually be replacing the water
00:03:36.570 --> 00:03:38.140
that was taken out by the pump,
00:03:38.140 --> 00:03:40.790
so saltwater intrusion couldn't happen.
00:03:40.790 --> 00:03:44.490
Adding more green spaces could
also help with air pollution
00:03:44.490 --> 00:03:48.630
because plants absorb carbon
dioxide and produce oxygen.
00:03:48.630 --> 00:03:51.730
Cities produce most of
the world's air pollution.
00:03:51.730 --> 00:03:54.350
Part of this is because of urban sprawl.
00:03:54.350 --> 00:03:56.130
As cities become more populated,
00:03:56.130 --> 00:03:59.800
they expand into suburban
areas and even exurban areas,
00:03:59.800 --> 00:04:01.830
the areas past the suburbs.
00:04:01.830 --> 00:04:03.360
All of that expansion leads people
00:04:03.360 --> 00:04:05.250
to live farther away from their jobs.
00:04:05.250 --> 00:04:08.700
This causes people to spend
a lot more time in their cars
00:04:08.700 --> 00:04:10.610
on their long commutes to work.
00:04:10.610 --> 00:04:14.380
And these long lines of cars
of people traveling to work
00:04:14.380 --> 00:04:17.330
emit a lot of carbon dioxide.
00:04:17.330 --> 00:04:19.820
Carbon dioxide is a greenhouse gas,
00:04:19.820 --> 00:04:22.470
which means it retains heat from the sun,
00:04:22.470 --> 00:04:24.660
and it contributes to climate change.
00:04:24.660 --> 00:04:26.930
But carbon dioxide isn't the only kind
00:04:26.930 --> 00:04:29.370
of air pollution that cities produce.
00:04:29.370 --> 00:04:30.890
Emissions from motor vehicles
00:04:30.890 --> 00:04:33.130
and industrial facilities in cities
00:04:33.130 --> 00:04:36.370
can create something
called photochemical smog.
00:04:36.370 --> 00:04:39.280
This is the kind of hazy, smoky pollution
00:04:39.280 --> 00:04:42.310
that you can sometimes see
in the horizon line of cities
00:04:42.310 --> 00:04:45.680
and it can be really
harmful to eyes and lungs.
00:04:45.680 --> 00:04:48.480
So, how could urban
planners solve this problem?
00:04:48.480 --> 00:04:50.320
Cities could cluster grocery stores,
00:04:50.320 --> 00:04:52.500
offices, and homes closer together,
00:04:52.500 --> 00:04:54.300
building up rather than out,
00:04:54.300 --> 00:04:57.080
making buildings taller rather than wider.
00:04:57.080 --> 00:04:59.570
This would mean that people
wouldn't have to travel as far
00:04:59.570 --> 00:05:00.610
to get where they need,
00:05:00.610 --> 00:05:03.030
so people could rely on walking or biking
00:05:03.030 --> 00:05:05.310
rather than
fossil-fuel-consuming vehicles.
00:05:05.310 --> 00:05:07.390
Cities can reduce vehicle emissions
00:05:07.390 --> 00:05:08.980
by making public transportation
00:05:08.980 --> 00:05:10.900
more convenient and affordable.
00:05:10.900 --> 00:05:12.200
This would mean that fewer people
00:05:12.200 --> 00:05:14.890
would need to use their
own cars to get around
00:05:14.890 --> 00:05:17.440
and it would cut down on traffic.
00:05:17.440 --> 00:05:19.600
Also, cities could build more paths,
00:05:19.600 --> 00:05:21.480
sidewalks, and bike lanes
00:05:21.480 --> 00:05:22.920
so people wouldn't have to rely
00:05:22.920 --> 00:05:25.810
on fossil-fuel-consuming
vehicles to get around.
00:05:25.810 --> 00:05:27.510
Encouraging walking and biking
00:05:27.510 --> 00:05:30.220
could also improve the
health of city residents.
00:05:30.220 --> 00:05:32.640
Cities can use clean forms of energy,
00:05:32.640 --> 00:05:36.320
like solar or wind power,
to reduce air pollution.
00:05:36.320 --> 00:05:39.130
They could also use fossil
fuels more effectively
00:05:39.130 --> 00:05:41.640
through energy co-generation,
00:05:41.640 --> 00:05:43.270
which is a way of using the heat
00:05:43.270 --> 00:05:45.770
given off by the burning of fossil fuels,
00:05:45.770 --> 00:05:47.850
not just the electricity.
00:05:47.850 --> 00:05:50.600
By creating goals and sustainable plans,
00:05:50.600 --> 00:05:53.350
cities can help reduce
air and water pollution
00:05:53.350 --> 00:05:56.270
and increase the wellbeing
of their residents.
00:05:56.270 --> 00:05:59.060
The city of Espoo in Finland, for example,
00:05:59.060 --> 00:06:03.240
was recognized as a world
leader in energy sustainability
00:06:03.240 --> 00:06:07.400
for its goal to become carbon
neutral by the year 2030.
00:06:07.400 --> 00:06:10.620
Cities are centers for economic
development, innovation,
00:06:10.620 --> 00:06:13.540
social and cultural diversity, and jobs.
00:06:13.540 --> 00:06:14.940
With some urban planning,
00:06:14.940 --> 00:06:17.913
cities can become centers
for sustainability too.
|
Impacts of Agricultural Practices | https://www.youtube.com/watch?v=dbEtcjNxGVQ | vtt | https://www.youtube.com/api/timedtext?v=dbEtcjNxGVQ&ei=5VWUZdrVHpChp-oP9cKL6AM&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=A61D2511D93E3F793B6F9EB10CE2B67940068604.8D891B2C7440848316C904372EABEC4755EA4D41&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.310 --> 00:00:01.470
- [Voiceover] Hey there.
00:00:01.470 --> 00:00:05.180
Today I'm gonna cover the impacts
of agricultural practices.
00:00:05.180 --> 00:00:08.800
And to do so, I'm gonna take
you through my morning ritual.
00:00:08.800 --> 00:00:12.260
It sounds weird, but my
bowl of multigrain Cheerios,
00:00:12.260 --> 00:00:16.180
and rice milk, and relaxing
in my super comfy pajamas,
00:00:16.180 --> 00:00:19.610
they're all connected to
intensive agricultural practices,
00:00:19.610 --> 00:00:23.770
in particular tilling,
slash and burn farming,
00:00:23.770 --> 00:00:25.123
and fertilizers.
00:00:27.960 --> 00:00:30.710
So let's take a closer look
at the Cheerios in my bowl.
00:00:32.350 --> 00:00:35.430
Most of my cereal here is
actually composed of grains
00:00:35.430 --> 00:00:39.280
like oats, corn and
barley, and growing grains
00:00:39.280 --> 00:00:41.700
typically starts with
tilling in good quality soil
00:00:41.700 --> 00:00:43.053
with lots of nutrients.
00:00:44.310 --> 00:00:45.970
But what is tilling?
00:00:45.970 --> 00:00:49.310
In short, tilling is the
process of turning soil,
00:00:49.310 --> 00:00:51.980
and it's really useful
because loosening the soil
00:00:51.980 --> 00:00:54.470
allows farmers to easily control weeds
00:00:54.470 --> 00:00:56.730
and other pests at the
surface of the soil,
00:00:56.730 --> 00:00:59.730
and it helps them to prepare
the soil for seeding.
00:00:59.730 --> 00:01:02.890
Sometimes in areas that
have been heavily farmed,
00:01:02.890 --> 00:01:05.540
the soil can become compacted over time.
00:01:05.540 --> 00:01:07.900
Here, tilling can help
to break down the soil
00:01:07.900 --> 00:01:11.120
into smaller pieces,
called soil aggregates,
00:01:11.120 --> 00:01:13.373
and allow for easier crop planting.
00:01:15.110 --> 00:01:18.260
Now, tillage has been done
for thousands of years,
00:01:18.260 --> 00:01:20.180
but it's changed a lot from the past
00:01:20.180 --> 00:01:23.050
when we used human labor
and big draft animals
00:01:23.050 --> 00:01:26.370
to till small fields,
usually once per year.
00:01:26.370 --> 00:01:29.550
Nowadays, in the era of
industrialized agriculture,
00:01:29.550 --> 00:01:32.390
large-scale farmers use
heavy mechanized equipment
00:01:32.390 --> 00:01:35.893
that can till thousands of
acres multiple times per year.
00:01:37.470 --> 00:01:42.210
Okay, we're growing more so
we're tilling more, a lot more.
00:01:42.210 --> 00:01:46.640
And while soil tillage can
help to loosen and aerate soil,
00:01:46.640 --> 00:01:49.070
what do you think happens
when heavy machinery
00:01:49.070 --> 00:01:51.420
passes over the land
and tears up the surface
00:01:51.420 --> 00:01:53.143
multiple times per year?
00:01:54.610 --> 00:01:57.800
This practice of repeated
intensive tilling
00:01:57.800 --> 00:02:00.300
compacts the lower layers of the soil
00:02:00.300 --> 00:02:02.650
and loosens the top soil to the point that
00:02:02.650 --> 00:02:07.490
it loses the ability to hold
water and nutrients in place.
00:02:07.490 --> 00:02:10.570
Tillage also reduces any
leftover crop residue
00:02:10.570 --> 00:02:11.750
like plant stocks.
00:02:11.750 --> 00:02:14.410
So, in turn, the exposed soil surface
00:02:14.410 --> 00:02:17.320
becomes really vulnerable
to wind and rain,
00:02:17.320 --> 00:02:19.900
because nothing is really
holding the soil down
00:02:19.900 --> 00:02:21.770
or providing cover.
00:02:21.770 --> 00:02:23.513
So, what happens next?
00:02:24.950 --> 00:02:27.980
Loose soil can start to
collect in surface runoff
00:02:27.980 --> 00:02:30.520
and become displaced through erosion.
00:02:30.520 --> 00:02:33.300
When this happens, soil, organic matter,
00:02:33.300 --> 00:02:36.673
and nutrients are literally
washed or blown away.
00:02:37.720 --> 00:02:39.440
Who would have thought that these Cheerios
00:02:39.440 --> 00:02:41.940
were doing so much damage?
00:02:41.940 --> 00:02:43.790
But, there's some good news here too.
00:02:45.150 --> 00:02:47.730
Low till or no till farming alternatives
00:02:47.730 --> 00:02:50.640
can alleviate some of
these problems thankfully.
00:02:50.640 --> 00:02:54.620
In the Palouse, a huge
agricultural area in the Western US
00:02:54.620 --> 00:02:57.290
where a lot of grains, just
like the ones in my cereal,
00:02:57.290 --> 00:02:58.160
are grown.
00:02:58.160 --> 00:03:02.140
No till farming is really
important because the fields are,
00:03:02.140 --> 00:03:04.590
well, they're really steep and hilly
00:03:04.590 --> 00:03:07.390
and wind and rain can
cause a lot of erosion
00:03:07.390 --> 00:03:10.020
when the soil is heavily tilled.
00:03:10.020 --> 00:03:13.340
By not tilling the fields,
farmers can prevent soil erosion,
00:03:13.340 --> 00:03:16.480
and, more importantly,
from my perspective,
00:03:16.480 --> 00:03:20.320
make sure that they can grow
lots of grains for my Cheerios
00:03:20.320 --> 00:03:23.183
But wait, cereals aren't
complete without milk.
00:03:25.240 --> 00:03:27.140
Now, I personally like rice milk
00:03:27.140 --> 00:03:29.020
because I'm lactose sensitive,
00:03:29.020 --> 00:03:31.360
and rice is commonly grown in temperate
00:03:31.360 --> 00:03:34.200
and tropical regions,
oftentimes in areas where
00:03:34.200 --> 00:03:37.963
soil quality isn't the best
and nutrients are lacking.
00:03:38.820 --> 00:03:42.500
So, how do farmers get
nutrients back into the soil?
00:03:42.500 --> 00:03:45.090
And, more importantly,
how do they grow rice
00:03:45.090 --> 00:03:47.300
for my rice milk at breakfast?
00:03:47.300 --> 00:03:50.530
Well, they often use
slash and burn farming.
00:03:50.530 --> 00:03:54.330
So, like the name, forest
plots are slashed or cut,
00:03:54.330 --> 00:03:56.700
left to dry and then burned.
00:03:56.700 --> 00:03:59.440
The ash left over from the
burning fertilizes the soil.
00:03:59.440 --> 00:04:01.733
But, it's only a temporary benefit.
00:04:02.920 --> 00:04:05.030
After about three to five years,
00:04:05.030 --> 00:04:06.900
the productivity of
slashed and burned plots
00:04:06.900 --> 00:04:09.780
goes down really quickly
due to the loss of nutrients
00:04:09.780 --> 00:04:12.170
and as weeds start to grow again.
00:04:12.170 --> 00:04:14.840
When this happens, farmers
simply abandon the field,
00:04:14.840 --> 00:04:18.090
move over to a new area
and repeat the process.
00:04:18.090 --> 00:04:20.970
But it can take decades
for these plots to recover
00:04:20.970 --> 00:04:23.370
once they've been slashed,
burned, and farmed,
00:04:23.370 --> 00:04:25.913
and this practice can
become a vicious cycle.
00:04:26.770 --> 00:04:29.770
In the Amazon, for example,
people in rural areas
00:04:29.770 --> 00:04:32.210
rely on slash-and-burn so
that they can make money
00:04:32.210 --> 00:04:35.040
selling the crops they grow
or create open pastures
00:04:35.040 --> 00:04:36.810
for animals to graze.
00:04:36.810 --> 00:04:40.480
In the process, thousands of
acres are burned each year.
00:04:40.480 --> 00:04:43.110
And as these trees and plants burn,
00:04:43.110 --> 00:04:45.360
enormous amounts of greenhouse gases,
00:04:45.360 --> 00:04:47.850
mainly carbon dioxide are produced,
00:04:47.850 --> 00:04:49.870
which contribute to climate change.
00:04:49.870 --> 00:04:53.260
And, sometimes too, fires
may not be well-managed
00:04:53.260 --> 00:04:57.823
and can burn out of control
causing huge, costly wildfires.
00:04:59.180 --> 00:05:00.840
But it's not all doom and gloom
00:05:00.840 --> 00:05:02.960
when it comes to my tasty rice milk.
00:05:02.960 --> 00:05:04.890
There are alternatives to slash and burn
00:05:04.890 --> 00:05:08.180
which include applying
animal fertilizer like manure
00:05:08.180 --> 00:05:10.770
on used plots to add
nutrients back to the soil
00:05:10.770 --> 00:05:14.270
or using alley cropping in
which trees or other vegetation
00:05:14.270 --> 00:05:16.530
are planted between crops
to help keep nutrients
00:05:16.530 --> 00:05:18.023
and moisture in the soil.
00:05:18.990 --> 00:05:21.380
All right, by now I've eaten my breakfast
00:05:21.380 --> 00:05:25.140
and I'm relaxing in my
super comfy cotton pajamas,
00:05:25.140 --> 00:05:27.640
but turns out that cotton is actually
00:05:27.640 --> 00:05:29.410
a really finicky crop to grow
00:05:29.410 --> 00:05:32.240
and it requires a lot of fertilizers.
00:05:32.240 --> 00:05:34.780
And fertilizers help plants grow,
00:05:34.780 --> 00:05:36.863
but that's not a bad thing, right?
00:05:37.730 --> 00:05:38.740
And it's not.
00:05:38.740 --> 00:05:41.860
In fact, we've been using
fertilizers for a millennia.
00:05:41.860 --> 00:05:45.030
For thousands of years, people
have used natural fertilizers
00:05:45.030 --> 00:05:47.780
to replenish or increase
nutrients in the soil
00:05:47.780 --> 00:05:49.420
and promote plant growth.
00:05:49.420 --> 00:05:51.960
Natural fertilizers meant
that farmers use things
00:05:51.960 --> 00:05:55.740
like leftover crops, manure,
wood ash, ground bones,
00:05:55.740 --> 00:05:58.933
fish or fish parts, and bird and bat poop.
00:06:00.170 --> 00:06:03.080
In the early 1800s though,
scientists discovered
00:06:03.080 --> 00:06:05.430
that nitrogen, phosphorus, and potassium
00:06:05.430 --> 00:06:07.130
were key to plant growth.
00:06:07.130 --> 00:06:09.620
And in time, many farmers began to switch
00:06:09.620 --> 00:06:12.430
from natural fertilizers
to artificial fertilizers
00:06:12.430 --> 00:06:14.830
with higher concentrations
of these nutrients
00:06:14.830 --> 00:06:17.130
which greatly increased crop yields.
00:06:17.130 --> 00:06:18.850
In other words, farmers could grow more,
00:06:18.850 --> 00:06:21.913
and that means more cotton
and more comfy pajamas.
00:06:22.990 --> 00:06:25.130
But, there's a catch.
00:06:25.130 --> 00:06:27.050
Now that farmers are growing more crops
00:06:27.050 --> 00:06:29.250
than any time in history, we've learned
00:06:29.250 --> 00:06:31.360
that there are impacts
to using large amounts
00:06:31.360 --> 00:06:33.800
of very concentrated fertilizers.
00:06:33.800 --> 00:06:36.730
Applying too much fertilizer
can pollute runoff water
00:06:36.730 --> 00:06:40.870
with excess fertilizer and
pollute local surface waters.
00:06:40.870 --> 00:06:43.270
As nutrient rich materials like fertilizer
00:06:43.270 --> 00:06:46.100
make their way into nearby
rivers, lakes, and oceans,
00:06:46.100 --> 00:06:49.210
they can cause major problems
in the balance of nutrients
00:06:49.210 --> 00:06:51.660
in marine ecosystems.
00:06:51.660 --> 00:06:53.860
When too many nutrients from fertilizers
00:06:53.860 --> 00:06:57.320
saturate a body of water,
called eutrophication,
00:06:57.320 --> 00:07:00.270
these nutrients feed the
rapid growth of algae.
00:07:00.270 --> 00:07:02.410
In turn, these massive algae blooms
00:07:02.410 --> 00:07:04.870
can suck up all the
oxygen in bodies of water
00:07:04.870 --> 00:07:08.200
and lead to enormous fish
die-offs called dead zones.
00:07:08.200 --> 00:07:11.160
Quite a morbid situation
and very different
00:07:11.160 --> 00:07:13.403
from the happy unicorns of my pajamas.
00:07:14.250 --> 00:07:17.050
But, there's ways to reduce
the amount of fertilizers
00:07:17.050 --> 00:07:18.720
released into waterways.
00:07:18.720 --> 00:07:22.100
Farmers can limit the amount
of fertilizer that they apply
00:07:22.100 --> 00:07:25.500
or use compost, which is
decomposed organic material,
00:07:25.500 --> 00:07:28.640
as a fertilizer which tends
to have lower and safer levels
00:07:28.640 --> 00:07:30.840
of nitrates and phosphates.
00:07:30.840 --> 00:07:32.370
And, there you have it.
00:07:32.370 --> 00:07:35.060
Common agricultural
practices and their impacts
00:07:35.060 --> 00:07:38.003
in a nutshell, or
really, a bowl of cereal.
|
Global wind patterns | https://www.youtube.com/watch?v=xp50_ixPOhY | vtt | https://www.youtube.com/api/timedtext?v=xp50_ixPOhY&ei=5VWUZcqUF_nDmLAP9dCqkAk&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=A323E9088CA64B9139BBDB899CFCC5825DB9FF69.5962D77FCA061C1B4A0782C69EF969C4CB8BB7BB&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.340 --> 00:00:01.570
- [Instructor] Today, we're going to talk
00:00:01.570 --> 00:00:03.623
about Global Wind Patterns.
00:00:04.730 --> 00:00:08.860
Wind determines more than just
the best places to fly kite.
00:00:08.860 --> 00:00:12.200
Global wind patterns help
control where it rains.
00:00:12.200 --> 00:00:15.020
What kinds of species
can survive in an area
00:00:15.020 --> 00:00:18.720
and even where tropical rainforests
and deserts are located.
00:00:18.720 --> 00:00:20.610
In other words, global wind patterns
00:00:20.610 --> 00:00:22.460
are really important to life.
00:00:22.460 --> 00:00:25.610
And one of the reasons we have
global wind patterns at all,
00:00:25.610 --> 00:00:28.220
is actually because of the sun.
00:00:28.220 --> 00:00:30.660
Sunlight shines on the earth like this.
00:00:30.660 --> 00:00:34.100
As you can see, the sunlight
hits the equator directly
00:00:34.100 --> 00:00:38.330
but, the light hits the North
and South poles at an angle
00:00:38.330 --> 00:00:42.430
kind of skimming the surface like this.
00:00:42.430 --> 00:00:45.060
So the equator is getting direct sunlight
00:00:46.290 --> 00:00:49.163
and the poles are only
getting indirect sunlight.
00:00:50.500 --> 00:00:51.920
With all the direct sunlight,
00:00:51.920 --> 00:00:54.580
the air on the equator gets really hot.
00:00:54.580 --> 00:00:57.290
And the air around the poles
doesn't heat up as much
00:00:57.290 --> 00:01:00.120
because it's only getting
indirect sunlight.
00:01:00.120 --> 00:01:01.570
And you may be thinking,
00:01:01.570 --> 00:01:04.000
what does this all have
to do with airflow?
00:01:04.000 --> 00:01:05.880
Let's take a closer look at the equator
00:01:05.880 --> 00:01:07.530
to see what's happening.
00:01:07.530 --> 00:01:10.100
So imagine you're standing
on a piece of land
00:01:10.100 --> 00:01:11.580
near the equator.
00:01:11.580 --> 00:01:14.600
When the direct sunlight hits the equator,
00:01:14.600 --> 00:01:18.610
the hot air near the
ground begins to rise up
00:01:18.610 --> 00:01:20.720
because hot air rises.
00:01:20.720 --> 00:01:24.750
All the direct sunlight also
causes evaporation to increase,
00:01:24.750 --> 00:01:27.120
which means that this air
that's rising up right here
00:01:27.120 --> 00:01:29.530
is both hot and moist.
00:01:29.530 --> 00:01:31.960
But once all this hot moist air reaches
00:01:31.960 --> 00:01:33.400
a high enough altitude,
00:01:33.400 --> 00:01:36.660
it begins to expand and cool down.
00:01:36.660 --> 00:01:40.540
The water vapor in the air
begins to condense into clouds
00:01:40.540 --> 00:01:43.193
and it eventually falls as
rain around the equator.
00:01:44.370 --> 00:01:47.630
The air which is now cool
and holds less moisture,
00:01:47.630 --> 00:01:51.930
sinks down to the ground
because cold air sinks
00:01:51.930 --> 00:01:53.270
and the cycle repeats
00:01:53.270 --> 00:01:56.973
with the hot moist air rising
and the cool dry air falling.
00:01:58.560 --> 00:02:00.710
And the fact that the hot air rises up,
00:02:00.710 --> 00:02:02.750
it means that this area right here
00:02:02.750 --> 00:02:04.803
is an area of low pressure.
00:02:07.430 --> 00:02:09.130
Because the air is rising up,
00:02:09.130 --> 00:02:11.210
it creates a space for cooler air
00:02:11.210 --> 00:02:15.250
in surrounding areas to
move in and take its place.
00:02:15.250 --> 00:02:18.340
And over here, where the
cool air is coming down
00:02:18.340 --> 00:02:21.120
to the ground, that's
an area of high pressure
00:02:22.640 --> 00:02:25.640
because all of that cool
dry air is coming down
00:02:25.640 --> 00:02:28.030
and pushing the air below it away.
00:02:28.030 --> 00:02:31.380
This cyclical movement
of air create something
00:02:31.380 --> 00:02:35.363
called a convection cell.
00:02:37.520 --> 00:02:39.540
If the earth wasn't spinning,
00:02:39.540 --> 00:02:42.930
we would just have one convection
cell in each hemisphere
00:02:42.930 --> 00:02:45.300
where the air would
heat up at the equator,
00:02:45.300 --> 00:02:48.940
move up towards the poles and sink down.
00:02:48.940 --> 00:02:50.900
And in the 18th century,
00:02:50.900 --> 00:02:52.420
this was how some scientists
00:02:52.420 --> 00:02:54.760
believe global wind patterns worked.
00:02:54.760 --> 00:02:57.210
But, because the earth is spinning,
00:02:57.210 --> 00:03:01.490
the earth's rotation pushes
air masses from East to West.
00:03:01.490 --> 00:03:04.700
This movement of air
creates a clockwise pattern
00:03:04.700 --> 00:03:07.870
in the Northern hemisphere and
a counter-clockwise pattern
00:03:07.870 --> 00:03:09.720
in the Southern hemisphere.
00:03:09.720 --> 00:03:11.763
This is called the Coriolis effect.
00:03:12.770 --> 00:03:16.070
And this movement of air
because of the earth's spin,
00:03:16.070 --> 00:03:19.670
causes us to actually get
three convection cells
00:03:19.670 --> 00:03:21.550
in each hemisphere.
00:03:21.550 --> 00:03:24.000
These two, the two closest to the equator
00:03:24.000 --> 00:03:26.910
are called the hadley cells.
00:03:26.910 --> 00:03:28.710
They're between the equator
00:03:28.710 --> 00:03:32.040
and the 30 degree latitude
marks in both hemispheres.
00:03:32.040 --> 00:03:35.510
These next two are called the ferrel cells
00:03:35.510 --> 00:03:37.500
or the temperate cells.
00:03:37.500 --> 00:03:40.890
And these are located between
a 30 and 60 degree marks
00:03:40.890 --> 00:03:43.550
in both the Northern and
Southern hemispheres.
00:03:43.550 --> 00:03:46.200
And lastly, we have the polar cells
00:03:46.200 --> 00:03:49.730
which as you can probably
guess are right by the poles.
00:03:49.730 --> 00:03:53.720
So we have polar cells
up here at the North pole
00:03:53.720 --> 00:03:58.210
and we also have polar cells
down here at the South pole.
00:03:58.210 --> 00:04:02.470
And these convection cells
create prevailing winds
00:04:02.470 --> 00:04:05.840
that move heat and
moisture around the earth.
00:04:05.840 --> 00:04:08.040
Let's take a look at what
happens in the bottom half
00:04:08.040 --> 00:04:09.470
of each convection cell,
00:04:09.470 --> 00:04:11.520
the parts closer to the ground.
00:04:11.520 --> 00:04:13.730
Because these parts are closer to us,
00:04:13.730 --> 00:04:16.560
we experience the air movement as wind.
00:04:16.560 --> 00:04:20.030
So on the bottom of this
convection cell, the hadley cells,
00:04:20.030 --> 00:04:23.430
the cold air is moving
towards the equator.
00:04:23.430 --> 00:04:25.420
So that means that the prevailing winds
00:04:25.420 --> 00:04:28.300
would also be moving towards the equator.
00:04:28.300 --> 00:04:31.500
Winds are named after
where they come from.
00:04:31.500 --> 00:04:35.030
So, these two winds are
called the Northeast
00:04:35.030 --> 00:04:36.650
and Southeast trade winds
00:04:36.650 --> 00:04:39.480
because they come from the
Northeast and Southeast
00:04:39.480 --> 00:04:41.560
and they move West.
00:04:41.560 --> 00:04:44.450
And the bottom halves of
the ferrel convection cells,
00:04:44.450 --> 00:04:46.900
take cool air from a 30 degree line
00:04:46.900 --> 00:04:50.610
and pull it towards the
60 degree latitude line.
00:04:50.610 --> 00:04:52.920
This creates the westerlies.
00:04:52.920 --> 00:04:55.270
And they're called the
westerlies because they pull air
00:04:55.270 --> 00:04:57.230
from the West to the East
00:04:57.230 --> 00:04:59.770
and the bottom halves of
the polar convection cells
00:04:59.770 --> 00:05:01.920
take the cool air from the poles
00:05:01.920 --> 00:05:04.570
and sweep it to the 60
degree latitude lines
00:05:04.570 --> 00:05:07.480
and this creates the Easterlies winds.
00:05:07.480 --> 00:05:10.300
It's important to remember
that everything in this diagram
00:05:10.300 --> 00:05:12.650
is just an overall model.
00:05:12.650 --> 00:05:15.150
Global wind patterns are
even more complicated
00:05:15.150 --> 00:05:18.490
because water covered areas
and land covered areas
00:05:18.490 --> 00:05:21.250
absorb solar energy differently.
00:05:21.250 --> 00:05:23.550
These prevailing wind
patterns distribute heat
00:05:23.550 --> 00:05:26.980
and precipitation unevenly
between the tropics, temperate
00:05:26.980 --> 00:05:28.970
and polar regions of the earth.
00:05:28.970 --> 00:05:33.830
And this uneven distribution
creates different biomes.
00:05:33.830 --> 00:05:37.360
And this helps determine what
species can survive where.
00:05:37.360 --> 00:05:40.620
The tropical rainforest will
be in the low pressure areas
00:05:40.620 --> 00:05:42.400
near the equator.
00:05:42.400 --> 00:05:44.980
And right here, between
the polar and ferrel cells
00:05:44.980 --> 00:05:47.270
is another area of low pressure.
00:05:47.270 --> 00:05:51.220
Just like near the equator,
hot moist air rises here
00:05:51.220 --> 00:05:54.600
causing more precipitation
in the surrounding areas.
00:05:54.600 --> 00:05:56.970
So along this longitudinal line,
00:05:56.970 --> 00:05:59.410
you'll find many coniferous forests
00:05:59.410 --> 00:06:02.550
that thrive because of
all that precipitation.
00:06:02.550 --> 00:06:04.910
And there's a high
pressure area right here
00:06:04.910 --> 00:06:06.940
where the cool dry air sinks down
00:06:06.940 --> 00:06:08.900
so there's not as much precipitation.
00:06:08.900 --> 00:06:10.410
The air is drier here.
00:06:10.410 --> 00:06:14.040
You'll find many deserts
along this line and this line.
00:06:14.040 --> 00:06:15.880
So even though convection cells
00:06:15.880 --> 00:06:18.240
and prevailing winds are invisible,
00:06:18.240 --> 00:06:20.853
the ways they shape the
environment are not.
|
El Niño and La Niña | https://www.youtube.com/watch?v=U2-ACg2kbTA | vtt | https://www.youtube.com/api/timedtext?v=U2-ACg2kbTA&ei=5VWUZevUE_Stp-oPwdexuAE&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=5B01CF1E1169AAC6850E99D6F8557CA57ACAB42F.8A3D1A0993BD6DE3DA6779E1DEE7C64A67AC0063&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.000 --> 00:00:02.720
- [Instructor] Every few years
you might hear about El Nino
00:00:02.720 --> 00:00:03.553
in the news.
00:00:03.553 --> 00:00:06.140
And this also might come
with powerful images
00:00:06.140 --> 00:00:10.179
of flooding and rainfall,
but it is not just a storm.
00:00:10.179 --> 00:00:13.470
It's actually a climate
pattern that takes place
00:00:13.470 --> 00:00:15.623
in the Pacific Ocean.
00:00:16.680 --> 00:00:17.830
And we'll get a little bit more
00:00:17.830 --> 00:00:21.130
into what that actually means.
00:00:21.130 --> 00:00:23.826
Now, fun fact about how El Nino is named
00:00:23.826 --> 00:00:25.800
is that a long time ago,
00:00:25.800 --> 00:00:28.760
South American fishermen
noticed one December
00:00:28.760 --> 00:00:31.810
that the Pacific Ocean was actually warmer
00:00:31.810 --> 00:00:33.090
than it normally is.
00:00:33.090 --> 00:00:35.470
And this brought about
an abundance of fish.
00:00:35.470 --> 00:00:38.770
So because they were grateful,
they named this event
00:00:38.770 --> 00:00:41.550
El Nino to correlate
with the commemoration
00:00:41.550 --> 00:00:45.560
of Christ in this part of the
world during Christmas time.
00:00:45.560 --> 00:00:47.940
So that's a little trivia you
can keep in your back pocket,
00:00:47.940 --> 00:00:52.330
but back to what we hear
about El Nino in the news,
00:00:52.330 --> 00:00:56.031
you might also notice
that it isn't talked about
00:00:56.031 --> 00:00:59.571
every single year and that's
because El Nino comes around
00:00:59.571 --> 00:01:04.220
every two to seven years on average.
00:01:04.220 --> 00:01:07.240
And scientists are still not sure exactly
00:01:07.240 --> 00:01:10.540
what triggers El Nino, but
they know what signs to look
00:01:10.540 --> 00:01:15.450
for once it is approaching
or once we're in that event.
00:01:15.450 --> 00:01:16.740
So even though it's true
00:01:16.740 --> 00:01:21.020
that El Nino can bring about
heavy rainfall and flooding,
00:01:21.020 --> 00:01:24.280
it can also cause severe drought.
00:01:24.280 --> 00:01:28.880
So it's really important to
note that different regions
00:01:28.880 --> 00:01:33.880
around the world experience
different effects of El Nino.
00:01:37.120 --> 00:01:39.810
And we'll see a few examples of those.
00:01:39.810 --> 00:01:43.205
So sometimes an El Nino year is actually,
00:01:43.205 --> 00:01:45.160
a little bit helpful and might bring
00:01:45.160 --> 00:01:46.980
about some much needed rain,
00:01:46.980 --> 00:01:50.796
but other times bigger and
more severe El Nino events
00:01:50.796 --> 00:01:55.796
can bring devastating weather
events all across the globe.
00:01:56.470 --> 00:01:58.130
So we can look at the different effects
00:01:58.130 --> 00:02:01.470
by looking at the biggest
El Nino on record,
00:02:01.470 --> 00:02:04.720
during the 1997 to 1998 season.
00:02:04.720 --> 00:02:07.450
And we can see how different
regions were affected.
00:02:07.450 --> 00:02:09.940
So for example, in California,
00:02:09.940 --> 00:02:13.380
we saw very destructive mudslides.
00:02:13.380 --> 00:02:16.433
In Ecuador, there was heavy rainfall.
00:02:19.286 --> 00:02:22.740
And in Indonesia there was actually
00:02:22.740 --> 00:02:25.873
extreme drought and fire.
00:02:30.170 --> 00:02:33.440
And overall, this El Nino
event was really large
00:02:33.440 --> 00:02:35.720
and very destructive, there are estimates
00:02:35.720 --> 00:02:40.720
of about $36 billion in
damage to infrastructure.
00:02:41.300 --> 00:02:43.050
So you might be asking yourself,
00:02:43.050 --> 00:02:46.950
how can the same climate
pattern caused such drastically
00:02:46.950 --> 00:02:49.490
different effects around the globe?
00:02:49.490 --> 00:02:51.220
So to understand this better,
00:02:51.220 --> 00:02:53.250
we have to look at what a quote unquote
00:02:53.250 --> 00:02:55.340
normal year looks like.
00:02:55.340 --> 00:02:57.570
So this is a map of the Pacific Ocean.
00:02:57.570 --> 00:03:01.735
And normally there are winds
that are pushing warm water
00:03:01.735 --> 00:03:03.620
towards the West.
00:03:03.620 --> 00:03:07.118
So towards Asia and the Pacific islands
00:03:07.118 --> 00:03:11.493
and warm water accumulates on this side,
00:03:12.860 --> 00:03:14.280
on the other side on the East side,
00:03:14.280 --> 00:03:16.080
near Central and South America,
00:03:16.080 --> 00:03:19.468
we have an accumulation of cool water.
00:03:19.468 --> 00:03:23.983
And this is also due to a
process called upwelling,
00:03:25.290 --> 00:03:29.880
where cold water from the bottom
of the ocean is pushed up.
00:03:29.880 --> 00:03:32.340
And during these conditions in general,
00:03:32.340 --> 00:03:35.403
you would see less rain on this side.
00:03:39.726 --> 00:03:42.809
Or you'll see more rain on this side.
00:03:44.940 --> 00:03:47.610
Okay, so now let's look
at what changes during
00:03:47.610 --> 00:03:49.460
an El Nino year.
00:03:49.460 --> 00:03:50.830
So during an El Nino year,
00:03:50.830 --> 00:03:54.642
you still have trade
winds pushing water West,
00:03:54.642 --> 00:03:58.775
but they're much weaker
and that's the key here,
00:03:58.775 --> 00:04:01.320
that your trade winds are weakened,
00:04:01.320 --> 00:04:04.300
which means less water is pushed
00:04:04.300 --> 00:04:07.820
towards Asia and the Pacific islands.
00:04:07.820 --> 00:04:10.457
So compared to a normal year,
00:04:10.457 --> 00:04:15.050
you actually have cooler water
that starts to accumulate
00:04:15.050 --> 00:04:17.720
on this side of the Pacific Ocean.
00:04:17.720 --> 00:04:19.630
Meanwhile, on the other side,
00:04:19.630 --> 00:04:23.680
since less water is being
pushed away from Central
00:04:23.680 --> 00:04:28.590
and South America, you get
more warm water accumulating.
00:04:28.590 --> 00:04:31.570
So now you can think back to
those South American fishermen
00:04:31.570 --> 00:04:34.980
and why they were experiencing warm water
00:04:34.980 --> 00:04:38.150
along their coasts during an El Nino year.
00:04:38.150 --> 00:04:40.090
So this map does a really great job
00:04:40.090 --> 00:04:42.090
of showing the temperature gradient,
00:04:42.090 --> 00:04:45.436
and how this warm water
is staying along the coast
00:04:45.436 --> 00:04:49.760
of Central and South America
during an El Nino year.
00:04:49.760 --> 00:04:54.760
Meanwhile, you have cold water
accumulating towards Asia.
00:04:55.460 --> 00:04:58.430
And this causes a lot of changes
00:04:58.430 --> 00:05:00.470
that affect weather patterns.
00:05:00.470 --> 00:05:03.480
So in the US the Pacific jet stream
00:05:03.480 --> 00:05:06.193
moves South of its neutral position.
00:05:07.140 --> 00:05:08.970
And because of that, we start to see
00:05:08.970 --> 00:05:13.360
that the Northern US and
Canada are actually warmer
00:05:13.360 --> 00:05:15.910
and drier than they usually are.
00:05:15.910 --> 00:05:19.200
The US Gulf Coast and Southwest regions
00:05:19.200 --> 00:05:21.170
of the US are wetter,
00:05:21.170 --> 00:05:24.460
and are there more
increased risk for flooding.
00:05:24.460 --> 00:05:29.210
And South Asia and the Pacific
islands experience warmer
00:05:29.210 --> 00:05:32.259
and drier conditions that lead to drought
00:05:32.259 --> 00:05:36.460
on the other side of the Pacific Ocean.
00:05:36.460 --> 00:05:40.150
So now you start to see
how one event El Nino,
00:05:40.150 --> 00:05:44.880
this one climate pattern
can cause both flooding
00:05:44.880 --> 00:05:47.150
on one side of the Pacific Ocean,
00:05:47.150 --> 00:05:50.870
while also causing
drought on the other side.
00:05:50.870 --> 00:05:53.820
And finally, we'll end with La Nina,
00:05:53.820 --> 00:05:56.190
because you might hear this come up too
00:05:56.190 --> 00:05:57.711
when talking about El Nino.
00:05:57.711 --> 00:06:00.310
So La Nina is essentially the opposite.
00:06:00.310 --> 00:06:02.020
So if you've got El Nino down,
00:06:02.020 --> 00:06:04.090
you can start to understand what happens
00:06:04.090 --> 00:06:06.680
during La Nina event.
00:06:06.680 --> 00:06:08.030
So in this situation,
00:06:08.030 --> 00:06:13.030
our trade winds are getting
stronger than our normal years.
00:06:13.970 --> 00:06:15.970
So they're pushing water West,
00:06:15.970 --> 00:06:18.780
but they're doing so even more
00:06:18.780 --> 00:06:20.910
than we normally would expect.
00:06:20.910 --> 00:06:24.520
So this warm water that accumulates
00:06:24.520 --> 00:06:28.440
towards Asia actually
accumulates more West
00:06:28.440 --> 00:06:32.320
than it would during our normal years.
00:06:32.320 --> 00:06:35.970
And on the other side, we
have even more upwelling
00:06:37.280 --> 00:06:40.610
causing this cold water to accumulate.
00:06:40.610 --> 00:06:45.220
So the next time you hear El
Nino or LA Nina in the news,
00:06:45.220 --> 00:06:46.860
you'll know that they're not just talking
00:06:46.860 --> 00:06:50.050
about a really big storm,
but they're actually talking
00:06:50.050 --> 00:06:53.072
about climate patterns
that can affect weather
00:06:53.072 --> 00:06:55.223
all across the globe.
|
Soil Texture Triangle | https://www.youtube.com/watch?v=Bn9ul9lxIdg | vtt | https://www.youtube.com/api/timedtext?v=Bn9ul9lxIdg&ei=5VWUZdL_KY_YxN8PkJqK2A0&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=E671E17F223E01808D2F404000138B6B5C7BD041.D95926EF6113E1C26882319F4BED5721BC99A7D4&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:01.670 --> 00:00:04.150
- [Narrator] Today, we're
going to talk about soil.
00:00:04.150 --> 00:00:05.450
And you've probably noticed
00:00:05.450 --> 00:00:07.830
that there are many
different kinds of soils.
00:00:07.830 --> 00:00:09.160
The soil near a beach
00:00:09.160 --> 00:00:10.730
looks and feels very different
00:00:10.730 --> 00:00:12.620
than the soil in a forest.
00:00:12.620 --> 00:00:14.190
And part of the reason for that difference
00:00:14.190 --> 00:00:17.620
is something called soil texture.
00:00:17.620 --> 00:00:19.470
Soil texture.
00:00:19.470 --> 00:00:21.290
So when soil is formed,
00:00:21.290 --> 00:00:24.140
different types of rock break down
00:00:24.140 --> 00:00:27.690
because of the wind and
the rain and the weather.
00:00:27.690 --> 00:00:31.200
And they become differently
sized particles.
00:00:31.200 --> 00:00:33.740
And the combination of these
differently sized particles
00:00:33.740 --> 00:00:35.810
creates soil texture.
00:00:35.810 --> 00:00:37.420
So these differently sized particles
00:00:37.420 --> 00:00:39.740
can be broken down into three groups.
00:00:39.740 --> 00:00:41.483
We have sand.
00:00:43.744 --> 00:00:44.577
We have silt.
00:00:46.100 --> 00:00:47.803
And we have clay.
00:00:48.760 --> 00:00:52.370
Sand is made up of the larger
and heavier particles of soil.
00:00:52.370 --> 00:00:55.430
Sand is around two millimeters.
00:00:55.430 --> 00:01:00.350
Two millimeters to 0.05 millimeters.
00:01:00.350 --> 00:01:03.720
Which is a 20th of a
millimeter in diameter.
00:01:03.720 --> 00:01:06.553
And if it feels very gritty to touch.
00:01:08.570 --> 00:01:12.310
Clay on the other hand is the
smallest particles of soil.
00:01:12.310 --> 00:01:16.680
It's around 0.002
millimeters and the smaller.
00:01:16.680 --> 00:01:18.640
That's a 500th of a millimeter.
00:01:18.640 --> 00:01:20.083
So really tiny.
00:01:20.930 --> 00:01:22.650
If you rubbed clay between your fingers,
00:01:22.650 --> 00:01:23.690
it would feel smooth,
00:01:23.690 --> 00:01:24.720
and you wouldn't be able to feel
00:01:24.720 --> 00:01:26.950
the individual particles of soil.
00:01:26.950 --> 00:01:29.870
And unlike sand, you can't
even see clay's particles
00:01:29.870 --> 00:01:30.883
with a naked eye.
00:01:31.840 --> 00:01:35.240
Most people are familiar with
sandy soils and clay soils,
00:01:35.240 --> 00:01:37.550
but silt is right in between.
00:01:37.550 --> 00:01:40.810
It's made of a particles between
the size of clay and sand.
00:01:40.810 --> 00:01:45.410
So, it's between 0.05 millimeters
00:01:45.410 --> 00:01:48.283
and 0.002 millimeters.
00:01:50.610 --> 00:01:53.240
So when you think of silt
imagine baking flour.
00:01:53.240 --> 00:01:55.180
It's powdery.
00:01:55.180 --> 00:01:56.013
Powdery.
00:01:58.280 --> 00:02:01.210
And it can be carried
easily by wind and water.
00:02:01.210 --> 00:02:02.840
But soil is more complicated
00:02:02.840 --> 00:02:05.160
than just these three soil types.
00:02:05.160 --> 00:02:07.810
If you grabbed a handful of
soil from outside your home,
00:02:07.810 --> 00:02:10.880
it would probably be a combination
of all three soil types,
00:02:10.880 --> 00:02:13.010
along with some organic material.
00:02:13.010 --> 00:02:14.870
A soil's unique texture,
00:02:14.870 --> 00:02:18.040
that is it's combination
of silt, sand, and clay,
00:02:18.040 --> 00:02:19.840
affects how plants will grow.
00:02:19.840 --> 00:02:22.560
And so gardeners often wanna
know about their soil textures.
00:02:22.560 --> 00:02:25.210
They know what kinds of
plants to grow in that area.
00:02:25.210 --> 00:02:26.600
This is where a helpful diagram
00:02:26.600 --> 00:02:29.610
called the soil texture triangle comes in.
00:02:29.610 --> 00:02:31.713
The soil texture triangle.
00:02:32.910 --> 00:02:35.660
The triangle allows us
to place any soil sample
00:02:35.660 --> 00:02:38.670
into one of 12 different
soil texture categories.
00:02:38.670 --> 00:02:40.850
The 12 different categories are broken up
00:02:40.850 --> 00:02:43.150
based on the percentage of silt, clay
00:02:43.150 --> 00:02:44.780
and sand in the soil.
00:02:44.780 --> 00:02:45.790
To see how this works,
00:02:45.790 --> 00:02:47.640
let's do an example.
00:02:47.640 --> 00:02:50.973
Let's say a gardener determined
that a soil was 30% sand,
00:02:52.270 --> 00:02:53.513
40% silt,
00:02:54.430 --> 00:02:56.253
and 30% clay.
00:02:57.310 --> 00:03:00.080
So, how can we figure out
what kind of soil have?
00:03:00.080 --> 00:03:03.570
First, we need to pick a side
of the triangle to start with.
00:03:03.570 --> 00:03:05.070
I'll start with sand.
00:03:05.070 --> 00:03:07.160
We know we have 30% sand.
00:03:07.160 --> 00:03:09.800
So, we go along the side of the triangle,
00:03:09.800 --> 00:03:12.620
until we find that 30% mark, right here.
00:03:12.620 --> 00:03:14.630
We want to draw a line from this point,
00:03:14.630 --> 00:03:15.540
to the side of the triangle,
00:03:15.540 --> 00:03:17.790
that this arrow is pointing to.
00:03:17.790 --> 00:03:20.070
The arrow is pointing
towards the clay side.
00:03:20.070 --> 00:03:23.570
So we draw the line
from the 30% sand mark,
00:03:23.570 --> 00:03:26.120
through the triangle, to the clay side.
00:03:26.120 --> 00:03:26.973
Like this.
00:03:27.850 --> 00:03:29.080
And by drawing this line,
00:03:29.080 --> 00:03:31.190
we already know that our soil sample
00:03:31.190 --> 00:03:34.030
will fall into a category along this line.
00:03:34.030 --> 00:03:39.000
So, it could be so silt loam,
loam, clay loam, or clay.
00:03:39.000 --> 00:03:41.020
But to figure out exactly where it is,
00:03:41.020 --> 00:03:42.810
let's draw another line.
00:03:42.810 --> 00:03:44.220
Let's do silt.
00:03:44.220 --> 00:03:46.153
The soil has 40% silt.
00:03:47.030 --> 00:03:48.900
We'll draw our line through the triangle
00:03:48.900 --> 00:03:51.263
towards the sand side
because of this arrow.
00:03:52.690 --> 00:03:54.750
So again, we do the same thing.
00:03:54.750 --> 00:03:58.030
We go along the percent silt's line.
00:03:58.030 --> 00:04:00.160
We find the 40% mark.
00:04:00.160 --> 00:04:03.270
And we're gonna draw a line from 40%
00:04:03.270 --> 00:04:05.063
to the other side of the triangle.
00:04:06.020 --> 00:04:07.920
And you can see when we draw that line,
00:04:07.920 --> 00:04:11.323
these two lines intersect
at the clay loam point.
00:04:12.300 --> 00:04:13.150
But to double-check,
00:04:13.150 --> 00:04:18.150
let's draw a line from the 30% clay mark,
00:04:19.300 --> 00:04:23.590
to the other side of
the triangle, like this.
00:04:23.590 --> 00:04:25.470
As you can see, these three lines,
00:04:25.470 --> 00:04:27.300
all intersected at the same point,
00:04:27.300 --> 00:04:28.603
right here in clay loam.
00:04:30.020 --> 00:04:31.943
So we know that we have clay loam.
00:04:32.970 --> 00:04:36.250
Notice that the percentage
of clay, silt and sand,
00:04:36.250 --> 00:04:38.860
all add up to a total of 100%.
00:04:38.860 --> 00:04:40.960
We could have picked
any two of these lines,
00:04:40.960 --> 00:04:43.090
just two, to find our answer.
00:04:43.090 --> 00:04:45.810
We don't need to draw
three lines every time.
00:04:45.810 --> 00:04:47.610
Let's do another example.
00:04:47.610 --> 00:04:50.370
Let's say our gardener has another plot,
00:04:50.370 --> 00:04:53.593
with soil that contains 58% sand,
00:04:54.560 --> 00:04:55.873
27% silt,
00:04:57.770 --> 00:04:59.693
and 15% clay.
00:05:00.890 --> 00:05:05.060
So, I'm gonna go along the
percent sand part and find 58%.
00:05:05.060 --> 00:05:07.400
So that's pretty close to 60.
00:05:07.400 --> 00:05:09.490
And I'm gonna draw a line from 58%,
00:05:09.490 --> 00:05:11.740
to the other side of the triangle.
00:05:11.740 --> 00:05:13.260
Sometimes the example question,
00:05:13.260 --> 00:05:15.630
doesn't give us round
numbers to work with.
00:05:15.630 --> 00:05:16.520
So when that's the case,
00:05:16.520 --> 00:05:18.270
I like to use a ruler or a straight edge,
00:05:18.270 --> 00:05:21.000
just to make sure that my
lines are in the correct spot.
00:05:21.000 --> 00:05:24.500
Next I'm gonna use the 15% clay.
00:05:24.500 --> 00:05:27.160
So I find the 15% clay mark,
00:05:27.160 --> 00:05:30.810
and we draw a line for 15% to
the other side of the triangle
00:05:30.810 --> 00:05:33.750
following the direction of
the lines within the triangle.
00:05:33.750 --> 00:05:36.660
And we can see that our two lines
00:05:36.660 --> 00:05:39.470
intersect at this point.
00:05:39.470 --> 00:05:41.690
So, we have sandy loam.
00:05:41.690 --> 00:05:46.690
The gardener has these two
plots clay loam and sandy loam.
00:05:48.550 --> 00:05:50.540
So when the gardener
looks at her two plots,
00:05:50.540 --> 00:05:52.160
she might wanna take into account
00:05:52.160 --> 00:05:53.670
the different kinds of soil.
00:05:53.670 --> 00:05:56.230
Certain kinds of plants do
better in clay loam soil
00:05:56.230 --> 00:05:58.970
while others would do better
in the sandy loam soil.
00:05:58.970 --> 00:06:00.960
This is partly because clay soils,
00:06:00.960 --> 00:06:04.050
hold onto moisture for
longer than sandy soils do.
00:06:04.050 --> 00:06:06.520
So the plants in the
gardeners sandy loam plot,
00:06:06.520 --> 00:06:08.610
would do better if they
had longer root systems
00:06:08.610 --> 00:06:10.800
to access water deeper in the ground.
00:06:10.800 --> 00:06:14.330
Or if they stored water inside
themselves to access later.
00:06:14.330 --> 00:06:16.690
The gardener could use a
gardening book or the internet
00:06:16.690 --> 00:06:18.340
to see what kinds of plants would do best
00:06:18.340 --> 00:06:20.320
in each of her two plots.
00:06:20.320 --> 00:06:23.353
Thanks for watching and
happy soil identification.
|
Hess's law | https://www.youtube.com/watch?v=QU3zVec5I_M | vtt | https://www.youtube.com/api/timedtext?v=QU3zVec5I_M&ei=5VWUZdD9GNm-mLAPrqqEgA4&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=482E3D5D68285B4BECAF4EF0CC9AB25197940059.216A2F393A1B9670800BE7CAB0D4239E3AD2A848&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.710 --> 00:00:03.040
- [Instructor] Hess's law
states that the overall change
00:00:03.040 --> 00:00:06.270
in enthalpy for a chemical
reaction is equal to the sum
00:00:06.270 --> 00:00:09.333
of the enthalpy changes for each step.
00:00:09.333 --> 00:00:12.020
And this is independent of the path taken.
00:00:12.020 --> 00:00:14.900
So it doesn't matter what
set of reactions you use.
00:00:14.900 --> 00:00:18.660
If you add up those reactions
and they equal the reaction
00:00:18.660 --> 00:00:19.891
that you're trying to find,
00:00:19.891 --> 00:00:22.270
you can also sum the enthalpies
00:00:22.270 --> 00:00:25.090
to find the enthalpy
change for the reaction.
00:00:25.090 --> 00:00:27.440
As an example, let's say we're
trying to find the change
00:00:27.440 --> 00:00:31.490
in enthalpy for the reaction
of carbon with hydrogen gas
00:00:31.490 --> 00:00:35.210
to form C2H2, which is acetylene.
00:00:35.210 --> 00:00:38.080
We can calculate the change
in enthalpy for the formation
00:00:38.080 --> 00:00:42.600
of acetylene using these
three reactions below.
00:00:42.600 --> 00:00:45.460
Our approach will involve
looking at these three reactions
00:00:45.460 --> 00:00:48.440
and comparing them to
the original reaction
00:00:48.440 --> 00:00:50.940
to see if we need to change anything.
00:00:50.940 --> 00:00:53.690
For example, if we look at reaction one,
00:00:53.690 --> 00:00:55.480
there's one mole of acetylene
00:00:55.480 --> 00:00:57.900
on the left side of the equation.
00:00:57.900 --> 00:01:00.980
And if we compare that
to the original reaction,
00:01:00.980 --> 00:01:03.670
there's one mole of
acetylene on the right side
00:01:03.670 --> 00:01:04.870
of the equation.
00:01:04.870 --> 00:01:07.480
So we need to reverse equation one
00:01:07.480 --> 00:01:11.240
to make it look more like
our original reaction.
00:01:11.240 --> 00:01:14.480
To save time, I've gone ahead
and reversed equation one.
00:01:14.480 --> 00:01:16.840
So you can see, I did that down here.
00:01:16.840 --> 00:01:19.820
Looking at the original
equation for equation one,
00:01:19.820 --> 00:01:21.160
here where the products
00:01:21.160 --> 00:01:24.730
and now we've made those
products the reactants.
00:01:24.730 --> 00:01:28.110
And what were the reactants
over here for equation one
00:01:28.110 --> 00:01:30.960
have now become the products.
00:01:30.960 --> 00:01:33.520
The change in enthalpy for equation one
00:01:33.520 --> 00:01:38.520
is -1,299.6 kilojoules
per mole of reaction.
00:01:38.740 --> 00:01:41.780
Kilojoules per mole reaction
just means how the reaction
00:01:41.780 --> 00:01:43.670
is written in the balanced equation.
00:01:43.670 --> 00:01:46.940
And since we reversed equation one,
00:01:46.940 --> 00:01:50.240
we also need to reverse
the sign for Delta H.
00:01:50.240 --> 00:01:52.800
So instead of this being a negative,
00:01:52.800 --> 00:01:53.840
instead of this being a negative,
00:01:53.840 --> 00:01:56.350
we're gonna go ahead and
change this into a positive.
00:01:56.350 --> 00:02:00.000
And also let's go ahead and
cross out the first equation.
00:02:00.000 --> 00:02:03.290
So we don't get confused.
00:02:03.290 --> 00:02:05.010
Next, we look at equation two
00:02:05.010 --> 00:02:07.360
and we compare it to our original.
00:02:07.360 --> 00:02:10.540
For equation two there's
one mole of solid carbon
00:02:10.540 --> 00:02:14.608
on the left side and looking
at our original reaction,
00:02:14.608 --> 00:02:18.200
there's two moles of
carbon on the left side.
00:02:18.200 --> 00:02:21.670
So to get equation two, to
look like our original equation
00:02:21.670 --> 00:02:25.710
we need to multiply everything
through, by a factor of two.
00:02:25.710 --> 00:02:29.080
So we're gonna multiply
everything in equation two
00:02:29.080 --> 00:02:30.623
by a factor of two.
00:02:31.630 --> 00:02:33.540
To save some time, I have
gone ahead and written out
00:02:33.540 --> 00:02:34.373
what we would get.
00:02:34.373 --> 00:02:37.330
We would get two carbons plus two O2s
00:02:37.330 --> 00:02:39.850
goes to 2CO2.
00:02:39.850 --> 00:02:42.170
The change in the
enthalpy for the formation
00:02:42.170 --> 00:02:44.350
of one mole of CO2
00:02:44.350 --> 00:02:49.050
was -393.5 kilojoules
per mole of reaction.
00:02:49.050 --> 00:02:52.250
But now we're forming two moles of CO2.
00:02:52.250 --> 00:02:55.070
And since we multiplied
the equation through
00:02:55.070 --> 00:02:56.860
by a factor of two, we also need
00:02:56.860 --> 00:02:58.910
to multiply the change in enthalpy
00:02:58.910 --> 00:03:01.200
by a factor of two as well.
00:03:01.200 --> 00:03:03.810
And also let's go ahead and cross out
00:03:03.810 --> 00:03:04.859
this first version here
00:03:04.859 --> 00:03:08.333
because now we're
forming two moles of CO2.
00:03:09.170 --> 00:03:10.670
Next, we look at equation three
00:03:10.670 --> 00:03:12.870
and we can see there's
one mole of hydrogen gas
00:03:12.870 --> 00:03:14.700
on the left side of the equation
00:03:14.700 --> 00:03:16.770
which matches the original reaction
00:03:16.770 --> 00:03:20.040
which also has one mole of
hydrogen gas on the left side.
00:03:20.040 --> 00:03:22.840
So we don't need to do
anything to equation three.
00:03:22.840 --> 00:03:25.020
And since we're not doing
anything to the equation,
00:03:25.020 --> 00:03:26.750
we're also not gonna do anything
00:03:26.750 --> 00:03:28.980
to the change in the enthalpy.
00:03:28.980 --> 00:03:33.980
So it's gonna stay -285.8
kilojoules per mole of reaction.
00:03:34.270 --> 00:03:37.210
Next we add up all of our
reactants and products.
00:03:37.210 --> 00:03:42.210
So we have two CO2 plus
H2O plus 2C plus 2O2
00:03:46.060 --> 00:03:48.830
plus H2 plus one half O2.
00:03:48.830 --> 00:03:52.460
So those are all written
down here for our reactants.
00:03:52.460 --> 00:03:56.210
And then for the products, let
me just change colors here.
00:03:56.210 --> 00:03:59.400
We have C2H2 plus 5O2
00:04:00.470 --> 00:04:04.410
plus 2CO2 plus H2O.
00:04:04.410 --> 00:04:08.623
And so those are written
over here for the products.
00:04:09.530 --> 00:04:11.310
Next we see what we can cancel out.
00:04:11.310 --> 00:04:13.220
There's 2CO2 on the left side
00:04:13.220 --> 00:04:15.250
and there's 2CO2 on the right side.
00:04:15.250 --> 00:04:16.540
So those cancel out.
00:04:16.540 --> 00:04:19.990
There's one water on the left
and one water on the right.
00:04:19.990 --> 00:04:23.598
And there's 2O2s plus one half O2
00:04:23.598 --> 00:04:28.430
which is 2.5O2s or five halves O2s.
00:04:28.430 --> 00:04:32.020
So the oxygen's cancel
out on both sides as well.
00:04:32.020 --> 00:04:37.020
And we can see we're left with
two carbons plus one hydrogen
00:04:37.390 --> 00:04:40.680
goes to form one C2H2
00:04:40.680 --> 00:04:45.560
which is the same as
our original equation.
00:04:45.560 --> 00:04:48.250
Since we were able to add up our equations
00:04:48.250 --> 00:04:50.310
and get the overall equation,
00:04:50.310 --> 00:04:51.640
according to Hess's law,
00:04:51.640 --> 00:04:55.310
we should also be able to
add the changes in enthalpies
00:04:55.310 --> 00:04:57.483
for these steps to get
the change in the enthalpy
00:04:57.483 --> 00:05:00.380
for the overall reaction.
00:05:00.380 --> 00:05:01.980
If we look at the changes in enthalpy
00:05:01.980 --> 00:05:06.910
for the individual steps, we had +1299.6
00:05:06.910 --> 00:05:08.090
for the first equation.
00:05:08.090 --> 00:05:09.470
And so that's up here.
00:05:09.470 --> 00:05:13.560
For the second equation we
had negative 393.5 times two,
00:05:13.560 --> 00:05:14.450
which is -787.
00:05:15.640 --> 00:05:19.570
And for our third equation, we had -285.8.
00:05:19.570 --> 00:05:22.120
So that's -285.8.
00:05:22.120 --> 00:05:23.360
When we add everything together
00:05:23.360 --> 00:05:28.360
we get +226.8 kilojoules
per mole of reaction.
00:05:29.600 --> 00:05:32.570
So for the formation of
one mole of acetylene
00:05:32.570 --> 00:05:35.920
from two moles of carbon
and one mole of hydrogen
00:05:35.920 --> 00:05:38.380
the change in enthalpy for this reaction
00:05:38.380 --> 00:05:43.163
is equal to +226.8 kilojoules
per mole of reaction.
|
Complex numbers with the same modulus (absolute value) | https://www.youtube.com/watch?v=uB5QDraFefs | vtt | https://www.youtube.com/api/timedtext?v=uB5QDraFefs&ei=5VWUZZqZMO_1mLAPi5uNyA0&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=64433670FF7007E349AD7BA8364010D1B9044077.07E24C22C794E452C52ECADF91371A98A7A9BF48&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.200 --> 00:00:02.890
- [Instructor] We are asked,
which of these complex numbers
00:00:02.890 --> 00:00:06.520
has a modulus of 13?
00:00:06.520 --> 00:00:08.430
And just as a bit of a hint,
00:00:08.430 --> 00:00:12.520
when we're talking about the
modulus of a complex number,
00:00:12.520 --> 00:00:15.510
we're really just talking
about its absolute value.
00:00:15.510 --> 00:00:18.410
Or if we were to plot
it in the complex plane,
00:00:18.410 --> 00:00:20.100
which is what we have right over here,
00:00:20.100 --> 00:00:23.290
what is its distance from the origin?
00:00:23.290 --> 00:00:26.650
So really you need to find
which of these complex numbers
00:00:26.650 --> 00:00:31.650
has a distance of 13 from the
origin in the complex plane.
00:00:31.940 --> 00:00:34.540
Pause this video and see
if you can figure that out.
00:00:35.640 --> 00:00:38.240
All right, now let's work
through this together.
00:00:38.240 --> 00:00:40.640
Now one might jump out at you immediately
00:00:40.640 --> 00:00:43.880
that's going to have a
distance of 13 from the origin.
00:00:43.880 --> 00:00:46.350
If this is the origin right over here,
00:00:46.350 --> 00:00:49.180
we see that if we go exactly 13 units down
00:00:49.180 --> 00:00:52.500
we have this point right
over here, negative 13i.
00:00:52.500 --> 00:00:55.117
So immediately right
out of the gate, I say,
00:00:55.117 --> 00:00:58.270
"Okay, that complex number
has a modulus of 13,"
00:00:58.270 --> 00:01:00.450
but is that the only one?
00:01:00.450 --> 00:01:03.290
Well, we can actually visualize
all of the complex numbers
00:01:03.290 --> 00:01:06.770
that have a modulus of
13 by drawing a circle
00:01:06.770 --> 00:01:09.840
with the radius 13 centered at the origin.
00:01:09.840 --> 00:01:12.160
So let's do that.
00:01:12.160 --> 00:01:14.630
And we can see that it contains
00:01:14.630 --> 00:01:17.000
the first complex number
that we looked for,
00:01:17.000 --> 00:01:20.900
but it also seems to have included in it
00:01:20.900 --> 00:01:24.160
this one right over
here, and we can verify
00:01:24.160 --> 00:01:27.360
that the modulus right over
here is going to be 13.
00:01:27.360 --> 00:01:29.910
We can just use the Pythagorean theorem.
00:01:29.910 --> 00:01:33.730
So this distance right over here is 12.
00:01:33.730 --> 00:01:36.920
And this distance right over here is 5.
00:01:36.920 --> 00:01:38.840
And so we just need to figure out
00:01:38.840 --> 00:01:41.600
the hypotenuse right over here.
00:01:41.600 --> 00:01:43.910
And so we know that the hypotenuse
00:01:43.910 --> 00:01:47.660
is going to be the
square root of 5 squared
00:01:47.660 --> 00:01:49.240
plus 12 squared,
00:01:49.240 --> 00:01:53.637
which is equal to the
square root of 25 plus 144,
00:01:54.530 --> 00:01:57.670
which is equal to the square root of 169,
00:01:57.670 --> 00:02:01.050
which indeed does equal 13.
00:02:01.050 --> 00:02:03.160
So I like that choice as well.
00:02:03.160 --> 00:02:05.760
And we can see visually that
none of these other points
00:02:05.760 --> 00:02:08.600
that they already plotted
sit on that circle.
00:02:08.600 --> 00:02:10.710
So they don't have a modulus of 13.
00:02:10.710 --> 00:02:13.860
If we wanted to come up with
some other interesting points,
00:02:13.860 --> 00:02:17.640
we could instead of having
negative 5 plus 12i,
00:02:17.640 --> 00:02:20.270
we could have negative 5 minus 12i.
00:02:20.270 --> 00:02:21.770
It would get us right over there.
00:02:21.770 --> 00:02:24.480
And that would have a modulus of 13.
00:02:24.480 --> 00:02:27.310
And notice, when you have
your complex conjugate,
00:02:27.310 --> 00:02:29.260
it has the same modulus.
00:02:29.260 --> 00:02:30.760
Or you could go the other way around.
00:02:30.760 --> 00:02:35.510
Instead of negative 5 plus
12i, you could have 5 plus 12i.
00:02:35.510 --> 00:02:38.130
That also would have a modulates of 13.
00:02:38.130 --> 00:02:41.240
Or you could have 5 minus 12i.
00:02:41.240 --> 00:02:43.730
That also would have a modulus of 13.
00:02:43.730 --> 00:02:45.670
Now there's an infinite number of points,
00:02:45.670 --> 00:02:47.590
any of these points on the circle,
00:02:47.590 --> 00:02:50.323
that will have a modulus of 13.
|
Factoring polynomials using complex numbers | https://www.youtube.com/watch?v=9NhTVXhfqzU | vtt | https://www.youtube.com/api/timedtext?v=9NhTVXhfqzU&ei=5VWUZYvWI4rVhcIP652h-AU&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=284557ABF9D3DDA954B25302F475B7C87319E5F6.B5AC8BE209B71D098AB368E42BB97DB2C4D1A5AB&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.340 --> 00:00:01.830
- [Instructor] We're told that Amat tried
00:00:01.830 --> 00:00:05.570
to write x to the fourth
plus 5x squared plus 4
00:00:05.570 --> 00:00:08.490
as a product of linear factors.
00:00:08.490 --> 00:00:10.140
This is his work.
00:00:10.140 --> 00:00:12.400
And then they'd tell us all
of the steps that he did.
00:00:12.400 --> 00:00:14.180
And then they say, in what step
00:00:14.180 --> 00:00:17.330
did Amat make his first mistake?
00:00:17.330 --> 00:00:20.203
So pause this video and see
if you can figure that out.
00:00:21.360 --> 00:00:24.190
All right, now let's work
through this together.
00:00:24.190 --> 00:00:26.530
So we're starting with x to
the fourth plus 10x squared
00:00:26.530 --> 00:00:27.760
plus 9.
00:00:27.760 --> 00:00:30.220
And it looks like Amat
tried to factor that
00:00:30.220 --> 00:00:33.570
into x squared plus 9
times x squared plus 1.
00:00:33.570 --> 00:00:35.920
And this indeed does make sense,
00:00:35.920 --> 00:00:38.100
because if we said that let's say,
00:00:38.100 --> 00:00:41.770
u is equal to x squared,
00:00:41.770 --> 00:00:43.840
we could rewrite this right over here
00:00:43.840 --> 00:00:48.097
as u squared plus 10u plus 9.
00:00:49.960 --> 00:00:51.640
The whole reason why you would do this is
00:00:51.640 --> 00:00:54.580
so that you could write
this higher order expression
00:00:54.580 --> 00:00:57.130
in terms of a second degree expression.
00:00:57.130 --> 00:00:59.090
And then we've learned
how to factor things like
00:00:59.090 --> 00:01:00.020
this many times.
00:01:00.020 --> 00:01:00.980
We look, we say, okay,
00:01:00.980 --> 00:01:03.570
what two numbers when I add them I get 10,
00:01:03.570 --> 00:01:05.620
and when I multiply them I get nine,
00:01:05.620 --> 00:01:07.270
and it would be nine and one?
00:01:07.270 --> 00:01:08.480
And so you could write this
00:01:08.480 --> 00:01:13.480
as u plus 9 times u plus 1.
00:01:13.800 --> 00:01:15.700
And of course, if u is equal to x squared,
00:01:15.700 --> 00:01:20.700
this would be x squared plus
9 times x squared plus 1.
00:01:21.220 --> 00:01:23.730
Which is exactly what
Amat has right over here.
00:01:23.730 --> 00:01:27.120
So step one is looking great.
00:01:27.120 --> 00:01:30.670
All right, now let's think
about what Amat did in step two.
00:01:30.670 --> 00:01:33.400
They didn't do anything
to x squared plus 9
00:01:33.400 --> 00:01:34.380
but it looks like they tried
00:01:34.380 --> 00:01:37.490
to further factor x squared plus 1.
00:01:37.490 --> 00:01:39.240
And this does seem right.
00:01:39.240 --> 00:01:41.560
We just have to remind ourselves just
00:01:41.560 --> 00:01:43.610
as you have a difference of squares
00:01:43.610 --> 00:01:45.620
if you're dealing with
non-complex numbers,
00:01:45.620 --> 00:01:47.540
so we could rewrite this right over here
00:01:47.540 --> 00:01:52.200
as x plus a times x minus a.
00:01:52.200 --> 00:01:54.840
We could have a sum of squares
00:01:54.840 --> 00:01:57.200
if we're thinking about complex numbers.
00:01:57.200 --> 00:02:02.200
This is going to be x
plus ai times x minus ai.
00:02:04.760 --> 00:02:08.170
And in this situation while the x is x
00:02:08.170 --> 00:02:10.880
and then our a would be one.
00:02:10.880 --> 00:02:13.760
So we're going to have x plus i,
00:02:13.760 --> 00:02:17.960
x plus i times x minus i .
00:02:17.960 --> 00:02:20.770
So step two is looking great.
00:02:20.770 --> 00:02:22.640
And now let's go do step three.
00:02:22.640 --> 00:02:24.150
So in step three,
00:02:24.150 --> 00:02:28.120
no change to this part of the expression.
00:02:28.120 --> 00:02:29.900
And it looks like Amat is trying
00:02:29.900 --> 00:02:33.280
to factor x squared plus 9
based on the same principle.
00:02:33.280 --> 00:02:35.480
Now x squared plus 9 is the same thing
00:02:35.480 --> 00:02:38.690
as x squared plus 3 squared.
00:02:38.690 --> 00:02:41.100
So if you use this exact same idea here,
00:02:41.100 --> 00:02:46.100
if you factored it should be
x plus 3i times x minus 3i.
00:02:48.420 --> 00:02:49.920
But what we see over here
00:02:49.920 --> 00:02:52.340
is Amat took the square root of three,
00:02:52.340 --> 00:02:54.090
instead of just having a three here.
00:02:54.090 --> 00:02:56.450
Amat treated it instead
of having a nine here
00:02:56.450 --> 00:02:58.790
as if we actually had a three
00:02:58.790 --> 00:03:01.730
so they made a little
bit of an error there.
00:03:01.730 --> 00:03:06.730
So this is the step where
Amat makes his first mistake
00:03:07.800 --> 00:03:08.633
and we're done.
|
Expected payoff example: protection plan | https://www.youtube.com/watch?v=mKPeuVjPDo0 | vtt | https://www.youtube.com/api/timedtext?v=mKPeuVjPDo0&ei=5VWUZZGVJv2dp-oPkJaXeA&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=0ECD94EABFB43094F74E96F6DFFC4EC37F2253A1.53798958353851084D5A21AB517E55B03BE62BE2&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.160 --> 00:00:01.790
- [Instructor] We're told
that an electronic store
00:00:01.790 --> 00:00:05.000
gives customers the option of
purchasing a protection plan
00:00:05.000 --> 00:00:06.720
when customers buy a new television.
00:00:06.720 --> 00:00:08.330
That's actually quite common.
00:00:08.330 --> 00:00:10.990
The customer pays $80 for the plan and,
00:00:10.990 --> 00:00:14.180
if their television is
damaged or stops working,
00:00:14.180 --> 00:00:17.420
the store will replace it
for no additional charge.
00:00:17.420 --> 00:00:21.010
The store knows that 2% of
customers who buy this plan
00:00:21.010 --> 00:00:22.426
end up needing a replacement
00:00:22.426 --> 00:00:25.860
that costs the store $1,200 each.
00:00:25.860 --> 00:00:28.685
Here's a table that summarizes
the possible outcomes
00:00:28.685 --> 00:00:31.269
from the store's perspective.
00:00:31.269 --> 00:00:34.490
Let X represent the store's net gain
00:00:34.490 --> 00:00:36.580
from one of these plans.
00:00:36.580 --> 00:00:39.680
Calculate the expected net gain.
00:00:39.680 --> 00:00:41.850
So pause this video, see if
you can have a go at that
00:00:41.850 --> 00:00:43.700
before we work through this together.
00:00:44.860 --> 00:00:46.780
So we have the two scenarios here.
00:00:46.780 --> 00:00:49.060
The first scenario is
that the store does need
00:00:49.060 --> 00:00:51.230
to replace the TV
because something happens
00:00:51.230 --> 00:00:53.660
and so it's gonna cost
$1,200 to the store.
00:00:53.660 --> 00:00:56.300
But remember they got $80
for the protection plan.
00:00:56.300 --> 00:00:59.900
So you have a net gain of negative $1,120
00:00:59.900 --> 00:01:01.520
from the store's perspective.
00:01:01.520 --> 00:01:02.540
There's the other scenario,
00:01:02.540 --> 00:01:03.960
which is more favorable for the store,
00:01:03.960 --> 00:01:07.330
which is a customer does
not need a replacement TV,
00:01:07.330 --> 00:01:09.360
so that has no cost and so their net gain
00:01:09.360 --> 00:01:11.520
is just the $80 for the plan.
00:01:11.520 --> 00:01:13.370
So to figure out the expected net gain,
00:01:13.370 --> 00:01:14.750
we just have to figure
out the probabilities
00:01:14.750 --> 00:01:17.400
of each of these and take
the weighted average of them.
00:01:17.400 --> 00:01:19.050
So what's the probability
that they will have
00:01:19.050 --> 00:01:20.640
to replace the TV?
00:01:20.640 --> 00:01:22.930
Well, we know 2% of
customers who buy this plan
00:01:22.930 --> 00:01:24.640
end up needing a replacement.
00:01:24.640 --> 00:01:26.840
So we could say this is two over 100
00:01:26.840 --> 00:01:29.300
or maybe I'll write it as 0.02.
00:01:29.300 --> 00:01:32.170
This is the probability of X.
00:01:32.170 --> 00:01:36.570
And then the probability of not
needing a replacement, 0.98.
00:01:36.570 --> 00:01:40.040
And so our expected net gain
00:01:40.040 --> 00:01:43.110
is going to be equal to the probability
00:01:43.110 --> 00:01:46.840
of needing replacement times
the net gain of a replacement.
00:01:46.840 --> 00:01:50.687
So it's going to be times -$1,120.
00:01:53.720 --> 00:01:56.150
And then we're gonna
have plus the probability
00:01:56.150 --> 00:01:58.980
of not needing replacement, which is 0.98
00:02:00.380 --> 00:02:01.870
times the net gain there.
00:02:01.870 --> 00:02:04.333
So that is $80.
00:02:05.690 --> 00:02:10.140
So we have 0.02x-1,120 is equal to that.
00:02:13.890 --> 00:02:15.850
And to that, we're gonna add,
00:02:15.850 --> 00:02:19.397
I'll open parentheses,
0.98x80, close parentheses,
00:02:23.170 --> 00:02:27.980
is going to be equal to $56.
00:02:27.980 --> 00:02:30.910
So this is equal to $56.
00:02:30.910 --> 00:02:33.410
And now you understand why the stores
00:02:33.410 --> 00:02:35.533
like to sell these replacement plans.
|
Expected payoff example: lottery ticket | https://www.youtube.com/watch?v=Ay1bVzqTKzg | vtt | https://www.youtube.com/api/timedtext?v=Ay1bVzqTKzg&ei=5VWUZe31KuOip-oP1PWsiA4&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=7654965341D18CE7F159559D8D8F7DC0CF5F63E9.D8DB599A363EE2AD730A079955C37FE2507607EC&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.200 --> 00:00:01.870
- [Instructor] We're told
a Pick 4 lottery game
00:00:01.870 --> 00:00:05.120
involves drawing four numbered
balls from separate bins,
00:00:05.120 --> 00:00:08.530
each containing balls labeled from 0 to 9.
00:00:08.530 --> 00:00:11.500
So there are 10,000 possible
selections in total.
00:00:11.500 --> 00:00:12.333
For example, you could get
00:00:12.333 --> 00:00:14.530
a 0, a 0, a 0 and a 0,
00:00:14.530 --> 00:00:16.670
a 0, a 0, a 0 and a 1,
00:00:16.670 --> 00:00:21.080
all the way up to 9,999, four nines.
00:00:21.080 --> 00:00:23.890
Players can choose to play a
straight bet, where the player
00:00:23.890 --> 00:00:27.470
wins if they match all four
digits in the correct order.
00:00:27.470 --> 00:00:32.470
The lottery pays $4,500 on a
successful $1 straight bet.
00:00:33.520 --> 00:00:38.520
Let X represent a player's
net gain on a $1 straight bet.
00:00:39.580 --> 00:00:42.860
Calculate the expected net gain.
00:00:42.860 --> 00:00:46.310
And they say, hint, the expected
net gain can be negative.
00:00:46.310 --> 00:00:47.610
So why don't you pause this video
00:00:47.610 --> 00:00:50.363
and see if you can calculate
the expected net gain?
00:00:51.780 --> 00:00:52.613
All right.
00:00:52.613 --> 00:00:54.570
So there's a couple of ways
that we can approach this.
00:00:54.570 --> 00:00:57.940
One way is to just think about
the two different outcomes.
00:00:57.940 --> 00:01:01.430
There's a scenario where you
win with your straight bet.
00:01:01.430 --> 00:01:04.420
There's a scenario where you
lose with your straight bet.
00:01:04.420 --> 00:01:05.253
Now let's think about
00:01:05.253 --> 00:01:09.090
the net gain in either
one of those scenarios.
00:01:09.090 --> 00:01:12.420
The scenario where you win, you pay $1,
00:01:12.420 --> 00:01:16.950
we know it's a $1 straight
bet, and you get $4,500.
00:01:16.950 --> 00:01:18.750
So what's the net gain?
00:01:18.750 --> 00:01:22.160
So it's going to be $4,500 minus one.
00:01:22.160 --> 00:01:24.887
So your net gain is going to be $4,499.
00:01:29.040 --> 00:01:32.020
Now what about the net gain in
the situation that you lose?
00:01:32.020 --> 00:01:33.880
Well, in the situation that you lose,
00:01:33.880 --> 00:01:35.280
you just lose a dollar.
00:01:35.280 --> 00:01:40.280
So this is just going to be
negative $1 right over here.
00:01:40.860 --> 00:01:41.693
Now let's think about
00:01:41.693 --> 00:01:44.230
the probabilities of
each of these situations.
00:01:44.230 --> 00:01:47.550
So the probability, so
the probability of a win
00:01:47.550 --> 00:01:49.770
we know is 1 in 10,000,
00:01:49.770 --> 00:01:52.800
1 in 10,000.
00:01:52.800 --> 00:01:55.010
And what's the probability of a loss?
00:01:55.010 --> 00:01:58.540
Well, that's going to be 9,999
00:01:58.540 --> 00:02:00.990
out of 10,000.
00:02:00.990 --> 00:02:02.984
And then our expected net gain is just
00:02:02.984 --> 00:02:05.320
going to be the weighted
average of these two.
00:02:05.320 --> 00:02:08.960
So I could write our expected net gain
00:02:08.960 --> 00:02:12.940
is going to be 4,499
00:02:12.940 --> 00:02:15.780
times the probability of that, 1 in 10,000
00:02:16.810 --> 00:02:19.030
plus negative 1 times this,
00:02:19.030 --> 00:02:20.020
so that I could just write that
00:02:20.020 --> 00:02:25.020
as minus 9,999 over 10,000.
00:02:26.250 --> 00:02:28.730
And so this is going to
be equal to, let's see,
00:02:28.730 --> 00:02:30.470
it's going to be 4,499
00:02:31.730 --> 00:02:35.120
minus 9,999,
00:02:35.120 --> 00:02:38.970
all of that over 10,000.
00:02:38.970 --> 00:02:43.380
And let's see, this is
going to be equal to
00:02:43.380 --> 00:02:45.943
negative 5,500 over 10,000,
00:02:47.028 --> 00:02:50.607
negative 5,500 over 10,000,
00:02:51.570 --> 00:02:55.410
which is the same thing
as negative 55 over 100,
00:02:55.410 --> 00:02:56.880
or I could write it this way.
00:02:56.880 --> 00:03:00.150
This is equal to negative .55.
00:03:00.150 --> 00:03:03.780
I could write it this way, 0.55.
00:03:03.780 --> 00:03:07.010
So that's one way to calculate
the expected net gain.
00:03:07.010 --> 00:03:09.070
Another way to approach
it is to say, all right,
00:03:09.070 --> 00:03:11.280
what if we were to get 10,000 tickets?
00:03:11.280 --> 00:03:15.280
What is our expected net
gain on the 10,000 tickets?
00:03:15.280 --> 00:03:19.460
Well, we would pay $10,000
00:03:21.120 --> 00:03:22.970
and we would expect to win once.
00:03:22.970 --> 00:03:25.830
It's not a guarantee, but
we would expect to win once.
00:03:25.830 --> 00:03:27.150
So expect
00:03:29.250 --> 00:03:32.570
4,500 in payout.
00:03:32.570 --> 00:03:36.600
And so you would then, let's
see, you would have a net gain
00:03:37.840 --> 00:03:41.860
of, it would be negative $5,500,
00:03:41.860 --> 00:03:45.240
negative $5,500.
00:03:45.240 --> 00:03:48.910
Now this is the net gain
when you do 10,000 tickets.
00:03:48.910 --> 00:03:52.130
Now, if you wanted to find the
expected net gain per ticket
00:03:52.130 --> 00:03:53.890
you would then just divide by 10,000.
00:03:53.890 --> 00:03:54.780
And if you did that,
00:03:54.780 --> 00:03:58.760
you would get exactly what we
just calculated the other way.
00:03:58.760 --> 00:04:00.950
So any way you try to approach this
00:04:00.950 --> 00:04:02.693
this is not a great bet.
|
Interpreting expected value | https://www.youtube.com/watch?v=SNIW7MmCdhA | vtt | https://www.youtube.com/api/timedtext?v=SNIW7MmCdhA&ei=5VWUZey-ItbUxN8P_tq54AY&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=C69322E1C4E1C02FBDC85F26D31867E4D2053226.25811F4F9863015D102430F52C499749ABA4DBD2&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.400 --> 00:00:03.380
- [Instructor] We're told a
certain lottery ticket costs $2
00:00:03.380 --> 00:00:05.057
and the back of the ticket says,
00:00:05.057 --> 00:00:08.020
"The overall odds of winning
a prize with this ticket
00:00:08.020 --> 00:00:09.500
are one to 50,
00:00:09.500 --> 00:00:13.530
and the expected return
for this ticket is $0.95."
00:00:13.530 --> 00:00:16.650
Which interpretations of the
expected value are correct?
00:00:16.650 --> 00:00:19.300
Choose all answers that apply.
00:00:19.300 --> 00:00:21.570
Pause this video, have a go at that.
00:00:21.570 --> 00:00:24.370
All right, now let's go
through each of these choices.
00:00:24.370 --> 00:00:26.160
So choice A says the probability
00:00:26.160 --> 00:00:31.160
that one of these tickets wins
a prize is 0.95 on average.
00:00:32.870 --> 00:00:34.940
Well, I see where they're
getting that 0.95.
00:00:34.940 --> 00:00:36.490
They're getting it from right over here,
00:00:36.490 --> 00:00:38.460
but that's not the probability
that you're winning,
00:00:38.460 --> 00:00:40.400
that's the expected return.
00:00:40.400 --> 00:00:42.830
The probability that
you win is much lower.
00:00:42.830 --> 00:00:44.750
If the odds are one to 50,
00:00:44.750 --> 00:00:49.340
that means that the probability
of winning is one to 51.
00:00:49.340 --> 00:00:52.490
So it's a much lower probability
than this right over here.
00:00:52.490 --> 00:00:54.530
So definitely rule that out.
00:00:54.530 --> 00:00:58.443
Someone who buys this ticket
is most likely to win $0.95.
00:01:00.390 --> 00:01:03.890
That is not necessarily the case either.
00:01:03.890 --> 00:01:08.660
We don't know what the different
outcomes are for the prize.
00:01:08.660 --> 00:01:10.760
It's very likely that there's no outcome
00:01:10.760 --> 00:01:13.420
for that prize where
you win exactly $0.95.
00:01:13.420 --> 00:01:16.610
Instead, there's likely to be
outcomes that are much larger
00:01:16.610 --> 00:01:18.550
than that with very low probabilities,
00:01:18.550 --> 00:01:20.440
and then when you take
the weighted average
00:01:20.440 --> 00:01:22.310
of all of the outcomes,
00:01:22.310 --> 00:01:25.690
then you get an expected return of $0.95.
00:01:25.690 --> 00:01:29.490
So it's actually maybe even
impossible to win exactly $0.95.
00:01:29.490 --> 00:01:31.410
So I would rule that out.
00:01:31.410 --> 00:01:33.080
If we looked at many of these tickets,
00:01:33.080 --> 00:01:37.523
the average return would
be about $0.95 per ticket.
00:01:38.370 --> 00:01:40.260
That one feels pretty interesting,
00:01:40.260 --> 00:01:42.460
'cause we're looking at
many of these tickets.
00:01:42.460 --> 00:01:46.720
And so across many of them, you
would expect to, on average,
00:01:46.720 --> 00:01:49.430
get the expected return as your return.
00:01:49.430 --> 00:01:51.720
And so this is what we are seeing here.
00:01:51.720 --> 00:01:53.370
The average return would be about that.
00:01:53.370 --> 00:01:54.600
It would be approximately that.
00:01:54.600 --> 00:01:56.140
So I like that choice.
00:01:56.140 --> 00:01:58.980
That is a good interpretation
of expected value.
00:01:58.980 --> 00:02:00.070
And then choice D,
00:02:00.070 --> 00:02:03.000
if 1,000 people each bought
one of these tickets,
00:02:03.000 --> 00:02:08.000
they'd expect a net gain
of about $950 in total.
00:02:09.100 --> 00:02:10.810
This one is tempting.
00:02:10.810 --> 00:02:14.540
Instead of net gain,
if it just said return,
00:02:14.540 --> 00:02:15.710
this would make a lot of sense.
00:02:15.710 --> 00:02:18.540
In fact, it would be completely
consistent with choice C.
00:02:18.540 --> 00:02:21.250
If you have 1,000 people,
that would be many tickets,
00:02:21.250 --> 00:02:23.500
and if on average, if their average return
00:02:23.500 --> 00:02:25.560
is about $0.95 per ticket,
00:02:25.560 --> 00:02:29.210
then their total return
would be about $950,
00:02:29.210 --> 00:02:32.550
but they didn't write return
here, they wrote net gain.
00:02:32.550 --> 00:02:36.640
Net gain would be how much you
get minus how much you paid.
00:02:36.640 --> 00:02:38.320
And 1,000 people would have to pay,
00:02:38.320 --> 00:02:41.530
if they each got a
ticket, would pay $2,000.
00:02:41.530 --> 00:02:43.210
So they would pay 2,000.
00:02:43.210 --> 00:02:46.590
They would expect a return of $950.
00:02:46.590 --> 00:02:50.690
Their net gain would
actually be negative $1,050.
00:02:50.690 --> 00:02:53.113
So we would rule that one out as well.
|
Probability distributions from empirical data | https://www.youtube.com/watch?v=wztjEa7893c | vtt | https://www.youtube.com/api/timedtext?v=wztjEa7893c&ei=5VWUZafEI9bAhcIPuuG72AI&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=E9F9BC002B98F5042F0B6103327E1D6A524DE96E.BD68CB7E14DDB663F65B23F9B9F72F080258E0B8&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.270 --> 00:00:02.140
- [Instructor] We're told
that Jada owns a restaurant
00:00:02.140 --> 00:00:05.200
where customers can make
their orders using an app.
00:00:05.200 --> 00:00:07.130
She decides to offer a discount
00:00:07.130 --> 00:00:09.610
on appetizers to attract more customers.
00:00:09.610 --> 00:00:12.130
And she's curious about the probability
00:00:12.130 --> 00:00:16.690
that a customer orders a
large number of appetizers.
00:00:16.690 --> 00:00:19.070
Jada tracked how many appetizers
00:00:19.070 --> 00:00:22.950
were in each of the past 500 orders.
00:00:22.950 --> 00:00:24.810
All right, so the number of appetizers,
00:00:24.810 --> 00:00:27.760
so 40 out of the 500
ordered zero appetizers,
00:00:27.760 --> 00:00:32.030
and for example, 120 out of the
500 ordered three appetizers
00:00:32.030 --> 00:00:33.600
and so on and so forth.
00:00:33.600 --> 00:00:37.990
Let X represent the number of
appetizers in a random order.
00:00:37.990 --> 00:00:40.560
Based on these results,
construct an approximate
00:00:40.560 --> 00:00:43.230
probability distribution of X.
00:00:43.230 --> 00:00:45.530
Pause this video and see if
you can have a go at this
00:00:45.530 --> 00:00:47.093
before we do this together.
00:00:48.030 --> 00:00:51.640
All right, so they're
telling us an approximate
00:00:51.640 --> 00:00:54.700
probability distribution,
because we don't know
00:00:54.700 --> 00:00:56.560
the actual probability.
00:00:56.560 --> 00:00:58.180
We can't get into people's minds
00:00:58.180 --> 00:01:00.530
and figure out the probability
that the neurons fire
00:01:00.530 --> 00:01:03.840
in exactly the right
way to order appetizers.
00:01:03.840 --> 00:01:06.880
But what we can do is
look at past results,
00:01:06.880 --> 00:01:09.260
empirical data right over here
00:01:09.260 --> 00:01:11.860
to approximate the distribution.
00:01:11.860 --> 00:01:14.810
So what we can do is look at the last 500,
00:01:14.810 --> 00:01:16.390
and for each of the outcomes
00:01:16.390 --> 00:01:19.710
think about what fraction of
the last 500 had that outcome.
00:01:19.710 --> 00:01:21.910
And that will be our approximation.
00:01:21.910 --> 00:01:24.610
And so the outcomes here, we
could have zero appetizers,
00:01:24.610 --> 00:01:29.610
one, two, three, four, five, or six.
00:01:29.680 --> 00:01:32.356
Now the approximate probability
00:01:32.356 --> 00:01:36.280
of zero appetizers is
going to be 40 over 500,
00:01:36.280 --> 00:01:40.140
which is the same thing as four over 50,
00:01:40.140 --> 00:01:44.160
which is the same thing as two over 25.
00:01:44.160 --> 00:01:47.410
So I'll write two 25th right over there.
00:01:47.410 --> 00:01:49.997
The probability of one appetizer,
00:01:49.997 --> 00:01:52.090
well, that's going to be 90, the over 500,
00:01:52.090 --> 00:01:55.390
which is the same thing as nine over 50.
00:01:55.390 --> 00:01:58.450
And I think that's
already in lowest terms.
00:01:58.450 --> 00:02:03.450
Then 160 over 500 is the
same thing as 16 over 50,
00:02:05.580 --> 00:02:08.773
which is the same thing as eight over 25.
00:02:10.546 --> 00:02:11.700
And we just keep going.
00:02:11.700 --> 00:02:16.700
120 out of 500 is the same
thing as 12 out of 50,
00:02:17.000 --> 00:02:19.263
or six out of 25.
00:02:20.444 --> 00:02:25.444
Six out of 25, and then 50 out of 500.
00:02:25.750 --> 00:02:27.510
Well, that's one out of every 10.
00:02:27.510 --> 00:02:29.900
So I'll just write it like that.
00:02:29.900 --> 00:02:34.900
30 out of 500 is the same
thing as three out of 50.
00:02:36.120 --> 00:02:38.370
I'll just write it like that.
00:02:38.370 --> 00:02:40.950
And that last but not least, 10 out of 500
00:02:40.950 --> 00:02:43.303
is the same thing as one in 50.
00:02:44.150 --> 00:02:45.330
And we're done.
00:02:45.330 --> 00:02:47.420
We have just constructed an approximate
00:02:47.420 --> 00:02:50.853
probability distribution
for our random variable X.
|
Theoretical probability distribution example: multiplication | https://www.youtube.com/watch?v=2jExPaoTrQE | vtt | https://www.youtube.com/api/timedtext?v=2jExPaoTrQE&ei=5VWUZfD2I9SAp-oPxpKHqAE&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=CA3AB67E27B98B1D63F13B13EEF354E406A2C754.2EF90C0A44B6AB36C734AF59AF4A7759114E113D&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.290 --> 00:00:02.180
- [Instructor] We're told
that Kai goes to a restaurant
00:00:02.180 --> 00:00:04.417
that advertises a promotion saying,
00:00:04.417 --> 00:00:07.910
"1 in 5 customers get a free dessert!"
00:00:07.910 --> 00:00:12.050
Suppose Kai goes to the
restaurant twice in a given week,
00:00:12.050 --> 00:00:15.330
and each time he has a 1/5 probability
00:00:15.330 --> 00:00:17.520
of getting a free dessert.
00:00:17.520 --> 00:00:21.400
Let X represent the
number of free desserts
00:00:21.400 --> 00:00:23.980
Kai gets in his two trips.
00:00:23.980 --> 00:00:28.560
Construct the theoretical
probability distribution of X.
00:00:28.560 --> 00:00:30.220
All right, so pause this video
00:00:30.220 --> 00:00:31.670
and see if you can work through this
00:00:31.670 --> 00:00:33.333
before we do it together.
00:00:34.260 --> 00:00:36.380
All right, so first let's just think about
00:00:36.380 --> 00:00:38.930
the possible values that X could take on.
00:00:38.930 --> 00:00:40.950
This is the number of
free desserts he gets,
00:00:40.950 --> 00:00:42.630
and he visits twice.
00:00:42.630 --> 00:00:44.760
So there's some world in which
00:00:44.760 --> 00:00:46.610
he doesn't get any free desserts.
00:00:46.610 --> 00:00:50.090
So that's 0 in his two visits.
00:00:50.090 --> 00:00:51.340
Maybe on one of the visits,
00:00:51.340 --> 00:00:53.410
he gets a dessert and
the other one he doesn't,
00:00:53.410 --> 00:00:55.170
and maybe in both of his visits
00:00:55.170 --> 00:00:57.420
he actually is able to get a free dessert.
00:00:57.420 --> 00:00:58.810
So he's going to have someplace
00:00:58.810 --> 00:01:02.310
from 0 to 2 free desserts in a given week.
00:01:02.310 --> 00:01:03.143
So we just have to figure out
00:01:03.143 --> 00:01:05.420
the probability of each of these.
00:01:05.420 --> 00:01:08.630
So let's first of all think
about the probability,
00:01:08.630 --> 00:01:10.010
let me write it over here,
00:01:10.010 --> 00:01:13.710
the probability that
capital X is equal to 0
00:01:13.710 --> 00:01:15.600
is going to be equal to what?
00:01:15.600 --> 00:01:16.960
Well, that's going to be the probability
00:01:16.960 --> 00:01:20.200
that he doesn't get a
dessert on both days.
00:01:20.200 --> 00:01:21.460
And it's important to realize
00:01:21.460 --> 00:01:23.110
that these are independent events.
00:01:23.110 --> 00:01:24.387
It's not like the restaurant's gonna say,
00:01:24.387 --> 00:01:26.080
"Oh, if you didn't get
a dessert on one day,
00:01:26.080 --> 00:01:27.530
you're more likely to get
another the other day,"
00:01:27.530 --> 00:01:29.850
or, "Somehow if you got
it on a previous day,
00:01:29.850 --> 00:01:31.700
you're less likely than another day."
00:01:31.700 --> 00:01:33.610
That they are independent events.
00:01:33.610 --> 00:01:36.730
So the probability of not
getting it on any one day
00:01:36.730 --> 00:01:39.540
is four out of five,
00:01:39.540 --> 00:01:42.600
and the probability of not
getting it on two of the days,
00:01:42.600 --> 00:01:43.640
I would just multiply them
00:01:43.640 --> 00:01:45.810
because they are independent events.
00:01:45.810 --> 00:01:49.400
So four over five times four over five.
00:01:49.400 --> 00:01:52.210
So the probability that X is equal to 0
00:01:52.210 --> 00:01:57.210
is going to be 16/25, 16 over 25.
00:01:57.490 --> 00:02:02.490
Now what about the probability
that X is equal to 1?
00:02:03.090 --> 00:02:05.040
What is this going to be?
00:02:05.040 --> 00:02:08.290
Well, there are two scenarios over here.
00:02:08.290 --> 00:02:12.670
There's one scenario
where let's say on day one
00:02:12.670 --> 00:02:14.370
he does not get the dessert,
00:02:14.370 --> 00:02:17.940
and on day two he does get the dessert.
00:02:17.940 --> 00:02:20.490
But then of course
there's the other scenario
00:02:20.490 --> 00:02:23.430
where on day one he gets the dessert,
00:02:23.430 --> 00:02:28.070
and then on day two he
doesn't get the dessert.
00:02:28.070 --> 00:02:29.670
These are the two scenarios
00:02:29.670 --> 00:02:31.770
where he's going to get X equals 1.
00:02:31.770 --> 00:02:34.280
And so if we add these
together, let's see.
00:02:34.280 --> 00:02:39.095
4/5 times 1/5, this is going to be 4/25,
00:02:39.095 --> 00:02:43.200
and then this is going to be 4/25 again.
00:02:43.200 --> 00:02:45.070
And you add these two together,
00:02:45.070 --> 00:02:48.890
you're going to get 8/25.
00:02:48.890 --> 00:02:50.050
And then last but not least,
00:02:50.050 --> 00:02:51.670
and actually we could
figure out this last one
00:02:51.670 --> 00:02:55.270
by subtracting 16 and 8 from 25,
00:02:55.270 --> 00:02:57.180
which would actually give us 1/25th,
00:02:57.180 --> 00:02:58.450
but let's just write this out.
00:02:58.450 --> 00:03:01.480
The probability that X equals 2,
00:03:01.480 --> 00:03:03.710
this is the probability that
he gets a dessert on both days.
00:03:03.710 --> 00:03:06.790
So 1/5 chance on day one
00:03:06.790 --> 00:03:09.080
and 1/5 chance on the second day.
00:03:09.080 --> 00:03:12.730
So 1/5 times 1/5 is 1/25.
00:03:12.730 --> 00:03:14.380
And you can do a reality check here.
00:03:14.380 --> 00:03:16.090
These all need to add up to one.
00:03:16.090 --> 00:03:17.830
And they do indeed add up to one.
00:03:17.830 --> 00:03:20.396
16 plus 8 plus 1 is 25.
00:03:20.396 --> 00:03:22.940
So 25/25 is what they all add up to.
00:03:22.940 --> 00:03:23.773
And we're done.
|
Theoretical probability distribution example: tables | https://www.youtube.com/watch?v=hA8VmhkKEJo | vtt | https://www.youtube.com/api/timedtext?v=hA8VmhkKEJo&ei=5VWUZfu2K4COp-oP-PebwAY&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=9D00BCBA06105636862D87BD5C8573FB996AD348.E74557E60B973C131C650F6AC31C1FE8B2CBBD0A&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.360 --> 00:00:01.560
- [Instructor] We're
told that a board game
00:00:01.560 --> 00:00:05.450
has players roll two
3-sided dice, these exist
00:00:05.450 --> 00:00:07.030
and actually I looked it up, they do exist
00:00:07.030 --> 00:00:08.280
and they're actually fascinating.
00:00:08.280 --> 00:00:12.120
And subtract the numbers
showing on the faces.
00:00:12.120 --> 00:00:16.290
The game only looks at
non-negative differences.
00:00:16.290 --> 00:00:20.490
For example, if a player
rolls a one and a three,
00:00:20.490 --> 00:00:22.660
the difference is two.
00:00:22.660 --> 00:00:26.690
Let D represent the
difference in a given roll.
00:00:26.690 --> 00:00:30.760
Construct the theoretical
probability distribution of D.
00:00:30.760 --> 00:00:32.840
So pause this video and see
if you can have a go at that
00:00:32.840 --> 00:00:35.410
before we work through it together.
00:00:35.410 --> 00:00:38.520
All right, now let's
work through it together.
00:00:38.520 --> 00:00:40.630
So let's just think about
all of the scenarios
00:00:40.630 --> 00:00:42.370
for the two die.
00:00:42.370 --> 00:00:44.560
So let me draw a little table here.
00:00:44.560 --> 00:00:46.220
So let me do it like that
00:00:46.220 --> 00:00:49.250
and let me do it like this.
00:00:49.250 --> 00:00:52.870
And then let me put a little
divider right over here.
00:00:52.870 --> 00:00:56.790
And for this top, this
is going to be die one
00:00:56.790 --> 00:00:59.010
and then this is going to be die two.
00:00:59.010 --> 00:01:03.660
Die one can take on one, two, or three
00:01:03.660 --> 00:01:08.250
and die two could be one, two, or three.
00:01:08.250 --> 00:01:12.103
And so let me finish making
this a bit of a table here.
00:01:13.850 --> 00:01:16.180
And what we wanna do is
look at the difference
00:01:16.180 --> 00:01:17.890
but the non-negative difference.
00:01:17.890 --> 00:01:21.480
So we'll always subtract the
lower die from the higher die.
00:01:21.480 --> 00:01:22.870
So what's the difference here?
00:01:22.870 --> 00:01:24.460
Well, this is going to be zero.
00:01:24.460 --> 00:01:26.590
If I roll a one and a one.
00:01:26.590 --> 00:01:28.420
Now, what if I roll a two and a one?
00:01:28.420 --> 00:01:30.990
Well, here the difference is
going to be two minus one,
00:01:30.990 --> 00:01:32.040
which is one.
00:01:32.040 --> 00:01:35.630
Here the difference is three
minus one, which is two.
00:01:35.630 --> 00:01:37.450
Now what about right over here?
00:01:37.450 --> 00:01:41.370
Well, here the higher die
is two the lower one is one,
00:01:41.370 --> 00:01:42.230
right over here.
00:01:42.230 --> 00:01:45.600
So two minus one is one,
00:01:45.600 --> 00:01:47.900
two minus two is zero.
00:01:47.900 --> 00:01:50.240
And now this is gonna be the higher roll,
00:01:50.240 --> 00:01:52.670
die one is gonna have the
high roll in this scenario.
00:01:52.670 --> 00:01:54.570
Three minus two is one.
00:01:54.570 --> 00:01:59.080
And then right over here,
three minus one is two.
00:01:59.080 --> 00:02:00.960
Now die one rolls a two,
00:02:00.960 --> 00:02:03.090
die two rolls a three.
00:02:03.090 --> 00:02:05.960
Die three is higher,
three minus two is one.
00:02:05.960 --> 00:02:08.350
And then three minus three is zero.
00:02:08.350 --> 00:02:10.470
So we've come up with all of the scenarios
00:02:10.470 --> 00:02:13.440
and we can see that we're
either gonna end up with a zero
00:02:13.440 --> 00:02:16.900
or one or a two when we look
at the positive difference.
00:02:16.900 --> 00:02:21.900
So there's a scenario of
getting a zero, a one or a two.
00:02:22.330 --> 00:02:24.570
Those are the different differences
00:02:24.570 --> 00:02:26.140
that we could actually get.
00:02:26.140 --> 00:02:28.780
And so let's think about the
probability of each of them.
00:02:28.780 --> 00:02:31.780
What's the probability that
the difference is zero.
00:02:31.780 --> 00:02:36.010
Well, we can see that one, two, three
00:02:36.010 --> 00:02:38.940
of the nine equally likely outcomes,
00:02:38.940 --> 00:02:40.580
result in a difference of zero.
00:02:40.580 --> 00:02:44.670
So it's gonna be three
out of nine or one-third.
00:02:44.670 --> 00:02:49.670
What about a difference of,
let me use the blue, one?
00:02:49.900 --> 00:02:54.300
Well, we could see there
are one, two, three, four
00:02:54.300 --> 00:02:56.450
of the nine scenarios have that.
00:02:56.450 --> 00:02:59.000
So there is a four ninths probability.
00:02:59.000 --> 00:03:02.070
And then last but not
least a difference of two.
00:03:02.070 --> 00:03:05.470
Well, there's two out of the
nine scenarios that have that.
00:03:05.470 --> 00:03:09.408
So there is a two ninths
probability right over there.
00:03:09.408 --> 00:03:10.390
And we're done.
00:03:10.390 --> 00:03:13.090
We've constructed the theoretical
probability distribution
00:03:13.090 --> 00:03:13.953
of D.
|
Interpreting general multiplication rule | https://www.youtube.com/watch?v=yTJawPRzCzI | vtt | https://www.youtube.com/api/timedtext?v=yTJawPRzCzI&ei=5VWUZZiFJPuJp-oPmPWP-A0&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=247827DB31AA70BA45C1A2514FCDCA3C6E0E8075.D29868C2F69F6097F43FF5238BA6C22A37F8871C&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.230 --> 00:00:01.610
- [Instructor] We're
told that two contestants
00:00:01.610 --> 00:00:03.990
are finalists in a cooking competition.
00:00:03.990 --> 00:00:06.530
For the final round,
each of them spin a wheel
00:00:06.530 --> 00:00:09.950
to determine what star
ingredient must be in their dish.
00:00:09.950 --> 00:00:11.420
I guess the primary ingredient,
00:00:11.420 --> 00:00:12.820
and we can see it could be chard, spinach,
00:00:12.820 --> 00:00:16.720
romaine lettuce, I'm guessing,
cabbage, arugula, or kale.
00:00:16.720 --> 00:00:19.510
And so then they give us these
different types of events,
00:00:19.510 --> 00:00:21.860
or at least the symbols for
these different types of events,
00:00:21.860 --> 00:00:23.040
and then give us their meaning.
00:00:23.040 --> 00:00:27.800
So K-sub 1 means, the first
contestant lands on kale,
00:00:27.800 --> 00:00:32.800
K-sub 2 means, the second
contestant lands on kale,
00:00:32.800 --> 00:00:36.030
K-sub 1 with this superscript C,
00:00:36.030 --> 00:00:37.730
which you could view as complement.
00:00:37.730 --> 00:00:39.480
So K-sub 1 one complement,
00:00:39.480 --> 00:00:44.350
the first contestant
does not land on kale.
00:00:44.350 --> 00:00:46.970
So it's the complement of
this one right over here.
00:00:46.970 --> 00:00:49.010
And then K-sub 2 complement,
00:00:49.010 --> 00:00:52.670
would be that the second
contestant does not land on kale.
00:00:52.670 --> 00:00:56.440
So the not of K-sub 2 right over here.
00:00:56.440 --> 00:00:59.570
Using the general multiplication rule,
00:00:59.570 --> 00:01:02.530
express symbolically the probability
00:01:02.530 --> 00:01:06.700
that neither contestant lands on kale.
00:01:06.700 --> 00:01:09.550
So pause this video and see
if you can have a go at this.
00:01:10.480 --> 00:01:14.760
All right, so the general
multiplication rule
00:01:14.760 --> 00:01:16.610
is just saying this notion
00:01:16.610 --> 00:01:21.610
that the probability
of two events, A and B,
00:01:22.810 --> 00:01:26.740
is going to be equal
to the probability of,
00:01:26.740 --> 00:01:31.740
let's say A given B, times
the probability of B.
00:01:33.020 --> 00:01:34.820
Now, if they're independent events,
00:01:34.820 --> 00:01:36.740
if the probability of A occurring
00:01:36.740 --> 00:01:40.930
does not depend in any way
on whether B occurred or not,
00:01:40.930 --> 00:01:45.160
then this would simplify to
this probability of A given B,
00:01:45.160 --> 00:01:47.100
would just become the probability of A.
00:01:47.100 --> 00:01:48.850
And so if you have two independent events,
00:01:48.850 --> 00:01:50.570
you would just multiply their probability.
00:01:50.570 --> 00:01:51.940
So that's just all they're talking about,
00:01:51.940 --> 00:01:53.870
the general multiplication rule.
00:01:53.870 --> 00:01:54.860
But let me express
00:01:54.860 --> 00:01:57.270
what they're actually
asking us to express.
00:01:57.270 --> 00:02:01.770
The probability that neither
contestant lands on kale.
00:02:01.770 --> 00:02:03.790
So that means that this
is going to happen,
00:02:03.790 --> 00:02:06.360
the first contestant
does not land on kale,
00:02:06.360 --> 00:02:07.800
and this is going to happen,
00:02:07.800 --> 00:02:10.990
the second contestant
does not land on kale.
00:02:10.990 --> 00:02:12.630
So I could write it this way.
00:02:12.630 --> 00:02:17.320
The probability that K-sub 1 complement
00:02:17.320 --> 00:02:22.320
and K-sub 2 complement, and
I could write it this way.
00:02:24.470 --> 00:02:25.960
This is going to be equal to,
00:02:25.960 --> 00:02:28.650
we know that these are independent events
00:02:28.650 --> 00:02:31.530
because if the first contestant gets kale
00:02:31.530 --> 00:02:32.740
or whatever they get it,
00:02:32.740 --> 00:02:34.600
it doesn't get taken out of the running
00:02:34.600 --> 00:02:35.730
for the second contestant.
00:02:35.730 --> 00:02:38.410
The second contestant still
has an equal probability
00:02:38.410 --> 00:02:40.080
of getting or not getting kale,
00:02:40.080 --> 00:02:42.780
regardless of what happened
for the first contestant.
00:02:42.780 --> 00:02:44.290
So that means we're just in the situation
00:02:44.290 --> 00:02:45.930
where we multiply these probabilities.
00:02:45.930 --> 00:02:50.930
So that's gonna be the
probability of K-sub 1 complement,
00:02:51.060 --> 00:02:56.060
times the probability
of K-sub 2 complement.
00:02:56.560 --> 00:02:58.570
All right, now let's do part two.
00:02:58.570 --> 00:03:00.380
Interpret what each part
00:03:00.380 --> 00:03:03.860
of this probability statement represents.
00:03:03.860 --> 00:03:05.010
So I encourage you like always,
00:03:05.010 --> 00:03:07.210
pause this video and
try to figure that out.
00:03:08.090 --> 00:03:11.950
All right, so first let's think
about what is going on here.
00:03:11.950 --> 00:03:13.340
So this is saying,
00:03:13.340 --> 00:03:18.340
the probability that this
is K-sub 1 complement.
00:03:19.130 --> 00:03:22.600
So the first contestant
does not land on kale.
00:03:22.600 --> 00:03:27.600
So first, first contestant
does not get kale,
00:03:33.790 --> 00:03:36.920
and, I'll write and in caps,
00:03:36.920 --> 00:03:39.600
and second contestant does get kale.
00:03:39.600 --> 00:03:44.130
And second does get kale.
00:03:45.490 --> 00:03:47.670
So that's what this left-hand is saying.
00:03:47.670 --> 00:03:51.190
And now they say that that
is going to be equal to,
00:03:51.190 --> 00:03:52.330
so this part right over here,
00:03:52.330 --> 00:03:57.330
probability that the first
contestant does not get kale.
00:03:58.270 --> 00:04:03.270
Probability that first does not get kale,
00:04:06.930 --> 00:04:10.440
times, right over here.
00:04:10.440 --> 00:04:12.450
And the second part right over here
00:04:12.450 --> 00:04:17.450
is the probability that the
second contestant gets kale,
00:04:18.600 --> 00:04:22.170
given that the first
contestant does not get kale.
00:04:22.170 --> 00:04:27.130
So probability that the second gets kale,
00:04:29.130 --> 00:04:32.920
given, that's what this vertical
line right over here means,
00:04:32.920 --> 00:04:35.110
it means given, shorthand for given.
00:04:35.110 --> 00:04:36.780
Given, I wrote it up there too.
00:04:36.780 --> 00:04:41.780
Given that first does not get kale.
00:04:46.350 --> 00:04:49.300
And we're done, we've just
explained what is going on here.
|
General multiplication rule example: independent events | https://www.youtube.com/watch?v=OqbkCYy37hI | vtt | https://www.youtube.com/api/timedtext?v=OqbkCYy37hI&ei=5VWUZbChHvahp-oPlPa_-Ac&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=A73E43CE5DA0AFFE7B486EB1CB9EA9489993AA51.E2C95CEC55D25E68A25093FF1A0FF875E83E4C2D&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.300 --> 00:00:01.310
- [Instructor] We're
told that Maya and Doug
00:00:01.310 --> 00:00:03.870
are finalists in a crafting competition.
00:00:03.870 --> 00:00:06.400
For the final round,
each of them spin a wheel
00:00:06.400 --> 00:00:10.510
to determine what star material
must be in their craft.
00:00:10.510 --> 00:00:14.640
Maya and Doug both want to get
silk as their star material.
00:00:14.640 --> 00:00:17.990
Maya will spin first, followed by Doug.
00:00:17.990 --> 00:00:22.410
What is the probability that
neither contestant gets silk?
00:00:22.410 --> 00:00:24.600
Pause this video and think
through this on your own
00:00:24.600 --> 00:00:26.450
before we work through this together.
00:00:27.630 --> 00:00:30.960
All right, so first let's think
about what they're asking.
00:00:30.960 --> 00:00:33.890
They want to figure out the
probability that neither
00:00:33.890 --> 00:00:35.970
gets silk, so I'm gonna
write this in shorthand.
00:00:35.970 --> 00:00:40.723
So I'm going to use MNS for Maya no silk.
00:00:41.610 --> 00:00:45.260
And we're also thinking about Doug
00:00:45.260 --> 00:00:47.990
not being able to pick silk.
00:00:47.990 --> 00:00:51.810
So Maya no silk and Doug no silk.
00:00:51.810 --> 00:00:54.200
So we know that this could be viewed
00:00:54.200 --> 00:00:59.200
as the probability that
Maya doesn't get silk.
00:00:59.420 --> 00:01:02.740
She, after all does get
to spin this wheel first,
00:01:02.740 --> 00:01:04.350
and then we can multiply that
00:01:04.350 --> 00:01:09.350
by the probability that
Doug doesn't get silk,
00:01:09.350 --> 00:01:13.860
Doug no silk, given that
Maya did not get silk.
00:01:13.860 --> 00:01:16.030
Maya no silk.
00:01:16.030 --> 00:01:19.390
Now it's important to think
about whether Doug's probability
00:01:19.390 --> 00:01:24.032
is independent or dependent on
whether Maya got silk or not.
00:01:24.032 --> 00:01:28.060
So let's remember Maya will
spin first, but it's not like
00:01:28.060 --> 00:01:30.430
if she picks silk, that somehow silk
00:01:30.430 --> 00:01:31.890
is taken out of the running.
00:01:31.890 --> 00:01:33.160
In fact, no matter what she picks,
00:01:33.160 --> 00:01:34.660
it's not taken out of the running.
00:01:34.660 --> 00:01:36.580
Doug will then spin it again.
00:01:36.580 --> 00:01:39.230
And so these are really
two independent events,
00:01:39.230 --> 00:01:42.090
and so the probability
that Doug doesn't get silk
00:01:42.090 --> 00:01:44.160
given that Maya doesn't get silk,
00:01:44.160 --> 00:01:45.400
this is going to be the same thing
00:01:45.400 --> 00:01:48.790
as the probability that
just Doug doesn't get silk.
00:01:48.790 --> 00:01:51.550
It doesn't matter what happens to Maya.
00:01:51.550 --> 00:01:53.930
And so what are each of these?
00:01:53.930 --> 00:01:55.300
Well, this is all going to be equal
00:01:55.300 --> 00:01:57.850
to the probability that
Maya does not get silk.
00:01:57.850 --> 00:02:00.630
There's six pieces or six options
00:02:00.630 --> 00:02:02.330
of this wheel right over here.
00:02:02.330 --> 00:02:06.730
Five of them entail her not
getting silk on her spin.
00:02:06.730 --> 00:02:09.080
So five over six.
00:02:09.080 --> 00:02:12.350
And then similarly, when
Doug goes to spin this wheel
00:02:12.350 --> 00:02:13.870
there are six possibilities.
00:02:13.870 --> 00:02:17.480
Five of them are showing
that he does not get silk,
00:02:17.480 --> 00:02:18.680
Doug no silk.
00:02:18.680 --> 00:02:23.480
So times 5/6, which is of
course going to be equal
00:02:23.480 --> 00:02:27.423
to 25/36, and we're done.
|
General multiplication rule example: dependent events | https://www.youtube.com/watch?v=iyQNk090FGM | vtt | https://www.youtube.com/api/timedtext?v=iyQNk090FGM&ei=5VWUZdjqKv6PmLAP8bqzqAQ&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=8939A89FCB9530A43547BE6E8789BA48B18A4707.27234CF6AD6C61A7DC7AAC0633AAE251A8F1158A&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.330 --> 00:00:02.390
- [Instructor] We're told that
Maya and Doug are finalists
00:00:02.390 --> 00:00:04.170
in a crafting competition.
00:00:04.170 --> 00:00:06.080
For the final round, each of them
00:00:06.080 --> 00:00:08.705
will randomly select a
card without replacement
00:00:08.705 --> 00:00:11.560
that will reveal what the star material
00:00:11.560 --> 00:00:13.460
must be in their craft.
00:00:13.460 --> 00:00:15.480
Here are the available cards.
00:00:15.480 --> 00:00:17.870
So I guess the star material
is the primary material
00:00:17.870 --> 00:00:20.540
they need to use in this competition.
00:00:20.540 --> 00:00:25.540
Maya and Doug both want to get
silk as their star material.
00:00:25.810 --> 00:00:29.630
Maya will draw first, followed by Doug.
00:00:29.630 --> 00:00:34.570
What is the probability that
neither contestant draws silk?
00:00:34.570 --> 00:00:36.480
Pause this video and see if
you can work through that
00:00:36.480 --> 00:00:38.330
before we work through this together.
00:00:39.980 --> 00:00:41.940
All right, now let's work
through this together.
00:00:41.940 --> 00:00:45.730
So the probably that neither
contestant draws silk.
00:00:45.730 --> 00:00:47.490
So that would be, I'll
just write it another way,
00:00:47.490 --> 00:00:52.310
the probability that, I'll
write MNS for Maya no silk.
00:00:52.310 --> 00:00:57.310
So Maya no silk and Doug no silk.
00:01:00.190 --> 00:01:02.029
That's just another way of
saying, what is the probability
00:01:02.029 --> 00:01:04.740
that neither contestant draws silk?
00:01:04.740 --> 00:01:09.540
And so this is going to be
equivalent to the probability
00:01:09.540 --> 00:01:14.540
that Maya does not get silk,
Maya no silk, right over here,
00:01:15.010 --> 00:01:20.010
times the probability that
Doug doesn't get silk,
00:01:20.800 --> 00:01:24.160
given that Maya did not get silk.
00:01:24.160 --> 00:01:26.060
Given Maya no silk.
00:01:26.060 --> 00:01:28.340
This line right over, this vertical line,
00:01:28.340 --> 00:01:30.560
this is shorthand for given.
00:01:30.560 --> 00:01:32.840
And so let's calculate each of these.
00:01:32.840 --> 00:01:35.020
So this is going to be
equal to the probability
00:01:35.020 --> 00:01:36.420
that Maya gets no silk.
00:01:36.420 --> 00:01:40.030
She picked first there's
six options out of here.
00:01:40.030 --> 00:01:44.680
Five of them are not silk,
so it is five over six.
00:01:44.680 --> 00:01:47.030
And then the probability
that Doug does not get silk,
00:01:47.030 --> 00:01:49.690
given that Maya did not get silk.
00:01:49.690 --> 00:01:52.212
So Maya did not get silk, then that means
00:01:52.212 --> 00:01:55.070
that silk is still in the mix,
00:01:55.070 --> 00:01:57.490
but there's only five possibilities left
00:01:57.490 --> 00:01:59.290
because Maya picked one of them,
00:01:59.290 --> 00:02:01.810
and four of them are not silk.
00:02:01.810 --> 00:02:03.800
There's still silk as an option.
00:02:03.800 --> 00:02:05.900
And it's important to
recognize that the probability
00:02:05.900 --> 00:02:09.130
that Doug gets no silk is dependent
00:02:09.130 --> 00:02:12.080
on whether Maya got silk or not.
00:02:12.080 --> 00:02:14.950
So it's very important to have
this given right over here.
00:02:14.950 --> 00:02:16.930
If these were independent events,
00:02:16.930 --> 00:02:19.770
if Maya picked and then
put her card back in
00:02:19.770 --> 00:02:21.840
and then Doug were to pick separately,
00:02:21.840 --> 00:02:24.080
then the probability
that Doug gets no silk,
00:02:24.080 --> 00:02:26.620
given that Maya got no silk,
would be the same thing,
00:02:26.620 --> 00:02:29.438
as a probability that Doug
gets no silk regardless
00:02:29.438 --> 00:02:30.930
of what Maya was doing.
00:02:30.930 --> 00:02:35.220
And so this will end up
becoming four over six
00:02:35.220 --> 00:02:37.713
which is the same thing as two thirds.
|
Probability with combinations example: choosing cards | https://www.youtube.com/watch?v=Tp-SjgG11G8 | vtt | https://www.youtube.com/api/timedtext?v=Tp-SjgG11G8&ei=5VWUZd_1KqKAp-oPtpOXoAc&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=C20E476E9813D4EC793753D5F6EED65983AF0196.7E56361667CA300B82DFDAA01B06D173B204F930&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.160 --> 00:00:02.560
- We're told that a standard
deck of 52 playing cards
00:00:02.560 --> 00:00:06.700
includes four aces, four
kings, and 44 other cards.
00:00:06.700 --> 00:00:09.950
Suppose that Luis
randomly draws four cards
00:00:09.950 --> 00:00:11.940
without replacement.
00:00:11.940 --> 00:00:15.310
What is the probability
that Luis gets two aces
00:00:15.310 --> 00:00:18.490
and two kings, in any order?
00:00:18.490 --> 00:00:19.340
So like always,
00:00:19.340 --> 00:00:22.040
pause this video and see if
you can work through this.
00:00:23.110 --> 00:00:23.943
All right.
00:00:23.943 --> 00:00:25.410
Now, to figure out this probability,
00:00:25.410 --> 00:00:26.243
we can think about this,
00:00:26.243 --> 00:00:29.110
it's going to be the number of,
00:00:29.110 --> 00:00:31.430
let's call them draws
00:00:31.430 --> 00:00:36.200
with exactly two aces and two kings,
00:00:36.200 --> 00:00:41.200
two aces and two kings.
00:00:42.220 --> 00:00:43.053
And that's going to be
00:00:43.053 --> 00:00:47.700
over the total number of
possible draws of four cards.
00:00:47.700 --> 00:00:48.700
So number
00:00:49.560 --> 00:00:54.130
of possible draws
00:00:55.760 --> 00:00:59.300
of four cards.
00:00:59.300 --> 00:01:00.300
Now, for many of y'all,
00:01:00.300 --> 00:01:01.920
this bottom, the denominator here,
00:01:01.920 --> 00:01:03.980
might be a little bit
easier to think about.
00:01:03.980 --> 00:01:06.760
We know that there's 52 total cards,
00:01:06.760 --> 00:01:09.030
of which we are choosing four.
00:01:09.030 --> 00:01:11.330
So we could say 52 choose four,
00:01:11.330 --> 00:01:13.270
and that will tell us the total number
00:01:13.270 --> 00:01:15.610
of possible draws of four cards.
00:01:15.610 --> 00:01:17.700
How many combinations
of four cards can we get
00:01:17.700 --> 00:01:19.880
when we're picking from 52?
00:01:19.880 --> 00:01:23.053
But the top here might be a
little bit more of a stumper.
00:01:24.170 --> 00:01:28.040
We can think we have
exactly two spots for aces,
00:01:28.040 --> 00:01:30.260
so we're choosing two aces
00:01:30.260 --> 00:01:32.400
out of how many possible aces?
00:01:32.400 --> 00:01:34.120
Well, there's four total aces.
00:01:34.120 --> 00:01:38.020
So if we say four choose two,
00:01:38.020 --> 00:01:40.270
this is the total number of ways,
00:01:40.270 --> 00:01:41.500
when you don't care about order,
00:01:41.500 --> 00:01:45.040
that you can have two out
of your four aces picked.
00:01:45.040 --> 00:01:45.873
And then separately,
00:01:45.873 --> 00:01:47.690
we can use similar logic to say,
00:01:47.690 --> 00:01:52.260
all right, there's also
four choose two ways
00:01:52.260 --> 00:01:55.940
of picking two kings out
of four possible kings.
00:01:55.940 --> 00:01:57.870
And now the total number of draws
00:01:57.870 --> 00:02:00.080
with two aces and two kings,
00:02:00.080 --> 00:02:02.950
this is going to be the
product of these two.
00:02:02.950 --> 00:02:05.540
And if you're wondering why
you can just multiply it,
00:02:05.540 --> 00:02:06.430
think about it.
00:02:06.430 --> 00:02:09.970
For every scenario that
you have these two aces,
00:02:09.970 --> 00:02:12.720
you have four choose two scenarios
00:02:12.720 --> 00:02:15.230
of which kings you're dealing with.
00:02:15.230 --> 00:02:17.700
So you would take the product of them.
00:02:17.700 --> 00:02:19.520
And we've already done many examples
00:02:19.520 --> 00:02:21.610
of computing combinatorics like this,
00:02:21.610 --> 00:02:22.660
so I will leave you there.
00:02:22.660 --> 00:02:24.810
If you're so motivated,
I encourage you to be,
00:02:24.810 --> 00:02:27.533
you can actually calculate this value.
|
Probability with combinations example: choosing groups | https://www.youtube.com/watch?v=gy8E0-wf4a0 | vtt | https://www.youtube.com/api/timedtext?v=gy8E0-wf4a0&ei=5VWUZcWwGZatp-oPso-gsAc&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=526AB37E98D2101AA9247B1049A4531B85A41ED5.CB628995F65FD9E1BB8E7CDC2C108C24EE8D1E77&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.420 --> 00:00:01.410
- [Instructor] We're told that Kyra works
00:00:01.410 --> 00:00:03.930
on a team of 13 total people.
00:00:03.930 --> 00:00:06.470
Her manager is randomly
selecting three members
00:00:06.470 --> 00:00:09.760
from her team to represent
the company at a conference.
00:00:09.760 --> 00:00:12.430
What is the probability
that Kyra is chosen
00:00:12.430 --> 00:00:13.810
for the conference?
00:00:13.810 --> 00:00:15.360
Pause this video and
see if you can have a go
00:00:15.360 --> 00:00:18.270
at this before we work
through this together.
00:00:18.270 --> 00:00:20.250
All right, now let's work
through this together.
00:00:20.250 --> 00:00:22.640
So we wanna figure out this probability.
00:00:22.640 --> 00:00:24.600
And so one way to think about it is,
00:00:24.600 --> 00:00:27.440
what are the number of
ways that Kyra can be
00:00:27.440 --> 00:00:31.245
on a team or the number of possible teams,
00:00:31.245 --> 00:00:34.463
teams with Kyra,
00:00:36.390 --> 00:00:41.390
and then over the total
number of possible teams,
00:00:41.400 --> 00:00:46.203
total number of possible teams.
00:00:48.760 --> 00:00:52.200
And if this little hint
gets you even more inspired.
00:00:52.200 --> 00:00:53.500
If you weren't able to
do it the first time,
00:00:53.500 --> 00:00:55.230
I encourage you to try to pause it again
00:00:55.230 --> 00:00:56.980
and then work through it.
00:00:56.980 --> 00:00:59.740
All right, now I will
continue to continue.
00:00:59.740 --> 00:01:01.590
So first let me do the denominator here.
00:01:01.590 --> 00:01:04.650
What are the total
possible number of teams?
00:01:04.650 --> 00:01:05.660
Some of y'all might've found
00:01:05.660 --> 00:01:07.900
that a little bit easier to figure out.
00:01:07.900 --> 00:01:10.810
Well, we know that we're
choosing from 13 people
00:01:10.810 --> 00:01:12.880
and we're picking three of them
00:01:12.880 --> 00:01:14.700
and we don't care about order.
00:01:14.700 --> 00:01:17.180
It's not like we're saying
someone's gonna be president
00:01:17.180 --> 00:01:18.013
of the team,
00:01:18.013 --> 00:01:19.120
someone's gonna be vice-president
00:01:19.120 --> 00:01:20.580
and someone's gonna be treasurer.
00:01:20.580 --> 00:01:23.250
We just say there are
three people in the team.
00:01:23.250 --> 00:01:26.680
And so this is a
situation where out of 13,
00:01:26.680 --> 00:01:30.210
we are choosing three people.
00:01:30.210 --> 00:01:32.160
Now, what are the total number of teams,
00:01:32.160 --> 00:01:35.660
possible teams that could have Kyra in it?
00:01:35.660 --> 00:01:38.330
Well, one way to think
about it is if we know
00:01:38.330 --> 00:01:41.600
that Kyra is on a team,
then the possibilities are
00:01:41.600 --> 00:01:44.310
who's gonna be the other
two people on the team,
00:01:44.310 --> 00:01:45.920
and who are the possible candidates
00:01:45.920 --> 00:01:47.260
for the other two people?
00:01:47.260 --> 00:01:49.260
Well, if Kyra is already on the team
00:01:49.260 --> 00:01:51.970
then there's a possible
12 people to pick from.
00:01:51.970 --> 00:01:53.810
So there's 12 people to choose from
00:01:53.810 --> 00:01:55.680
for those other two slots.
00:01:55.680 --> 00:01:57.430
And so we're gonna choose two.
00:01:57.430 --> 00:01:58.510
And once again, we don't care
00:01:58.510 --> 00:02:00.920
about the order with which
we are choosing them.
00:02:00.920 --> 00:02:04.290
So once again, it is
gonna be a combination.
00:02:04.290 --> 00:02:05.960
And then we can just go ahead
00:02:05.960 --> 00:02:09.690
and calculate each of
these combinations here.
00:02:09.690 --> 00:02:11.890
What is 12 choose two?
00:02:11.890 --> 00:02:13.890
Well, there's 12 possible people
00:02:13.890 --> 00:02:16.370
for that first nine Kyra's seat.
00:02:16.370 --> 00:02:18.750
And then there would be 11 people there
00:02:18.750 --> 00:02:21.270
for that other non Kyra's spot.
00:02:21.270 --> 00:02:22.640
And of course it's a combination.
00:02:22.640 --> 00:02:24.550
We don't care what order we picked it in.
00:02:24.550 --> 00:02:27.580
And so there are two ways
to get these two people.
00:02:27.580 --> 00:02:28.750
We could say two factorial
00:02:28.750 --> 00:02:31.250
but that's just the same
thing as two or two times one.
00:02:31.250 --> 00:02:33.210
And then the denominator here.
00:02:33.210 --> 00:02:37.250
For that first spot, there's
13 people to pick from ,
00:02:37.250 --> 00:02:39.410
then in that second spot, there are 12.
00:02:39.410 --> 00:02:42.240
Then in that third spot, there are 11.
00:02:42.240 --> 00:02:45.210
And then once again, we
don't care about order,
00:02:45.210 --> 00:02:47.530
three factorial ways to
arrange three people.
00:02:47.530 --> 00:02:50.540
So I could write three times two,
00:02:50.540 --> 00:02:52.800
and for kicks I could
write one right over here,
00:02:52.800 --> 00:02:55.030
and then we can, let's go down here.
00:02:55.030 --> 00:02:57.150
This is gonna be equal to my numerator
00:02:57.150 --> 00:03:00.700
over here is gonna be six times 11.
00:03:00.700 --> 00:03:05.700
And then my denominator is
going to be 12 divided by six
00:03:06.560 --> 00:03:08.180
right over here is two.
00:03:08.180 --> 00:03:13.180
So it's gonna be 13 times 11 times two.
00:03:14.410 --> 00:03:16.700
Just to be clear, I divided
both the denominator
00:03:16.700 --> 00:03:18.520
and this numerator over here
00:03:18.520 --> 00:03:21.160
by six to get two right over there.
00:03:21.160 --> 00:03:23.530
Now this cancels with that.
00:03:23.530 --> 00:03:26.790
And then if we divide the
numerator and denominator by two,
00:03:26.790 --> 00:03:28.380
this is gonna be three here.
00:03:28.380 --> 00:03:29.580
This is gonna be one.
00:03:29.580 --> 00:03:33.120
And so we are left with a probability
00:03:33.120 --> 00:03:37.623
of 3/13 that Kyra is
chosen for the conference.
|
Representing systems of any number of equations with matrices | https://www.youtube.com/watch?v=lVle8hJTZAk | vtt | https://www.youtube.com/api/timedtext?v=lVle8hJTZAk&ei=5VWUZauuK-W5mLAP1YiNqAE&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=D51183FB69CDAC882CEE2F1F1A8987A46FBF04E9.171D2E03A36EE809F9985BA6523D8D6AFA126BD0&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.170 --> 00:00:01.070
- [Instructor] In a previous video,
00:00:01.070 --> 00:00:02.240
we saw that if you have a system
00:00:02.240 --> 00:00:04.900
of three equations with
three unknowns like this,
00:00:04.900 --> 00:00:08.360
you can represent it as
a matrix vector equation,
00:00:08.360 --> 00:00:10.520
where this matrix right over here
00:00:10.520 --> 00:00:13.740
is a three-by-three matrix.
00:00:13.740 --> 00:00:16.180
That is essentially a coefficient matrix.
00:00:16.180 --> 00:00:18.300
It has all of the coefficients of the Xs,
00:00:18.300 --> 00:00:21.350
the Ys, and the Zs as its various columns.
00:00:21.350 --> 00:00:24.660
and then you're going to
multiply that times this vector,
00:00:24.660 --> 00:00:27.070
which is really the vector
of the unknown variables,
00:00:27.070 --> 00:00:29.570
and this is a three-by-one vector.
00:00:29.570 --> 00:00:30.830
And then you would result
00:00:30.830 --> 00:00:35.450
in this other three-by-one
vector, which is a vector
00:00:35.450 --> 00:00:40.050
that contains these constant
terms right over here.
00:00:40.050 --> 00:00:42.160
What we're gonna do in
this video is recognize
00:00:42.160 --> 00:00:44.570
that you can generalize this phenomenon.
00:00:44.570 --> 00:00:46.340
It's not just true with a system
00:00:46.340 --> 00:00:48.580
of three equations with three unknowns.
00:00:48.580 --> 00:00:52.490
It actually generalizes to
N equations with N unknowns.
00:00:52.490 --> 00:00:55.600
But just to appreciate that
that is indeed the case,
00:00:55.600 --> 00:00:59.610
let us look at a system of two
equations with two unknowns.
00:00:59.610 --> 00:01:04.020
So let's say you had 2x
plus y is equal to nine,
00:01:04.020 --> 00:01:09.020
and we had 3x minus y is equal to five.
00:01:09.230 --> 00:01:10.630
I encourage you, pause this video
00:01:10.630 --> 00:01:12.610
and think about how that
would be represented
00:01:12.610 --> 00:01:15.253
as a matrix vector equation.
00:01:16.520 --> 00:01:19.520
All right, now let's
work on this together.
00:01:19.520 --> 00:01:23.710
So this is a system of two
equations with two unknowns.
00:01:23.710 --> 00:01:27.010
So the matrix that represents
the coefficients is going
00:01:27.010 --> 00:01:29.390
to be a two-by-two matrix
00:01:29.390 --> 00:01:31.680
and then that's going to be multiplied
00:01:31.680 --> 00:01:35.200
by a vector that represents
the unknown variables.
00:01:35.200 --> 00:01:37.090
We have two unknown variables over here.
00:01:37.090 --> 00:01:40.120
So this is going to be
a two-by-one vector,
00:01:40.120 --> 00:01:42.910
and then that's going
to be equal to a vector
00:01:42.910 --> 00:01:45.520
that represents the constants
on the right-hand side,
00:01:45.520 --> 00:01:46.810
and obviously we have two of those.
00:01:46.810 --> 00:01:49.430
So that's going to be a
two-by-one vector as well.
00:01:49.430 --> 00:01:51.870
And then we can do exactly what we did
00:01:51.870 --> 00:01:54.410
in that previous example
in a previous video.
00:01:54.410 --> 00:01:58.850
The coefficients on the
X terms, two and three,
00:01:58.850 --> 00:02:02.570
and then we have the
coefficients on the Y terms.
00:02:02.570 --> 00:02:04.530
This would be a positive one
00:02:04.530 --> 00:02:06.930
and then this would be a negative one.
00:02:06.930 --> 00:02:09.570
And then we multiply it times the vector
00:02:09.570 --> 00:02:12.490
of the variables, X, Y,
00:02:12.490 --> 00:02:14.700
and then last but not least,
00:02:14.700 --> 00:02:19.200
you have this nine and this
five over here, nine and five.
00:02:19.200 --> 00:02:22.040
And I encourage you and multiply this out.
00:02:22.040 --> 00:02:25.390
Multiply this matrix times this vector.
00:02:25.390 --> 00:02:28.560
And when you do that and you
still set up this equality,
00:02:28.560 --> 00:02:30.620
you're going to see that
it essentially turns
00:02:30.620 --> 00:02:32.770
into this exact same system
00:02:32.770 --> 00:02:36.010
of two equations and two unknowns.
00:02:36.010 --> 00:02:37.650
Now, what's interesting about this is
00:02:37.650 --> 00:02:40.730
that we see a generalizable form.
00:02:40.730 --> 00:02:43.860
In general, you can represent a system
00:02:43.860 --> 00:02:47.890
of N equations and N unknowns in the form.
00:02:47.890 --> 00:02:51.740
Sum N-by-N matrix A,
00:02:51.740 --> 00:02:53.400
N by N,
00:02:53.400 --> 00:02:58.340
times sum N-by-one vector X.
00:02:58.340 --> 00:02:59.523
This isn't just the variable X.
00:02:59.523 --> 00:03:03.950
This is a vector X that
has N dimensions to it.
00:03:03.950 --> 00:03:08.610
So times sum N-by-one vector X is going
00:03:08.610 --> 00:03:13.530
to be equal to sum N-by-one vector B.
00:03:14.480 --> 00:03:17.360
These are the letters that
people use by convention.
00:03:17.360 --> 00:03:19.030
This is going to be N by one.
00:03:19.030 --> 00:03:21.890
And so you can see in
these different scenarios.
00:03:21.890 --> 00:03:24.850
In that first one, this is
a three-by-three matrix.
00:03:24.850 --> 00:03:26.870
We could call that A,
00:03:26.870 --> 00:03:29.580
and then we could call this the vector X,
00:03:29.580 --> 00:03:31.760
and then we could call this the vector B.
00:03:31.760 --> 00:03:32.850
Now in that second scenario,
00:03:32.850 --> 00:03:34.800
we could call this the matrix A,
00:03:34.800 --> 00:03:36.850
we could call this the vector X,
00:03:36.850 --> 00:03:39.320
and then we could call this the vector B,
00:03:39.320 --> 00:03:42.820
but we can generalize
that to N dimensions.
00:03:42.820 --> 00:03:44.760
And as I talked about
in the previous video,
00:03:44.760 --> 00:03:47.880
what's interesting about this
is you could think about,
00:03:47.880 --> 00:03:49.890
for example, in this
system of two equations
00:03:49.890 --> 00:03:52.300
with two unknowns, as all
right, I have a line here,
00:03:52.300 --> 00:03:53.490
I have a line here,
00:03:53.490 --> 00:03:57.640
and X and Y represent the
intersection of those lines.
00:03:57.640 --> 00:03:58.850
But when you represent it this way,
00:03:58.850 --> 00:04:00.580
you could also imagine it as saying,
00:04:00.580 --> 00:04:04.470
okay, I have some unknown
vector in the coordinate plane
00:04:04.470 --> 00:04:07.460
and I'm transforming it using this matrix
00:04:07.460 --> 00:04:10.030
to get this vector nine five.
00:04:10.030 --> 00:04:12.410
And so I have to figure out what vector,
00:04:12.410 --> 00:04:15.510
when transformed in this
way, gets us to nine five,
00:04:15.510 --> 00:04:18.160
and we also thought about it
in the three-by-three case.
00:04:18.160 --> 00:04:20.950
What three-dimensional vector,
when transformed in this way,
00:04:20.950 --> 00:04:23.360
gets us to this vector right over here?
00:04:23.360 --> 00:04:24.910
And so that hints,
00:04:24.910 --> 00:04:27.410
that foreshadows where
we might be able to go.
00:04:27.410 --> 00:04:30.530
If we can unwind this
transformation somehow,
00:04:30.530 --> 00:04:33.850
then we can figure out what
these unknown vectors are.
00:04:33.850 --> 00:04:37.270
And if we can do it in two
dimensions or three dimensions,
00:04:37.270 --> 00:04:40.010
why not be able to do it in N dimensions?
00:04:40.010 --> 00:04:41.980
Which you'll see is actually very useful
00:04:41.980 --> 00:04:43.650
if you ever become a data scientist,
00:04:43.650 --> 00:04:45.220
or you go into computer science,
00:04:45.220 --> 00:04:47.670
or if you go into computer
graphics of some kind.
|
Probability with permutations & combinations example: taste testing | https://www.youtube.com/watch?v=C6gQZ7qKtdM | vtt | https://www.youtube.com/api/timedtext?v=C6gQZ7qKtdM&ei=5VWUZaPiG4_YxN8Plc-K6AQ&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=3902749BC808D138091AE242970BD068198DF69E.9954A4236EAED0F00FDF6A9F47A45EA00E06D57E&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.210 --> 00:00:02.080
- [Instructor] We're told
that Samara is setting up
00:00:02.080 --> 00:00:05.130
an olive tasting
competition for a festival.
00:00:05.130 --> 00:00:07.630
From 15 distinct varieties,
00:00:07.630 --> 00:00:11.160
Samara will choose three
different olive oils
00:00:11.160 --> 00:00:12.870
and blend them together.
00:00:12.870 --> 00:00:14.990
A contestant will taste the blend
00:00:14.990 --> 00:00:18.870
and try to identify which
three of the 15 varieties
00:00:18.870 --> 00:00:20.860
were used to make it.
00:00:20.860 --> 00:00:24.020
Assume that a contestant
can't taste any difference
00:00:24.020 --> 00:00:26.050
and is randomly guessing.
00:00:26.050 --> 00:00:27.560
What is the probability
00:00:27.560 --> 00:00:29.730
that a contestant correctly guesses
00:00:29.730 --> 00:00:33.090
which three varieties were used?
00:00:33.090 --> 00:00:35.840
So pause this video and see
if you can think about that.
00:00:35.840 --> 00:00:37.330
And if you can just come
up with the expression,
00:00:37.330 --> 00:00:38.640
you don't have to compute it.
00:00:38.640 --> 00:00:41.493
That is probably good enough,
at least for our purposes.
00:00:42.420 --> 00:00:45.420
All right, now let's work
through this together.
00:00:45.420 --> 00:00:48.040
So we know several things here.
00:00:48.040 --> 00:00:51.410
We have 15 distinct varieties
00:00:51.410 --> 00:00:55.860
and we are choosing
three of those varieties.
00:00:55.860 --> 00:00:57.080
And anytime we're talking
00:00:57.080 --> 00:00:59.470
about probability and combinatorics,
00:00:59.470 --> 00:01:02.230
it's always interesting to
say, "Does order matter?
00:01:02.230 --> 00:01:04.440
Does it matter what order that Samara
00:01:04.440 --> 00:01:07.590
is picking those three from the 15?"
00:01:07.590 --> 00:01:09.000
It doesn't look like it matters.
00:01:09.000 --> 00:01:10.610
It looks like we just have to think
00:01:10.610 --> 00:01:11.740
about what three they are.
00:01:11.740 --> 00:01:15.390
It doesn't matter what order
either she picked them in,
00:01:15.390 --> 00:01:18.410
or the order in which the
contestant guesses them in.
00:01:18.410 --> 00:01:20.290
And so if you think about the total number
00:01:20.290 --> 00:01:24.540
of ways of picking three
things from a group of 15,
00:01:24.540 --> 00:01:28.913
you could write that as 15, choose three.
00:01:30.700 --> 00:01:33.020
Once again, this is
just shorthand notation
00:01:33.020 --> 00:01:35.610
for how many combinations are there,
00:01:35.610 --> 00:01:38.630
so you can pick three
things from a group of 15?
00:01:38.630 --> 00:01:40.657
So some of you might
have been tempted to say,
00:01:40.657 --> 00:01:43.730
"Hey, let me think
about permutations here.
00:01:43.730 --> 00:01:46.340
And I have 15 things.
00:01:46.340 --> 00:01:49.180
And from that, I wanna
figure out how many ways
00:01:49.180 --> 00:01:54.160
can I pick three things that
actually has order mattering?"
00:01:54.160 --> 00:01:56.010
But this would be the
situation where we're talking
00:01:56.010 --> 00:01:58.960
about the contestant actually
having to maybe guess
00:01:58.960 --> 00:02:02.120
in the same order in which the varieties
00:02:02.120 --> 00:02:04.710
were originally blended,
or something like that,
00:02:04.710 --> 00:02:05.543
but we're not doing that,
00:02:05.543 --> 00:02:08.400
we just care about getting
the right three varieties.
00:02:08.400 --> 00:02:11.930
So this will tell us
the total number of ways
00:02:11.930 --> 00:02:14.930
that you can pick three out of 15.
00:02:14.930 --> 00:02:16.170
And so what's the probability
00:02:16.170 --> 00:02:17.870
that the contestant correctly guesses
00:02:17.870 --> 00:02:19.430
which three varieties were used?
00:02:19.430 --> 00:02:21.610
Well, the contestant is
going to be guessing one
00:02:21.610 --> 00:02:24.450
out of the possible
number of scenarios here.
00:02:24.450 --> 00:02:29.450
So the probability would be
one over 15, choose three.
00:02:30.200 --> 00:02:31.860
And if you wanted to compute this,
00:02:31.860 --> 00:02:35.310
this would be equal to one over,
00:02:35.310 --> 00:02:37.930
now, how many ways can you
pick three things from 15?
00:02:37.930 --> 00:02:39.530
And of course there is a formula here,
00:02:39.530 --> 00:02:41.470
but I always like to reason through it.
00:02:41.470 --> 00:02:44.450
Well, you could say, "All
right, if there's three slots,
00:02:44.450 --> 00:02:46.910
there's 15 different varieties
00:02:46.910 --> 00:02:49.260
that could've gone into that first slot,
00:02:49.260 --> 00:02:52.310
and then there's 14 that could
go into that second slot,
00:02:52.310 --> 00:02:55.720
and then there's 13 that can
go into that third slot."
00:02:55.720 --> 00:02:56.760
But then we have to remember
00:02:56.760 --> 00:02:59.600
that it doesn't matter
what order we pick them in.
00:02:59.600 --> 00:03:02.730
So how many ways can you
rearrange three things?
00:03:02.730 --> 00:03:04.700
Well, it would be three factorial,
00:03:04.700 --> 00:03:08.050
or three times two times one.
00:03:08.050 --> 00:03:12.580
So this would be the same thing
as three times two times one
00:03:12.580 --> 00:03:17.580
over 15 times 14 times 13.
00:03:17.900 --> 00:03:19.190
See, I can simplify this,
00:03:19.190 --> 00:03:22.330
divide numerator and denominator by two,
00:03:22.330 --> 00:03:25.850
divide numerator and denominator by three.
00:03:25.850 --> 00:03:30.423
This is going to be equal
to one over 35 times 13.
00:03:32.030 --> 00:03:37.030
This is going to be one over
350 plus 105, which is 455.
00:03:42.090 --> 00:03:44.103
And we are done.
|
Vector word problem: resultant force | https://www.youtube.com/watch?v=Ga1Di84GcgM | vtt | https://www.youtube.com/api/timedtext?v=Ga1Di84GcgM&ei=5VWUZc7pKsW2mLAPi5umqA4&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=C5B144EA765B1056F778C47F9AB1B7CA904B8B76.165AAB36BAC1D130A75C333A2BC0E26689F699DD&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.480 --> 00:00:01.730
- [Instructor] We're
told that a metal ball
00:00:01.730 --> 00:00:04.290
lies on a flat, horizontal surface.
00:00:04.290 --> 00:00:07.800
It is attracted by two
magnets placed around it.
00:00:07.800 --> 00:00:12.800
We're told that the first
magnets force on the ball is 5 N.
00:00:14.220 --> 00:00:17.700
We're then told the second
magnets force on the ball
00:00:17.700 --> 00:00:20.858
is 3 N in a direction
00:00:20.858 --> 00:00:25.650
that is 100 degree rotation
from the first magnets force.
00:00:25.650 --> 00:00:27.080
And we can see that drawn here.
00:00:27.080 --> 00:00:29.950
This is the first magnets force, it's 5 N.
00:00:29.950 --> 00:00:34.110
And then the second magnets force is 3 N
00:00:34.110 --> 00:00:37.130
at 100 degree angle, 100 degree rotation
00:00:37.130 --> 00:00:39.460
from the first magnets force.
00:00:39.460 --> 00:00:42.040
Now they're asking us a
few interesting questions.
00:00:42.040 --> 00:00:46.000
What is the combined strength
of the magnets' pulls?
00:00:46.000 --> 00:00:47.110
And then they also say,
00:00:47.110 --> 00:00:49.930
what is the direction of
the magnets' combined pulls,
00:00:49.930 --> 00:00:53.350
relative to the direction
of the first magnets pull?
00:00:53.350 --> 00:00:56.340
So I encourage you, pause this video
00:00:56.340 --> 00:00:58.250
and have a go at this on your own
00:00:58.250 --> 00:01:00.100
before we work through this together.
00:01:01.290 --> 00:01:03.440
All right, now let's work
through this together.
00:01:03.440 --> 00:01:05.120
So they're really saying,
00:01:05.120 --> 00:01:07.210
if I take the sum of these two vectors,
00:01:07.210 --> 00:01:09.450
what is gonna be the
resultant force vector?
00:01:09.450 --> 00:01:10.810
What is going to be the magnitude
00:01:10.810 --> 00:01:12.457
of that result in force vector?
00:01:12.457 --> 00:01:16.690
And what is its direction going to be?
00:01:16.690 --> 00:01:18.340
There's two ways we could approach this.
00:01:18.340 --> 00:01:20.440
We could break it down
each of these vectors
00:01:20.440 --> 00:01:22.260
into their respective components,
00:01:22.260 --> 00:01:24.330
and then add the respect of components,
00:01:24.330 --> 00:01:26.750
and then from that figure
out what the magnitude
00:01:26.750 --> 00:01:27.583
and direction is.
00:01:27.583 --> 00:01:29.160
And we do that in other videos,
00:01:29.160 --> 00:01:31.430
or we could take the geometric approach.
00:01:31.430 --> 00:01:32.680
So that's what we're gonna do here.
00:01:32.680 --> 00:01:34.030
And to help us with that,
00:01:34.030 --> 00:01:36.770
we're gonna use what we've
called the Parallelogram rule
00:01:36.770 --> 00:01:38.730
which is really the same idea
00:01:38.730 --> 00:01:42.030
as the head to tail addition of vectors.
00:01:42.030 --> 00:01:44.030
I can take the 3 N vector,
00:01:44.030 --> 00:01:45.510
I can shift it over,
00:01:45.510 --> 00:01:48.750
so its tails at the
head of the 5 N vector.
00:01:48.750 --> 00:01:51.930
It would look something like this.
00:01:51.930 --> 00:01:54.590
So this is 3 N right over there.
00:01:54.590 --> 00:01:57.100
And then I could also
go the other way around.
00:01:57.100 --> 00:01:59.000
I could take the 3 N vector first,
00:01:59.000 --> 00:02:01.330
and take the tail of the 5 N vector
00:02:01.330 --> 00:02:06.270
at the head of the 3 N vector
and shift it like this.
00:02:06.270 --> 00:02:08.230
You can add an either direction
00:02:09.100 --> 00:02:10.940
and either way you look at it,
00:02:10.940 --> 00:02:13.590
when you start at the tails
and you get to the head
00:02:13.590 --> 00:02:15.360
of the second vector,
00:02:15.360 --> 00:02:17.920
you're going to have a resultant force
00:02:17.920 --> 00:02:19.130
that looks like this,
00:02:19.130 --> 00:02:22.390
which is the diagonal
of this parallelogram.
00:02:22.390 --> 00:02:24.600
So there we go.
00:02:24.600 --> 00:02:28.900
And let me just call that our
force vector right over there.
00:02:28.900 --> 00:02:32.190
So if we can figure out
the length of this line
00:02:32.190 --> 00:02:33.680
of this diagonal right over here,
00:02:33.680 --> 00:02:37.200
that would be the magnitude
of this force vector.
00:02:37.200 --> 00:02:38.950
Now, how can we do that?
00:02:38.950 --> 00:02:40.290
Well, let's just think geometrically
00:02:40.290 --> 00:02:44.100
what else we can figure out
about what's going on over here?
00:02:44.100 --> 00:02:45.810
This is a parallelogram.
00:02:45.810 --> 00:02:49.000
So if this is 100 degree
angle right over here,
00:02:49.000 --> 00:02:53.850
this angle right over here is
also going to be 100 degree.
00:02:53.850 --> 00:02:57.420
And we also know that
these two opposite angles
00:02:57.420 --> 00:02:59.930
are also gonna have the same
measure right over here.
00:02:59.930 --> 00:03:02.850
And we also know that the
sum of all of the angles
00:03:02.850 --> 00:03:06.850
in a quadrilateral are
going to be 360 degrees.
00:03:06.850 --> 00:03:08.930
So these two make up 200 degrees,
00:03:08.930 --> 00:03:11.610
we have 160 degrees left
that have to be split
00:03:11.610 --> 00:03:13.290
between that one and that one.
00:03:13.290 --> 00:03:15.310
So we know that this is 80 degrees,
00:03:15.310 --> 00:03:17.700
and we know that this is 80 degrees.
00:03:17.700 --> 00:03:19.320
Well, how does that help us?
00:03:19.320 --> 00:03:21.730
So we know the length of this brown side,
00:03:21.730 --> 00:03:24.950
we know the length of
this side right over here.
00:03:24.950 --> 00:03:26.860
We know the angle between them,
00:03:26.860 --> 00:03:28.030
and what we're trying to do,
00:03:28.030 --> 00:03:31.310
is figure out the length of
the side opposite this angle,
00:03:31.310 --> 00:03:33.200
opposite this 80 degree angle.
00:03:33.200 --> 00:03:37.370
And some of you might remember
the Law of Cosines here.
00:03:37.370 --> 00:03:39.880
And the Law of Cosines I always imagine it
00:03:39.880 --> 00:03:42.950
as an adaptation of the
Pythagorean theorem,
00:03:42.950 --> 00:03:46.340
so that we can deal with
non-right triangles.
00:03:46.340 --> 00:03:49.080
And the Law of Cosines will tell us
00:03:49.080 --> 00:03:52.380
that the magnitude, I'll
just write it over here,
00:03:52.380 --> 00:03:54.770
the magnitude of this vector,
00:03:54.770 --> 00:03:57.130
which is the length of this diagonal,
00:03:57.130 --> 00:04:01.650
is going to be equal
to the square root of,
00:04:01.650 --> 00:04:04.830
we're going to have this side squared,
00:04:04.830 --> 00:04:07.910
so let me write 3 squared,
00:04:07.910 --> 00:04:09.730
plus this side squared,
00:04:09.730 --> 00:04:13.580
plus 5 squared minus
00:04:13.580 --> 00:04:15.863
2 times this side.
00:04:16.910 --> 00:04:19.800
So times 3 times that side.
00:04:19.800 --> 00:04:24.800
So times 5 times the cosine of 80 degrees.
00:04:27.620 --> 00:04:30.450
And so let's get our calculator
out to calculate that.
00:04:30.450 --> 00:04:34.510
I'll start with taking
the cosine of 80 degrees,
00:04:34.510 --> 00:04:38.370
then I'm just gonna multiply
that times looks like 30.
00:04:38.370 --> 00:04:41.890
So times 30 is equal to that.
00:04:41.890 --> 00:04:44.610
Let's put it a little negative there.
00:04:44.610 --> 00:04:49.610
And then to that, I'm going
to add 25 and 9, which is 34.
00:04:51.200 --> 00:04:55.280
So plus 34 is equal to that.
00:04:55.280 --> 00:04:57.380
And now I just take the
square root of all of that.
00:04:57.380 --> 00:04:59.770
And they tell us to round our
answer to the nearest tenths.
00:04:59.770 --> 00:05:03.960
So I can round this to approximately 5.4.
00:05:03.960 --> 00:05:08.423
So this is approximately 5.4 N.
00:05:10.343 --> 00:05:11.820
Now they say, what is the direction
00:05:11.820 --> 00:05:13.140
of the magnets combined poles
00:05:13.140 --> 00:05:16.470
relative to the direction
of the first magnets pole?
00:05:16.470 --> 00:05:18.070
So really what we want to do,
00:05:18.070 --> 00:05:21.340
is figure out this angle right over here,
00:05:21.340 --> 00:05:23.040
let's call that data.
00:05:23.040 --> 00:05:25.780
Well, we know what the length
of the side opposite is.
00:05:25.780 --> 00:05:29.060
So maybe we could use the Law of Sines.
00:05:29.060 --> 00:05:30.650
The Law of Sines would tell us
00:05:30.650 --> 00:05:33.630
that the sine of theta
00:05:33.630 --> 00:05:36.210
over the length of the side opposite to it
00:05:36.210 --> 00:05:39.630
is going to be equal to, let's
pick another angle we know,
00:05:39.630 --> 00:05:41.180
sine of this angle.
00:05:41.180 --> 00:05:44.310
Sine of 80 degrees
00:05:44.310 --> 00:05:47.100
over the length of the
side opposite to it.
00:05:47.100 --> 00:05:50.230
And so this is approximately 5.4.
00:05:50.230 --> 00:05:52.390
And so if we wanna solve a for theta,
00:05:52.390 --> 00:05:54.970
we can multiply both sides by 3.
00:05:54.970 --> 00:05:57.950
So we're going to get sine of theta,
00:05:57.950 --> 00:06:00.620
I'll just stay in this
purple color for simplicity,
00:06:00.620 --> 00:06:05.620
is equal to 3 times sine of 80 degrees
00:06:07.170 --> 00:06:09.510
divided by 5.4.
00:06:09.510 --> 00:06:11.580
And then we could say that theta
00:06:11.580 --> 00:06:16.450
is equal to the inverse sine
of all of this business.
00:06:16.450 --> 00:06:21.107
Three sine of 80 degrees over 5.4.
00:06:22.310 --> 00:06:26.380
So we're going to take 80
degrees, take the sine of it,
00:06:26.380 --> 00:06:29.860
we're going to multiply that by 3,
00:06:29.860 --> 00:06:33.740
divide that by 5.4, that equals that,
00:06:33.740 --> 00:06:37.780
and then I'm going to take the
inverse sine of all of that.
00:06:37.780 --> 00:06:41.210
And they want us to round
to the nearest integer.
00:06:41.210 --> 00:06:44.860
So that's approximately 33 degrees.
00:06:44.860 --> 00:06:46.220
When you do the Law of Sines,
00:06:46.220 --> 00:06:49.120
it's possible that you're also
dealing with an obtuse angle.
00:06:49.120 --> 00:06:51.070
And when you do all of
this, you get the acute one,
00:06:51.070 --> 00:06:53.010
and then you would have
to make an adjustment.
00:06:53.010 --> 00:06:54.640
But that's not what we're dealing here,
00:06:54.640 --> 00:06:58.020
so we know that this data is approximately
00:06:58.020 --> 00:06:59.840
equal to 33 degrees.
00:06:59.840 --> 00:07:02.340
So we know the magnitude of the force
00:07:02.340 --> 00:07:04.240
and we know that it forms an angle
00:07:04.240 --> 00:07:06.330
of approximately 33 degrees
00:07:06.330 --> 00:07:10.003
with the direction of the
force of that first magnet.
|
Vector word problem: resultant velocity | https://www.youtube.com/watch?v=Neon4dpvmUk | vtt | https://www.youtube.com/api/timedtext?v=Neon4dpvmUk&ei=5VWUZZyuJoygp-oP5fKH0A8&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=3268E322AA007AC3FF8DBB35239037AABC21C7AA.AD94C16B97E6B80737D35B11C38707FF17DF1903&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.350 --> 00:00:02.260
- [Instructor] We're
told a boat is traveling
00:00:02.260 --> 00:00:05.900
at a speed of 26 kilometers
per hour in a direction
00:00:05.900 --> 00:00:09.940
that is a 300 degree rotation from East.
00:00:09.940 --> 00:00:12.630
At a certain point it encounters a current
00:00:12.630 --> 00:00:16.070
at a speed of 15 kilometers
per hour in a direction
00:00:16.070 --> 00:00:19.720
that is a 25 degree rotation from East.
00:00:19.720 --> 00:00:22.380
Answer two questions
about the boat's velocity
00:00:22.380 --> 00:00:24.470
after it meets the current.
00:00:24.470 --> 00:00:25.850
Alright, the first question is,
00:00:25.850 --> 00:00:29.110
what is the boat's speed
after it meets the current?
00:00:29.110 --> 00:00:31.390
And it says, round your
answer to the nearest 10th.
00:00:31.390 --> 00:00:34.140
You can round intermediate
values to the nearest 100th.
00:00:34.140 --> 00:00:37.070
And what is the direction
of the boat's velocity
00:00:37.070 --> 00:00:38.670
after it meets the current?
00:00:38.670 --> 00:00:40.730
And they say the same, well,
they actually here it say,
00:00:40.730 --> 00:00:42.500
round your answer to the nearest integer
00:00:42.500 --> 00:00:45.570
and you can round intermediate
values to the nearest 100th.
00:00:45.570 --> 00:00:47.170
So like always pause this video
00:00:47.170 --> 00:00:49.020
and see if you can work through this.
00:00:50.070 --> 00:00:52.120
All right, now let's
work on this together.
00:00:52.120 --> 00:00:54.230
So first let's visualize
each of these vectors.
00:00:54.230 --> 00:00:57.610
We have this vector 26 kilometers
per hour in a direction
00:00:57.610 --> 00:01:00.270
that is a 300 degree rotation from East.
00:01:00.270 --> 00:01:04.110
And we have this vector
15 kilometers per hour
00:01:04.110 --> 00:01:08.210
in a direction that is a 25
degree rotation from East.
00:01:08.210 --> 00:01:12.120
And so let me draw some axes here.
00:01:12.120 --> 00:01:16.990
So let's say that is my Y-axis.
00:01:16.990 --> 00:01:21.990
And then let's say that
this over here is my X-axis.
00:01:22.000 --> 00:01:26.140
And then that first vector
300 degree rotation from East,
00:01:26.140 --> 00:01:28.660
East is in the positive X direction.
00:01:28.660 --> 00:01:33.170
This would be 90 degrees,
180 degrees, 270 degrees.
00:01:33.170 --> 00:01:35.390
I'm going counter-clockwise
cause that's the convention
00:01:35.390 --> 00:01:37.280
for a positive angle.
00:01:37.280 --> 00:01:40.490
And then we'd go a little bit past 270,
00:01:40.490 --> 00:01:44.810
we would go right, right over there.
00:01:44.810 --> 00:01:48.240
And the magnitude of this vector
is 26 kilometers per hour.
00:01:48.240 --> 00:01:50.970
I'll just write a 26 right over there.
00:01:50.970 --> 00:01:54.230
And then this other vector
which is the current
00:01:54.230 --> 00:01:56.060
15 kilometers per hour in a direction
00:01:56.060 --> 00:01:58.230
that is a 25 degree rotation from East.
00:01:58.230 --> 00:02:02.880
So 25 degree rotation might
be something like this
00:02:02.880 --> 00:02:04.340
and it's going to be shorter.
00:02:04.340 --> 00:02:06.720
It's 15 kilometers per hour.
00:02:06.720 --> 00:02:10.540
So, it's going to be
roughly about that long.
00:02:10.540 --> 00:02:12.780
I'm obviously just approximating it
00:02:12.780 --> 00:02:15.860
and I'll just write 15
there for its magnitude.
00:02:15.860 --> 00:02:19.410
So we can visualize what the boat's speed
00:02:19.410 --> 00:02:21.770
and direction it is after
it meets the current.
00:02:21.770 --> 00:02:24.350
It's going to be the sum
of these two vectors.
00:02:24.350 --> 00:02:27.480
And so if we wanted to
sum these two vectors
00:02:27.480 --> 00:02:30.640
we could put the tail of one
at the head of the other.
00:02:30.640 --> 00:02:33.440
And so let's shift this
blue vector down here.
00:02:33.440 --> 00:02:36.260
So it's at the head of the red vector.
00:02:36.260 --> 00:02:38.310
So it would be something like this.
00:02:38.310 --> 00:02:43.010
And so our resulting speed
after it meets the current
00:02:43.010 --> 00:02:44.790
would look something like this.
00:02:44.790 --> 00:02:48.360
We've seen this in many
other videos so far
00:02:48.360 --> 00:02:50.410
but we don't want to just
figure it out visually.
00:02:50.410 --> 00:02:52.640
We want to actually figure
out its actual speed
00:02:52.640 --> 00:02:54.430
which would be the
magnitude of this vector
00:02:54.430 --> 00:02:55.900
and its actual direction.
00:02:55.900 --> 00:02:57.030
So what is the angle?
00:02:57.030 --> 00:02:58.620
And we could say it as a positive angle.
00:02:58.620 --> 00:03:01.410
So what the rotation,
the positive rotation
00:03:01.410 --> 00:03:05.230
from the positive X-axis or from due East.
00:03:05.230 --> 00:03:07.530
So to do that, what I'm
going to do is represent each
00:03:07.530 --> 00:03:11.430
of our original vectors in
terms of their components.
00:03:11.430 --> 00:03:14.060
And so this red vector up here
00:03:14.060 --> 00:03:17.370
and we've done this multiple
times explaining the intuition.
00:03:17.370 --> 00:03:20.680
It's X component is
going to be its magnitude
00:03:20.680 --> 00:03:23.920
26 times the cosine of this angle,
00:03:23.920 --> 00:03:26.980
cosine of 300 degrees.
00:03:26.980 --> 00:03:31.290
And it's Y component is
going to be 26 times the sine
00:03:31.290 --> 00:03:33.280
of 300 degrees.
00:03:33.280 --> 00:03:35.760
If that's unfamiliar to you,
I encourage you to review it
00:03:35.760 --> 00:03:37.600
in other videos where we first introduced
00:03:37.600 --> 00:03:40.030
the notion of components,
it comes straight out
00:03:40.030 --> 00:03:43.930
of our unit circle
definition of trig functions.
00:03:43.930 --> 00:03:47.040
And similarly, this vector right over here
00:03:47.040 --> 00:03:49.710
it's X component is going
to be its magnitude times
00:03:49.710 --> 00:03:53.150
the cosine of 25 degrees.
00:03:53.150 --> 00:03:58.150
And it's Y component is
going to be 15 times the sine
00:03:58.250 --> 00:04:00.740
of 25 degrees.
00:04:00.740 --> 00:04:03.070
And now when we have
it expressed this way,
00:04:03.070 --> 00:04:05.870
if we want to have the resulting vector,
00:04:05.870 --> 00:04:08.490
let's call the resulting vector S
00:04:08.490 --> 00:04:10.970
for maybe the resulting speed.
00:04:10.970 --> 00:04:13.970
Its components are going to
be the sum of each of these.
00:04:13.970 --> 00:04:16.120
So we can write it over here.
00:04:16.120 --> 00:04:19.860
Vector S is going to be equal to
00:04:19.860 --> 00:04:22.550
it's going to be the X
component of this red vector
00:04:22.550 --> 00:04:23.970
of our original speed vector.
00:04:23.970 --> 00:04:28.880
So, 26 cosine of 300 degrees
00:04:28.880 --> 00:04:31.710
plus the X component of the current.
00:04:31.710 --> 00:04:36.710
So, 15 times cosine of 25 degrees
and then the Y components.
00:04:37.340 --> 00:04:40.230
Once again, I add the
corresponding Y components
00:04:40.230 --> 00:04:45.080
26 sine of 300 degrees
00:04:45.080 --> 00:04:50.080
plus 15 sine of 25 degrees.
00:04:50.290 --> 00:04:52.170
And now we could use a
calculator to figure out
00:04:52.170 --> 00:04:55.170
what these are, to say what
these approximately are.
00:04:55.170 --> 00:04:57.780
So first the X component,
we're going to take
00:04:57.780 --> 00:05:02.513
the cosine of 300 degrees, times 26,
00:05:03.380 --> 00:05:06.400
plus I'll open a parenthesis here.
00:05:06.400 --> 00:05:11.343
We're going to take the cosine
of 25 degrees, times 15,
00:05:12.280 --> 00:05:14.210
close our parentheses.
00:05:14.210 --> 00:05:19.210
And that is equal to 26.59 if
I round to the nearest 100th.
00:05:20.689 --> 00:05:23.960
26.59.
00:05:23.960 --> 00:05:25.960
And now let's do the Y component.
00:05:25.960 --> 00:05:30.960
We have the sine of 300 degrees, times 26,
00:05:32.190 --> 00:05:34.960
plus I'll open parentheses,
00:05:34.960 --> 00:05:39.960
the sine of 25 degrees
times 15, close parentheses,
00:05:40.480 --> 00:05:45.480
is equal to negative 16.18 to
round to the nearest 100th.
00:05:45.720 --> 00:05:48.690
Negative 16.18.
00:05:48.690 --> 00:05:52.200
And let's just make sure that
this makes intuitive sense.
00:05:52.200 --> 00:05:54.460
So, 26.59.
00:05:54.460 --> 00:05:56.610
So we're going to go
forward in this direction
00:05:56.610 --> 00:05:59.340
26.59 on the X direction.
00:05:59.340 --> 00:06:03.340
And then we go negative
16.18 in the Y direction.
00:06:03.340 --> 00:06:06.890
So this does seem to match our intuition
00:06:06.890 --> 00:06:09.260
when we tried to look at this visually.
00:06:09.260 --> 00:06:11.650
So we now have the X and Y components
00:06:11.650 --> 00:06:13.410
of the resulting vector
00:06:13.410 --> 00:06:14.720
but that's not what they're asking for.
00:06:14.720 --> 00:06:17.500
They're asking for the speed
which would be the magnitude
00:06:17.500 --> 00:06:19.670
of this vector right over here.
00:06:19.670 --> 00:06:24.430
And so I could write the
magnitude of that vector
00:06:24.430 --> 00:06:26.360
which is going to be its speed.
00:06:26.360 --> 00:06:28.510
We'll just use the
Pythagorean theorem here.
00:06:28.510 --> 00:06:31.750
It is going to be the
square root of this squared
00:06:31.750 --> 00:06:33.620
plus this squared, because once again
00:06:33.620 --> 00:06:35.100
this forms a right triangle here.
00:06:35.100 --> 00:06:37.340
And we review this in other videos,
00:06:37.340 --> 00:06:41.457
it's going to be the square
root of 26.59 squared
00:06:42.780 --> 00:06:47.780
plus negative 16.18 squared
which is approximately equal to,
00:06:48.810 --> 00:06:50.706
they want us to round to the nearest 10th,
00:06:50.706 --> 00:06:55.706
26.59 squared plus.
00:06:57.070 --> 00:06:58.600
And it doesn't matter that
there's a negative here
00:06:58.600 --> 00:06:59.433
cause I'm squaring it.
00:06:59.433 --> 00:07:04.370
So I'll just write 16.18
squared is equal to that.
00:07:06.770 --> 00:07:09.500
And then we want to take
the square root of that.
00:07:09.500 --> 00:07:13.693
We get 31 point, if we round
to the nearest 10th, 31.1.
00:07:15.670 --> 00:07:20.360
So it's approximately 31.1 and
we'll write the units here,
00:07:20.360 --> 00:07:25.240
kilometers per hour is
the speed the boat's speed
00:07:25.240 --> 00:07:27.340
after it meets the current.
00:07:27.340 --> 00:07:29.720
And now the second question
is what is the direction
00:07:29.720 --> 00:07:33.500
of the boat's velocity
after it meets the current?
00:07:33.500 --> 00:07:35.870
Well, one way to think about it is
00:07:35.870 --> 00:07:38.250
if we look at this angle right over here
00:07:38.250 --> 00:07:40.360
which would tell us the direction
00:07:40.360 --> 00:07:44.220
the tangent of that angle,
theta, let me write this down.
00:07:44.220 --> 00:07:47.070
Tangent of that angle theta.
00:07:47.070 --> 00:07:48.950
We know your tangent is your change in Y
00:07:48.950 --> 00:07:50.050
over your change in X.
00:07:50.050 --> 00:07:51.660
You can even view it as the slope
00:07:51.660 --> 00:07:53.570
of this vector right over here.
00:07:53.570 --> 00:07:56.130
We know what our changes in X or Y are.
00:07:56.130 --> 00:07:58.100
Those are X and Y components.
00:07:58.100 --> 00:07:59.460
So it's going to be our change in Y
00:07:59.460 --> 00:08:04.063
which is negative 16.18, over 26.59,
00:08:06.870 --> 00:08:08.320
our change in X.
00:08:08.320 --> 00:08:10.520
And so to solve for theta, we could say
00:08:10.520 --> 00:08:15.320
that theta will be equal
to the inverse tangent.
00:08:15.320 --> 00:08:16.930
And we'll have to think
about this for a second
00:08:16.930 --> 00:08:19.650
because this might not get us
the exact theta that we want
00:08:19.650 --> 00:08:21.160
because the inverse tangent function
00:08:21.160 --> 00:08:24.030
is going to give us something
between positive 90 degrees
00:08:24.030 --> 00:08:25.830
and negative 90 degrees.
00:08:25.830 --> 00:08:27.740
But the number we want, actually it looks
00:08:27.740 --> 00:08:31.811
like it's going to be
between 270 and 360 degrees
00:08:31.811 --> 00:08:33.650
because we're doing a,
00:08:33.650 --> 00:08:35.630
we want to think about a positive rotation
00:08:35.630 --> 00:08:38.380
instead of a negative one but
let's just try to evaluate it.
00:08:38.380 --> 00:08:40.530
The inverse tan of this,
00:08:40.530 --> 00:08:45.073
of negative 16.18, over 26.59.
00:08:47.284 --> 00:08:50.010
16.18 negative
00:08:50.910 --> 00:08:55.910
divided by 26.59 is equal to this.
00:08:57.100 --> 00:09:00.840
And now I am going to take
the inverse tangent of that.
00:09:00.840 --> 00:09:05.690
And that gets us negative 31
degrees, which makes sense.
00:09:05.690 --> 00:09:06.740
This looks intuitive sense
00:09:06.740 --> 00:09:09.230
that if you were to do
a clockwise rotation
00:09:09.230 --> 00:09:11.660
which would be a negative
angle from the positive X-axis
00:09:11.660 --> 00:09:14.290
it looks like what we
drew, but let's just go
00:09:14.290 --> 00:09:15.880
with the convention of
everything else here.
00:09:15.880 --> 00:09:17.680
And let's try to have a positive angle.
00:09:17.680 --> 00:09:21.070
So what we can do is
add 360 degrees to that
00:09:21.070 --> 00:09:22.570
to make a full rotation around.
00:09:22.570 --> 00:09:24.710
And we essentially have
the equivalent angle.
00:09:24.710 --> 00:09:29.480
So let's add 360 to that to
get that right over there.
00:09:29.480 --> 00:09:31.170
So if we round to the nearest integer
00:09:31.170 --> 00:09:35.840
we're looking at
approximately 329 degrees.
00:09:35.840 --> 00:09:40.840
So theta is approximately 329 degrees.
00:09:41.110 --> 00:09:43.680
So here, when I said theta is
equal to this I could write
00:09:43.680 --> 00:09:48.680
theta is going to be equal
to this plus 360 degrees.
00:09:49.140 --> 00:09:52.110
Now what's interesting is, I
was able to add 360 degrees
00:09:52.110 --> 00:09:54.120
to get to the exact same place.
00:09:54.120 --> 00:09:57.350
If we had a situation where
our angle was actually
00:09:57.350 --> 00:09:59.310
this angle right over
here not the situation
00:09:59.310 --> 00:10:00.270
that we actually dealt with,
00:10:00.270 --> 00:10:02.170
but if it was in the second quadrant,
00:10:02.170 --> 00:10:04.070
we would have gotten this theta.
00:10:04.070 --> 00:10:06.510
And we would have had to
be able to realize that,
00:10:06.510 --> 00:10:08.030
hey we're dealing with the second quadrant
00:10:08.030 --> 00:10:09.420
that has the same slope.
00:10:09.420 --> 00:10:11.080
So instead of adding 360 degrees
00:10:11.080 --> 00:10:12.950
we would have added 180 degrees.
00:10:12.950 --> 00:10:16.153
And we've also covered that
in other videos as well.
|
Help Khan Academy supercharge learning | https://www.youtube.com/watch?v=T7QKMp6AS90 | vtt | https://www.youtube.com/api/timedtext?v=T7QKMp6AS90&ei=5VWUZbuUI_rKp-oPkpmMiAM&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=51A03A3A69D9D19C99E24B3E5FB9C58A17AD0368.71AC76459953149BB63129D9125DB98DCB3BCD7F&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.320 --> 00:00:01.153
- Hi everyone.
00:00:01.153 --> 00:00:02.870
Sal Khan here from Khan Academy
00:00:02.870 --> 00:00:05.400
which you probably know
is a not-for-profit
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with a mission of providing
a free world-class education
00:00:08.130 --> 00:00:09.810
for anyone anywhere.
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And not for profit means
no one owns Khan Academy,
00:00:12.450 --> 00:00:13.560
we are a public charity.
00:00:13.560 --> 00:00:15.870
You own as much of Khan Academy as I do.
00:00:15.870 --> 00:00:17.970
It's there for the public good.
00:00:17.970 --> 00:00:19.030
And the way that we're able
00:00:19.030 --> 00:00:21.330
to provide this service, the videos,
00:00:21.330 --> 00:00:24.450
the software, the exercises for free
00:00:24.450 --> 00:00:27.180
to tens of millions of
learners around the world is
00:00:27.180 --> 00:00:29.120
because of philanthropic donations
00:00:29.120 --> 00:00:31.570
from generous folks like yourself.
00:00:31.570 --> 00:00:33.060
So if you're in a position to do so,
00:00:33.060 --> 00:00:35.900
please think about making
a donation to Khan Academy.
00:00:35.900 --> 00:00:39.870
As you probably know, in 2020
the world leaned more heavily
00:00:39.870 --> 00:00:41.880
on Khan Academy than ever before
00:00:41.880 --> 00:00:44.760
to keep the learning
going during the pandemic.
00:00:44.760 --> 00:00:46.690
We had 12 billion learning minutes
00:00:46.690 --> 00:00:47.950
on the platform last year.
00:00:47.950 --> 00:00:50.130
6 billion students coming on their own.
00:00:50.130 --> 00:00:52.310
6 billion is hundreds of thousands
00:00:52.310 --> 00:00:53.910
of teachers getting
their students to do it
00:00:53.910 --> 00:00:57.220
as part of the distance
learning classroom experience
00:00:57.220 --> 00:00:58.350
during the pandemic.
00:00:58.350 --> 00:01:00.820
And as now we get, hopefully, to the light
00:01:00.820 --> 00:01:02.900
at the end of the tunnel on the pandemic
00:01:02.900 --> 00:01:04.760
and hopefully over the next couple
00:01:04.760 --> 00:01:07.290
of months things are able to normalize,
00:01:07.290 --> 00:01:10.240
it's even more important
that we don't let up
00:01:10.240 --> 00:01:12.460
because when all of the
stuff has been thrown up
00:01:12.460 --> 00:01:14.210
into the air, we, one, need to make sure
00:01:14.210 --> 00:01:16.540
that as it falls things don't break.
00:01:16.540 --> 00:01:19.720
Students have accrued
gaps in their learning.
00:01:19.720 --> 00:01:23.450
Teachers need more support,
families need more support.
00:01:23.450 --> 00:01:27.110
And also there's a unique
window of time right now,
00:01:27.110 --> 00:01:30.240
over the next six to 12 months,
where as things come back
00:01:30.240 --> 00:01:32.000
to earth, not only should they not break
00:01:32.000 --> 00:01:33.550
but there's an opportunity to make sure
00:01:33.550 --> 00:01:36.160
that the post-pandemic
world could even be better
00:01:36.160 --> 00:01:38.030
than the pre-pandemic world.
00:01:38.030 --> 00:01:41.180
A world where every student
is able to fill in their gaps,
00:01:41.180 --> 00:01:42.790
learn at their own time and space
00:01:42.790 --> 00:01:45.280
and really reach whatever
that potential is,
00:01:45.280 --> 00:01:48.300
that every teacher has
the tools to personalize
00:01:48.300 --> 00:01:50.770
for their students and
feels optimally informed
00:01:50.770 --> 00:01:53.180
and optimally empowered
and every parent feels
00:01:53.180 --> 00:01:55.220
like there are resources
regardless of your zip code,
00:01:55.220 --> 00:01:56.530
regardless of your income
00:01:56.530 --> 00:01:59.570
where your children can
reach their potential.
00:01:59.570 --> 00:02:02.020
So I hope you can consider
making a donation.
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In particular, we're hoping
00:02:03.120 --> 00:02:06.630
to get at least 12,000
new donors of any level.
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Any donation makes a huge difference
00:02:08.830 --> 00:02:10.610
to become part of this mission
00:02:10.610 --> 00:02:14.713
to provide a free world-class
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Kind: captions
Language: en
00:00:00.700 --> 00:00:04.850
- The intention for today's
hour is really just to relax
00:00:04.850 --> 00:00:08.050
just to unwind, not a lot of
information coming at you,
00:00:08.050 --> 00:00:10.290
just embodied practices.
00:00:10.290 --> 00:00:13.040
And I know that a lot of you
probably have commitments
00:00:13.040 --> 00:00:15.440
at home right now, maybe kids coming in.
00:00:15.440 --> 00:00:18.500
And so really just do what you can
00:00:18.500 --> 00:00:20.160
and take those breaks as needed
00:00:20.160 --> 00:00:23.090
and really there's no pressure to do this
00:00:23.090 --> 00:00:24.193
in any certain way.
00:00:25.510 --> 00:00:29.820
So we're just gonna start with
something that helps us relax
00:00:29.820 --> 00:00:33.170
and that's stretching and
a little bit of massage.
00:00:33.170 --> 00:00:35.862
So Jeremy, if you wouldn't
mind, we're gonna just have
00:00:35.862 --> 00:00:38.283
some background music while we do this.
00:00:39.320 --> 00:00:44.040
And wherever you are, if
you're seated at a chair
00:00:44.040 --> 00:00:46.130
or I'm sitting on the floor right now
00:00:46.130 --> 00:00:48.350
'cause that helps me relax a little more
00:00:48.350 --> 00:00:50.360
but wherever you are,
if you're comfortable
00:00:50.360 --> 00:00:53.130
you can just close your
eyes just to shut off
00:00:53.130 --> 00:00:55.913
some stimuli that's unneeded right now.
00:01:10.270 --> 00:01:12.980
It might be nighttime or
evening where you are,
00:01:12.980 --> 00:01:17.980
so it might be cooler to
just take a moment to notice
00:01:18.960 --> 00:01:21.327
the temperature and the
environment around you.
00:01:32.059 --> 00:01:35.060
And then just take a moment
to notice the feeling
00:01:35.060 --> 00:01:38.193
of your body on the chair,
the surface that you're on,
00:01:45.420 --> 00:01:47.420
and notice where your hands are resting,
00:01:52.200 --> 00:01:55.150
maybe notice if you're leaning
forward or leaning back,
00:01:55.150 --> 00:01:58.600
or if there's any adjustment
that you'd like to make.
00:01:58.600 --> 00:02:00.533
So there's more ease in your body.
00:02:07.644 --> 00:02:12.227
And we're gonna set the
intention of letting go of time
00:02:14.186 --> 00:02:15.870
and that sounds like a giant task,
00:02:15.870 --> 00:02:18.610
but we'll see if we can touch
00:02:18.610 --> 00:02:20.430
into this sense of timelessness
00:02:21.270 --> 00:02:23.420
as if we had all the time in the world
00:02:25.080 --> 00:02:27.113
to let go and unwind.
00:02:32.340 --> 00:02:35.000
Just take a moment to
connect with your breath
00:02:37.700 --> 00:02:40.104
breathing in through your nose
00:02:40.104 --> 00:02:42.370
(inhales)
00:02:42.370 --> 00:02:44.210
and then breathing out a little slower
00:02:44.210 --> 00:02:45.773
through your nose or mouth,
00:02:56.500 --> 00:03:00.140
just letting our nervous
systems start to unwind
00:03:09.660 --> 00:03:12.490
and then just let your
breath find its own natural
00:03:12.490 --> 00:03:17.070
easy rhythm, letting go of any effort
00:03:26.002 --> 00:03:30.410
and then just notice any
sensations in your body.
00:03:30.410 --> 00:03:35.410
So you might be hungry, you might be full,
00:03:40.210 --> 00:03:42.530
you might notice your eyes are fluttering
00:03:47.620 --> 00:03:50.150
and just as we notice these sensations
00:03:50.150 --> 00:03:54.080
we don't have to try and change
them or make them different
00:03:54.080 --> 00:03:58.940
but we can just kind of
greet them with curiosity
00:03:58.940 --> 00:04:02.140
and acceptance, and that this
is how things are right now
00:04:02.140 --> 00:04:03.023
and that's okay.
00:04:05.270 --> 00:04:07.650
If you happen to notice pain
00:04:07.650 --> 00:04:11.090
it might be difficult to
stay with that sensation
00:04:11.090 --> 00:04:14.410
so you can just touch
into any sensation of pain
00:04:14.410 --> 00:04:17.283
and then find a place in
your body where there's ease.
00:04:19.680 --> 00:04:22.200
And sometimes we really
have to search for ease
00:04:22.200 --> 00:04:24.800
maybe it's at the tip of our big toe
00:04:24.800 --> 00:04:29.800
or one of our thumbs,
but somewhere in the body
00:04:29.880 --> 00:04:33.403
usually there's a contact with ease.
00:04:38.120 --> 00:04:41.803
So just allowing us to be
as we are in this moment,
00:04:43.350 --> 00:04:46.523
less than perfect, just as we are.
00:04:51.350 --> 00:04:54.880
And we're just going to add in
a little bit of movement here
00:04:54.880 --> 00:04:57.560
just to stretch our body gently
00:04:57.560 --> 00:05:00.400
and if any of these
movements don't work for you
00:05:00.400 --> 00:05:01.910
you can just stay resting
00:05:01.910 --> 00:05:03.823
and whatever position is comfortable.
00:05:04.710 --> 00:05:07.820
So if you'd like to open your
eyes to see these stretches
00:05:07.820 --> 00:05:09.927
you can, or you can keep your eyes closed
00:05:09.927 --> 00:05:13.083
and just follow my verbal instructions.
00:05:14.070 --> 00:05:16.990
So go ahead and anchor your
hand to a spot next to you
00:05:16.990 --> 00:05:18.760
maybe you're holding onto a chair
00:05:18.760 --> 00:05:23.760
or your fingertips are
resting on a couch or a desk
00:05:23.830 --> 00:05:27.040
and then we're gonna lift our left arm up,
00:05:27.040 --> 00:05:30.260
lift our left fingertips toward the sky
00:05:30.260 --> 00:05:32.850
and just feel that length all the way down
00:05:32.850 --> 00:05:34.623
from your fingertips to your hip.
00:05:36.450 --> 00:05:40.680
And then we're just gonna
slowly reach over to our right
00:05:40.680 --> 00:05:44.210
you can look down that
is nice on your neck
00:05:44.210 --> 00:05:48.340
or you can look up and I'm
just keeping my eyes closed
00:05:48.340 --> 00:05:51.720
just to stay embodied, just to stay with
00:05:51.720 --> 00:05:54.760
the pleasant sensations of stretch
00:05:54.760 --> 00:05:56.863
and loosening up the muscles.
00:05:58.820 --> 00:06:02.310
Take a deep breath here
feeling your lungs expand
00:06:05.100 --> 00:06:06.473
and a deep breath out,
00:06:11.710 --> 00:06:14.210
and then reaching back up to the center
00:06:15.420 --> 00:06:18.227
and then just letting
that left arm float down
00:06:20.324 --> 00:06:24.050
and just pause to notice
different sensations
00:06:24.050 --> 00:06:25.600
between the side we stretched
00:06:25.600 --> 00:06:27.253
and the one we haven't stretched.
00:06:32.417 --> 00:06:35.010
*Subtle tingling or heat
00:06:36.720 --> 00:06:40.513
maybe more space in your
diaphragm to breathe.
00:06:44.820 --> 00:06:46.520
And then we'll go to the other side
00:06:46.520 --> 00:06:50.260
so just lifting that right
arm up toward the sky
00:06:50.260 --> 00:06:54.890
reaching the fingertips up,
anchoring your left hand
00:06:54.890 --> 00:06:58.173
then reach up and over toward your left,
00:06:59.140 --> 00:07:02.010
feeling that stretch from
your right hip all the way
00:07:02.010 --> 00:07:04.080
through to your right fingertips
00:07:04.080 --> 00:07:07.510
and again, you can look
down, you can look up
00:07:12.455 --> 00:07:17.372
and just take a few deep breaths
feeling your lungs expand.
00:07:24.380 --> 00:07:27.610
And then on your next in
breath just reaching back up
00:07:30.230 --> 00:07:35.110
and as you exhale slowly letting
that right arm drift down
00:07:39.200 --> 00:07:41.230
again, just pausing here
00:07:42.710 --> 00:07:45.740
noticing if you feel a little
different than when we started
00:07:48.260 --> 00:07:52.713
maybe you can feel the nervous
systems start to unwind.
00:07:55.800 --> 00:07:57.520
And if not, that's okay too,
00:07:57.520 --> 00:08:02.080
sometimes our nervous system
kind of holds on tight
00:08:02.080 --> 00:08:07.080
to what's going on or
what kind of day we had.
00:08:07.280 --> 00:08:08.533
So that's okay too.
00:08:12.000 --> 00:08:15.350
And then you can open your
eyes and just follow along
00:08:15.350 --> 00:08:18.440
we're just going to do a few movements
00:08:18.440 --> 00:08:21.610
to give ourselves some love,
give our muscles some love.
00:08:21.610 --> 00:08:23.560
So just go ahead, if
it's comfortable for you
00:08:23.560 --> 00:08:26.750
and you don't have any injuries
just go ahead and squeeze,
00:08:26.750 --> 00:08:30.880
gentle squeeze here, right
in your shoulder blades.
00:08:30.880 --> 00:08:32.710
This is where we hold a lot of tension
00:08:32.710 --> 00:08:37.270
and then down the arm all
the way down to your forearm
00:08:38.549 --> 00:08:41.343
and give a little squeezed
her hand and your fingers,
00:08:43.870 --> 00:08:47.133
and let's just do that one
more time going back up,
00:08:48.100 --> 00:08:53.100
squeezing and then again, pause,
00:08:53.330 --> 00:08:56.950
just to notice the difference
between the side we squeezed
00:08:56.950 --> 00:08:58.423
and the side we haven't yet.
00:09:07.214 --> 00:09:08.610
A head, it's all about awareness, right?
00:09:08.610 --> 00:09:13.610
We're just bringing awareness
to ease so we can identify it.
00:09:13.760 --> 00:09:15.160
And then let's go to the other side
00:09:15.160 --> 00:09:18.320
so just giving it a nice
squeeze to that shoulder blade
00:09:20.310 --> 00:09:22.900
anywhere you feel tight
you can stay in that area
00:09:22.900 --> 00:09:26.320
if you'd like and then you
can just work your way down
00:09:26.320 --> 00:09:31.320
the arm, giving a squeeze to
the shoulder and the forearm
00:09:32.760 --> 00:09:34.683
all the way down to your hand.
00:09:36.310 --> 00:09:39.190
Maybe just look down at
your hand and your fingers
00:09:39.190 --> 00:09:41.850
thinking about all the
things that they do,
00:09:41.850 --> 00:09:46.760
they type, and they hug,
cook dinner, wash dishes
00:09:46.760 --> 00:09:47.713
just giving love.
00:09:51.730 --> 00:09:55.350
And then again, just pausing and seeing
00:09:55.350 --> 00:09:58.223
if you can really feel
into the sensations,
00:10:00.080 --> 00:10:05.080
maybe tingling, maybe lightness,
maybe some ease emerged
00:10:16.304 --> 00:10:18.230
then we're gonna do one last movement.
00:10:18.230 --> 00:10:20.650
So we're gonna make fists
with our hands like this,
00:10:20.650 --> 00:10:22.880
you can tuck the thumbs
and do your fingers
00:10:23.820 --> 00:10:26.553
and just hold the squeeze
for a few moments.
00:10:27.810 --> 00:10:31.290
Noticing what happens in
the mind is we tense up
00:10:33.240 --> 00:10:35.940
this is kind of representative
of how we sometimes
00:10:35.940 --> 00:10:38.800
hold on to things or
resist what's happening
00:10:40.560 --> 00:10:43.461
and then take a deep breath
in through your nose.
00:10:43.461 --> 00:10:44.900
(inhales)
00:10:44.900 --> 00:10:47.980
And as you breathe out,
just release the hands
00:10:50.020 --> 00:10:55.020
opening the palms and
this hand gesture kind of
00:10:55.960 --> 00:11:00.030
represents letting go or accepting,
00:11:00.030 --> 00:11:04.633
or being open and curious,
notice how different that is.
00:11:10.979 --> 00:11:12.340
And then the last movement we'll do
00:11:12.340 --> 00:11:15.080
if you wanna open your
eyes to look is just
00:11:15.080 --> 00:11:17.050
imagine you're kind of hugging a tree
00:11:17.990 --> 00:11:19.550
and relax the shoulders down.
00:11:19.550 --> 00:11:21.800
We don't want them to
be up toward your ears.
00:11:23.630 --> 00:11:26.510
And imagine this gesture,
this posture is like
00:11:26.510 --> 00:11:31.360
we're holding whatever we
encounter in this next 40 minutes
00:11:31.360 --> 00:11:32.873
together with kindness,
00:11:34.070 --> 00:11:38.340
whether someone interrupts our
session or we don't feel it,
00:11:38.340 --> 00:11:41.790
we don't feel what we think
we're supposed to be feeling.
00:11:41.790 --> 00:11:46.083
See if we can hold all of that
with kindness and compassion.
00:11:50.870 --> 00:11:55.870
And then we can rest our hands
back down, opening our eyes.
00:12:00.980 --> 00:12:05.870
So hopefully the nervous
system has started to enter
00:12:05.870 --> 00:12:09.590
what we call the rest and
digest mode of operating, right?
00:12:09.590 --> 00:12:12.170
Our parasympathetic nervous system.
00:12:12.170 --> 00:12:15.420
The next few activities we're
gonna do are all about that.
00:12:15.420 --> 00:12:18.400
All about activating our
parasympathetic nervous system
00:12:18.400 --> 00:12:22.030
which is the opposite of our
sympathetic nervous system
00:12:22.030 --> 00:12:24.820
which is our, what we call
fight or flight, right?
00:12:24.820 --> 00:12:27.440
When we're stressed or we're
trying to get things done
00:12:27.440 --> 00:12:30.980
or we're rushed, we wanna
move into the other way,
00:12:30.980 --> 00:12:32.880
the opposite of that.
00:12:32.880 --> 00:12:36.400
So I have a little exercise,
00:12:36.400 --> 00:12:39.700
which is about thinking about teachers
00:12:39.700 --> 00:12:41.060
that you've had in your life.
00:12:41.060 --> 00:12:43.290
And these don't have to be
teachers you've had at school
00:12:43.290 --> 00:12:46.000
but any kind of teacher that's
left an impression on you,
00:12:46.000 --> 00:12:50.870
someone that has taught you
something or connected with you
00:12:50.870 --> 00:12:53.700
someone with whom you felt really seen.
00:12:53.700 --> 00:12:55.960
And I want you just to reflect on that
00:12:55.960 --> 00:13:00.060
and maybe a few people
could share what comes up
00:13:00.060 --> 00:13:01.650
when you think about that.
00:13:01.650 --> 00:13:03.790
And as you're thinking,
as you're processing,
00:13:03.790 --> 00:13:06.940
I'll just share a person I thought of.
00:13:06.940 --> 00:13:09.740
She was my 11th grade science teacher
00:13:09.740 --> 00:13:13.530
and I was really disenchanted with school,
00:13:13.530 --> 00:13:16.880
at the time, I felt like I
wasn't able to really focus on
00:13:16.880 --> 00:13:18.160
what I wanted to focus on,
00:13:18.160 --> 00:13:20.870
which was neuroscience and psychology.
00:13:20.870 --> 00:13:22.850
And she happened to go to UCLA
00:13:22.850 --> 00:13:25.180
which at the time was my dream school
00:13:25.180 --> 00:13:27.310
and she gave me a textbook from one
00:13:27.310 --> 00:13:30.070
of her neuroscience
classes that she still had
00:13:30.070 --> 00:13:32.320
and she told me that at
any time I could go sit
00:13:32.320 --> 00:13:35.670
in *on classes at UCLA.
00:13:35.670 --> 00:13:39.816
And I was so appreciative of
that because first of all,
00:13:39.816 --> 00:13:43.040
she took my interests seriously,
00:13:43.040 --> 00:13:45.630
she gave me a book that was special to her
00:13:45.630 --> 00:13:49.440
and she let me know that I
could pursue my interests
00:13:49.440 --> 00:13:50.830
and I didn't have to wait for it,
00:13:50.830 --> 00:13:53.080
I could go sit in on a
lecture and be part of it
00:13:53.080 --> 00:13:56.650
even though I hadn't
graduated high school yet.
00:13:56.650 --> 00:14:01.050
So that was a teacher
that I'll never forget,
00:14:01.050 --> 00:14:03.910
I'll remember her for the rest of my life.
00:14:03.910 --> 00:14:06.200
So is there anyone who'd like to share
00:14:06.200 --> 00:14:09.200
just a story of a teacher
you can share verbally,
00:14:09.200 --> 00:14:11.270
I would love to hear your voices,
00:14:11.270 --> 00:14:12.620
and I totally understand too,
00:14:12.620 --> 00:14:15.520
if you you're not able to share verbally
00:14:15.520 --> 00:14:17.710
'cause of what's going on at home.
00:14:17.710 --> 00:14:21.080
But yeah, who's a teacher
in your life that you've had
00:14:21.080 --> 00:14:23.900
maybe it's even a teacher
who inspired you to go
00:14:23.900 --> 00:14:28.063
into this profession and yeah-
00:14:28.063 --> 00:14:30.180
- [Jeremy] We're getting a
number of great responses
00:14:30.180 --> 00:14:32.970
in the question section, which is awesome.
00:14:32.970 --> 00:14:36.500
Carrie says her ninth to
12th grade music teacher
00:14:36.500 --> 00:14:38.480
was totally present and authentic,
00:14:38.480 --> 00:14:41.180
such an encouragement to all students.
00:14:41.180 --> 00:14:43.620
And Katie says, fifth
grade teacher that I worked
00:14:43.620 --> 00:14:45.140
with when I was a para,
00:14:45.140 --> 00:14:47.623
I still think about him
and my classroom plans.
00:14:48.590 --> 00:14:51.600
And then just to get a couple
of folks to share live,
00:14:51.600 --> 00:14:53.140
I see some folks have raised their hands
00:14:53.140 --> 00:14:56.053
so I'm gonna actually
unmute crystal Davis here.
00:14:58.948 --> 00:15:02.193
So crystal, if you like,
you are now live with Sam.
00:15:03.810 --> 00:15:04.743
- Hi crystal.
00:15:08.040 --> 00:15:09.170
- Sometimes it can take a little while
00:15:09.170 --> 00:15:11.206
for the audio to kick it.
00:15:11.206 --> 00:15:13.350
Crystal, feel free to share,
00:15:13.350 --> 00:15:16.093
I'm also gonna go over to Theresa here.
00:15:18.460 --> 00:15:20.670
Theresa, if you're there,
feel free to share.
00:15:20.670 --> 00:15:22.740
- [Crystal] Okay, they said I was muted,
00:15:22.740 --> 00:15:24.080
can you hear me now?
00:15:24.080 --> 00:15:25.650
- Yeah, we can hear you-
- Pretty great, yeah.
00:15:25.650 --> 00:15:27.150
- [Crystal] Okay, awesome.
00:15:27.150 --> 00:15:29.990
So for me, it's my fifth grade teacher,
00:15:29.990 --> 00:15:31.280
her name was Gail Lidy,
00:15:31.280 --> 00:15:33.710
I remember her like it was yesterday.
00:15:33.710 --> 00:15:35.420
I had a very challenging childhood,
00:15:35.420 --> 00:15:36.270
I'll just leave it at that
00:15:36.270 --> 00:15:38.290
to make it comfortable for everyone
00:15:38.290 --> 00:15:40.690
but she showed me that she loved me
00:15:40.690 --> 00:15:43.320
even though I felt so uncomfortable.
00:15:43.320 --> 00:15:45.190
And the biggest thing of all is that
00:15:45.190 --> 00:15:46.640
I was actually able to meet her
00:15:46.640 --> 00:15:49.410
after I finally got my
degree six years ago
00:15:49.410 --> 00:15:51.520
and I did my student teaching
00:15:51.520 --> 00:15:55.290
and she told me how
proud of me that she was.
00:15:55.290 --> 00:15:57.760
And so I got a chance to
have that last conversation
00:15:57.760 --> 00:15:59.630
with her before she passed away,
00:15:59.630 --> 00:16:02.820
so just very super precious.
00:16:02.820 --> 00:16:04.540
That's my share.
00:16:04.540 --> 00:16:05.683
- That's amazing.
00:16:06.780 --> 00:16:07.880
Thank you for sharing that
00:16:07.880 --> 00:16:11.300
and I heard that the word
love really resonated with me.
00:16:11.300 --> 00:16:13.170
Like you know when you're loved,
00:16:13.170 --> 00:16:18.170
you know when you're cherished by someone,
00:16:18.540 --> 00:16:22.270
even if it is a teacher,
that kind of connection
00:16:23.160 --> 00:16:27.000
can translate or transcend to love
00:16:27.000 --> 00:16:29.300
and that's why we're here,
00:16:29.300 --> 00:16:30.850
I would say that's why
we're here on earth.
00:16:30.850 --> 00:16:33.410
You know, we're here to
connect, we're here to love.
00:16:33.410 --> 00:16:36.040
So it's an amazing connection you had
00:16:36.040 --> 00:16:39.780
and so great that you
were able to meet with her
00:16:39.780 --> 00:16:42.590
and let her know what
impact she had on you
00:16:42.590 --> 00:16:44.140
because when we're kids
00:16:44.140 --> 00:16:46.040
and my husband just told
me this too, he's like
00:16:46.040 --> 00:16:48.020
we never get thank yous.
00:16:48.020 --> 00:16:49.700
You know, the only thing he's that come
00:16:49.700 --> 00:16:52.700
or when maybe when the students are older
00:16:52.700 --> 00:16:55.660
and they realize, you
know, how important and
00:16:56.520 --> 00:16:58.320
what sacrifices teachers made
00:16:58.320 --> 00:17:01.690
and what effort they brought
forth to the classroom.
00:17:01.690 --> 00:17:04.883
So, yeah and I'm sure
it meant a lot to her.
00:17:07.050 --> 00:17:10.310
- Thank you so much Crystal
for that amazing share.
00:17:10.310 --> 00:17:11.660
Let's go over to Theresa.
00:17:11.660 --> 00:17:14.050
Theresa, I'm gonna unmute your line,
00:17:14.050 --> 00:17:15.786
are you still there?
00:17:15.786 --> 00:17:17.240
- [Theresa] Yes.
00:17:17.240 --> 00:17:20.630
So I had a college professor in Algebra
00:17:20.630 --> 00:17:23.130
that was a very difficult class.
00:17:23.130 --> 00:17:26.210
It was my third algebra class
trying to take just to get
00:17:26.210 --> 00:17:28.860
through so I could even take
a college Algebra course
00:17:30.050 --> 00:17:33.400
was feeling very overwhelmed
and quite frankly
00:17:33.400 --> 00:17:35.853
very stupid when it came to Algebra.
00:17:36.760 --> 00:17:41.760
And he told me that even
if you don't get it one way
00:17:43.817 --> 00:17:45.920
and showed me that if
you don't get it one way
00:17:45.920 --> 00:17:48.410
there's always another
way to solve a problem
00:17:49.530 --> 00:17:51.100
which is something that I've taken,
00:17:51.100 --> 00:17:52.650
not just when it comes to math
00:17:52.650 --> 00:17:54.800
but I've taken it into life as well.
00:17:54.800 --> 00:17:57.310
That there's multiple
ways to solve our problems
00:17:58.500 --> 00:18:01.230
and don't just stick
with that one message.
00:18:01.230 --> 00:18:03.310
That's something that I brought
into my teaching as well
00:18:03.310 --> 00:18:05.760
because I do the same
thing with my students now,
00:18:07.050 --> 00:18:08.250
if they can't get it one way
00:18:08.250 --> 00:18:10.670
then let's look at it a different way.
00:18:10.670 --> 00:18:12.440
And it's been very successful
00:18:12.440 --> 00:18:15.070
and has been a good thing for me to learn.
00:18:15.070 --> 00:18:17.720
So I'm very thankful to Mr. Cherry,
00:18:17.720 --> 00:18:19.853
who was an algebra teacher in college.
00:18:20.770 --> 00:18:23.420
- Wow, that's a beautiful story
00:18:23.420 --> 00:18:25.350
and the fact that he
was able to connect it
00:18:25.350 --> 00:18:27.000
or you are connecting it to life
00:18:27.000 --> 00:18:31.710
just that when we hit a
roadblock we have this capacity
00:18:31.710 --> 00:18:34.330
to come up with creative solutions
00:18:34.330 --> 00:18:37.400
or ways of looking at problems differently
00:18:37.400 --> 00:18:40.100
and not just by ourselves,
but even asking for help
00:18:40.100 --> 00:18:41.323
and being able to ask our teachers
00:18:41.323 --> 00:18:46.173
to help us look at something
a new way, that's beautiful.
00:18:47.360 --> 00:18:49.070
- Thank you so much.
00:18:49.070 --> 00:18:50.170
- [Theresa] Thank you.
00:18:51.840 --> 00:18:54.173
- So I would love for us to,
00:18:55.266 --> 00:18:57.010
you might not know this practice
00:18:57.010 --> 00:18:59.940
but it's called loving
kindness meditation,
00:18:59.940 --> 00:19:04.720
and for the skeptics out there,
it can sound kind of wooey
00:19:04.720 --> 00:19:09.170
because we're sending kind
wishes to someone else.
00:19:09.170 --> 00:19:11.360
And it's not that we're in any kind
00:19:11.360 --> 00:19:15.360
of delusional state that
we think we can send wishes
00:19:15.360 --> 00:19:16.960
and they'll somehow be received,
00:19:18.065 --> 00:19:19.300
we're doing it for ourselves.
00:19:19.300 --> 00:19:23.720
There's been a lot of research
on this form of meditation
00:19:23.720 --> 00:19:27.413
and the research has shown
that it connects us to,
00:19:28.290 --> 00:19:29.880
well it has a lot of health benefits,
00:19:29.880 --> 00:19:32.227
reduces inflammation, increases
00:19:32.227 --> 00:19:34.390
and boosts our immune system.
00:19:34.390 --> 00:19:38.500
But it also puts us in touch
with the neurocircuitry
00:19:38.500 --> 00:19:40.370
that makes us wanna connect,
00:19:40.370 --> 00:19:42.300
that helps us attune to each other
00:19:42.300 --> 00:19:45.810
and helps us to be present
for another human being
00:19:45.810 --> 00:19:48.232
and to be present for ourselves.
00:19:48.232 --> 00:19:51.560
So it's really a selfish exercise
00:19:51.560 --> 00:19:53.320
even though we're doing something
00:19:54.590 --> 00:19:57.170
that sounds really benevolent for others
00:19:57.170 --> 00:19:58.790
but it also makes you want,
00:19:58.790 --> 00:20:01.320
sometimes it stimulates this desire
00:20:01.320 --> 00:20:04.250
to reach out to the person or to write
00:20:04.250 --> 00:20:07.170
a letter of thank you or to really just
00:20:07.170 --> 00:20:09.430
be with them in a deeper way.
00:20:09.430 --> 00:20:11.560
So we don't know exactly
what it's gonna do
00:20:11.560 --> 00:20:15.053
but we go into it knowing it
will be in some way beneficial.
00:20:16.240 --> 00:20:19.360
So I would love for us
to send some kind wishes
00:20:19.360 --> 00:20:22.520
to the teachers that you thought of,
00:20:22.520 --> 00:20:26.060
the teacher that came to mind
and I'll lead you through.
00:20:26.060 --> 00:20:28.610
It's a very brief practice,
I'll lead you through it.
00:20:28.610 --> 00:20:30.590
And just keep this person in mind
00:20:30.590 --> 00:20:33.264
and keep the feeling alive in you,
00:20:33.264 --> 00:20:37.490
the feeling of connection of being seen of
00:20:39.127 --> 00:20:44.127
that freedom that you had when you
00:20:44.410 --> 00:20:46.110
from your algebra
teacher, when you learned
00:20:46.110 --> 00:20:47.840
that you could look at
something a different way
00:20:47.840 --> 00:20:49.730
or that there were
multiple ways of solving it
00:20:49.730 --> 00:20:54.700
how that kind of opened
it, like on tied the knot
00:20:54.700 --> 00:20:57.370
that you may have felt when
you didn't get something.
00:20:57.370 --> 00:20:59.220
So just keeping that feeling alive
00:20:59.220 --> 00:21:01.570
and we can close our eyes,
00:21:01.570 --> 00:21:04.090
if we're comfortable, you
can always rest your eyes
00:21:04.090 --> 00:21:05.230
on a spot in front of you,
00:21:05.230 --> 00:21:07.080
if you don't like to close your eyes.
00:21:08.920 --> 00:21:11.363
And let's just bring that teacher to mind.
00:21:15.120 --> 00:21:18.207
You can imagine that they're
in front of you or next to you,
00:21:19.640 --> 00:21:24.200
maybe recall what they
look like, their demeanor
00:21:33.110 --> 00:21:36.270
and just recall the moment of connection
00:21:36.270 --> 00:21:38.113
that you had with this teacher.
00:21:39.840 --> 00:21:42.130
And if no teacher came to
mind, you can just think
00:21:42.130 --> 00:21:44.943
of someone you like or
love, someone in your life.
00:21:52.890 --> 00:21:56.200
And if you'd like, you can
put a hand on your heart
00:21:56.200 --> 00:21:58.073
but you definitely don't have to.
00:21:59.550 --> 00:22:02.440
And I'm just gonna say some
words of kindness out loud
00:22:02.440 --> 00:22:05.270
and just imagine that you're
sending this kindness,
00:22:05.270 --> 00:22:08.943
you're genuinely wishing for
this person to feel this way.
00:22:11.690 --> 00:22:13.083
May you be happy,
00:22:17.010 --> 00:22:19.183
may you know you're appreciated,
00:22:22.930 --> 00:22:26.660
may you be free from
pain, may you be healthy.
00:22:34.290 --> 00:22:38.010
I'm just taking a breath to
reconnect to that feeling
00:22:38.010 --> 00:22:40.933
of appreciation you have for this person.
00:22:43.930 --> 00:22:45.283
May you be happy,
00:22:47.980 --> 00:22:49.373
may you be safe,
00:22:52.040 --> 00:22:54.423
may you be healthy and at ease.
00:22:57.056 --> 00:22:59.223
(sighing)
00:23:04.560 --> 00:23:05.750
And while we're here
00:23:05.750 --> 00:23:09.020
just bringing to mind your own efforts
00:23:09.020 --> 00:23:11.570
you can place your hand
down if it's getting tired.
00:23:12.590 --> 00:23:16.150
But bringing to mind your efforts to show
00:23:16.150 --> 00:23:18.763
up when you don't feel like it sometimes,
00:23:20.540 --> 00:23:23.040
your efforts to be on time,
00:23:23.040 --> 00:23:27.110
to be present your genuine
desire to show care
00:23:31.290 --> 00:23:36.060
and concern for your
students, for your family
00:23:39.060 --> 00:23:43.393
all of that effort and goodness
that you show to the world.
00:23:51.380 --> 00:23:53.020
And if exceptions come up,
00:23:53.020 --> 00:23:54.250
if you start thinking about,
00:23:54.250 --> 00:23:57.380
well not always like
that, that's okay too.
00:23:57.380 --> 00:23:59.660
Just notice what the mind does,
00:23:59.660 --> 00:24:01.940
what the mind shows you greet it with,
00:24:01.940 --> 00:24:05.640
remember that holding with
compassion and kindness
00:24:08.840 --> 00:24:12.150
and we're just gonna send
some kind wishes to ourselves.
00:24:12.150 --> 00:24:13.780
We're gonna use the word you,
00:24:13.780 --> 00:24:17.080
just so we have that little bit of space
00:24:17.080 --> 00:24:22.080
where our loving kind self
wishing it to our vulnerable,
00:24:22.860 --> 00:24:24.823
maybe sometimes hesitant self.
00:24:27.190 --> 00:24:30.420
So may you be happy, may you be safe,
00:24:39.170 --> 00:24:41.343
may you be free from pain,
00:24:44.870 --> 00:24:46.623
may you have ease.
00:24:52.056 --> 00:24:54.620
(inhales) Taking a deep
breath in (exhales)
00:24:54.620 --> 00:24:57.800
and out just to reconnect
with your efforts
00:24:59.065 --> 00:25:00.103
and your goodness.
00:25:02.370 --> 00:25:07.370
May you be happy, may you be safe,
00:25:11.380 --> 00:25:13.553
may you know you're appreciated,
00:25:17.610 --> 00:25:19.613
I may you feel at ease.
00:25:23.890 --> 00:25:27.630
I'm just staying with the feeling of ease
00:25:27.630 --> 00:25:32.113
that maybe has bubbled
up from this exercise,
00:25:33.020 --> 00:25:36.833
we're holding whatever's here, skepticism.
00:25:38.480 --> 00:25:41.250
May be you feeling of
difficulty or hesitation,
00:25:41.250 --> 00:25:44.707
holding that with kindness,
not resisting it (sighs).
00:25:49.125 --> 00:25:54.125
And when you feel ready,
you can open your eyes
00:25:57.210 --> 00:26:00.490
and I just wanna open it up
again to the group to see
00:26:00.490 --> 00:26:04.350
if anyone would like to share
what that was like for you.
00:26:04.350 --> 00:26:06.880
Often, when we do this
loving kindness practice
00:26:06.880 --> 00:26:10.030
for the first time, it can be,
00:26:10.030 --> 00:26:12.820
we have what we call the
inner heckler, right?
00:26:12.820 --> 00:26:15.310
We have this voice inner
voice kind of heckling us
00:26:15.310 --> 00:26:16.650
and saying, what are you doing?
00:26:16.650 --> 00:26:17.623
What is this?
00:26:18.520 --> 00:26:19.930
But maybe you've tried it before,
00:26:19.930 --> 00:26:21.790
maybe it just felt really natural to you.
00:26:21.790 --> 00:26:25.500
So yeah, just feel free to jump in
00:26:25.500 --> 00:26:27.993
and share what that
experience was like for you.
00:26:31.230 --> 00:26:33.750
And again, we can do
it verbally or in chat.
00:26:33.750 --> 00:26:35.854
I love hearing your voices,
00:26:35.854 --> 00:26:38.970
that's my preference,
but whatever you can do
00:26:43.360 --> 00:26:44.210
- [Jeremy] Christy says,
00:26:44.210 --> 00:26:47.373
I'm always surprised of this
exercise can bring me to tears.
00:26:49.540 --> 00:26:50.990
And Abby said, it made me wanna
00:26:50.990 --> 00:26:53.073
call my guiding teacher and say, thanks.
00:26:55.580 --> 00:26:57.950
And then I know there were a couple
00:26:57.950 --> 00:26:59.250
of folks who'd wanna share online,
00:26:59.250 --> 00:27:01.063
so I'm gonna go with Carol first.
00:27:02.180 --> 00:27:04.310
So Carol, I've got open up your line,
00:27:04.310 --> 00:27:07.690
if you wanna unmute yourself,
feel free to say hi to Sam.
00:27:07.690 --> 00:27:09.110
- [Carol] Hello, can you hear me?
00:27:09.110 --> 00:27:10.843
- Yeah, hi Carol.
00:27:10.843 --> 00:27:12.923
- [Carol] Hi, for me,
00:27:14.780 --> 00:27:18.440
I tell my students to do these things
00:27:18.440 --> 00:27:20.590
and I don't always tell myself to.
00:27:20.590 --> 00:27:25.590
And so to hear you, as
the teacher telling me
00:27:25.830 --> 00:27:30.060
as the student to just send myself love,
00:27:30.060 --> 00:27:34.160
it's that kind of switch that I think
00:27:34.160 --> 00:27:36.043
teachers need more often.
00:27:37.681 --> 00:27:39.480
So thank you.
00:27:39.480 --> 00:27:41.550
- You're welcome, it's so true.
00:27:41.550 --> 00:27:42.780
We get in the habit
00:27:42.780 --> 00:27:46.780
of wanting to give advice, give tools
00:27:46.780 --> 00:27:49.893
and then we're we forget to
do it for ourselves, right?
00:27:51.332 --> 00:27:52.770
And we need teachers, right?
00:27:52.770 --> 00:27:55.570
Just like we never
stopped needing teachers
00:27:55.570 --> 00:27:57.433
and helpers as we get older.
00:28:01.760 --> 00:28:04.050
- [Jeremy] And let's go next
to Elizabeth and Elizabeth
00:28:04.050 --> 00:28:06.053
feel free to share your story with Sam.
00:28:06.930 --> 00:28:08.080
- [Elizabeth] Sure, hi.
00:28:10.079 --> 00:28:11.280
I always think it's awesome because
00:28:11.280 --> 00:28:13.390
I have so many people I wanna thank
00:28:13.390 --> 00:28:15.960
and I'm grateful for and appreciate,
00:28:15.960 --> 00:28:18.810
but I can't remember your name
00:28:18.810 --> 00:28:21.920
but you said it brings you to tears.
00:28:21.920 --> 00:28:25.540
And that's what always
surprises me when I do stuff
00:28:25.540 --> 00:28:30.170
like this, you'd come
in and like, it happens
00:28:30.170 --> 00:28:33.260
and mine is, my brother
passed away at age 48,
00:28:33.260 --> 00:28:34.880
a couple of years ago.
00:28:34.880 --> 00:28:38.400
And we had a teacher we
both had in sixth grade
00:28:38.400 --> 00:28:41.600
and she ended up moving
across the street from my mom.
00:28:41.600 --> 00:28:46.210
And 15 years later, she had a picture
00:28:46.210 --> 00:28:49.113
that my brother had given
her like a school picture.
00:28:50.760 --> 00:28:51.920
And she told the story.
00:28:51.920 --> 00:28:53.350
She said, he asked, well
00:28:53.350 --> 00:28:54.900
do you want a school picture of me?
00:28:54.900 --> 00:28:56.610
And she said, well, of course I do.
00:28:56.610 --> 00:28:59.780
And so the next day he
came in with an eight by 10
00:28:59.780 --> 00:29:03.010
and this is like in
the mid early eighties.
00:29:03.010 --> 00:29:07.030
So she kept it and had it when she moved
00:29:07.030 --> 00:29:09.870
in across the street from
my mom, like 15 years later.
00:29:09.870 --> 00:29:13.800
And so it just was a pretty
amazing story that she
00:29:13.800 --> 00:29:16.480
was able to tell us, you
know, at my brother's funeral.
00:29:16.480 --> 00:29:19.150
And like she made a difference then
00:29:19.150 --> 00:29:21.950
and continue to, you know.
00:29:21.950 --> 00:29:25.633
- Wow, what a special woman.
00:29:27.810 --> 00:29:29.233
Thank you for sharing that.
00:29:33.750 --> 00:29:35.470
- [Jeremy] And Sam, do we
have time for one more share?
00:29:35.470 --> 00:29:37.020
- Yes, we do.
00:29:37.020 --> 00:29:40.960
- [Jeremy] Let's go over to
the Jamie (mumbles) actually.
00:29:40.960 --> 00:29:43.560
So Jamie, I'm gonna unmute your line,
00:29:43.560 --> 00:29:45.793
feel free to open it up yourself.
00:29:49.140 --> 00:29:49.973
Hi, Jamie.
00:29:53.380 --> 00:29:55.530
It looks like you might have
a little trouble with Jamie.
00:29:55.530 --> 00:29:56.680
- Oh, okay.
00:29:56.680 --> 00:29:59.500
- [Jeremy] Let me try with Jennifer here.
00:29:59.500 --> 00:30:00.453
Hold on one second.
00:30:02.700 --> 00:30:03.900
Jennifer, are you there?
00:30:11.098 --> 00:30:13.100
Hi, Jennifer, how are you?
00:30:13.100 --> 00:30:15.040
- [Jennifer] I'm good, how are you?
00:30:15.040 --> 00:30:17.230
- Great, thank you so much for joining?
00:30:17.230 --> 00:30:19.030
- [Jennifer] Yeah, again like everyone
00:30:19.030 --> 00:30:21.210
I'm echoing just the sentiments of tears
00:30:21.210 --> 00:30:22.760
and I was surprised
00:30:22.760 --> 00:30:25.270
with how my other senses really connected
00:30:25.270 --> 00:30:27.570
to when I was thinking about
my fourth grade teacher,
00:30:27.570 --> 00:30:29.820
going back to that, I could
00:30:29.820 --> 00:30:31.090
just like it was in the classroom
00:30:31.090 --> 00:30:33.400
and I could hear his
laugh and see his smile
00:30:33.400 --> 00:30:35.800
and it just felt so good.
00:30:35.800 --> 00:30:37.160
And I made the connection that,
00:30:37.160 --> 00:30:38.340
what made him so special,
00:30:38.340 --> 00:30:40.930
he was always a hundred percent present
00:30:40.930 --> 00:30:42.410
with us as his students.
00:30:42.410 --> 00:30:46.563
And that gift of being
present is not forgotten.
00:30:47.460 --> 00:30:52.460
- Yeah, wow, that's incredible.
00:30:52.640 --> 00:30:56.020
The presence it's love, you know
00:30:56.020 --> 00:30:59.150
it's the ultimate show of care
00:30:59.150 --> 00:31:01.940
when you're present and it's hard,
00:31:01.940 --> 00:31:04.840
it gets harder to develop in these times.
00:31:04.840 --> 00:31:09.840
So when we need this time
to stop and just reflect
00:31:11.000 --> 00:31:14.490
and I think we need people
to bring us into it,
00:31:14.490 --> 00:31:16.650
we need all the tools we can get
00:31:16.650 --> 00:31:20.590
to pull us in to this time,
to connect with each other,
00:31:20.590 --> 00:31:23.500
to commune, to share stories.
00:31:23.500 --> 00:31:26.610
So it's so precious and
when we do it, I don't know.
00:31:26.610 --> 00:31:28.830
It sounds like a lot of
you are expressing this too
00:31:28.830 --> 00:31:31.260
but when we do it, we
remember how good it is,
00:31:31.260 --> 00:31:33.590
how good it feels and we wanna do it again
00:31:33.590 --> 00:31:34.530
and again and again.
00:31:34.530 --> 00:31:38.700
So yeah, it's just
rediscovering the importance
00:31:38.700 --> 00:31:41.070
of community and connection, lovely.
00:31:45.050 --> 00:31:48.100
I wanna take us into our next exercise
00:31:48.100 --> 00:31:51.630
which is all about all awe, A-W-E.
00:31:51.630 --> 00:31:53.760
I feel like we don't
use that word very often
00:31:53.760 --> 00:31:55.780
because these moments of awe
00:31:56.770 --> 00:31:59.123
for most of us happen infrequently.
00:32:00.431 --> 00:32:04.300
A moment of awe to me
and how it's been defined
00:32:04.300 --> 00:32:07.880
by the research is these
moments that leave you
00:32:07.880 --> 00:32:11.430
or inspire this feeling of surprise
00:32:11.430 --> 00:32:14.660
and you kind of feel small
00:32:14.660 --> 00:32:19.365
because the thing feels
so big in a good way.
00:32:19.365 --> 00:32:20.570
You feels you feel expansive,
00:32:20.570 --> 00:32:24.620
you feel inspired, you feel,
00:32:24.620 --> 00:32:27.930
you're completely absorbed in that moment,
00:32:27.930 --> 00:32:29.480
you're not thinking about anything else
00:32:29.480 --> 00:32:32.410
because the thing you're
witnessing is so beautiful
00:32:32.410 --> 00:32:35.690
or so touching or so magnificent, right?
00:32:35.690 --> 00:32:39.650
So these are moments
of awe and reflecting,
00:32:39.650 --> 00:32:41.080
there's a lot of research, and I can share
00:32:41.080 --> 00:32:44.924
with you the research
literature that the authors
00:32:44.924 --> 00:32:46.750
there's a woman actually in Canada
00:32:46.750 --> 00:32:49.570
who does this and these
amazing workshops on awe
00:32:49.570 --> 00:32:53.475
but she's found in the research that awe
00:32:53.475 --> 00:32:56.160
is really good for our mental health,
00:32:56.160 --> 00:32:59.420
it stimulates our vagus nerve which again
00:32:59.420 --> 00:33:01.730
activates our parasympathetic
nervous system
00:33:01.730 --> 00:33:06.730
and helps us to actually feel
like we're suspended in time.
00:33:07.420 --> 00:33:10.420
We lose track of time,
we're in this flow state,
00:33:10.420 --> 00:33:12.010
so it's really good for us.
00:33:12.010 --> 00:33:14.400
So I wanna introduce you to this activity
00:33:14.400 --> 00:33:17.160
so that you can put yourself
in that state of awe
00:33:17.160 --> 00:33:19.160
and then hopefully find a lot
00:33:19.160 --> 00:33:22.606
of extraordinary moments
in the ordinariness
00:33:22.606 --> 00:33:25.600
of life, of day-to-day life.
00:33:25.600 --> 00:33:27.610
So what I'm gonna have you do is
00:33:27.610 --> 00:33:29.920
and you can do this again
with your eyes open or closed.
00:33:29.920 --> 00:33:32.980
I like to shut my eyes just to close out
00:33:32.980 --> 00:33:37.490
all the visual stimuli
but we're going to think
00:33:37.490 --> 00:33:40.063
of a moment of awe that we've had.
00:33:41.150 --> 00:33:46.150
So think of a moment
when you were surprised
00:33:47.680 --> 00:33:52.257
and suspended for a moment
in this feeling of amazement,
00:33:55.470 --> 00:34:00.210
this feeling of connection,
maybe it was a connection
00:34:01.402 --> 00:34:06.170
with a person or a moment of
witnessing a child being born
00:34:06.170 --> 00:34:10.890
or seeing a wedding or someone's,
00:34:10.890 --> 00:34:15.530
some experience where
you felt really present
00:34:15.530 --> 00:34:17.543
and in awe of the beauty.
00:34:22.220 --> 00:34:23.580
I'm gonna give you a few moments
00:34:23.580 --> 00:34:26.800
in silence just to allow this memory
00:34:26.800 --> 00:34:29.643
to bubble up without
pushing it or rushing it.
00:34:39.061 --> 00:34:43.644
And as a moment comes to
mind, see if you can expand it
00:34:44.480 --> 00:34:48.760
by noticing the details,
the sensory details.
00:34:48.760 --> 00:34:51.440
So if there were people involved,
00:34:51.440 --> 00:34:53.280
remembering what people were there
00:34:56.290 --> 00:34:58.040
maybe even as you take a deep breath
00:34:58.040 --> 00:35:01.723
you can remember the smell,
the sense in the air.
00:35:05.730 --> 00:35:08.093
Maybe you can remember the sounds,
00:35:13.110 --> 00:35:17.260
maybe you remember the
temperature, if it was a hot day
00:35:17.260 --> 00:35:20.663
or a cold day, neutral.
00:35:25.470 --> 00:35:30.470
And then remember what you
saw the colors, the shapes,
00:35:32.020 --> 00:35:36.703
the facial expressions, the movements.
00:35:43.940 --> 00:35:46.960
Then we're gonna connect with a movement
00:35:46.960 --> 00:35:49.963
that represents this moment of awe.
00:35:51.680 --> 00:35:55.350
So maybe it's your arms
open, or if you were
00:35:57.808 --> 00:36:01.110
holding something, you might
put your arms in that position.
00:36:01.110 --> 00:36:03.720
So just find a movement
in your body right now
00:36:06.552 --> 00:36:08.323
or a gesture that represents
this moment of awe.
00:36:13.200 --> 00:36:16.520
And just hold that movement or posture
00:36:16.520 --> 00:36:20.940
for few breaths, helping
you connect to that feeling
00:36:23.350 --> 00:36:24.650
to let it sock in (sighs).
00:36:34.540 --> 00:36:37.145
Maybe you notice the thoughts that you had
00:36:37.145 --> 00:36:38.495
at the time or the emotions
00:36:43.800 --> 00:36:46.170
and you can place your hands back down
00:36:49.800 --> 00:36:53.380
and just let that feeling simmer
00:36:53.380 --> 00:36:55.343
for just a few more moments.
00:37:15.370 --> 00:37:17.630
Then when you're ready, you can
00:37:19.641 --> 00:37:21.991
if your eyes are closed,
you can open your eyes
00:37:24.343 --> 00:37:25.293
coming back to the space
that we have together.
00:37:27.150 --> 00:37:31.350
And I wanted to share
when I did this exercise
00:37:31.350 --> 00:37:34.130
for the first time, what
moment of awe came to mind?
00:37:34.130 --> 00:37:39.130
And I think Jeremy has a
photograph to pull up to show you.
00:37:41.580 --> 00:37:45.450
It was, when I was 15
00:37:45.450 --> 00:37:47.530
I went to Europe for the first time
00:37:47.530 --> 00:37:52.203
and I saw the Coliseum, oh
that's a beautiful picture.
00:37:53.140 --> 00:37:54.750
Yeah and I looked at it
00:37:54.750 --> 00:37:56.840
and I heard the tour guide starting
00:37:56.840 --> 00:37:59.579
to talk about the history and
00:37:59.579 --> 00:38:03.030
some major points they
were making stuck out
00:38:03.030 --> 00:38:05.800
like how old it was and the events
00:38:05.800 --> 00:38:08.123
that used to take place inside.
00:38:09.178 --> 00:38:12.633
But what got me was how old it was just,
00:38:12.633 --> 00:38:16.400
how it withstood all this time passing
00:38:16.400 --> 00:38:19.030
and all these different events in history
00:38:19.030 --> 00:38:22.170
and it just stood there and it remained.
00:38:22.170 --> 00:38:24.600
And my gesture was this,
00:38:24.600 --> 00:38:26.300
you can't see my hands in the shot
00:38:27.336 --> 00:38:29.760
but like, wow, Kind of pushed back by it
00:38:29.760 --> 00:38:32.470
by how huge it was and how beautiful.
00:38:32.470 --> 00:38:35.720
And I also just felt so lucky to be there,
00:38:35.720 --> 00:38:39.310
I felt so lucky to
witness this living piece
00:38:39.310 --> 00:38:42.560
of history that I had learned
about and in a textbook
00:38:42.560 --> 00:38:43.860
and now I got to see it.
00:38:43.860 --> 00:38:46.400
So that was my moment of awe
00:38:46.400 --> 00:38:50.070
and I just, I really
did lose track of time,
00:38:50.070 --> 00:38:51.400
I think I was there for hours
00:38:51.400 --> 00:38:53.433
but it felt like only minutes went by.
00:38:54.980 --> 00:38:57.480
So I would love to hear from you again
00:38:57.480 --> 00:39:00.630
just what was your moment of
awe, what came up for you?
00:39:00.630 --> 00:39:05.620
What sensory details did you recall?
00:39:05.620 --> 00:39:09.090
And what did it feel like to just stay in
00:39:09.090 --> 00:39:11.150
that feeling of awe?
00:39:11.150 --> 00:39:14.746
There's a lot of research
showing that it takes 30 seconds
00:39:14.746 --> 00:39:19.130
to a minute for a positive
emotion to really register
00:39:19.130 --> 00:39:22.590
in our system for us to
kind of what they say
00:39:22.590 --> 00:39:24.970
or what they call hard-wiring happiness so
00:39:24.970 --> 00:39:29.050
that our default state becomes more likely
00:39:29.050 --> 00:39:32.350
to look for the good, to look
for what we're grateful for,
00:39:32.350 --> 00:39:34.450
to recall these moments of awe.
00:39:34.450 --> 00:39:36.960
It becomes more of a habit over time,
00:39:36.960 --> 00:39:39.088
if we really let it simmer
00:39:39.088 --> 00:39:41.670
and stay with us for
longer periods of time.
00:39:41.670 --> 00:39:43.750
So even talking about it
00:39:43.750 --> 00:39:46.380
and listening to each other is helping us
00:39:46.380 --> 00:39:50.070
to really develop that
hard wiring for the good
00:39:50.070 --> 00:39:52.380
looking for the good, so
we can be fully present
00:39:52.380 --> 00:39:55.740
with each other as we're
listening to these stories of awe.
00:39:55.740 --> 00:39:57.630
And if you'd like, you
can share your gesture
00:39:57.630 --> 00:40:01.750
and I can try to replicate it
and we can all do it together
00:40:01.750 --> 00:40:03.180
so that we're mirroring each other
00:40:03.180 --> 00:40:05.800
and really maybe even touching deeply
00:40:05.800 --> 00:40:08.123
into empathizing with your experience.
00:40:09.380 --> 00:40:10.933
So who would like to share?
00:40:11.890 --> 00:40:13.430
- [Jeremy] We heard a number of great ones
00:40:13.430 --> 00:40:15.970
in the question section, Sam needs to talk
00:40:15.970 --> 00:40:18.593
about sunset on the rim
of the Grand Canyon.
00:40:19.512 --> 00:40:21.600
Jackline talked about
the first time I was out
00:40:21.600 --> 00:40:24.860
on the ocean without being
able to see the shore.
00:40:24.860 --> 00:40:26.700
You met said the moment of owe
00:40:26.700 --> 00:40:28.480
that really struck her
when she was presented
00:40:28.480 --> 00:40:30.270
with her daughter for the first time
00:40:30.270 --> 00:40:32.483
and she looked in her daughter's eyes
00:40:32.483 --> 00:40:33.970
and has had a connection with her,
00:40:33.970 --> 00:40:35.920
this lasted all the way into adulthood.
00:40:38.800 --> 00:40:42.160
- It's an incredible
moment, I'm not a parent yet
00:40:42.160 --> 00:40:46.470
but I imagine that moment
of, I mean overwhelming awe
00:40:46.470 --> 00:40:49.033
when your child is placed in your arms.
00:40:50.310 --> 00:40:53.500
And sometimes we'll do
these exercises with parents
00:40:53.500 --> 00:40:56.020
and kids and have them
look into each other's eyes
00:40:56.020 --> 00:40:58.230
and talk about the color of their eyes.
00:40:58.230 --> 00:41:00.410
Like I noticed you have a little ring
00:41:00.410 --> 00:41:02.775
around your eye and it's
light brown or whatever it is
00:41:02.775 --> 00:41:06.770
but for me witnessing
those moments of connection
00:41:06.770 --> 00:41:10.730
and seeing parents just
their whole face light up
00:41:10.730 --> 00:41:13.810
as their child, children
are looking into their eyes
00:41:13.810 --> 00:41:16.239
is for me, that's a moment of awe
00:41:16.239 --> 00:41:21.080
that I happily get to
relive a lot of the time.
00:41:21.080 --> 00:41:24.033
So yeah, just thank you for sharing that.
00:41:25.590 --> 00:41:27.603
Let's invite some folks that join live.
00:41:28.690 --> 00:41:30.460
Let's start with Michelle.
00:41:30.460 --> 00:41:32.810
So Michelle, I'm gonna unmute your line,
00:41:32.810 --> 00:41:34.710
feel free to do the same on your side.
00:41:38.860 --> 00:41:40.510
Michelle, are you there?
00:41:40.510 --> 00:41:42.360
- [Michelle] Yes, I am.
00:41:42.360 --> 00:41:43.770
- Hi Michelle.
00:41:43.770 --> 00:41:46.653
- [Michelle] Hi, this is amazing.
00:41:47.990 --> 00:41:51.720
The first time I held each of my children
00:41:51.720 --> 00:41:56.720
and it washed over me the enormity of
00:41:59.040 --> 00:42:01.800
how my life would change after that
00:42:02.860 --> 00:42:06.300
life as I had known, it
would never be the same
00:42:06.300 --> 00:42:11.300
and in ways I couldn't
even at that time imagine,
00:42:14.595 --> 00:42:18.928
so that, that was awesome (laughs).
00:42:24.250 --> 00:42:27.780
- Beautiful, I got chills
all through my head
00:42:27.780 --> 00:42:29.933
and back as you were describing that.
00:42:31.650 --> 00:42:33.300
- [Michelle] Took my breath away.
00:42:38.430 --> 00:42:39.263
- That's beautiful.
00:42:39.263 --> 00:42:40.830
Was there a movement that came to mind?
00:42:40.830 --> 00:42:42.602
Was it like holding?
00:42:42.602 --> 00:42:47.602
- [Michelle] Yes, it was as
I cradled them in my arms
00:42:48.590 --> 00:42:50.963
and looked down at their little faces.
00:42:54.610 --> 00:42:58.040
And that was so many years
ago they're adults now,
00:42:58.040 --> 00:43:03.040
but I can cherish that moment once again,
00:43:04.570 --> 00:43:06.630
so I appreciate this.
00:43:06.630 --> 00:43:10.280
I hadn't thought about
that in many, many years,
00:43:10.280 --> 00:43:12.920
so thank you for that.
00:43:12.920 --> 00:43:15.593
- Yeah, you're so welcome,
thank you for sharing.
00:43:17.100 --> 00:43:22.100
Sometimes I look into, I work
with children quite a bit
00:43:22.300 --> 00:43:25.100
and I look into their eyes
as if I was their parent.
00:43:25.100 --> 00:43:28.130
Like I try to connect with
them with that kind of love
00:43:28.130 --> 00:43:31.850
and unconditional positive regard,
00:43:31.850 --> 00:43:33.610
if you wanna use therapy terms
00:43:33.610 --> 00:43:35.880
but that feeling of connection.
00:43:35.880 --> 00:43:37.870
And we can kind of do that
00:43:37.870 --> 00:43:39.747
with other people, even
strangers, we can look
00:43:39.747 --> 00:43:44.190
at them through the eyes of
a mother or a sister friend
00:43:44.190 --> 00:43:49.190
and really connect to
each other on this level.
00:43:49.770 --> 00:43:51.330
You know, we have that capacity
00:43:51.330 --> 00:43:53.920
reminds me of the algebra teacher,
00:43:53.920 --> 00:43:57.860
kind of asking us to look at
the problem of disconnection
00:43:57.860 --> 00:44:01.273
or loneliness and maybe
one solution is to recall
00:44:03.010 --> 00:44:05.060
that feeling of love that we have
00:44:05.060 --> 00:44:07.380
for people in our lives and to maybe look
00:44:07.380 --> 00:44:10.003
at each other through that lens.
00:44:12.589 --> 00:44:15.033
- [Jeremy] Let's go over to Lindsay.
00:44:15.880 --> 00:44:18.270
Lindsay, I'm gonna unmute your line,
00:44:18.270 --> 00:44:20.080
feel free to connect with Sam.
00:44:20.080 --> 00:44:21.770
- [Lindsay] Hi there,
can you guys hear me?
00:44:21.770 --> 00:44:23.103
- Yeah, hi Lindsey.
00:44:24.400 --> 00:44:28.000
- Thank you so much Sam, I
appreciate this, this is awesome.
00:44:28.000 --> 00:44:29.870
So for me, it was also
when I was traveling
00:44:29.870 --> 00:44:31.180
and I think there was a few of us
00:44:31.180 --> 00:44:34.160
said we were somewhere
far, far away from home.
00:44:34.160 --> 00:44:36.910
So I was in *** me and
(mumbles) a couple of years ago
00:44:36.910 --> 00:44:39.000
and I was watching the sunrise
00:44:39.000 --> 00:44:42.400
over hundreds of thousands of pagodas
00:44:42.400 --> 00:44:45.810
and it literally just
seemed like time stopped
00:44:45.810 --> 00:44:47.890
and the sun took forever to come up,
00:44:47.890 --> 00:44:49.840
the transformation of the sky.
00:44:49.840 --> 00:44:52.990
And so that was really
nice to kind of go back
00:44:52.990 --> 00:44:54.230
and revisit that I haven't looked
00:44:54.230 --> 00:44:55.430
at those photos in forever
00:44:55.430 --> 00:44:58.380
but I was sitting on the
pagoda, looking at the sunrise,
00:44:58.380 --> 00:45:00.990
I was right there back in that moment.
00:45:00.990 --> 00:45:04.410
And I try not to focus
too much on the past,
00:45:04.410 --> 00:45:07.970
try to focus on the present
and maybe the next day
00:45:07.970 --> 00:45:09.660
or the next week but
this was a nice reminder
00:45:09.660 --> 00:45:12.590
that it is okay to kind
of go back to the past
00:45:12.590 --> 00:45:15.010
and think of those, those moments of awe,
00:45:15.010 --> 00:45:17.113
so thank you for that so much.
00:45:18.116 --> 00:45:19.690
- Oh, thank you.
00:45:19.690 --> 00:45:21.430
Again, I got chills for my whole body.
00:45:21.430 --> 00:45:24.240
I could see them as these pagodas
00:45:24.240 --> 00:45:26.190
as you were describing them in my mind.
00:45:27.170 --> 00:45:28.922
You know, when we listened to stories
00:45:28.922 --> 00:45:31.430
each other's stories, we're giving gifts.
00:45:31.430 --> 00:45:33.560
That's how I see stories
where we're really
00:45:33.560 --> 00:45:37.970
gifting each other with
these pleasant experiences
00:45:37.970 --> 00:45:40.340
because our brain doesn't
really know the difference
00:45:40.340 --> 00:45:43.080
between living it, like being there again
00:45:43.080 --> 00:45:45.400
and being here now,
00:45:45.400 --> 00:45:47.980
the only differences are our motor cortex
00:45:47.980 --> 00:45:51.280
which is activated when we're
actually physically moving.
00:45:51.280 --> 00:45:53.900
But our brain, you know,
going back to the past
00:45:53.900 --> 00:45:57.714
and really reliving some of
these moments is so good.
00:45:57.714 --> 00:46:01.880
The researcher who I love and
I've done these workshops with
00:46:01.880 --> 00:46:04.730
she talks about it like
a multivitamin, you know,
00:46:04.730 --> 00:46:06.510
the benefits you're giving yourself
00:46:06.510 --> 00:46:09.040
by recalling the past and sharing stories
00:46:09.040 --> 00:46:13.410
and listening to stories is
medicinal in so many ways.
00:46:13.410 --> 00:46:18.410
So yeah, I encourage you all
to really go there often.
00:46:19.110 --> 00:46:21.670
and every time we go there,
we're reinforcing it,
00:46:21.670 --> 00:46:25.550
so it's easier to drop in, before bed,
00:46:25.550 --> 00:46:27.780
if you're having a hard
time falling asleep,
00:46:27.780 --> 00:46:31.540
go to the pagodas, go to your child,
00:46:31.540 --> 00:46:35.430
looking into their eyes,
go to the Coliseum,
00:46:35.430 --> 00:46:39.870
wherever it is, but touch
into it because it's this pool
00:46:39.870 --> 00:46:44.870
of nourishment and it
really, you know changes.
00:46:46.600 --> 00:46:50.090
I think hopefully you all feel a shift,
00:46:50.090 --> 00:46:51.960
our nervous system has settled down
00:46:51.960 --> 00:46:55.430
and if I was just
listening to these stories
00:46:55.430 --> 00:46:58.040
after a busy day and didn't ground myself
00:46:58.040 --> 00:47:01.090
I wouldn't have gotten all
these wonderful sensations
00:47:01.090 --> 00:47:04.435
of tingling and warmth and
the visions of your stories.
00:47:04.435 --> 00:47:09.435
So we need that rest,
we need that stillness
00:47:09.760 --> 00:47:14.110
and rejuvenation to then access
each other more intimately
00:47:14.110 --> 00:47:17.463
and have empathy this deep,
deep embodied empathy.
00:47:19.110 --> 00:47:21.710
So that's what I would
love you to take away
00:47:21.710 --> 00:47:25.850
the time has flown by, but that it,
00:47:25.850 --> 00:47:30.820
to take away looking for
the good, it's a practice,
00:47:30.820 --> 00:47:34.740
looking around and even just
the space you're in right now
00:47:34.740 --> 00:47:39.630
and appreciating, I have
photos of my family up here
00:47:39.630 --> 00:47:41.010
and all these wonderful memories
00:47:41.010 --> 00:47:44.283
but just looking for the good and finding
00:47:44.283 --> 00:47:47.449
extraordinariness in the ordinary
00:47:47.449 --> 00:47:50.590
especially in your students,
and maybe even try looking
00:47:50.590 --> 00:47:55.120
at them through the eyes of a parent
00:47:55.120 --> 00:48:00.110
or that feeling of unconditional
positive regard, even,
00:48:00.110 --> 00:48:02.490
especially I should say
the most difficult students
00:48:02.490 --> 00:48:06.910
who challenge us in so many ways, but yeah
00:48:06.910 --> 00:48:11.690
also teach her some
really beautiful lessons.
00:48:11.690 --> 00:48:15.250
So it has just been such
a pleasure to be with you
00:48:15.250 --> 00:48:19.630
I really hope that you
feel refreshed, rejuvenated
00:48:19.630 --> 00:48:22.880
that the tank is a little bit more full
00:48:22.880 --> 00:48:25.709
and we can just close our
eyes for one last moment
00:48:25.709 --> 00:48:30.709
and just connect there, how
many people on this cal?
00:48:30.720 --> 00:48:35.720
Over 400, 600, 650
people that we can't see,
00:48:35.749 --> 00:48:39.750
we heard some voices, but
we know they're there.
00:48:39.750 --> 00:48:44.750
All of us educator, teaching,
learning from our students
00:48:45.030 --> 00:48:48.690
giving of ourselves, we're
part of this community
00:48:49.610 --> 00:48:52.000
even though we can't see
each other, we're here
00:48:54.797 --> 00:48:58.710
to just taking a moment
to send these kind wishes
00:48:58.710 --> 00:49:02.140
to our whole community,
can think of these beams
00:49:02.140 --> 00:49:05.030
of light going out from
our home all the way around
00:49:05.030 --> 00:49:08.300
the world and at least the country,
00:49:08.300 --> 00:49:11.513
but we can include the
world community of teachers.
00:49:13.290 --> 00:49:18.290
May we all find joy, may
we all have as many moments
00:49:23.210 --> 00:49:26.303
of awe as possible in our lives.
00:49:30.080 --> 00:49:32.283
May we all know we're not alone,
00:49:35.720 --> 00:49:39.913
may we all feel connected
and safe and healthy.
00:49:43.124 --> 00:49:46.050
(exhales)
00:49:46.050 --> 00:49:47.290
And you've sent that out
00:49:47.290 --> 00:49:50.200
and now just take a few breaths receiving
00:49:50.200 --> 00:49:53.720
from the 650 people
that have sent it to you
00:49:53.720 --> 00:49:58.720
just breathing in all the
good that's been sent your way
00:50:00.340 --> 00:50:04.683
and letting it land in your
body, your mind, your heart.
00:50:14.510 --> 00:50:18.400
Letting this feeling of
connection and ease, linger
00:50:23.070 --> 00:50:26.173
and just taking it into
the rest of your evening.
00:50:27.500 --> 00:50:31.140
Maybe the next person you make eye contact
00:50:31.140 --> 00:50:35.300
with just sending them
kindness through your eyes
00:50:41.070 --> 00:50:45.870
and can open our eyes and
for all the timekeepers,
00:50:45.870 --> 00:50:47.900
it's exactly five o'clock.
00:50:47.900 --> 00:50:50.570
So I wanna honor and respect your time
00:50:51.450 --> 00:50:55.690
and just say thank you so
much to our whole team,
00:50:55.690 --> 00:50:57.840
to Jeremy and Alice and Leno
00:50:57.840 --> 00:51:01.950
for putting this all together
and all of you for coming.
00:51:01.950 --> 00:51:05.210
It's been a pleasure and I
hope we can do this again soon.
00:51:05.210 --> 00:51:06.463
Really genuinely.
00:51:11.580 --> 00:51:13.160
- Thank you so much, Sam.
00:51:13.160 --> 00:51:15.825
I just wanted to end on
this note from Michelle
00:51:15.825 --> 00:51:16.790
which I thought was so perfect.
00:51:16.790 --> 00:51:19.400
Michelle says thank you
for this brief respite
00:51:19.400 --> 00:51:20.517
from the rigors of the day to day.
00:51:20.517 --> 00:51:23.080
And we all know that
teaching has those rigors,
00:51:23.080 --> 00:51:24.520
it was a precious gift.
00:51:24.520 --> 00:51:27.530
Maybe you also find joy
and time that you can share
00:51:27.530 --> 00:51:29.470
with others in this wonderful practice.
00:51:29.470 --> 00:51:31.370
So thank you all for joining today.
00:51:31.370 --> 00:51:34.110
Thank you, Sam, for
sharing your gifts with us
00:51:34.110 --> 00:51:36.180
and we wish you all a wonderful spring.
00:51:36.180 --> 00:51:37.013
- Thank you.
00:51:38.240 --> 00:51:39.163
Bye everybody.
|
Subtracting vectors with parallelogram rule | https://www.youtube.com/watch?v=4mRDJf6tShs | vtt | https://www.youtube.com/api/timedtext?v=4mRDJf6tShs&ei=5VWUZam0KabCmLAP_4ediAM&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=A3F8E2A10BE29DE522BCF7E1BE9A5FA512CC4085.B414A17448B429D1EC58AF9A5603934011CE9D97&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.170 --> 00:00:01.430
- [Instructor] In this
video, we're gonna think
00:00:01.430 --> 00:00:04.140
about what it means to subtract vectors,
00:00:04.140 --> 00:00:06.620
especially in the context
of what we talked about
00:00:06.620 --> 00:00:08.760
as the parallelogram rule.
00:00:08.760 --> 00:00:11.880
So let's say we want
to start with vector a
00:00:11.880 --> 00:00:15.360
and from that we want
to subtract vector b.
00:00:15.360 --> 00:00:18.300
And we have vectors a and b depicted here.
00:00:18.300 --> 00:00:19.740
What do you think this is going to be?
00:00:19.740 --> 00:00:22.210
What do you think is going
to be the resulting vector?
00:00:22.210 --> 00:00:24.110
Pause this video and think about that.
00:00:25.060 --> 00:00:25.893
All right.
00:00:25.893 --> 00:00:30.893
Now the key thing to realize
is a minus b is the same thing
00:00:31.360 --> 00:00:36.360
as vector a plus the negative of vector b.
00:00:38.720 --> 00:00:42.000
Now, what is the negative
of vector b look like?
00:00:42.000 --> 00:00:43.850
Well, that's going to be a vector
00:00:43.850 --> 00:00:46.980
that has the exact same
magnitude as vector b
00:00:46.980 --> 00:00:49.500
but just in the opposite direction.
00:00:49.500 --> 00:00:53.320
For example this vector right over here
00:00:53.320 --> 00:00:55.043
would be the vector -b.
00:00:56.501 --> 00:00:57.960
Now we just have to think about
00:00:57.960 --> 00:01:01.230
what is vector a plus the vector -b?
00:01:01.230 --> 00:01:03.400
Well, there's two ways
of thinking about that.
00:01:03.400 --> 00:01:05.200
I could put the tails of both of them
00:01:05.200 --> 00:01:08.010
at the same starting point,
might as well do the origin.
00:01:08.010 --> 00:01:10.650
So let me draw -b over here.
00:01:10.650 --> 00:01:15.650
So we know the vector -b looks like that.
00:01:16.160 --> 00:01:18.410
So one way that you are probably familiar
00:01:18.410 --> 00:01:22.630
is you have vector a and then
what you do is you take a copy
00:01:22.630 --> 00:01:24.690
or you could think of shifting vector b
00:01:24.690 --> 00:01:27.940
so its tail starts at
the head of vector a.
00:01:27.940 --> 00:01:32.940
And if you did that, it
would look like this.
00:01:33.100 --> 00:01:35.060
It would look like this.
00:01:35.060 --> 00:01:36.553
This is also the vector -b.
00:01:38.060 --> 00:01:42.553
And then the sum of vector a and vector -b
00:01:44.210 --> 00:01:48.570
is going to be going
from the tail of vector a
00:01:48.570 --> 00:01:50.802
to the head of vector -b.
00:01:50.802 --> 00:01:55.510
So this would be the
result, right over here.
00:01:55.510 --> 00:01:58.860
Which you could view
as the sum of a plus -b
00:01:58.860 --> 00:02:01.650
or the difference of vectors a and b
00:02:01.650 --> 00:02:04.070
or vector a minus vector b.
00:02:04.070 --> 00:02:05.230
Now, if we wanna think about it
00:02:05.230 --> 00:02:07.400
in terms of the parallelogram rule,
00:02:07.400 --> 00:02:09.504
we could take another copy of vector a
00:02:09.504 --> 00:02:14.380
and put it so that it's
tail's at the head of this -b
00:02:14.380 --> 00:02:18.220
and then we would get it right over here
00:02:18.220 --> 00:02:20.400
and we are forming the parallelogram.
00:02:20.400 --> 00:02:22.340
And then the resulting vector
00:02:22.340 --> 00:02:24.960
is the diagonal of the parallelogram.
00:02:24.960 --> 00:02:26.900
And this just helps us appreciate
00:02:26.900 --> 00:02:28.510
that we could start with -b
00:02:28.510 --> 00:02:31.540
and then add vector a to that.
00:02:31.540 --> 00:02:33.510
Or we could start with vector a
00:02:33.510 --> 00:02:35.810
and then add -b to that.
00:02:35.810 --> 00:02:39.370
But either way you get this
white vector right over here
00:02:39.370 --> 00:02:44.370
which we can view as the
vector a minus vector b,
00:02:44.620 --> 00:02:45.453
and we're done.
|
Adding vectors in magnitude and direction form | https://www.youtube.com/watch?v=yFPfO_eHJdY | vtt | https://www.youtube.com/api/timedtext?v=yFPfO_eHJdY&ei=5VWUZaX1JeiAp-oP_Z-awAw&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=D5CFCCD6ACD1FCEC4C5641415FF17E971FDFB5A3.43C87059E6EF65E2C7B2FB4C7C646BC9A757999E&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.910 --> 00:00:03.030
- [Instructor] We're told that
vector a has magnitude four
00:00:03.030 --> 00:00:06.340
and direction 170 degrees
from the positive x-axis.
00:00:06.340 --> 00:00:09.180
Vector b has magnitude three
and direction 240 degrees
00:00:09.180 --> 00:00:10.960
from the positive x-axis.
00:00:10.960 --> 00:00:15.490
Find the magnitude and direction
of vector a plus vector b.
00:00:15.490 --> 00:00:18.510
So pause this video and see
if you can have a go at that.
00:00:18.510 --> 00:00:19.960
All right, now let's work
through this together.
00:00:19.960 --> 00:00:21.390
And the way that I'm going to approach it,
00:00:21.390 --> 00:00:24.410
I'm going to represent each
vector in component form.
00:00:24.410 --> 00:00:26.270
And then I'm going to add
the corresponding components.
00:00:26.270 --> 00:00:28.650
And from that, I'll try to
figure out the magnitude
00:00:28.650 --> 00:00:30.550
and the direction of the sum.
00:00:30.550 --> 00:00:33.660
So vector a, what is its x-component?
00:00:33.660 --> 00:00:36.160
Well, the change in x
here, there's multiple ways
00:00:36.160 --> 00:00:39.150
that you could try to do
this using trigonometry.
00:00:39.150 --> 00:00:42.390
But we've reviewed this or
gone over this in other videos.
00:00:42.390 --> 00:00:43.830
The simplest way to think about it is
00:00:43.830 --> 00:00:46.057
our change in x here is
going to be the length.
00:00:46.057 --> 00:00:49.620
And we know vector a has
magnitude four times the cosine
00:00:49.620 --> 00:00:51.160
of the angle that the vector makes
00:00:51.160 --> 00:00:54.910
with the positive x-axis,
cosine of 170 degrees.
00:00:54.910 --> 00:00:56.730
And so that's our
x-component right over here,
00:00:56.730 --> 00:01:00.530
four times cosine of 170 degrees.
00:01:00.530 --> 00:01:03.140
And then what's our y-component?
00:01:03.140 --> 00:01:06.670
Well, our y-component is going
to be this change in y here.
00:01:06.670 --> 00:01:08.870
And as we've reviewed in other videos,
00:01:08.870 --> 00:01:11.470
that's going to be the
length times the sine
00:01:11.470 --> 00:01:13.810
of the angle we make
with a positive x-axis,
00:01:13.810 --> 00:01:17.800
sine of 170 degrees.
00:01:17.800 --> 00:01:19.760
And we can maybe use a calculator in a bit
00:01:19.760 --> 00:01:22.130
to get approximations for these values.
00:01:22.130 --> 00:01:25.750
But then we can do the exact
same thing for vector b.
00:01:25.750 --> 00:01:30.670
Vector b here is going
to be, by the same logic,
00:01:30.670 --> 00:01:34.290
it's x-component is going to
be the length of the vector,
00:01:34.290 --> 00:01:36.230
and it would be three.
00:01:36.230 --> 00:01:37.220
They tell us that.
00:01:37.220 --> 00:01:39.930
So it's going to be three times the cosine
00:01:39.930 --> 00:01:43.290
of this angle, 240 degrees.
00:01:43.290 --> 00:01:46.990
And then the y-component
is going to be the length
00:01:46.990 --> 00:01:50.200
of our vector three times the sine
00:01:50.200 --> 00:01:53.650
of 240 degrees.
00:01:53.650 --> 00:01:56.270
Now, when we wanna take
the sum of the two vectors,
00:01:56.270 --> 00:01:57.103
let me write it here,
00:01:57.103 --> 00:02:01.350
vector a plus vector b,
00:02:01.350 --> 00:02:04.490
I can just add the
corresponding components.
00:02:04.490 --> 00:02:08.520
This is going to be equal to four cosine
00:02:08.520 --> 00:02:13.520
of 170 degrees plus three cosine
00:02:14.130 --> 00:02:16.160
of 240 degrees.
00:02:16.160 --> 00:02:20.137
And then the y-component
is going to be four sine
00:02:21.880 --> 00:02:26.880
of 170 degrees plus three sine
00:02:27.860 --> 00:02:30.750
of 240 degrees.
00:02:30.750 --> 00:02:34.360
And so let me get my calculator
out to evaluate these.
00:02:34.360 --> 00:02:36.350
We say 170 degrees.
00:02:36.350 --> 00:02:41.350
We take the cosine times
four, that equals this.
00:02:41.720 --> 00:02:43.500
And then we're going to add to that.
00:02:43.500 --> 00:02:45.430
I'll open parentheses.
00:02:45.430 --> 00:02:47.240
We'll take the cosine of 240.
00:02:47.240 --> 00:02:52.240
240 cosine times three, close parentheses,
00:02:53.000 --> 00:02:54.840
is equal to this, negative,
00:02:54.840 --> 00:02:58.210
approximately negative 5.44.
00:02:58.210 --> 00:03:03.210
So this is approximately negative 5.44.
00:03:03.690 --> 00:03:07.120
And then if we were to take 170 degrees,
00:03:07.120 --> 00:03:10.740
take the sine of it, multiply it by four.
00:03:10.740 --> 00:03:13.670
And then to that, I'm
going to open parentheses.
00:03:13.670 --> 00:03:17.310
I'm gonna take 240 degrees, take the sine,
00:03:17.310 --> 00:03:20.950
multiply that times three,
close my parentheses.
00:03:20.950 --> 00:03:23.800
That is going to be equal to
approximately negative 1.90.
00:03:25.250 --> 00:03:28.773
So this is approximately negative 1.90.
00:03:30.280 --> 00:03:32.460
And this is consistent with our intuition.
00:03:32.460 --> 00:03:35.590
If the sum has both negative components,
00:03:35.590 --> 00:03:37.240
that means it's going to
be in the third quadrant.
00:03:37.240 --> 00:03:39.000
And if I were to do
the head to tail method
00:03:39.000 --> 00:03:41.120
of adding vectors, if
I were to take vector b
00:03:41.120 --> 00:03:44.080
and I were to put it right over here,
00:03:44.080 --> 00:03:45.890
we see that the resulting vector,
00:03:45.890 --> 00:03:48.960
the sum will sit in the third quadrant.
00:03:48.960 --> 00:03:51.540
It makes sense that our x and y-components
00:03:51.540 --> 00:03:53.120
would indeed be negative.
00:03:53.120 --> 00:03:54.270
Now, the question didn't ask
00:03:54.270 --> 00:03:56.070
just to find the components of the sum.
00:03:56.070 --> 00:03:59.210
It asked to find the
magnitude and the direction
00:03:59.210 --> 00:04:00.980
of the resulting sum.
00:04:00.980 --> 00:04:02.320
And so to do that,
00:04:02.320 --> 00:04:05.730
we just have to use a little
bit more of our trigonometry
00:04:05.730 --> 00:04:07.880
and actually a little bit of our geometry.
00:04:07.880 --> 00:04:12.210
For example, our change in x
is this value right over here
00:04:12.210 --> 00:04:14.350
as we go from the tail to the tip.
00:04:14.350 --> 00:04:16.650
It's negative 5.44.
00:04:16.650 --> 00:04:19.260
If we're just thinking in terms
of length right over here,
00:04:19.260 --> 00:04:23.563
the absolute value, this
side would have length 5.44.
00:04:24.880 --> 00:04:27.040
And then same way, you are
changing y, its negative,
00:04:27.040 --> 00:04:29.080
we're going down in y.
00:04:29.080 --> 00:04:30.992
But if we were just thinking
in terms of a triangle,
00:04:30.992 --> 00:04:33.533
the length on this side
of a triangle is 1.90.
00:04:35.570 --> 00:04:38.500
And we can see from
the Pythagorean theorem
00:04:38.500 --> 00:04:42.400
that the length of our hypotenuse,
00:04:42.400 --> 00:04:44.670
which is the same thing as
the magnitude of this vector,
00:04:44.670 --> 00:04:47.400
squared is going to be equal
to the sum of the squares
00:04:47.400 --> 00:04:48.710
of these two sides.
00:04:48.710 --> 00:04:50.280
Or another way of thinking about it is,
00:04:50.280 --> 00:04:53.560
the length of this vector,
the magnitude of this vector,
00:04:53.560 --> 00:04:56.140
which we can write as
a magnitude of vector a
00:04:56.140 --> 00:05:00.070
plus vector b is going to be equal to,
00:05:00.070 --> 00:05:01.660
or I should say approximately equal to
00:05:01.660 --> 00:05:04.350
since we're already
approximating these values,
00:05:04.350 --> 00:05:09.350
the principal root of 5.44 squared.
00:05:09.620 --> 00:05:10.660
And that's 'cause I'm just thinking
00:05:10.660 --> 00:05:12.750
about the absolute length of the side.
00:05:12.750 --> 00:05:14.330
I could also think about a change in x.
00:05:14.330 --> 00:05:16.770
But if I had a negative
5.44 and I square that,
00:05:16.770 --> 00:05:18.440
that would still become positive.
00:05:18.440 --> 00:05:23.000
And then I'll have plus 1.90 squared.
00:05:23.000 --> 00:05:25.330
And I can get our calculator out for that.
00:05:25.330 --> 00:05:26.860
This is going to be
00:05:26.860 --> 00:05:31.860
approximately equal to 5.44 squared
00:05:32.490 --> 00:05:37.000
plus 1.9 squared,
00:05:37.000 --> 00:05:38.330
is equal to that.
00:05:38.330 --> 00:05:40.120
Take the square root of that.
00:05:40.120 --> 00:05:43.533
It's approximately equal to 5.76,
00:05:45.540 --> 00:05:50.010
5.76, which is going to be our magnitude.
00:05:50.010 --> 00:05:51.880
And then to figure out the direction,
00:05:51.880 --> 00:05:54.610
so we essentially want to figure out
00:05:54.610 --> 00:05:57.210
this angle right over here.
00:05:57.210 --> 00:06:01.340
You might recognize that
the tangent of this angle,
00:06:01.340 --> 00:06:02.720
theta right over here,
00:06:02.720 --> 00:06:05.790
should be equal to, and I'll
do approximately equal to
00:06:05.790 --> 00:06:07.810
since we're using these approximations,
00:06:07.810 --> 00:06:11.280
our change in y over our change in x.
00:06:11.280 --> 00:06:12.190
So negative 1.90
00:06:14.020 --> 00:06:17.920
over negative 5.44,
00:06:17.920 --> 00:06:20.070
or we could say that theta
00:06:20.070 --> 00:06:24.640
is going to be approximately
equal to the inverse tangent
00:06:24.640 --> 00:06:26.150
of negative 1.90
00:06:29.100 --> 00:06:33.980
over negative 5.44.
00:06:33.980 --> 00:06:35.500
And we're gonna see in a second
00:06:35.500 --> 00:06:37.560
whether this is actually
going to get us the answer
00:06:37.560 --> 00:06:38.393
that we want.
00:06:38.393 --> 00:06:39.890
So let's try this out.
00:06:39.890 --> 00:06:44.210
If we were to take 1.9 negative
00:06:44.210 --> 00:06:48.270
divided by 5.44 negative,
00:06:48.270 --> 00:06:49.770
that gets us that, which makes sense.
00:06:49.770 --> 00:06:52.100
Negative divided by a
negative is a positive.
00:06:52.100 --> 00:06:55.490
And now let's try to take
the inverse tangent of that.
00:06:55.490 --> 00:06:59.290
So here I press second, and
then I'll do inverse tangent.
00:06:59.290 --> 00:07:00.123
So I'm getting
00:07:00.123 --> 00:07:04.740
19.25 degrees, approximately.
00:07:04.740 --> 00:07:05.650
So this is saying
00:07:05.650 --> 00:07:10.420
that this is approximately 19.25 degrees.
00:07:10.420 --> 00:07:13.263
And my question to you
is, does that seem right?
00:07:14.490 --> 00:07:18.030
Well, 19.25 degrees would
put us in the first quadrant.
00:07:18.030 --> 00:07:19.070
It would get us a vector
00:07:19.070 --> 00:07:22.630
that looks something like this.
00:07:22.630 --> 00:07:26.630
This would be 19.25 degrees.
00:07:26.630 --> 00:07:28.680
But clearly, that's not the
vector we're talking about.
00:07:28.680 --> 00:07:31.120
We're talking about a vector
in the third quadrant.
00:07:31.120 --> 00:07:33.190
And the reason why we got this result,
00:07:33.190 --> 00:07:34.900
is that when you take the inverse tangent
00:07:34.900 --> 00:07:36.290
on most calculators,
00:07:36.290 --> 00:07:37.920
it's going to give you an angle
00:07:37.920 --> 00:07:39.840
that's between negative 90 degrees
00:07:39.840 --> 00:07:41.690
and positive 90 degrees.
00:07:41.690 --> 00:07:43.300
While here we are at an angle
00:07:43.300 --> 00:07:45.370
that puts us out in the third quadrant.
00:07:45.370 --> 00:07:46.870
So we have to adjust.
00:07:46.870 --> 00:07:51.060
And to adjust here, we just
have to add 180 degrees
00:07:51.060 --> 00:07:54.580
to get to the actual angle
that we are talking about.
00:07:54.580 --> 00:07:57.920
So in our situation, the magnitude here
00:07:57.920 --> 00:08:01.200
is going to be approximately 5.76
00:08:03.690 --> 00:08:07.010
and then the direction is going to be
00:08:07.010 --> 00:08:12.010
approximately 19.25 plus 180 degrees,
00:08:12.100 --> 00:08:14.970
which is going to be 199.25 degrees.
00:08:17.820 --> 00:08:19.423
And now we are done.
|
Parallelogram rule for vector addition | https://www.youtube.com/watch?v=Mep0foZMOCg | vtt | https://www.youtube.com/api/timedtext?v=Mep0foZMOCg&ei=5VWUZZ3HK_rYmLAPqeS6gAM&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=909F66E4B5BC31E27D0153AD4C9E49B1D84FDAD8.88D61B6A8F178DC74003C76537ACF7CF5AB14CC4&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.110 --> 00:00:01.460
- [Instructor] So we
have two vectors here,
00:00:01.460 --> 00:00:03.280
vector A and vector B.
00:00:03.280 --> 00:00:05.110
And what we're gonna do in this video
00:00:05.110 --> 00:00:08.480
is think about what it
means to add vectors.
00:00:08.480 --> 00:00:10.180
So for example, how could we think
00:00:10.180 --> 00:00:12.960
about what does it mean to take vector A
00:00:12.960 --> 00:00:15.630
and add to that vector B.
00:00:15.630 --> 00:00:19.265
And as we'll see, we'll
get another third vector.
00:00:19.265 --> 00:00:23.490
And there's two ways that we
can think about this visually.
00:00:23.490 --> 00:00:25.520
One way is to say, all right,
00:00:25.520 --> 00:00:30.120
if we want start with vector
A and then add vector B to it,
00:00:30.120 --> 00:00:33.440
what we can do, let me
take a copy of vector B
00:00:33.440 --> 00:00:36.970
and put its tail right
at the head of vector A.
00:00:36.970 --> 00:00:38.810
Notice I have not changed the magnitude
00:00:38.810 --> 00:00:40.650
or the direction of vector B.
00:00:40.650 --> 00:00:43.850
If I did, I would actually
be changing the vector.
00:00:43.850 --> 00:00:47.270
And when I do it like that,
this defines a third vector
00:00:47.270 --> 00:00:49.680
which can be use the sum of a plus B.
00:00:49.680 --> 00:00:54.010
And the sum is going to
start at the tail of vector A
00:00:54.010 --> 00:00:57.240
and end at the head of vector B here.
00:00:57.240 --> 00:00:58.200
So let me draw that.
00:00:58.200 --> 00:01:00.680
So it would look something like that.
00:01:00.680 --> 00:01:03.360
And we can call this
right over here, vector C.
00:01:03.360 --> 00:01:08.360
So we could say A plus
B is equal to vector C.
00:01:08.450 --> 00:01:09.970
Now we could have also thought about it
00:01:09.970 --> 00:01:11.540
the other way around.
00:01:11.540 --> 00:01:15.010
We could have said,
let's start with vector B
00:01:15.010 --> 00:01:19.430
and then add vector A to that.
00:01:19.430 --> 00:01:22.220
So I'll start with the tail of vector B
00:01:22.220 --> 00:01:25.070
and then at the head of vector
B, I'm going to put the tail
00:01:25.070 --> 00:01:26.250
of vector A.
00:01:26.250 --> 00:01:29.800
So it could look something like that.
00:01:29.800 --> 00:01:33.490
And then once again, the sum
is going to have its tail
00:01:33.490 --> 00:01:34.830
at our starting point here
00:01:34.830 --> 00:01:37.440
and its head at our finishing point.
00:01:37.440 --> 00:01:39.780
Now, another way of thinking about it is
00:01:39.780 --> 00:01:42.460
we've just constructed a parallelogram
00:01:42.460 --> 00:01:45.490
with these two vectors by putting both
00:01:45.490 --> 00:01:48.450
of their tails together,
and then by taking a copy
00:01:48.450 --> 00:01:51.420
of each of them and
putting that copy's tail
00:01:51.420 --> 00:01:53.240
at the head of the other vector,
00:01:53.240 --> 00:01:55.400
you construct a parallelogram like this,
00:01:55.400 --> 00:01:57.830
and then the sum is
going to be the diagonal
00:01:57.830 --> 00:01:59.440
of the parallelogram.
00:01:59.440 --> 00:02:02.900
But hopefully you appreciate
this is the same exact idea.
00:02:02.900 --> 00:02:05.422
If you just add by
putting the head to tail
00:02:05.422 --> 00:02:08.220
of the two vectors and
you construct a triangle,
00:02:08.220 --> 00:02:10.470
the parallelogram just helps us appreciate
00:02:10.470 --> 00:02:12.140
that you can start with the yellow vector
00:02:12.140 --> 00:02:15.090
and then the blue vector
or the blue vector first
00:02:15.090 --> 00:02:16.290
and then the yellow vector.
00:02:16.290 --> 00:02:19.353
But either way, the sum is
going to be this vector C.
|
Cosine equation solution set in an interval | https://www.youtube.com/watch?v=0_4uTKBI99o | vtt | https://www.youtube.com/api/timedtext?v=0_4uTKBI99o&ei=5VWUZfn5I-qsp-oPg9S_2Aw&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=4E59D7B2C9985D95321C4CFC323EC61011B4938F.67582CD09F5A4B7726EEBE78549D247F86397248&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.123 --> 00:00:02.550
- [Instructor] In a previous
video, we established
00:00:02.550 --> 00:00:05.850
the entire solution set
for the following equation.
00:00:05.850 --> 00:00:09.840
And we saw that all the x's
that can satisfy this equation
00:00:09.840 --> 00:00:14.150
are a combination of these
x's and these x's here.
00:00:14.150 --> 00:00:16.350
The reason why I'm
referring to each of them
00:00:17.721 --> 00:00:21.390
as numerous xs is that for
any integer value of n,
00:00:21.390 --> 00:00:22.950
you'll get another solution.
00:00:22.950 --> 00:00:26.480
For any integer value of n,
you'll get another solution.
00:00:26.480 --> 00:00:27.860
What I wanna do in this video
00:00:27.860 --> 00:00:30.800
is to make things a
little bit more concrete.
00:00:30.800 --> 00:00:33.450
And the way that we're going
to do it is by exploring
00:00:33.450 --> 00:00:37.610
all of the x values that
satisfy this equation
00:00:37.610 --> 00:00:40.120
that sit in the closed interval
00:00:40.120 --> 00:00:44.400
from negative pi over two to zero.
00:00:44.400 --> 00:00:46.030
So I encourage you like always,
00:00:46.030 --> 00:00:48.730
pause this video and have
a go at it by yourself
00:00:48.730 --> 00:00:51.210
before we work through it together.
00:00:51.210 --> 00:00:54.240
All right, now let's work
through this together.
00:00:54.240 --> 00:00:56.330
So the first helpful thing is
00:00:56.330 --> 00:00:58.500
we have these algebraic expressions.
00:00:58.500 --> 00:01:00.720
We have things written in terms of pi.
00:01:00.720 --> 00:01:04.530
Let's approximate them
all in terms of decimals.
00:01:04.530 --> 00:01:07.950
So even pi over two, we
can approximate that.
00:01:07.950 --> 00:01:10.570
Let's see, if pi is approximately 3.14,
00:01:11.968 --> 00:01:14.363
half of that is approximately 1.57,
00:01:15.420 --> 00:01:17.030
so we could say this is approximately
00:01:17.030 --> 00:01:22.030
the closed interval from -1.57 to zero.
00:01:24.160 --> 00:01:26.790
- 1.57 isn't exactly negative pi over two,
00:01:26.790 --> 00:01:28.550
but it'll hopefully be suitable
00:01:28.550 --> 00:01:31.040
for what we're trying to do here.
00:01:31.040 --> 00:01:32.710
And now let's see if we can write
00:01:32.710 --> 00:01:34.500
the different parts of these expressions,
00:01:34.500 --> 00:01:37.600
or at least approximate them as decimals.
00:01:37.600 --> 00:01:41.060
So this could be rewritten
as x is approximately,
00:01:41.060 --> 00:01:44.210
if you were to take 1/8
times the inverse cosine
00:01:44.210 --> 00:01:46.720
of -1/6, I encourage you to verify this
00:01:46.720 --> 00:01:48.380
on your own on a calculator,
00:01:48.380 --> 00:01:51.003
you would get that that's
approximately 0.22.
00:01:53.000 --> 00:01:57.153
And then pi over four
is approximately 0.785.
00:02:00.810 --> 00:02:04.940
So this expression would
be approximately 0.22
00:02:04.940 --> 00:02:09.940
minus 0.785 times n,
00:02:11.480 --> 00:02:13.140
where n could be any integer.
00:02:13.140 --> 00:02:15.330
And then this one over here on the right,
00:02:15.330 --> 00:02:18.960
let me do that in this yellow,
x could be approximately
00:02:18.960 --> 00:02:23.960
equal to, well if this
evaluates to approximately 0.22,
00:02:25.480 --> 00:02:26.910
then this is just the negative of it,
00:02:26.910 --> 00:02:30.630
so it's going to be -0.22.
00:02:30.630 --> 00:02:33.570
And then it's plus what approximately
00:02:33.570 --> 00:02:36.993
pi over four is, so 0.785n.
00:02:39.970 --> 00:02:42.660
And now what we could do
is just try different n's
00:02:42.660 --> 00:02:45.170
and see if we're starting
above or below this interval,
00:02:45.170 --> 00:02:47.220
and then see which of
the x values actually
00:02:47.220 --> 00:02:49.230
fall in this interval.
00:02:49.230 --> 00:02:50.860
So let's just start here.
00:02:50.860 --> 00:02:53.620
If we just start at n equals zero,
00:02:53.620 --> 00:02:56.210
actually why don't I set
up a little table here,
00:02:56.210 --> 00:02:59.730
we have n here and if we
have the x value here,
00:02:59.730 --> 00:03:03.320
when n is zero, well, then
you don't see this term,
00:03:03.320 --> 00:03:06.663
and you just get approximately 0.22.
00:03:08.920 --> 00:03:11.020
Now let's compare that to the interval.
00:03:11.020 --> 00:03:13.070
The upper bound of that interval is zero.
00:03:13.070 --> 00:03:14.710
So this does not sit in the interval.
00:03:14.710 --> 00:03:18.980
So this is too high and we would want to
00:03:18.980 --> 00:03:20.610
define the x's that sit in the interval.
00:03:20.610 --> 00:03:22.470
We wanna find lower values.
00:03:22.470 --> 00:03:26.740
So it's good that here, where
you're subtracting 0.785,
00:03:26.740 --> 00:03:29.490
so I would use positive
integer values of n
00:03:29.490 --> 00:03:32.930
to decrease this 0.22 here.
00:03:32.930 --> 00:03:37.690
So when n equals one, we would
subtract 0.785 from that,
00:03:37.690 --> 00:03:39.800
and I'll round all of these
to the hundredths place,
00:03:39.800 --> 00:03:44.213
and that would get us to -0.57,
00:03:45.860 --> 00:03:47.910
and that does sit in the interval.
00:03:47.910 --> 00:03:48.840
So this looks good.
00:03:48.840 --> 00:03:50.340
So this would be a solution
00:03:50.340 --> 00:03:52.770
in that interval right over here.
00:03:52.770 --> 00:03:54.580
And let's try n equals two.
00:03:54.580 --> 00:03:58.070
So we would subtract 0.785 again,
00:03:58.070 --> 00:04:01.273
and that would get us to -1.35,
00:04:05.130 --> 00:04:09.640
not 25, 35, and that also
00:04:09.640 --> 00:04:10.740
sits in the interval.
00:04:10.740 --> 00:04:14.410
It's larger than -1.57,
so that looks good.
00:04:14.410 --> 00:04:19.030
Let's subtract 0.785
again, when n equals three,
00:04:19.030 --> 00:04:22.790
that would get us -2.14.
00:04:22.790 --> 00:04:24.440
Well, that's all of a
sudden out of the interval
00:04:24.440 --> 00:04:26.860
because that's below the lower bound here.
00:04:26.860 --> 00:04:29.690
So this is too low.
00:04:29.690 --> 00:04:33.350
So using this expression,
we've been able to find
00:04:33.350 --> 00:04:38.000
two x values that sit in the
interval that we care about.
00:04:38.000 --> 00:04:41.870
Now let's use these x
values right over here
00:04:41.870 --> 00:04:44.150
and I'll set up another table.
00:04:44.150 --> 00:04:47.750
So, let's see we have our n
and then we have our x values.
00:04:47.750 --> 00:04:50.370
So let's start with n equals
zero 'cause that's easy
00:04:50.370 --> 00:04:52.160
to compute, and then
this term would go away,
00:04:52.160 --> 00:04:56.560
and we'd have -0.22, and that's actually
00:04:56.560 --> 00:04:58.370
in this interval here, it's below zero,
00:04:58.370 --> 00:05:02.660
it's larger than -1.57,
so that one checks out.
00:05:02.660 --> 00:05:05.880
But now to really explore, we
have to go in both directions.
00:05:05.880 --> 00:05:08.610
We have to increase it or decrease it.
00:05:08.610 --> 00:05:10.110
So if we wanted to increase it,
00:05:10.110 --> 00:05:12.760
we could have a situation
where n equals one.
00:05:12.760 --> 00:05:16.740
So if n equals one, we're
gonna add 0.785 to this.
00:05:16.740 --> 00:05:18.290
Now you immediately know
that that's going to be
00:05:18.290 --> 00:05:22.130
a positive value, if you
computed it, it'd be 0.57,
00:05:22.130 --> 00:05:26.600
which is larger than
zero, so this is too high.
00:05:26.600 --> 00:05:30.180
So now we could try going lower than -0.22
00:05:30.180 --> 00:05:32.500
by having negative values of n.
00:05:32.500 --> 00:05:37.060
So if n is equal to -1, that
means we're subtracting 0.785
00:05:37.060 --> 00:05:41.653
from this right over here
which would get us to -1.01.
00:05:44.870 --> 00:05:47.780
Well, that one works out,
so that's in our interval.
00:05:47.780 --> 00:05:50.570
And now let's subtract 0.785 again.
00:05:50.570 --> 00:05:53.020
So I'll have n equals -2.
00:05:53.020 --> 00:05:57.410
And so if I subtract 0.785 again,
00:05:57.410 --> 00:06:01.413
I could round that to -1.79,
00:06:02.270 --> 00:06:04.640
which is lower than -1.57,
00:06:04.640 --> 00:06:08.200
so it's out of our
interval, so it's too low.
00:06:08.200 --> 00:06:11.050
So all of the x values
that are in our interval
00:06:11.050 --> 00:06:15.020
that satisfy this equation
are these two right over here.
00:06:15.020 --> 00:06:19.410
And this one and this one,
00:06:19.410 --> 00:06:20.923
and we are done.
|
Cosine equation algebraic solution set | https://www.youtube.com/watch?v=JoOfBpdaAiw | vtt | https://www.youtube.com/api/timedtext?v=JoOfBpdaAiw&ei=5VWUZbb9M-2ghcIPut6P-AU&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=E8EA65FAE1E101774497F5A095EFAC72BEF49979.D6A7FABA5E8E03CE622DEB80E48175490BFA638C&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.380 --> 00:00:01.470
- [Lecturer] The goal of this video
00:00:01.470 --> 00:00:04.740
is to find the solution set
for the following equation,
00:00:04.740 --> 00:00:06.760
negative six times the cosine
00:00:06.760 --> 00:00:10.640
of 8x plus four is equal to five.
00:00:10.640 --> 00:00:12.720
And like always, I encourage
you to pause this video
00:00:12.720 --> 00:00:14.380
and see if you can have a go at this
00:00:14.380 --> 00:00:15.370
before we do it together.
00:00:15.370 --> 00:00:18.680
And a reminder, we want
the entire solution set,
00:00:18.680 --> 00:00:20.123
not just one solution.
00:00:21.110 --> 00:00:23.210
All right, now let's work
through this together.
00:00:23.210 --> 00:00:24.780
Some of you might recognize
00:00:24.780 --> 00:00:29.030
that it would be valuable
to isolate the cosine of 8x,
00:00:29.030 --> 00:00:30.530
and a good way of doing that
00:00:30.530 --> 00:00:33.820
would be, first, to subtract
four from both sides,
00:00:33.820 --> 00:00:35.560
and then that would get us
00:00:35.560 --> 00:00:39.600
negative six times cosine of 8x,
00:00:39.600 --> 00:00:41.080
I subtracted four from the left,
00:00:41.080 --> 00:00:42.620
so that four is going to be gone,
00:00:42.620 --> 00:00:45.720
and then if I subtract four from the five,
00:00:45.720 --> 00:00:47.630
I am going to get a one there.
00:00:47.630 --> 00:00:50.700
And now I can multiply both sides
00:00:50.700 --> 00:00:55.700
of this equation by negative 1/6,
00:00:56.550 --> 00:00:59.040
I just wanna have a one
in front of the cosine,
00:00:59.040 --> 00:01:01.080
so negative 1/6.
00:01:01.080 --> 00:01:03.010
And so this is going to be one,
00:01:03.010 --> 00:01:06.390
so I'm just gonna have cosine of 8x
00:01:07.560 --> 00:01:10.660
is equal to negative 1/6.
00:01:10.660 --> 00:01:12.290
Now, if I just keep going,
00:01:12.290 --> 00:01:15.220
I could take the inverse
cosine of negative 1/6,
00:01:15.220 --> 00:01:17.160
and whatever that is divided by eight,
00:01:17.160 --> 00:01:19.010
I would get a solution,
00:01:19.010 --> 00:01:20.710
but this is a good time to pause
00:01:20.710 --> 00:01:24.370
and to make sure that we are
capturing all of the solutions.
00:01:24.370 --> 00:01:26.600
And I'll give us, or
I'll refresh our memories
00:01:26.600 --> 00:01:28.910
with some identities.
00:01:28.910 --> 00:01:30.130
And to help with these identities,
00:01:30.130 --> 00:01:33.023
I like to draw a quick unit circle.
00:01:34.270 --> 00:01:38.600
So this is our x-axis, this is our y-axis,
00:01:38.600 --> 00:01:43.310
and so my quick hand-drawn unit circle
00:01:45.250 --> 00:01:47.140
might look something like this, (laughing)
00:01:47.140 --> 00:01:49.020
it's not that nice looking,
00:01:49.020 --> 00:01:51.240
but we wanna think about all of the angles
00:01:51.240 --> 00:01:54.360
that when I take the cosine,
I get to negative 1/6.
00:01:54.360 --> 00:01:59.360
So negative 1/6 might be
something like right over here.
00:01:59.400 --> 00:02:02.760
And so you can see that
there might be an angle
00:02:02.760 --> 00:02:04.810
like this that would get us there,
00:02:04.810 --> 00:02:07.140
so let me draw that, draw the radius.
00:02:07.140 --> 00:02:11.610
We know the cosine of an
angle is the x-coordinate
00:02:11.610 --> 00:02:15.210
of where that radius that's
defined by that angle,
00:02:15.210 --> 00:02:17.710
where that radius
intersects the unit circle.
00:02:17.710 --> 00:02:19.790
But we also see there's another place,
00:02:19.790 --> 00:02:23.010
if we essentially take the
negative of that angle,
00:02:23.010 --> 00:02:25.420
we could go right over here
00:02:25.420 --> 00:02:27.490
and we would also get the same cosine.
00:02:27.490 --> 00:02:30.060
So we could go to the negative
of the angle, go that way.
00:02:30.060 --> 00:02:31.430
And that's where we get the identity
00:02:31.430 --> 00:02:34.040
that cosine of negative theta
00:02:34.040 --> 00:02:37.450
is equal to cosine of theta.
00:02:37.450 --> 00:02:39.480
And so if cosine of 8x
00:02:39.480 --> 00:02:41.400
is equal to negative 1/6,
00:02:41.400 --> 00:02:43.550
using this identity, we also know
00:02:43.550 --> 00:02:45.760
that cosine of the negative of this
00:02:45.760 --> 00:02:48.480
will also be equal to negative 1/6.
00:02:48.480 --> 00:02:49.530
So let me write that down,
00:02:49.530 --> 00:02:51.690
cosine of negative 8x
00:02:52.650 --> 00:02:55.723
is also going to be equal to negative 1/6.
00:02:56.700 --> 00:02:59.730
Now, already we have
expanded our solution set
00:02:59.730 --> 00:03:02.560
because this is going to
give us another x-value
00:03:02.560 --> 00:03:05.370
that's going to get us
the result that we want,
00:03:05.370 --> 00:03:06.720
but are we done?
00:03:06.720 --> 00:03:09.290
Well, the other thing to realize is,
00:03:09.290 --> 00:03:11.680
let's say I have some angle here,
00:03:11.680 --> 00:03:15.770
where if I take the cosine,
I get to negative 1/6,
00:03:15.770 --> 00:03:17.750
but then if I had two pi again,
00:03:17.750 --> 00:03:19.000
I'm gonna get to the same place,
00:03:19.000 --> 00:03:21.480
and the cosine is, once again,
going to be negative 1/6,
00:03:21.480 --> 00:03:23.260
and I could add two pi again,
00:03:23.260 --> 00:03:24.940
I could essentially add two pi
00:03:24.940 --> 00:03:27.820
an arbitrary integer number of times.
00:03:27.820 --> 00:03:32.340
So I could rewrite this
right over here as cosine,
00:03:32.340 --> 00:03:33.530
instead of just 8x,
00:03:33.530 --> 00:03:38.120
it's 8x plus an integer
multiple of two pi,
00:03:38.120 --> 00:03:41.270
that's also going to be
equal to negative 1/6.
00:03:41.270 --> 00:03:43.820
And similarly for negative 8x,
00:03:43.820 --> 00:03:48.060
I could say cosine of negative 8x
00:03:48.060 --> 00:03:50.670
plus an integer multiple of two pi,
00:03:50.670 --> 00:03:54.620
and is going to be some integer
in both of these situations,
00:03:54.620 --> 00:03:57.550
that's also going to
get us to negative 1/6.
00:03:57.550 --> 00:03:59.130
And so now we can feel pretty good
00:03:59.130 --> 00:04:00.820
that we're capturing all of the solutions
00:04:00.820 --> 00:04:02.380
when we solve for x.
00:04:02.380 --> 00:04:03.213
So in both of these,
00:04:03.213 --> 00:04:05.630
now let's take the inverse
cosine of negative 1/6
00:04:05.630 --> 00:04:08.420
in order to solve for x here.
00:04:08.420 --> 00:04:12.090
So if we were to take the
inverse cosine of both sides,
00:04:12.090 --> 00:04:15.370
we could get that 8x plus two pi
00:04:15.370 --> 00:04:17.750
times some arbitrary integer n
00:04:17.750 --> 00:04:22.553
is equal to the inverse
cosine of negative 1/6.
00:04:23.640 --> 00:04:25.560
And then now let's solve for x,
00:04:25.560 --> 00:04:28.770
we can subtract two pi n from both sides.
00:04:28.770 --> 00:04:33.770
So we could get 8x is
equal to the inverse cosine
00:04:33.920 --> 00:04:38.920
of negative 1/6 minus two pi n.
00:04:39.270 --> 00:04:40.330
Now, it's interesting to note
00:04:40.330 --> 00:04:42.300
that the sign on this two pi n term
00:04:42.300 --> 00:04:43.730
actually doesn't matter so much,
00:04:43.730 --> 00:04:45.560
'cause n could be a negative integer,
00:04:45.560 --> 00:04:48.420
but I'll just stick with
this negative two pi n.
00:04:48.420 --> 00:04:50.390
And so if we wanted to solve for x,
00:04:50.390 --> 00:04:52.410
we'd just divide both sides by eight,
00:04:52.410 --> 00:04:55.650
we get x is equal to 1/8
00:04:55.650 --> 00:04:59.890
times the inverse cosine of negative 1/6
00:04:59.890 --> 00:05:04.890
minus pi over four n.
00:05:05.080 --> 00:05:07.060
And now we can do the exact same thing
00:05:07.060 --> 00:05:10.690
in the other scenario, I'll
call this the yellow scenario,
00:05:10.690 --> 00:05:12.070
where if I take the inverse cosine,
00:05:12.070 --> 00:05:15.940
I get negative 8x plus two pi,
00:05:15.940 --> 00:05:20.073
n is equal to the inverse
cosine of negative 1/6.
00:05:21.060 --> 00:05:24.320
And now I can subtract
two pi n from both sides,
00:05:24.320 --> 00:05:25.570
so I get negative 8x
00:05:26.590 --> 00:05:31.550
is equal to inverse cosine of negative 1/6
00:05:31.550 --> 00:05:34.330
minus two pi n.
00:05:34.330 --> 00:05:36.550
Now I can multiply both
sides by negative 1/8,
00:05:36.550 --> 00:05:38.560
or divide both sides by negative eight,
00:05:38.560 --> 00:05:42.010
and I get x is equal to negative 1/8
00:05:42.010 --> 00:05:45.380
times the inverse cosine of negative 1/6
00:05:46.740 --> 00:05:50.303
plus pi over four n.
00:05:51.410 --> 00:05:53.660
So I will stop here for this video,
00:05:53.660 --> 00:05:56.610
where at least algebraically
we know the solution set,
00:05:56.610 --> 00:05:58.460
and this is the complete solution set
00:06:01.447 --> 00:06:04.220
if you take the combination
of both of these expressions.
00:06:04.220 --> 00:06:07.600
In a future video, we'll
evaluate this with a calculator,
00:06:07.600 --> 00:06:09.790
and we'll think about the solutions
00:06:09.790 --> 00:06:12.083
that fit within a given interval.
|
Proof of the tangent angle sum and difference identities | https://www.youtube.com/watch?v=nUlElr4LXz8 | vtt | https://www.youtube.com/api/timedtext?v=nUlElr4LXz8&ei=5VWUZai1I8G3mLAPjc6c-AE&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=B17B03BB3571EF337543E1ECDB42AF7458E21A95.CCD27137E0EA781423BAF430267B76A48C42C10A&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.150 --> 00:00:01.300
- [Instructor] In this
video I'm going to assume
00:00:01.300 --> 00:00:02.550
that you already know a few things
00:00:02.550 --> 00:00:03.383
and we've covered this.
00:00:03.383 --> 00:00:04.690
We've proved this in other videos
00:00:04.690 --> 00:00:08.810
that sine of x plus y is
equal to sine of x cosine y
00:00:08.810 --> 00:00:11.020
plus and then you swap
the cosines and the sines,
00:00:11.020 --> 00:00:13.430
cosine of x sine y,
00:00:13.430 --> 00:00:18.430
and then cosine of x plus y
is equal to cosine x cosine y
00:00:18.620 --> 00:00:20.770
minus sine x sin y.
00:00:20.770 --> 00:00:23.150
Once again, we've proven
this in this in other videos
00:00:23.150 --> 00:00:25.820
and then there's some other
properties we know of cosine
00:00:25.820 --> 00:00:27.610
and sine that we have
looked at another video's.
00:00:27.610 --> 00:00:30.972
Cosine of -x is equal to cosine of x
00:00:30.972 --> 00:00:35.450
and that sine of negative
x is equal to -sine of x.
00:00:35.450 --> 00:00:36.380
And that of course,
00:00:36.380 --> 00:00:38.540
the tangent of something is defined
00:00:38.540 --> 00:00:42.320
as a sine over cosine of that something.
00:00:42.320 --> 00:00:43.510
Now with that out of the way,
00:00:43.510 --> 00:00:44.980
I wanna come up with a formula
00:00:44.980 --> 00:00:48.380
for tangent of x plus y expressed just
00:00:48.380 --> 00:00:52.560
in terms of tangent of x and tangent of y.
00:00:52.560 --> 00:00:54.180
You can view it as the antilog
00:00:54.180 --> 00:00:56.663
for what we did up here
for sine and cosine.
00:00:57.690 --> 00:00:59.850
Well, the immediate thing
that you might recognize
00:00:59.850 --> 00:01:03.060
is that tangent of x plus
y based on the definition
00:01:03.060 --> 00:01:08.060
of tangent is the same
thing as sine of x plus y
00:01:08.210 --> 00:01:12.630
over cosine of x plus y.
00:01:12.630 --> 00:01:15.130
And what's that going to be equal to?
00:01:15.130 --> 00:01:17.350
Well, we know that sine of x plus y
00:01:17.350 --> 00:01:19.610
can be expressed this way.
00:01:19.610 --> 00:01:21.540
So let me write that down.
00:01:21.540 --> 00:01:26.447
So that's going to be sine of x cosine y
00:01:27.880 --> 00:01:32.120
plus cosine of x sine of y.
00:01:34.510 --> 00:01:36.230
And then, and actually,
00:01:36.230 --> 00:01:37.970
so that we can save a
little bit of writing,
00:01:37.970 --> 00:01:40.240
I'm gonna awkwardly write,
00:01:40.240 --> 00:01:42.400
make the line down here,
00:01:42.400 --> 00:01:44.990
because we're gonna put
something here in a second,
00:01:44.990 --> 00:01:46.100
but I think you'll get the idea.
00:01:46.100 --> 00:01:49.140
So there's going to be that
over cosine of x plus y
00:01:49.140 --> 00:01:52.060
which is this expression when
you just express it in terms
00:01:52.060 --> 00:01:55.620
of cosines of x and
cosines of y and sines of x
00:01:55.620 --> 00:01:56.550
and sines of y.
00:01:56.550 --> 00:01:57.720
So let me write it here.
00:01:57.720 --> 00:02:02.720
So you're gonna have cosine
of x cosine y minus sine of x,
00:02:07.100 --> 00:02:10.780
and then sine y.
00:02:10.780 --> 00:02:14.100
Now we wanna express
everything in terms of tangents
00:02:14.100 --> 00:02:16.080
of xs and ys.
00:02:16.080 --> 00:02:18.530
And so it might make sense here to say,
00:02:18.530 --> 00:02:22.410
all right, well, we know
tangent is sine over cosine.
00:02:22.410 --> 00:02:24.990
So what if we were to
divide both the numerator
00:02:24.990 --> 00:02:27.970
and the denominator by some
expression that can start
00:02:27.970 --> 00:02:30.110
to make the numerator
and denominator express
00:02:30.110 --> 00:02:31.700
in terms of tangents.
00:02:31.700 --> 00:02:33.950
And I will cut a little
bit to the chase here.
00:02:33.950 --> 00:02:35.400
So in the numerator,
00:02:35.400 --> 00:02:37.450
what I can do is,
00:02:37.450 --> 00:02:38.990
and I'm gonna do this
just in the numerator,
00:02:38.990 --> 00:02:40.920
and then I'm gonna do it
in the denominator as well.
00:02:40.920 --> 00:02:44.213
I'm gonna divide the numerator
by cosine of x cosine y.
00:02:47.780 --> 00:02:49.990
And of course, I can't
just divide the numerator
00:02:49.990 --> 00:02:51.570
by cosine of x cosine of y
00:02:51.570 --> 00:02:53.330
that would change the value of the,
00:02:53.330 --> 00:02:54.515
this rational expression.
00:02:54.515 --> 00:02:56.400
I have to do that to
the denominator as well.
00:02:56.400 --> 00:02:58.830
So I know this is a very
complex looking fraction here
00:02:58.830 --> 00:03:00.510
but it's going to simplify in a second.
00:03:00.510 --> 00:03:02.020
So I'm also going to
divide the denominator
00:03:02.020 --> 00:03:06.180
by cosine of x cosine of y.
00:03:06.180 --> 00:03:08.550
And now let's see if we can simplify this
00:03:08.550 --> 00:03:10.520
in certain ways.
00:03:10.520 --> 00:03:13.860
In the numerator, we can see
that this cosine y cancels
00:03:13.860 --> 00:03:15.340
with this cosine y.
00:03:15.340 --> 00:03:17.230
And so that first term becomes slightly
00:03:17.230 --> 00:03:18.220
in another color here.
00:03:18.220 --> 00:03:21.810
So this sine of x over cosine of x.
00:03:21.810 --> 00:03:23.200
And so the numerator,
00:03:23.200 --> 00:03:26.140
I can say this is going
to be equal to sine of x
00:03:26.140 --> 00:03:30.200
over cosine of x is tangent of x.
00:03:30.200 --> 00:03:32.490
And then the second term here,
00:03:32.490 --> 00:03:35.540
we can see that this cosine of x cancels
00:03:35.540 --> 00:03:36.960
with this cosine of x .
00:03:36.960 --> 00:03:41.120
So we're left with sine
of y over cosine of y,
00:03:41.120 --> 00:03:42.130
which is of course,
00:03:42.130 --> 00:03:43.620
tangent of y.
00:03:43.620 --> 00:03:47.500
So plus tangent of y
00:03:47.500 --> 00:03:49.860
and then all of that is going to be over,
00:03:49.860 --> 00:03:52.680
now we can look at the denominator.
00:03:52.680 --> 00:03:55.570
So this first term here,
00:03:55.570 --> 00:03:59.610
we can see the cosine of x
cancels with the cosine of x
00:03:59.610 --> 00:04:03.380
and the cosine of y cancels
out with the cosine of y.
00:04:03.380 --> 00:04:05.920
So you could view this first
term here when you divide
00:04:05.920 --> 00:04:08.130
by this cosine of x cosine y,
00:04:08.130 --> 00:04:10.400
it just becomes one
00:04:10.400 --> 00:04:13.240
and then we're going to have the minus.
00:04:13.240 --> 00:04:15.850
And now this second term is interesting.
00:04:15.850 --> 00:04:19.090
We have sine of x over cosine of x,
00:04:19.090 --> 00:04:20.523
sine of y over cosine of y.
00:04:21.569 --> 00:04:24.800
So sine of x over cosine of x
00:04:24.800 --> 00:04:26.910
that over there is tangent of x,
00:04:26.910 --> 00:04:31.850
and then sine of y over
cosine of y its tangent of y.
00:04:31.850 --> 00:04:36.850
So this is going to be tangent
of x times tangent of y.
00:04:38.850 --> 00:04:39.710
And just like that,
00:04:39.710 --> 00:04:41.190
we have come up with an expression
00:04:41.190 --> 00:04:44.550
for tangent of x plus y that just deals
00:04:44.550 --> 00:04:48.400
with tangent of xs and tangent of ys.
00:04:48.400 --> 00:04:49.840
Now the next question you might say,
00:04:49.840 --> 00:04:52.950
well, all right, that's
great for tangent of x plus y
00:04:52.950 --> 00:04:57.950
but what about tangent of x minus y?
00:04:58.250 --> 00:05:00.830
Well, here we just have
to recognize a little bit
00:05:00.830 --> 00:05:02.690
of what we've seen before.
00:05:02.690 --> 00:05:03.730
Let me write it over here.
00:05:03.730 --> 00:05:08.670
Tangent of -x is equal to sine of -x
00:05:10.790 --> 00:05:13.830
over cosine of negative x
00:05:13.830 --> 00:05:15.990
and what's that going to be equal to?
00:05:15.990 --> 00:05:17.600
And I know I'm running out of space.
00:05:17.600 --> 00:05:20.120
This is going to be equal to
sine of -x is the same thing
00:05:20.120 --> 00:05:24.360
as -sine of x, -sine of x,
00:05:24.360 --> 00:05:27.163
and then cosine of -x is just cosine of x.
00:05:28.490 --> 00:05:32.350
Well, this is just the
negative of the tangent of x.
00:05:32.350 --> 00:05:37.340
So this is negative tangent of x.
00:05:37.340 --> 00:05:40.460
And the reason why that is useful
00:05:40.460 --> 00:05:43.020
is I can rewrite this as being,
00:05:43.020 --> 00:05:43.853
write here.
00:05:43.853 --> 00:05:48.710
This is the same thing
as tangent of x plus -y.
00:05:50.950 --> 00:05:52.740
So everywhere we saw a y here,
00:05:52.740 --> 00:05:54.410
we can replace it with a -y.
00:05:54.410 --> 00:05:59.407
So this is going to be
equal to tangent of x
00:06:00.500 --> 00:06:05.500
plus the tangent of -y,
00:06:05.510 --> 00:06:10.510
all of that over 1 minus the tangent of x
00:06:11.900 --> 00:06:14.313
times the tangent of -y.
00:06:15.520 --> 00:06:16.900
Well, we know the tangent of -y
00:06:16.900 --> 00:06:21.900
is the same thing as the
negative tangent of y.
00:06:21.950 --> 00:06:24.070
And we know that over here as well.
00:06:24.070 --> 00:06:25.070
So this could just be,
00:06:25.070 --> 00:06:26.980
we could write the tangent of y here,
00:06:26.980 --> 00:06:30.010
and then the negative would
turn this into a plus.
00:06:30.010 --> 00:06:33.290
And so just to write everything neatly,
00:06:33.290 --> 00:06:38.290
we know that also the tangent of x minus y
00:06:38.300 --> 00:06:43.300
can be rewritten as tangent
of x minus tangent of y
00:06:46.010 --> 00:06:51.010
all of that over 1 plus
tangent of x and tangent of y.
|
Interpreting statements about vectors | https://www.youtube.com/watch?v=eA2AW5F4N_M | vtt | https://www.youtube.com/api/timedtext?v=eA2AW5F4N_M&ei=5VWUZbiMHrGJp-oPpviXkAQ&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=412521F97FEBA436407FAD54FBF0D4A07E19DA2D.3576153C6B156090009E015860D453D4929A142F&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.240 --> 00:00:01.770
- [Instructor] We're told
that particles A and B
00:00:01.770 --> 00:00:03.780
are moving along a plane.
00:00:03.780 --> 00:00:06.750
Their velocities are
represented by the vectors,
00:00:06.750 --> 00:00:09.490
vector a and vector b respectively.
00:00:09.490 --> 00:00:12.080
Which option best describes the meaning
00:00:12.080 --> 00:00:13.830
of the following statement.
00:00:13.830 --> 00:00:14.820
Choose one answer.
00:00:14.820 --> 00:00:17.340
So pause this video and try to
work through this on your own
00:00:17.340 --> 00:00:19.190
before we work through this together.
00:00:20.090 --> 00:00:22.810
All right, now let's work
through this together.
00:00:22.810 --> 00:00:26.190
So this is saying that
the magnitude of vector a
00:00:26.190 --> 00:00:30.180
is equal to the magnitude of vector b.
00:00:30.180 --> 00:00:31.730
So we know that a vector is specified
00:00:31.730 --> 00:00:34.090
by both a magnitude and a direction.
00:00:34.090 --> 00:00:36.870
And this is just saying that
the magnitudes are the same.
00:00:36.870 --> 00:00:41.870
So for example, vector
a could look like this,
00:00:42.100 --> 00:00:44.850
and vector b could look like this.
00:00:44.850 --> 00:00:48.490
It could do something like that
00:00:48.490 --> 00:00:52.070
where it has the same magnitude
and the same direction.
00:00:52.070 --> 00:00:55.700
Or vector b might be in a
completely different direction.
00:00:55.700 --> 00:00:57.213
The magnitudes being
equivalent just tells us
00:00:57.213 --> 00:00:59.920
that the length of these
arrows are the same,
00:00:59.920 --> 00:01:02.320
but we could have
different directions here.
00:01:02.320 --> 00:01:05.960
So what this tells me is
that we have the same speed
00:01:05.960 --> 00:01:07.830
which is the magnitude of velocity,
00:01:07.830 --> 00:01:10.670
but not necessarily the same direction.
00:01:10.670 --> 00:01:12.200
Now let's look at the choices here.
00:01:12.200 --> 00:01:14.540
The first choice is
that two particles move
00:01:14.540 --> 00:01:18.410
at the same speed and
in the same direction.
00:01:18.410 --> 00:01:21.430
So we've already said that
that's not necessarily the case.
00:01:21.430 --> 00:01:23.530
In order for choice A to be correct,
00:01:23.530 --> 00:01:26.330
they would essentially have
to be equivalent vectors.
00:01:26.330 --> 00:01:29.130
Choice A would be the case
if we said that vector a
00:01:29.130 --> 00:01:31.140
is equal to vector b,
00:01:31.140 --> 00:01:33.390
then they would have to
have the same magnitude
00:01:33.390 --> 00:01:34.550
and the same direction,
00:01:34.550 --> 00:01:37.270
the same magnitude and the same direction.
00:01:37.270 --> 00:01:38.310
But that's not what they told us.
00:01:38.310 --> 00:01:40.520
They just told us that the
magnitudes are the same,
00:01:40.520 --> 00:01:42.420
not necessarily the directions.
00:01:42.420 --> 00:01:44.130
So I'll rule that one out.
00:01:44.130 --> 00:01:45.950
The two particles move at the same speed,
00:01:45.950 --> 00:01:48.980
but not necessarily in the same direction.
00:01:48.980 --> 00:01:50.850
Yes, that's what we just talked about.
00:01:50.850 --> 00:01:51.990
They have the same speed,
00:01:51.990 --> 00:01:54.070
which is the magnitude of velocity,
00:01:54.070 --> 00:01:55.990
but they didn't tell us
anything about the direction,
00:01:55.990 --> 00:01:57.300
just the magnitudes.
00:01:57.300 --> 00:02:00.250
So I like this choice, but
let's look at choice C.
00:02:00.250 --> 00:02:03.040
The two particles move
in the same direction,
00:02:03.040 --> 00:02:06.240
but not necessarily at the same speed.
00:02:06.240 --> 00:02:08.230
Well, we know they move at the same speed.
00:02:08.230 --> 00:02:09.910
That's what this is telling us.
00:02:09.910 --> 00:02:11.610
The magnitudes are the same.
00:02:11.610 --> 00:02:13.620
We just don't know anything
about the direction.
00:02:13.620 --> 00:02:16.610
So I would rule this one out as well.
00:02:16.610 --> 00:02:18.890
In order for choice C to be the case,
00:02:18.890 --> 00:02:21.120
you would see something like this,
00:02:21.120 --> 00:02:24.160
maybe that is vector a right here,
00:02:24.160 --> 00:02:27.610
and then vector b would
move in the same direction,
00:02:27.610 --> 00:02:29.880
but it would have a different magnitude.
00:02:29.880 --> 00:02:31.810
And here you would visualize the magnitude
00:02:31.810 --> 00:02:33.140
as the length of the arrow.
00:02:33.140 --> 00:02:34.560
But that's not what they told us.
00:02:34.560 --> 00:02:37.003
They told us this right over there.
|
Representing quantities with vectors | https://www.youtube.com/watch?v=TCOQzIONaz8 | vtt | https://www.youtube.com/api/timedtext?v=TCOQzIONaz8&ei=5VWUZYHgKre5mLAP-9Ka4AI&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=71BCA7EC900A45534F28D91D544C4BA624F9BBF0.1CCF2775004D6D6723408664F1979C1E61C64CDC&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.380 --> 00:00:01.860
- [Instructor] We're
told a powerful magnet
00:00:01.860 --> 00:00:05.410
is attracting a metal
ball on a flat surface.
00:00:05.410 --> 00:00:07.530
The magnet is pulling the ball
00:00:07.530 --> 00:00:10.120
at a force of 15 Newtons,
00:00:10.120 --> 00:00:13.890
and the magnet is 20 degrees to the south
00:00:13.890 --> 00:00:18.280
from the eastward direction
relative to the ball.
00:00:18.280 --> 00:00:21.500
Here are a few vectors where
the magnitude of vector A
00:00:21.500 --> 00:00:23.510
is equal to the magnitude of vector C
00:00:23.510 --> 00:00:25.230
is equal to 15 Newtons,
00:00:25.230 --> 00:00:27.180
and the magnitude of vector B is equal to
00:00:27.180 --> 00:00:30.530
the magnitude of vector D
which is equal to 20 Newtons.
00:00:30.530 --> 00:00:35.130
Which vectors can represent
the force of the team's pull?
00:00:35.130 --> 00:00:36.580
All right, pause this video and see
00:00:36.580 --> 00:00:38.300
if you can think about that on your own
00:00:38.300 --> 00:00:40.370
before we do it together.
00:00:40.370 --> 00:00:41.810
All right, now let's do it together.
00:00:41.810 --> 00:00:43.180
So before I even look at this,
00:00:43.180 --> 00:00:44.740
I'm just gonna look at the description.
00:00:44.740 --> 00:00:47.520
It has a magnitude of 15 Newtons.
00:00:47.520 --> 00:00:48.660
If we're talking about a force,
00:00:48.660 --> 00:00:51.800
you can view it as a
strength of 15 Newtons,
00:00:51.800 --> 00:00:54.760
and the magnet which
is pulling on the ball
00:00:54.760 --> 00:00:56.890
is 20 degrees to the south
00:00:56.890 --> 00:00:59.730
from the eastward direction
relative to the ball.
00:00:59.730 --> 00:01:01.800
So if this is the ball right over here,
00:01:01.800 --> 00:01:04.203
and if this is the eastward direction,
00:01:05.170 --> 00:01:07.570
it says that the magnet
is 20 degrees to the south
00:01:07.570 --> 00:01:10.010
from the eastward direction
relative to the ball.
00:01:10.010 --> 00:01:12.893
So the magnet would be in this direction,
00:01:13.780 --> 00:01:17.030
and this angle right
over here is 20 degrees,
00:01:17.030 --> 00:01:19.130
and the magnet is pulling on the ball,
00:01:19.130 --> 00:01:22.280
so the vector would go in that
direction towards the magnet,
00:01:22.280 --> 00:01:25.270
and we know it has a force of 15 Newtons,
00:01:25.270 --> 00:01:26.330
that's the magnitude.
00:01:26.330 --> 00:01:30.550
So it has to be a 15 Newton
magnitude right over here.
00:01:30.550 --> 00:01:32.770
So when we look at the choices,
00:01:32.770 --> 00:01:34.810
choice A is interesting,
00:01:34.810 --> 00:01:36.590
at least the direction looks right.
00:01:36.590 --> 00:01:39.520
It looks like it's 20
degrees south of due east,
00:01:39.520 --> 00:01:43.360
and they also tell us that the
magnitude of A is 15 Newtons.
00:01:43.360 --> 00:01:46.650
So I am liking A, now let's look at B.
00:01:46.650 --> 00:01:50.160
Well B looks 15 degrees south of due east,
00:01:50.160 --> 00:01:51.540
not 20 degrees south,
00:01:51.540 --> 00:01:52.860
so I will rule that out.
00:01:52.860 --> 00:01:56.330
And also B's magnitude is
wrong, it's 20 Newtons.
00:01:56.330 --> 00:01:59.880
C, the magnitude is
right, it's 15 Newtons,
00:01:59.880 --> 00:02:03.450
but the direction looks like
20 degrees north of due east.
00:02:03.450 --> 00:02:04.920
So I'll rule that one out.
00:02:04.920 --> 00:02:06.810
And last but not least, D,
00:02:06.810 --> 00:02:08.560
the direction is clearly wrong,
00:02:08.560 --> 00:02:10.850
it looks like 15 degrees
north of due east,
00:02:10.850 --> 00:02:14.150
and its magnitude is 20
Newtons, not 15 Newtons,
00:02:14.150 --> 00:02:15.453
so I'd rule that one out.
00:02:16.450 --> 00:02:19.290
Now to be clear a vector is only defined
00:02:19.290 --> 00:02:21.040
by its magnitude and its direction,
00:02:21.040 --> 00:02:22.710
not by its starting point.
00:02:22.710 --> 00:02:24.120
So if I had some other vector
00:02:24.120 --> 00:02:26.550
that looked like this right over here,
00:02:26.550 --> 00:02:28.690
that had the same magnitude and direction
00:02:28.690 --> 00:02:31.920
if this was right over
here, a 20 degree angle
00:02:31.920 --> 00:02:33.910
and it had a magnitude of 50 Newtons,
00:02:33.910 --> 00:02:36.420
then I would have
selected this one as well.
00:02:36.420 --> 00:02:38.830
You can shift a vector around like this
00:02:38.830 --> 00:02:41.060
as long as it has the same magnitude
00:02:41.060 --> 00:02:42.560
and it has the same direction,
00:02:42.560 --> 00:02:44.433
it is an equivalent vector.
|
Introduction to vector components | https://www.youtube.com/watch?v=hJkKADcQWj0 | vtt | https://www.youtube.com/api/timedtext?v=hJkKADcQWj0&ei=5VWUZZHkGZqdxgKMnpWIBA&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=85D0D2E878778749C6E7FC745A6D8DA7F8A802F7.2E0B530A42AB57024590E585CB62ADA50D7DBC3E&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.630 --> 00:00:02.090
- [Instructor] In other
videos, we have talked
00:00:02.090 --> 00:00:04.100
about how a vector can
be completely defined
00:00:04.100 --> 00:00:06.880
by a magnitude and a
direction, you need both.
00:00:06.880 --> 00:00:08.260
And here we have done that.
00:00:08.260 --> 00:00:09.880
We have said that the magnitude
00:00:09.880 --> 00:00:12.570
of vector a is equal to three units,
00:00:12.570 --> 00:00:15.190
these parallel lines here on both sides,
00:00:15.190 --> 00:00:17.170
it looks like a double absolute value.
00:00:17.170 --> 00:00:19.090
That means the magnitude of vector a.
00:00:19.090 --> 00:00:23.150
And you can also specify
that visually by making sure
00:00:23.150 --> 00:00:26.200
that the length of this vector
arrow is three units long.
00:00:26.200 --> 00:00:27.560
And we also have its direction.
00:00:27.560 --> 00:00:29.610
We see the direction of
vector a is 30 degrees
00:00:29.610 --> 00:00:32.270
counter-clockwise of due East.
00:00:32.270 --> 00:00:34.860
Now in this video, we're
gonna talk about other ways
00:00:34.860 --> 00:00:38.220
or another way to specify
or to define a vector.
00:00:38.220 --> 00:00:41.050
And that's by using components.
00:00:41.050 --> 00:00:42.530
And the way that we're gonna do it is,
00:00:42.530 --> 00:00:44.100
we're gonna think about the tail
00:00:44.100 --> 00:00:47.300
of this vector and the
head of this vector.
00:00:47.300 --> 00:00:50.450
And think about as we go
from the tail to the head,
00:00:50.450 --> 00:00:53.990
what is our change in x?
00:00:53.990 --> 00:00:55.180
And we could see our change
00:00:55.180 --> 00:00:58.340
in x would be that right over there.
00:00:58.340 --> 00:01:00.980
We're going from this x
value to this x value.
00:01:00.980 --> 00:01:05.370
And then what is going
to be our change in y.
00:01:05.370 --> 00:01:07.980
And if we're going from
down here to up here,
00:01:07.980 --> 00:01:12.310
our change in y, we can
also specify like that.
00:01:12.310 --> 00:01:13.500
So let me label these.
00:01:13.500 --> 00:01:18.500
This is my change in x, and
then this is my change in y.
00:01:19.060 --> 00:01:19.920
And if you think about it,
00:01:19.920 --> 00:01:22.780
if someone told you your
change in x and change in y,
00:01:22.780 --> 00:01:25.390
you could reconstruct this
vector right over here
00:01:25.390 --> 00:01:27.490
by starting here, having that change in x,
00:01:27.490 --> 00:01:31.200
then having the change in y
and then defining where the tip
00:01:31.200 --> 00:01:34.740
of the vector would be
relative to the tail.
00:01:34.740 --> 00:01:38.800
The notation for this is
we would say that vector a
00:01:38.800 --> 00:01:42.870
is equal to, and we'll have parenthesis,
00:01:42.870 --> 00:01:46.290
and we'll have our change
in x comma, change in y.
00:01:46.290 --> 00:01:47.780
And so if we wanted to get tangible
00:01:47.780 --> 00:01:50.340
for this particular
vector right over here,
00:01:50.340 --> 00:01:53.550
we know the length of
this vector is three.
00:01:53.550 --> 00:01:55.540
Its magnitude is three.
00:01:55.540 --> 00:01:58.350
We know that this is, since
this is going due horizontally
00:01:58.350 --> 00:02:00.290
and then this is going
straight up and down.
00:02:00.290 --> 00:02:02.420
This is a right triangle.
00:02:02.420 --> 00:02:05.170
And so we can use a little
bit of geometry from the past.
00:02:05.170 --> 00:02:08.020
Don't worry if you need a little
bit of a refresher on this,
00:02:08.020 --> 00:02:09.620
but we could use a little bit of geometry,
00:02:09.620 --> 00:02:11.490
or a little bit of
trigonometry to establish,
00:02:11.490 --> 00:02:13.610
if we know this angle,
if we know the length
00:02:13.610 --> 00:02:17.210
of this hypotenuse, that
this side that's opposite
00:02:17.210 --> 00:02:20.180
the 30 degree angle is gonna
be half the hypotenuse,
00:02:20.180 --> 00:02:22.020
so it's going to be 3/2.
00:02:22.020 --> 00:02:24.200
And that the change in x is going to be
00:02:24.200 --> 00:02:26.960
the square root of three times the 3/2.
00:02:26.960 --> 00:02:31.080
So it's going to be three,
square roots of three over two.
00:02:31.080 --> 00:02:33.980
And so up here, we would
write our x component
00:02:33.980 --> 00:02:37.680
is three times the square
root of three over two.
00:02:37.680 --> 00:02:42.420
And we would write that
the y component is 3/2.
00:02:42.420 --> 00:02:43.820
Now I know a lot of you might be thinking
00:02:43.820 --> 00:02:47.260
this looks a lot like coordinates
in the coordinate plane,
00:02:47.260 --> 00:02:48.580
where this would be the x coordinate
00:02:48.580 --> 00:02:50.300
and this would be the y coordinate.
00:02:50.300 --> 00:02:51.970
But when you're dealing with vectors,
00:02:51.970 --> 00:02:54.610
that's not exactly the interpretation.
00:02:54.610 --> 00:02:57.000
It is the case that if the vector's tail
00:02:57.000 --> 00:03:00.860
were at the origin right
over here, then its head
00:03:00.860 --> 00:03:04.670
would be at these coordinates
on the coordinate plane.
00:03:04.670 --> 00:03:07.470
But we know that a vector is not defined
00:03:07.470 --> 00:03:10.180
by its position, by the
position of the tail.
00:03:10.180 --> 00:03:12.200
I could shift this vector around wherever
00:03:12.200 --> 00:03:13.840
and it would still be the same vector.
00:03:13.840 --> 00:03:15.590
It can start wherever.
00:03:15.590 --> 00:03:19.000
So when you use this
notation in a vector context,
00:03:19.000 --> 00:03:21.440
these aren't x coordinates
and y coordinates.
00:03:21.440 --> 00:03:26.440
This is our change in x,
and this is our change in y.
00:03:27.070 --> 00:03:28.480
Let me do one more example to show
00:03:28.480 --> 00:03:30.880
that we can actually go the other way.
00:03:30.880 --> 00:03:34.790
So let's say I defined some vector b,
00:03:34.790 --> 00:03:39.200
and let's say that its x
component is square root of two.
00:03:39.200 --> 00:03:43.520
And let's say that its y
component is square root of two.
00:03:43.520 --> 00:03:46.260
So let's think about what
that vector would look like.
00:03:46.260 --> 00:03:49.380
So it would, if this is its tail,
00:03:49.380 --> 00:03:51.410
and its x component which is its change
00:03:51.410 --> 00:03:53.030
in x is square root of two.
00:03:53.030 --> 00:03:55.460
So it might look something like this.
00:03:55.460 --> 00:04:00.460
So that would be change in x
is equal to square root of two.
00:04:00.800 --> 00:04:03.980
And then its y component would
also be square root of two.
00:04:03.980 --> 00:04:07.230
So I could write our change in y over here
00:04:07.230 --> 00:04:08.970
is square root of two.
00:04:08.970 --> 00:04:12.850
And so the vector would
look something like this.
00:04:12.850 --> 00:04:17.850
It would start here and
then it would go over here,
00:04:18.580 --> 00:04:20.590
and we can use a little bit of geometry
00:04:20.590 --> 00:04:21.980
to figure out the magnitude
00:04:21.980 --> 00:04:24.260
and the direction of this vector.
00:04:24.260 --> 00:04:26.760
You can use the Pythagorean
theorem to establish
00:04:26.760 --> 00:04:28.760
that this squared plus this squared
00:04:28.760 --> 00:04:30.410
is gonna be equal to that squared.
00:04:30.410 --> 00:04:32.380
And if you do that,
you're going to get this
00:04:32.380 --> 00:04:34.510
having a length of two, which tells you
00:04:34.510 --> 00:04:39.370
that the magnitude of
vector b is equal to two.
00:04:39.370 --> 00:04:42.420
And if you wanted to figure
out this angle right over here,
00:04:42.420 --> 00:04:43.870
you could do a little bit of trigonometry
00:04:43.870 --> 00:04:46.110
or even a little bit
of geometry recognizing
00:04:46.110 --> 00:04:49.500
that this is going to be a
right angle right over here,
00:04:49.500 --> 00:04:52.130
and that this side and that
side have the same length.
00:04:52.130 --> 00:04:53.410
So these are gonna be the same angles
00:04:53.410 --> 00:04:55.600
which are gonna be 45 degree angles.
00:04:55.600 --> 00:04:58.690
And so just like that, you could
also specify the direction,
00:04:58.690 --> 00:05:02.770
45 degrees counter-clockwise of due East.
00:05:02.770 --> 00:05:05.360
So hopefully you appreciate
that these are equivalent ways
00:05:05.360 --> 00:05:06.540
of representing a vector.
00:05:06.540 --> 00:05:08.950
You either can have a
magnitude and a direction,
00:05:08.950 --> 00:05:10.200
or you can have your components
00:05:10.200 --> 00:05:12.350
and you can go back and
forth between the two.
00:05:12.350 --> 00:05:15.283
And we'll get more practice
of that in future videos.
|
Personal Pronouns | https://www.youtube.com/watch?v=qtkivKA4h9w | vtt | https://www.youtube.com/api/timedtext?v=qtkivKA4h9w&ei=5VWUZen0NeyIp-oPv7K2kAI&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=32C4353C078B5EBA68D24ECDEE02169DF4D359EF.D7356FBB963EAA7BAEF523B94FD15A5FCDC7649B&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.660 --> 00:00:02.190
- [Instructor] Hello, grammarians,
00:00:02.190 --> 00:00:04.140
let's talk about personal pronouns,
00:00:04.140 --> 00:00:07.040
but first let me lay
some sentences on you.
00:00:07.040 --> 00:00:10.050
Jake and I baked a loaf of bread.
00:00:10.050 --> 00:00:12.450
We baked a loaf of bread.
00:00:12.450 --> 00:00:14.053
You can learn anything.
00:00:14.940 --> 00:00:17.140
My friends are cool.
00:00:17.140 --> 00:00:18.890
They are cool.
00:00:18.890 --> 00:00:20.650
Now I'm gonna circle a few of these words,
00:00:20.650 --> 00:00:23.120
so the ones I wrote in yellow,
and point them out to you.
00:00:23.120 --> 00:00:24.650
I, we,
00:00:24.650 --> 00:00:27.540
you, my, they,
00:00:27.540 --> 00:00:29.130
these are personal pronouns.
00:00:29.130 --> 00:00:30.500
They're pronouns that change
00:00:30.500 --> 00:00:32.210
depending on how you're using them.
00:00:32.210 --> 00:00:34.780
On whether you're using them
as the object of a sentence,
00:00:34.780 --> 00:00:37.580
as the subject to show
ownership, and so on.
00:00:37.580 --> 00:00:39.220
But we'll get to those in later videos.
00:00:39.220 --> 00:00:40.730
For now, I'm gonna talk about
00:00:40.730 --> 00:00:44.290
the three basic types of English pronoun.
00:00:44.290 --> 00:00:47.100
Broadly speaking, there
are pronouns about me,
00:00:47.100 --> 00:00:48.840
pronouns about you,
00:00:48.840 --> 00:00:52.190
and pronouns about
something or someone else.
00:00:52.190 --> 00:00:54.610
This is an idea called grammatical person.
00:00:54.610 --> 00:00:56.950
Pronouns about me are first person,
00:00:56.950 --> 00:00:59.230
pronouns about you are second person,
00:00:59.230 --> 00:01:01.630
and pronouns about
something or someone else
00:01:01.630 --> 00:01:03.410
are third person.
00:01:03.410 --> 00:01:06.750
So, when I say I love my dog, Phryne.
00:01:06.750 --> 00:01:09.450
I is a first person pronoun.
00:01:09.450 --> 00:01:10.283
In the sentence,
00:01:10.283 --> 00:01:13.720
she is an excellent dog,
where she subs out for Phryne,
00:01:13.720 --> 00:01:16.860
she is a third person pronoun.
00:01:16.860 --> 00:01:18.420
Here is a picture of Phryne,
00:01:18.420 --> 00:01:21.040
I think we can all agree, she is perfect.
00:01:21.040 --> 00:01:21.873
Thank you.
00:01:21.873 --> 00:01:22.940
Okay. So what I want to do here
00:01:22.940 --> 00:01:24.330
is fill out this table
00:01:24.330 --> 00:01:25.970
with some of the basic pronouns
00:01:25.970 --> 00:01:27.730
we use to talk about ourselves
00:01:27.730 --> 00:01:30.560
divided between singular,
that is one person,
00:01:30.560 --> 00:01:33.600
and plural, or more than one person.
00:01:33.600 --> 00:01:37.990
Some first person pronouns
are I, me, my, and mine.
00:01:37.990 --> 00:01:39.780
But what if there's more than one of me?
00:01:39.780 --> 00:01:40.920
What if I'm part of a group
00:01:40.920 --> 00:01:43.280
and I wanna refer to that group?
00:01:43.280 --> 00:01:44.840
Well, then I'd use a plural pronoun
00:01:44.840 --> 00:01:48.290
like we, us, our, or ours.
00:01:48.290 --> 00:01:49.960
Second and third person are interesting
00:01:49.960 --> 00:01:52.750
because they have pronouns
that pull double duty.
00:01:52.750 --> 00:01:53.850
In second person,
00:01:53.850 --> 00:01:56.950
the singular and plural are identical.
00:01:56.950 --> 00:02:00.940
Singular second person
is you, your, and yours.
00:02:00.940 --> 00:02:02.760
And plural second person is the same,
00:02:02.760 --> 00:02:04.940
you, your, and yours.
00:02:04.940 --> 00:02:06.810
That is to say, it's
the same whether or not
00:02:06.810 --> 00:02:09.850
you're referring to one
person, here in singular,
00:02:09.850 --> 00:02:12.420
or many people, here in plural.
00:02:12.420 --> 00:02:14.570
Understanding whether you meet one you
00:02:14.570 --> 00:02:16.910
or a plural you depends on context.
00:02:16.910 --> 00:02:19.900
And it's usually very easy to figure out.
00:02:19.900 --> 00:02:22.870
Third person pronouns belong
to the most crowded category
00:02:22.870 --> 00:02:25.460
because the world is
full of things and people
00:02:25.460 --> 00:02:27.290
who are neither me nor you.
00:02:27.290 --> 00:02:30.750
For singular pronouns we
have she, her, and hers,
00:02:30.750 --> 00:02:33.080
he, him, and his,
00:02:33.080 --> 00:02:35.210
they, them, their and theirs
00:02:35.210 --> 00:02:37.660
and it, and its.
00:02:37.660 --> 00:02:41.100
They, like you, can refer
to both a single person
00:02:41.100 --> 00:02:42.140
or multiple people,
00:02:42.140 --> 00:02:45.570
but it doesn't specify a
gender like she and he do.
00:02:45.570 --> 00:02:47.190
This is extremely useful.
00:02:47.190 --> 00:02:49.010
I'd take note that the word it
00:02:49.010 --> 00:02:50.950
only refers to inanimate objects
00:02:50.950 --> 00:02:52.820
and sometimes non-human animals,
00:02:52.820 --> 00:02:54.370
but never to people.
00:02:54.370 --> 00:02:55.690
A robot? Yes.
00:02:55.690 --> 00:02:57.303
A person? Not so much.
00:02:58.180 --> 00:02:59.940
Now, in the plural category, much simpler,
00:02:59.940 --> 00:03:03.930
we have they, them, their, and theirs.
00:03:03.930 --> 00:03:06.430
Similar to singular versus plural you
00:03:06.430 --> 00:03:09.220
singular versus plural
they depends on context
00:03:09.220 --> 00:03:11.400
and it'll be obvious
from the words around it
00:03:11.400 --> 00:03:12.900
which one you mean.
00:03:12.900 --> 00:03:15.280
This is a lot of information to swallow.
00:03:15.280 --> 00:03:17.410
Pause this if you need to practice saying
00:03:17.410 --> 00:03:19.210
the different pronouns aloud,
00:03:19.210 --> 00:03:22.420
do the exercises on the
Khan Academy site or app.
00:03:22.420 --> 00:03:24.380
This is not the only time I'll be talking
00:03:24.380 --> 00:03:26.330
about personal pronouns in this course.
00:03:26.330 --> 00:03:28.480
So we have an opportunity to go deeper,
00:03:28.480 --> 00:03:30.660
especially if you want to
know more about the history
00:03:30.660 --> 00:03:33.623
of the singular use of
they, which is super cool.
00:03:34.490 --> 00:03:35.540
In the meantime,
00:03:35.540 --> 00:03:38.240
please enjoy this second
image of my dog, Phryne,
00:03:38.240 --> 00:03:41.930
who is, again, as I said, a perfect dog.
00:03:41.930 --> 00:03:43.540
You can learn anything.
00:03:43.540 --> 00:03:44.373
David out.
|
Cosine, sine and tangent of π/6 and π/3 | https://www.youtube.com/watch?v=Tt_ATh5mCGw | vtt | https://www.youtube.com/api/timedtext?v=Tt_ATh5mCGw&ei=5VWUZZqNNN2UvdIP4vuo8AQ&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=D4BAB4B60650BCBCC5A6DB7B7851B95F3E76C497.6FB3C3E040F8CD0B4F232B07392A277D84BF9759&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.330 --> 00:00:01.290
- [Instructor] In this video,
00:00:01.290 --> 00:00:05.870
we're going to figure out what
the sine, cosine and tangent
00:00:05.870 --> 00:00:07.640
of two very important angles are.
00:00:07.640 --> 00:00:10.000
Angles that you will see a
lot in your trigonometric
00:00:10.000 --> 00:00:12.610
and just in general in your regular life.
00:00:12.610 --> 00:00:13.860
So these are the angles,
00:00:13.860 --> 00:00:17.720
pi over 3 radians and pi over 6 radians.
00:00:17.720 --> 00:00:21.540
And sometimes it's useful to
visualize them as degrees.
00:00:21.540 --> 00:00:25.030
pi over 3, you might remember
pi radians is 180 degrees,
00:00:25.030 --> 00:00:26.690
so you divide that by three,
00:00:26.690 --> 00:00:28.111
this is equivalent to 60 degrees.
00:00:28.111 --> 00:00:30.760
And once again, 180 degrees,
00:00:30.760 --> 00:00:32.990
which is the same thing as
pi radians divided by six
00:00:32.990 --> 00:00:35.500
is the same thing as 30 degrees.
00:00:35.500 --> 00:00:38.470
Now, I'm going to do it using
the unit circle definition
00:00:38.470 --> 00:00:40.430
of trig functions.
00:00:40.430 --> 00:00:41.480
But to help us there,
00:00:41.480 --> 00:00:43.160
I'm going to give us a
little bit of a reminder
00:00:43.160 --> 00:00:45.010
of what some of you might be familiar with
00:00:45.010 --> 00:00:46.980
as 30, 60, 90 triangles,
00:00:46.980 --> 00:00:48.660
which I guess we could
also call pi over six,
00:00:48.660 --> 00:00:51.250
pi over three, pi over two triangles.
00:00:51.250 --> 00:00:53.420
And so let me just draw one
00:00:53.420 --> 00:00:55.400
because this is going to be really helpful
00:00:55.400 --> 00:00:57.960
in establishing these trig functions
00:00:57.960 --> 00:01:00.520
using the unit circle definition.
00:01:00.520 --> 00:01:03.190
So let me draw a triangle here,
00:01:03.190 --> 00:01:04.180
it's hand drawn,
00:01:04.180 --> 00:01:06.190
so it's not as neat as it could be.
00:01:06.190 --> 00:01:08.840
So this right over here is a right angle,
00:01:08.840 --> 00:01:13.430
and let's say that this one
is pi over three radians
00:01:13.430 --> 00:01:15.640
which is the same thing as 60 degrees,
00:01:15.640 --> 00:01:18.890
and this one over here
is pi over six radians
00:01:18.890 --> 00:01:21.890
which is the same thing as 30 degrees.
00:01:21.890 --> 00:01:24.330
Now, let's also say that the longest side,
00:01:24.330 --> 00:01:26.453
the hypotenuse here has length one.
00:01:27.460 --> 00:01:29.850
Now, to help us think about
what the other two sides are,
00:01:29.850 --> 00:01:32.650
what I'm going to do is
flip this triangle over
00:01:32.650 --> 00:01:33.960
this side right over here,
00:01:33.960 --> 00:01:36.980
and essentially construct a mirror image.
00:01:36.980 --> 00:01:41.150
So because this right over
here is a mirror image,
00:01:41.150 --> 00:01:42.780
we immediately know a few things.
00:01:42.780 --> 00:01:44.600
We know that this length right over here
00:01:44.600 --> 00:01:48.040
is going to be congruent
to this length over here.
00:01:48.040 --> 00:01:51.530
And let me actually finish
drawing the entire triangle,
00:01:51.530 --> 00:01:53.920
it's going to look something like this.
00:01:53.920 --> 00:01:56.350
And since once again, it's a reflection,
00:01:56.350 --> 00:01:59.120
this length over here is
going to have length one,
00:01:59.120 --> 00:02:03.250
this is going to be pi over six radians,
00:02:03.250 --> 00:02:07.610
this is going to be pi over three radians.
00:02:07.610 --> 00:02:11.350
So what else do we know about
this larger triangle now?
00:02:11.350 --> 00:02:13.470
Well, we know it's an
equilateral triangle.
00:02:13.470 --> 00:02:15.610
All the angles, pi over three radians,
00:02:15.610 --> 00:02:16.443
pi over three radians
00:02:16.443 --> 00:02:18.080
and if you add two pi over sixes together,
00:02:18.080 --> 00:02:19.440
you're going to get pi over three as well,
00:02:19.440 --> 00:02:22.540
so it's a 60 degree, 60
degree, 60 degree triangle.
00:02:22.540 --> 00:02:24.790
And so all the sides are
going to have the same length,
00:02:24.790 --> 00:02:27.000
so it's going to be one, one and one.
00:02:27.000 --> 00:02:29.500
And if these two sides are congruent
00:02:29.500 --> 00:02:30.960
of the smaller triangles,
00:02:30.960 --> 00:02:32.600
of the smaller right triangles,
00:02:32.600 --> 00:02:35.310
well then this right over
here must be one half,
00:02:35.310 --> 00:02:39.770
and then this right over here
must be one half as well.
00:02:39.770 --> 00:02:41.310
Now, that's going to be useful
00:02:41.310 --> 00:02:44.900
for figuring out what this
length right over here
00:02:44.900 --> 00:02:45.960
is going to be.
00:02:45.960 --> 00:02:48.450
Because we have two right triangles,
00:02:48.450 --> 00:02:49.360
we could use either one,
00:02:49.360 --> 00:02:51.600
but if we just use this
bottom right triangle here
00:02:51.600 --> 00:02:53.530
the Pythagorean theorem tells us
00:02:53.530 --> 00:02:56.700
that one half squared, let's call this B,
00:02:56.700 --> 00:02:58.550
so plus B squared,
00:02:58.550 --> 00:02:59.990
I'm just pattern matching,
00:02:59.990 --> 00:03:02.440
A squared plus B squared
is equal to C squared
00:03:02.440 --> 00:03:04.660
where C is the length of the hypotenuse,
00:03:04.660 --> 00:03:06.650
is equal to one squared.
00:03:06.650 --> 00:03:11.270
And so we get that one
fourth plus B squared
00:03:11.270 --> 00:03:12.580
is equal to one
00:03:12.580 --> 00:03:14.970
or subtracting one fourth from both sides.
00:03:14.970 --> 00:03:17.540
B squared is equal to three-fourths,
00:03:17.540 --> 00:03:19.580
and then taking the
principle root of both sides,
00:03:19.580 --> 00:03:23.750
we get B is equal to the
square root of three over two.
00:03:23.750 --> 00:03:25.460
So just like that, we have figured out
00:03:25.460 --> 00:03:28.870
what all the lengths of this
30, 60, 90 triangle are.
00:03:28.870 --> 00:03:33.240
So B here is equal to square
root of three over two.
00:03:33.240 --> 00:03:35.200
Now, I said this would
be useful as we go into
00:03:35.200 --> 00:03:38.150
the unit circle definitions
of sine, cosine and tangent.
00:03:38.150 --> 00:03:39.910
And we're about to see why.
00:03:39.910 --> 00:03:42.790
So here I have two different unit circles,
00:03:42.790 --> 00:03:45.200
I'm going to use one for
each of these angles.
00:03:45.200 --> 00:03:48.310
So first, let's think about
pi over three radians.
00:03:48.310 --> 00:03:50.340
And so pi over three,
00:03:50.340 --> 00:03:53.513
would look something like this,
00:03:54.710 --> 00:03:58.940
this is pi over three radians.
00:03:58.940 --> 00:04:02.240
And the cosine and sine can be determined
00:04:02.240 --> 00:04:04.860
by the X and Y coordinates of this point
00:04:04.860 --> 00:04:08.200
where this radius intersects
the actual unit circle.
00:04:08.200 --> 00:04:10.887
The coordinates here
are going to be cosine
00:04:10.887 --> 00:04:13.006
of pi over three radians
00:04:13.006 --> 00:04:15.839
and sine of pi over three radians.
00:04:16.810 --> 00:04:18.400
Or another way to think about it is,
00:04:18.400 --> 00:04:20.780
I can set up a 30, 60, 90 triangle here,
00:04:20.780 --> 00:04:22.740
so I'm going to drop a perpendicular.
00:04:22.740 --> 00:04:26.370
This would be 90 degrees
or pi over two radians.
00:04:26.370 --> 00:04:27.740
And then this angle over here,
00:04:27.740 --> 00:04:30.260
this is 60, this is 90,
this is going to be 30,
00:04:30.260 --> 00:04:31.320
or another way of thinking about it,
00:04:31.320 --> 00:04:34.390
it's going to be pi over six radians.
00:04:34.390 --> 00:04:36.650
It's going to be just like
one of these triangles here.
00:04:36.650 --> 00:04:38.260
And so the X coordinate,
00:04:38.260 --> 00:04:41.460
which is going to be the
same thing as the cosine
00:04:41.460 --> 00:04:42.650
of pi over three,
00:04:42.650 --> 00:04:46.740
is going to be the length of
this side, right over here.
00:04:46.740 --> 00:04:48.320
Well, what's that going to be?
00:04:48.320 --> 00:04:50.470
Well, when your hypotenuse is one,
00:04:50.470 --> 00:04:52.270
we know that the shorter side,
00:04:52.270 --> 00:04:56.280
the side opposite the pi over
six radians, is one half.
00:04:56.280 --> 00:04:58.390
So just like that, we have
been able to establish
00:04:58.390 --> 00:05:03.310
that cosine of pi over three
radians is equal to one half.
00:05:03.310 --> 00:05:04.920
This right over here is one half,
00:05:04.920 --> 00:05:06.410
that is the X coordinate
00:05:06.410 --> 00:05:09.140
where this radius
intersects the units circle.
00:05:09.140 --> 00:05:11.540
Now, what about the Y coordinate?
00:05:11.540 --> 00:05:13.970
What is sine of pi over three going to be?
00:05:13.970 --> 00:05:15.710
Well, the Y coordinate is the same thing
00:05:15.710 --> 00:05:18.200
as the length of this side,
00:05:18.200 --> 00:05:21.100
and once again, it goes
back to being this triangle.
00:05:21.100 --> 00:05:22.800
If this is one, this is one half,
00:05:22.800 --> 00:05:24.390
this is one, this is one half,
00:05:24.390 --> 00:05:26.330
this other side is going to be square root
00:05:26.330 --> 00:05:27.540
of three over two.
00:05:27.540 --> 00:05:29.140
So sine of pi over three
00:05:29.140 --> 00:05:31.780
is going to be square
root of three over two,
00:05:31.780 --> 00:05:32.840
so let me write that down.
00:05:32.840 --> 00:05:35.610
Sine of pi over three
00:05:35.610 --> 00:05:37.840
is equal to square root of three over two.
00:05:37.840 --> 00:05:39.250
And these are good ones to know.
00:05:39.250 --> 00:05:41.400
I never say really memorize things,
00:05:41.400 --> 00:05:43.770
it's always good to know
how to derive things
00:05:43.770 --> 00:05:45.340
in case you forget.
00:05:45.340 --> 00:05:47.200
But if you have to memorize them
00:05:47.200 --> 00:05:49.320
I would highly recommend memorizing these,
00:05:49.320 --> 00:05:52.320
and then of course from these
we can figure out the tangent.
00:05:52.320 --> 00:05:54.470
The tangent is just going to
be the sine over the cosine,
00:05:54.470 --> 00:05:57.210
so let me write it down here.
00:05:57.210 --> 00:06:01.840
The tangent of pi over three
00:06:01.840 --> 00:06:03.350
is going to be the sine,
00:06:03.350 --> 00:06:05.950
which is square root of three over two,
00:06:05.950 --> 00:06:09.130
over the cosine which is one half,
00:06:09.130 --> 00:06:10.550
got a little squanchy down there,
00:06:10.550 --> 00:06:12.093
and so this is just going to be
00:06:12.093 --> 00:06:13.760
square root of three over two times two
00:06:13.760 --> 00:06:16.860
is just going to be square root of three.
00:06:16.860 --> 00:06:19.780
So now let's just use that
same logic for pi over six.
00:06:19.780 --> 00:06:21.410
And in fact, I encourage
you to pause this video
00:06:21.410 --> 00:06:23.353
and see if you can do that on your own.
00:06:24.430 --> 00:06:25.840
All right, now let's draw a radius
00:06:25.840 --> 00:06:30.190
that forms a pi over six radian angle
00:06:30.190 --> 00:06:32.340
with a positive X axis,
might look like that.
00:06:32.340 --> 00:06:35.670
So if that's going to
be pi over six radians,
00:06:35.670 --> 00:06:38.330
you might imagine it's interesting
00:06:38.330 --> 00:06:40.590
to drop a perpendicular here
00:06:40.590 --> 00:06:43.030
and see what type of
triangle we've constructed.
00:06:43.030 --> 00:06:44.380
So this has length one,
00:06:44.380 --> 00:06:46.240
this is pi over six radians,
00:06:46.240 --> 00:06:47.990
this is a right angle.
00:06:47.990 --> 00:06:50.960
So this again, is going to
follow the same pattern.
00:06:50.960 --> 00:06:54.610
This will be pi over three radians.
00:06:54.610 --> 00:06:57.150
And so the sides are
exactly the exact same
00:06:57.150 --> 00:06:59.910
as this top blue triangle here.
00:06:59.910 --> 00:07:02.280
So we know that this length over here
00:07:02.280 --> 00:07:04.610
is going to be one half.
00:07:04.610 --> 00:07:07.480
We know that this length over here
00:07:07.480 --> 00:07:11.670
is going to be square
root of three over two.
00:07:11.670 --> 00:07:13.910
And that's useful because that tells us
00:07:13.910 --> 00:07:15.110
the coordinates here.
00:07:15.110 --> 00:07:16.370
The coordinates here,
00:07:16.370 --> 00:07:18.480
the X coordinate of this
point where the radius
00:07:18.480 --> 00:07:20.060
intersects the unit circle
00:07:20.060 --> 00:07:22.840
is square root of three over two,
00:07:22.840 --> 00:07:26.450
and then the Y coordinate is one half.
00:07:26.450 --> 00:07:28.360
And that immediately tells us the cosine
00:07:28.360 --> 00:07:30.390
and the sine of pi over six,
00:07:30.390 --> 00:07:31.770
let's just write it down.
00:07:31.770 --> 00:07:35.350
So this tells us that
cosine of pi over six
00:07:35.350 --> 00:07:38.490
is equal to square root of three over two.
00:07:38.490 --> 00:07:41.930
And sine of pi over six
00:07:43.230 --> 00:07:45.540
is equal to one half.
00:07:45.540 --> 00:07:48.530
Notice, we actually just
swap these two things around
00:07:48.530 --> 00:07:50.380
because now the angle that we're taking
00:07:50.380 --> 00:07:51.530
the sine or cosine of,
00:07:51.530 --> 00:07:54.870
is a different angle on
a 30, 60, 90 triangle,
00:07:54.870 --> 00:07:57.900
but we're essentially utilizing
the same side measure,
00:07:57.900 --> 00:07:59.090
just one way to think about it.
00:07:59.090 --> 00:08:01.340
And then what's the tangent going to be?
00:08:01.340 --> 00:08:02.730
I'll write it down here.
00:08:02.730 --> 00:08:06.250
The tangent of pi over six
00:08:06.250 --> 00:08:09.520
is going to be the sine over the cosine
00:08:09.520 --> 00:08:11.660
square root of three over two,
00:08:11.660 --> 00:08:14.320
and so that's going to
be equal to one half
00:08:14.320 --> 00:08:17.580
times two over the square root of three,
00:08:17.580 --> 00:08:21.150
which is equal to one over
the square root of three.
00:08:21.150 --> 00:08:24.210
Now some people sometimes
don't like radicals
00:08:24.210 --> 00:08:25.043
in the denominator
00:08:25.043 --> 00:08:27.220
and so you can multiply the
numerator and the denominator
00:08:27.220 --> 00:08:29.210
by square root of three if you like
00:08:29.210 --> 00:08:30.270
to get something like this,
00:08:30.270 --> 00:08:31.580
you multiply the numerator and denominator
00:08:31.580 --> 00:08:32.413
by square root of three
00:08:32.413 --> 00:08:34.660
you get square root of three over three,
00:08:34.660 --> 00:08:37.560
which is another way of
writing tangent of pi over six.
00:08:37.560 --> 00:08:38.880
But either way, we're done,
00:08:38.880 --> 00:08:41.820
it's very useful to know
the cosine, sine and tangent
00:08:41.820 --> 00:08:44.570
of both pi over three and pi over six.
00:08:44.570 --> 00:08:46.823
And now you also know how to derive it.
|
Rule of 70 to approximate population doubling time | https://www.youtube.com/watch?v=KBXec1ctCjg | vtt | https://www.youtube.com/api/timedtext?v=KBXec1ctCjg&ei=5VWUZZHiIue_p-oPsJWeCA&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=30EEC74951D749CC05F44C38296773C691B83B7B.46C655B2019186020123BA0F22BF069C30FFC449&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:01.230 --> 00:00:02.063
- [Instructor] When we're dealing
00:00:02.063 --> 00:00:03.280
with population growth rates
00:00:03.280 --> 00:00:05.050
an interesting question is,
00:00:05.050 --> 00:00:06.440
how long would it take
00:00:06.440 --> 00:00:10.650
for a given rate for the
population to double?
00:00:10.650 --> 00:00:13.120
So we're gonna think about doubling time.
00:00:13.120 --> 00:00:15.640
Now if you were to actually
calculate it precisely
00:00:15.640 --> 00:00:19.020
mathematically precisely,
it gets a little bit mathy.
00:00:19.020 --> 00:00:20.960
You need to use a little bit of logarithms
00:00:20.960 --> 00:00:23.220
and you'll probably need a calculator,
00:00:23.220 --> 00:00:25.070
but I did that here in this spreadsheet
00:00:25.070 --> 00:00:27.130
by calculating the exact doubling time.
00:00:27.130 --> 00:00:29.790
So this is saying that if
a population is growing
00:00:29.790 --> 00:00:31.800
at 1% a year,
00:00:31.800 --> 00:00:34.750
it's going to take almost 70 years
00:00:34.750 --> 00:00:36.700
for that population to double.
00:00:36.700 --> 00:00:41.250
But if that population
is growing at 5% per year
00:00:41.250 --> 00:00:44.130
then it's going to take
a little over 14 years
00:00:44.130 --> 00:00:46.240
for that population to double.
00:00:46.240 --> 00:00:48.790
If the population is growing at 10%,
00:00:48.790 --> 00:00:51.160
we know mathematically it's
going to take a little bit
00:00:51.160 --> 00:00:54.400
over seven years for that
population to double.
00:00:54.400 --> 00:00:56.840
Now, I was able to calculate
this as I just mentioned
00:00:56.840 --> 00:00:59.420
using a little bit of fancy math,
00:00:59.420 --> 00:01:01.000
but what we see in this next column
00:01:01.000 --> 00:01:03.120
is there's actually a pretty
00:01:03.120 --> 00:01:06.490
easy way to approximate doubling time.
00:01:06.490 --> 00:01:08.840
And this is known as the rule of 70.
00:01:08.840 --> 00:01:12.480
And the rule of 70 is used
in a lot of different areas,
00:01:12.480 --> 00:01:13.550
a lot of different subjects,
00:01:13.550 --> 00:01:15.780
people in finance would
use it because once again,
00:01:15.780 --> 00:01:17.710
you're thinking about things growing
00:01:17.710 --> 00:01:19.190
at a certain percent every year,
00:01:19.190 --> 00:01:20.530
but you can also use it
00:01:20.530 --> 00:01:23.540
for things like population growth rates.
00:01:23.540 --> 00:01:26.120
So what we see with the rule of 70,
00:01:26.120 --> 00:01:27.580
and let me just write that down,
00:01:27.580 --> 00:01:32.580
rule of 70 is that you can
approximate the doubling time
00:01:32.930 --> 00:01:34.960
by taking the number 70
00:01:34.960 --> 00:01:38.890
and dividing it by the, not
actually the percentage,
00:01:38.890 --> 00:01:41.110
but just the number of the percentage.
00:01:41.110 --> 00:01:42.480
So for example,
00:01:42.480 --> 00:01:47.480
this right over here is 70
divided by this one here,
00:01:48.920 --> 00:01:50.980
which is equal to 70.
00:01:50.980 --> 00:01:55.330
And notice this 70 is
pretty close to 69.7.
00:01:55.330 --> 00:01:56.760
If you wanted to figure out
00:01:56.760 --> 00:01:59.750
or you wanted to approximate
the doubling time,
00:01:59.750 --> 00:02:02.800
if the population is growing at 7% a year,
00:02:02.800 --> 00:02:04.330
well what you would say is, all right,
00:02:04.330 --> 00:02:08.090
what is 70 divided by seven?
00:02:08.090 --> 00:02:09.280
Well, that is equal to 10.
00:02:09.280 --> 00:02:10.950
So this would be your approximation.
00:02:10.950 --> 00:02:13.440
And if you were to do it in
a mathematically precise way,
00:02:13.440 --> 00:02:15.400
it would be 10.2.
00:02:15.400 --> 00:02:17.400
So if you're taking,
00:02:17.400 --> 00:02:20.000
say an AP environmental science course
00:02:20.000 --> 00:02:22.040
and they're asking you for the,
00:02:22.040 --> 00:02:24.400
how long it takes for something to double
00:02:24.400 --> 00:02:27.150
let's say a population
that's growing 7% a year,
00:02:27.150 --> 00:02:31.563
they're probably expecting
you to use the rule of 70.
00:02:32.830 --> 00:02:35.370
So let's say that we have a population
00:02:35.370 --> 00:02:40.370
that is growing at 14% per year,
00:02:41.390 --> 00:02:44.320
and that would actually be
a very huge growth rate.
00:02:44.320 --> 00:02:45.970
What I want you to do is pause this video
00:02:45.970 --> 00:02:48.210
and approximate how long would it take
00:02:48.210 --> 00:02:50.853
for that population to double?
00:02:52.460 --> 00:02:54.240
All right, now let's work
through this together.
00:02:54.240 --> 00:02:56.210
So as I mentioned, we're approximating,
00:02:56.210 --> 00:02:58.380
we don't have to do calculate
the exact doubling time.
00:02:58.380 --> 00:03:00.170
So if we're approximating,
00:03:00.170 --> 00:03:05.170
it's going to be 70 divided
by the rate of growth.
00:03:05.330 --> 00:03:09.603
So in this situation, this is
going to be 70 divided by 14,
00:03:11.240 --> 00:03:13.600
which is equal to five.
00:03:13.600 --> 00:03:15.550
So if a population is growing at 14%,
00:03:15.550 --> 00:03:18.863
it'll take it roughly
five years to double.
|
Worked example: Using bond enthalpies to calculate enthalpy of reaction | https://www.youtube.com/watch?v=TdBY-so0H0Q | vtt | https://www.youtube.com/api/timedtext?v=TdBY-so0H0Q&ei=5VWUZfDsKpu4vdIP0Lu6sAU&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=EEE2E7E5D4F92408B9F94D53424883D1929CC5EE.2C41732D90CFB5F532B24D63AFF3D453E4517089&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.510 --> 00:00:02.330
- [Educator] Bond enthalpies can be used
00:00:02.330 --> 00:00:05.100
to estimate the standard
change in enthalpy
00:00:05.100 --> 00:00:07.490
for a chemical reaction.
00:00:07.490 --> 00:00:08.900
Let's use bond enthalpies
00:00:08.900 --> 00:00:11.740
to estimate the enthalpy of combustion
00:00:11.740 --> 00:00:13.100
of ethanol.
00:00:13.100 --> 00:00:14.510
Looking at our balanced equation,
00:00:14.510 --> 00:00:16.840
we have one mole of ethanol reacting
00:00:16.840 --> 00:00:18.920
with three moles of oxygen gas
00:00:18.920 --> 00:00:21.600
to produce two moles of carbon dioxide
00:00:21.600 --> 00:00:25.990
and three moles of water
in the gaseous state.
00:00:25.990 --> 00:00:27.720
To find the standard change in enthalpy
00:00:27.720 --> 00:00:29.110
for this chemical reaction,
00:00:29.110 --> 00:00:31.980
we need to sum the bond enthalpies
00:00:31.980 --> 00:00:33.900
of the bonds that are broken.
00:00:33.900 --> 00:00:36.400
And from that, we subtract the sum
00:00:36.400 --> 00:00:38.670
of the bond enthalpies of the bonds
00:00:38.670 --> 00:00:41.550
that are formed in this chemical reaction.
00:00:41.550 --> 00:00:43.170
To figure out which bonds are broken
00:00:43.170 --> 00:00:44.450
and which bonds are formed,
00:00:44.450 --> 00:00:46.590
it's helpful to look at the dot structures
00:00:46.590 --> 00:00:48.130
for our molecules.
00:00:48.130 --> 00:00:51.180
So let's start with the ethanol molecule.
00:00:51.180 --> 00:00:52.770
We're gonna approach this problem first
00:00:52.770 --> 00:00:55.840
like we're breaking all of
the bonds in these molecules.
00:00:55.840 --> 00:00:58.570
And we're also not gonna worry
about units until the end,
00:00:58.570 --> 00:01:01.160
just to save some space on the screen.
00:01:01.160 --> 00:01:03.130
So looking at the ethanol molecule,
00:01:03.130 --> 00:01:06.820
we would need to break
a carbon-carbon bond.
00:01:06.820 --> 00:01:08.530
So let's go ahead and
write this down here.
00:01:08.530 --> 00:01:10.850
Right now, we're summing
the bond enthalpies
00:01:10.850 --> 00:01:12.860
of the bonds that are broken.
00:01:12.860 --> 00:01:15.490
So we have one carbon-carbon bond.
00:01:15.490 --> 00:01:16.323
So let's write in here,
00:01:16.323 --> 00:01:20.590
the bond enthalpy for
a carbon-carbon bond.
00:01:20.590 --> 00:01:24.630
Next, we have five carbon-hydrogen bonds
00:01:24.630 --> 00:01:26.390
that we need to break.
00:01:26.390 --> 00:01:27.640
So to this,
00:01:27.640 --> 00:01:30.140
we're going to write in here, a five,
00:01:30.140 --> 00:01:32.740
and then the bond enthalpy
00:01:32.740 --> 00:01:35.920
of a carbon-hydrogen bond.
00:01:35.920 --> 00:01:39.820
Next, we have to break a
carbon-oxygen single bond.
00:01:39.820 --> 00:01:41.840
So we write a one,
00:01:41.840 --> 00:01:43.930
and then the bond enthalpy
00:01:43.930 --> 00:01:47.310
for a carbon-oxygen single bond.
00:01:47.310 --> 00:01:49.260
And then for this ethanol molecule,
00:01:49.260 --> 00:01:52.650
we also have an
oxygen-hydrogen single bond.
00:01:52.650 --> 00:01:54.850
So we'll write in here, a one,
00:01:54.850 --> 00:01:56.880
and the bond enthalpy
00:01:56.880 --> 00:01:59.920
for an oxygen-hydrogen single bond.
00:01:59.920 --> 00:02:01.150
We saw in the balanced equation
00:02:01.150 --> 00:02:02.870
that one mole of ethanol reacts
00:02:02.870 --> 00:02:05.310
with three moles of oxygen gas.
00:02:05.310 --> 00:02:07.550
So to represent the three
moles of oxygen gas,
00:02:07.550 --> 00:02:08.500
I've drawn in here,
00:02:08.500 --> 00:02:11.370
three molecules of O2.
00:02:11.370 --> 00:02:13.970
And we can see in each molecule of O2,
00:02:13.970 --> 00:02:16.160
there's an oxygen-oxygen double bond.
00:02:16.160 --> 00:02:20.610
So we would need to break three
oxygen-oxygen double bonds.
00:02:20.610 --> 00:02:21.840
So to this,
00:02:21.840 --> 00:02:26.840
we're going to add a three
times the bond enthalpy
00:02:27.140 --> 00:02:30.450
of an oxygen-oxygen double bond.
00:02:30.450 --> 00:02:34.650
And this now gives us the
sum of the bond enthalpies
00:02:34.650 --> 00:02:37.360
for all the bonds that need to be broken.
00:02:37.360 --> 00:02:39.240
It takes energy to break a bond.
00:02:39.240 --> 00:02:41.340
So the summation of the bond enthalpies
00:02:41.340 --> 00:02:42.720
of the bonds that are broken
00:02:42.720 --> 00:02:45.230
is going to be a positive value.
00:02:45.230 --> 00:02:47.130
And since it takes energy to break bonds,
00:02:47.130 --> 00:02:49.580
energy is given off when bonds form.
00:02:49.580 --> 00:02:51.950
So next, we're gonna
sum the bond enthalpies
00:02:51.950 --> 00:02:53.390
of the bonds that are formed.
00:02:53.390 --> 00:02:55.900
And notice we have this
negative sign in here
00:02:55.900 --> 00:02:58.160
because this energy is given off.
00:02:58.160 --> 00:03:00.320
So we're gonna write a minus sign in here,
00:03:00.320 --> 00:03:02.910
and then we're gonna put some brackets
00:03:02.910 --> 00:03:05.620
because next we're going
to sum the bond enthalpies
00:03:05.620 --> 00:03:07.580
of the bonds that are formed.
00:03:07.580 --> 00:03:08.550
In our balanced equation,
00:03:08.550 --> 00:03:12.250
we formed two moles of carbon dioxide.
00:03:12.250 --> 00:03:14.530
So to represent those two moles,
00:03:14.530 --> 00:03:15.400
I've drawn in here,
00:03:15.400 --> 00:03:18.620
two molecules of CO2.
00:03:18.620 --> 00:03:22.110
And we can see that in
each molecule of CO2,
00:03:22.110 --> 00:03:27.110
we're going to form two
carbon-oxygen double bonds.
00:03:27.540 --> 00:03:31.350
So that's a total of four
carbon-oxygen double bonds.
00:03:31.350 --> 00:03:32.780
So down here,
00:03:32.780 --> 00:03:37.780
we're going to write a four
times the bond enthalpy
00:03:38.020 --> 00:03:41.890
of a carbon-oxygen double bond.
00:03:41.890 --> 00:03:44.910
We also formed three moles of H2O.
00:03:44.910 --> 00:03:47.580
And in each molecule of
water that's drawn here,
00:03:47.580 --> 00:03:51.950
we form two oxygen-hydrogen single bonds.
00:03:51.950 --> 00:03:54.290
And since we have three moles,
00:03:54.290 --> 00:03:58.340
we have a total of six
oxygen-hydrogen single bonds.
00:03:58.340 --> 00:03:59.173
So to this,
00:03:59.173 --> 00:04:03.900
we're going to add six
times the bond enthalpy
00:04:03.900 --> 00:04:07.623
of an oxygen-hydrogen single bond.
00:04:08.810 --> 00:04:11.120
The next step is to look
up the bond enthalpies
00:04:11.120 --> 00:04:13.090
of all of these different bonds.
00:04:13.090 --> 00:04:14.640
For example, the bond enthalpy
00:04:14.640 --> 00:04:19.480
for a carbon-carbon single
bond is about 348 kilojoules
00:04:19.480 --> 00:04:20.313
per mole.
00:04:20.313 --> 00:04:21.540
You might see a different value,
00:04:21.540 --> 00:04:23.620
if you look in a different textbook.
00:04:23.620 --> 00:04:26.640
However, we're gonna go
with 348 kilojoules per mole
00:04:26.640 --> 00:04:28.350
for our calculation.
00:04:28.350 --> 00:04:29.450
And we're gonna multiply this
00:04:29.450 --> 00:04:32.960
by one mole of carbon-carbon single bonds.
00:04:32.960 --> 00:04:34.470
Next, we look up the bond enthalpy
00:04:34.470 --> 00:04:36.640
for our carbon-hydrogen single bond.
00:04:36.640 --> 00:04:39.840
And that's about 413 kilojoules per mole
00:04:39.840 --> 00:04:41.390
of carbon-hydrogen bonds.
00:04:41.390 --> 00:04:43.060
And we're multiplying this by five.
00:04:43.060 --> 00:04:45.560
And we continue with everything else
00:04:45.560 --> 00:04:47.820
for the summation of
the the bond enthalpies
00:04:47.820 --> 00:04:49.560
of the bonds broken.
00:04:49.560 --> 00:04:51.000
When we do this,
00:04:51.000 --> 00:04:56.000
we get positive 4,719 kilojoules.
00:04:56.530 --> 00:04:57.670
Next, we do the same thing
00:04:57.670 --> 00:04:59.430
for the bond enthalpies
00:04:59.430 --> 00:05:00.590
of the bonds that are formed.
00:05:00.590 --> 00:05:01.450
So the bond enthalpy
00:05:01.450 --> 00:05:05.460
for our carbon-oxygen double
bond is 799 kilojoules
00:05:05.460 --> 00:05:06.293
per mole,
00:05:06.293 --> 00:05:08.020
and we multiply that by four.
00:05:08.020 --> 00:05:10.760
The bonds enthalpy for an
oxygen hydrogen single bond
00:05:10.760 --> 00:05:13.030
is 463 kilojoules per mole,
00:05:13.030 --> 00:05:14.940
and we multiply that by six.
00:05:14.940 --> 00:05:15.880
When we add these together,
00:05:15.880 --> 00:05:20.350
we get 5,974.
00:05:20.350 --> 00:05:23.210
So for the final standard
change in enthalpy
00:05:23.210 --> 00:05:25.090
for our chemical reaction,
00:05:25.090 --> 00:05:30.090
it's positive 4,719 minus 5,974,
00:05:31.540 --> 00:05:36.540
which gives us negative 1,255 kilojoules.
00:05:37.280 --> 00:05:39.460
Notice that we got a negative value
00:05:39.460 --> 00:05:41.420
for the change in enthalpy.
00:05:41.420 --> 00:05:43.860
And that means the combustion of ethanol
00:05:43.860 --> 00:05:46.160
is an exothermic reaction.
00:05:46.160 --> 00:05:50.840
And 1,255 kilojoules
of energy are given off
00:05:50.840 --> 00:05:52.880
for the combustion of one mole
00:05:52.880 --> 00:05:54.390
of ethanol.
00:05:54.390 --> 00:05:56.750
Also notice that the sum
of the bond enthalpies
00:05:56.750 --> 00:05:57.950
of the bonds formed,
00:05:57.950 --> 00:06:01.040
which is 5,974,
00:06:01.040 --> 00:06:03.790
is greater than the sum
of the bond enthalpies
00:06:03.790 --> 00:06:04.830
of the bonds broken,
00:06:04.830 --> 00:06:07.480
which is 4,719.
00:06:07.480 --> 00:06:10.270
And since we're
subtracting a larger number
00:06:10.270 --> 00:06:11.500
from a smaller number,
00:06:11.500 --> 00:06:12.980
we get that negative sign
00:06:12.980 --> 00:06:15.240
for the change in enthalpy.
00:06:15.240 --> 00:06:17.160
If the sum of the bond enthalpies
00:06:17.160 --> 00:06:18.480
of the bonds that are broken,
00:06:18.480 --> 00:06:21.180
if this number is larger than the sum
00:06:21.180 --> 00:06:22.030
of the bond enthalpies
00:06:22.030 --> 00:06:23.120
of the bonds that have formed,
00:06:23.120 --> 00:06:24.700
we would've gotten a positive value
00:06:24.700 --> 00:06:26.480
for the change in enthalpy.
00:06:26.480 --> 00:06:29.950
And that would be true for
an endothermic reaction.
00:06:29.950 --> 00:06:30.783
We did this problem,
00:06:30.783 --> 00:06:32.290
assuming that all of the bonds
00:06:32.290 --> 00:06:34.540
that we drew in our dots
structures were broken
00:06:34.540 --> 00:06:35.470
and all of the bonds
00:06:35.470 --> 00:06:37.890
that we drew in the dot
structures were formed.
00:06:37.890 --> 00:06:39.950
However, if we look
closely to dots structures
00:06:39.950 --> 00:06:41.810
or just look closely
to what we wrote here,
00:06:41.810 --> 00:06:46.810
we show breaking one oxygen-hydrogen
single bonds over here,
00:06:47.640 --> 00:06:48.780
and we show the formation
00:06:48.780 --> 00:06:53.270
of six oxygen-hydrogen
single bonds over here.
00:06:53.270 --> 00:06:55.320
So we could have just canceled out one
00:06:55.320 --> 00:06:57.840
of those oxygen-hydrogen single bonds.
00:06:57.840 --> 00:06:59.600
So we could have canceled this out.
00:06:59.600 --> 00:07:01.300
And instead of showing a six here,
00:07:01.300 --> 00:07:04.920
we could have written a
five times the bond enthalpy
00:07:04.920 --> 00:07:08.520
of an oxygen-hydrogen single bond.
00:07:08.520 --> 00:07:10.630
We still would have ended
up with the same answer
00:07:10.630 --> 00:07:14.250
of negative 1,255 kilojoules.
00:07:14.250 --> 00:07:15.910
So if you look at your dot structures,
00:07:15.910 --> 00:07:18.930
if you see a bond that's the
same on the reactant side
00:07:18.930 --> 00:07:21.116
and the same on the product side,
00:07:21.116 --> 00:07:23.640
you don't have to show the breaking
00:07:23.640 --> 00:07:25.360
and forming of that bond.
00:07:25.360 --> 00:07:27.410
You can make the problem
a little bit shorter,
00:07:27.410 --> 00:07:28.373
if you want to.
00:07:29.280 --> 00:07:31.400
Finally, let's show how we get our units.
00:07:31.400 --> 00:07:34.420
So to get kilojoules as your final answer,
00:07:34.420 --> 00:07:35.790
if we go back up to here,
00:07:35.790 --> 00:07:38.770
we wrote a one times 348.
00:07:38.770 --> 00:07:42.400
The one is referring to breaking one mole
00:07:42.400 --> 00:07:44.870
of carbon-carbon single bonds.
00:07:44.870 --> 00:07:46.690
And the 348, of course,
00:07:46.690 --> 00:07:48.160
is the bond enthalpy
00:07:48.160 --> 00:07:50.030
for a carbon-carbon single bond.
00:07:50.030 --> 00:07:54.340
So this was 348 kilojoules per one mole
00:07:54.340 --> 00:07:57.220
of carbon-carbon single bonds.
00:07:57.220 --> 00:07:59.140
When you multiply these two together,
00:07:59.140 --> 00:08:02.530
the moles of carbon-carbon
single bonds cancels
00:08:02.530 --> 00:08:06.317
and this gives you 348 kilojoules.
00:08:06.317 --> 00:08:07.630
And so, that's how to end up
00:08:07.630 --> 00:08:11.270
with kilojoules as your final answer.
00:08:11.270 --> 00:08:14.880
You also might see kilojoules
per mole of reaction
00:08:14.880 --> 00:08:16.880
as the units for this.
00:08:16.880 --> 00:08:19.580
And, kilojoules per mole reaction means
00:08:19.580 --> 00:08:21.510
how the reaction is written.
00:08:21.510 --> 00:08:22.670
So for the combustion
00:08:22.670 --> 00:08:24.780
of one mole of ethanol,
00:08:24.780 --> 00:08:29.720
1,255 kilojoules of energy are released.
00:08:29.720 --> 00:08:33.980
To get kilojoules per mole
of reaction as our units,
00:08:33.980 --> 00:08:36.620
the balanced equation had
a one as the coefficient
00:08:36.620 --> 00:08:38.630
in front of ethanol.
00:08:38.630 --> 00:08:41.070
Therefore, you're breaking one mole
00:08:41.070 --> 00:08:45.080
of carbon-carbon single bonds per one mole
00:08:45.080 --> 00:08:46.160
of reaction.
00:08:46.160 --> 00:08:48.950
So we can use this conversion factor.
00:08:48.950 --> 00:08:51.410
Now, when we multiply through the moles
00:08:51.410 --> 00:08:52.900
of carbon-carbon single bonds,
00:08:52.900 --> 00:08:57.900
cancel and this gives us
348 kilojoules per mole
00:08:59.000 --> 00:09:00.533
of reaction.
|
Bond enthalpies | https://www.youtube.com/watch?v=VxcqAIaO-cA | vtt | https://www.youtube.com/api/timedtext?v=VxcqAIaO-cA&ei=5VWUZeOOJJLXxN8Pz9idoA0&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=4C1532868C4A8BEC4C1DF614961B372A98739079.1AA6FD6E7CCAC430663C4EF3220534A4C8D376C3&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.960 --> 00:00:03.300
- [Instructor] Bond enthalpy
is the change in enthalpy
00:00:03.300 --> 00:00:06.200
or delta H for breaking a particular bond
00:00:06.200 --> 00:00:08.710
in one mole of a gaseous substance.
00:00:08.710 --> 00:00:11.040
If we think about the
diatomic chlorine molecule,
00:00:11.040 --> 00:00:14.280
so Cl2, down here is a
little picture of Cl2,
00:00:14.280 --> 00:00:16.540
each of the green spheres
is a chlorine atom
00:00:16.540 --> 00:00:19.510
and they're bonded together
by a single covalent bond.
00:00:19.510 --> 00:00:21.990
It would take energy to break this bond
00:00:21.990 --> 00:00:23.840
in diatomic chlorine gas
00:00:23.840 --> 00:00:26.570
and turn diatomic chlorine gas, Cl2
00:00:26.570 --> 00:00:29.210
in to two individual chlorine atoms.
00:00:29.210 --> 00:00:33.580
So we're going from Cl2 in
the gaseous state to 2Cl.
00:00:33.580 --> 00:00:37.280
Bond enthalpy can be
symbolized by the letters BE.
00:00:37.280 --> 00:00:41.100
So the bond enthalpy of the
chlorine-chlorine single bond
00:00:41.100 --> 00:00:45.900
is equal to +242 kilojoules per mole.
00:00:45.900 --> 00:00:46.810
And what this means is,
00:00:46.810 --> 00:00:49.160
if we have one mole of
chlorine-chlorine bonds,
00:00:49.160 --> 00:00:54.160
it takes +242 kilojoules of
energy to break those bonds.
00:00:55.008 --> 00:00:57.150
Bond enthalpies are always positive
00:00:57.150 --> 00:01:00.370
because it takes energy to break bonds.
00:01:00.370 --> 00:01:04.270
Another name for bond enthalpy
is bond dissociation energy.
00:01:04.270 --> 00:01:07.600
So you might see this symbolized as BDE
00:01:07.600 --> 00:01:10.800
or just simply the letter D.
00:01:10.800 --> 00:01:12.680
Bond enthalpies are often found
00:01:12.680 --> 00:01:15.965
in the appendices of chemistry textbooks.
00:01:15.965 --> 00:01:19.610
For example, we just saw the
chlorine-chlorine single bond,
00:01:19.610 --> 00:01:23.290
the bond enthalpy is
242 kilojoules per mole.
00:01:23.290 --> 00:01:26.160
Whereas to break a
carbon-carbon single bond
00:01:26.160 --> 00:01:29.300
takes 348 kilojoules of energy per mole
00:01:29.300 --> 00:01:31.620
of carbon-carbon single bonds.
00:01:31.620 --> 00:01:34.100
A carbon-carbon double
bond has a bond enthalpy
00:01:34.100 --> 00:01:37.310
of 614 kilojoules per mole.
00:01:37.310 --> 00:01:40.320
Since the carbon-carbon
double bond is stronger
00:01:40.320 --> 00:01:42.000
than a carbon-carbon single bond,
00:01:42.000 --> 00:01:44.910
it takes more energy to
break the double bond.
00:01:44.910 --> 00:01:47.010
And that's why the
carbon-carbon double bond
00:01:47.010 --> 00:01:50.320
has a high higher bond enthalpy.
00:01:50.320 --> 00:01:52.460
So the higher the value
for the bond enthalpy,
00:01:52.460 --> 00:01:54.410
the stronger the bond.
00:01:54.410 --> 00:01:56.810
Notice that these are
average bond enthalpies.
00:01:56.810 --> 00:01:58.400
So the average bond enthalpy
00:01:58.400 --> 00:02:00.480
for a carbon-carbon single bond
00:02:00.480 --> 00:02:03.530
is around 348 kilojoules per mole.
00:02:03.530 --> 00:02:05.920
You might see slightly
different values for this,
00:02:05.920 --> 00:02:08.100
depending on which
textbook you're looking in,
00:02:08.100 --> 00:02:10.700
but they're all pretty
close to the same value.
00:02:10.700 --> 00:02:12.905
The reason why these are
average bond enthalpies
00:02:12.905 --> 00:02:16.640
is because if we look at two
different molecules down here,
00:02:16.640 --> 00:02:20.060
this is ethane on the left
and propane on the right,
00:02:20.060 --> 00:02:23.250
if we break a carbon-carbon
single bond in ethane,
00:02:23.250 --> 00:02:25.460
the bond enthalpy is slightly different
00:02:25.460 --> 00:02:28.580
from breaking a carbon-carbon
single bond in propane.
00:02:28.580 --> 00:02:32.830
And that's why we use
average bond enthalpies.
00:02:32.830 --> 00:02:35.740
We've already seen that it
takes energy to break bonds.
00:02:35.740 --> 00:02:39.100
So to break the
chlorine-chlorine single bond
00:02:39.100 --> 00:02:44.100
in diatomic chlorine gas takes
+242 kilojoules per mole.
00:02:44.500 --> 00:02:46.320
If it takes energy to break bonds,
00:02:46.320 --> 00:02:49.890
that means energy is
given off when bonds form.
00:02:49.890 --> 00:02:53.510
So when two individual chlorine
gas atoms come together
00:02:53.510 --> 00:02:56.740
to form a chlorine-chlorine bond,
00:02:56.740 --> 00:02:58.270
so let's go into highlight that in here.
00:02:58.270 --> 00:03:02.020
So this bond is forming,
energy is given off.
00:03:02.020 --> 00:03:06.310
The magnitude of energy is
still 242 kilojoules per mole,
00:03:06.310 --> 00:03:08.700
however, now we have this
negative sign in here
00:03:08.700 --> 00:03:12.660
to indicate the energy is
given off when bonds form.
00:03:12.660 --> 00:03:14.660
Bond enthalpies can be used to estimate
00:03:14.660 --> 00:03:16.240
enthalpies of reactions.
00:03:16.240 --> 00:03:17.970
So to find the change in the enthalpy
00:03:17.970 --> 00:03:20.577
for a chemical reaction, you take the sum
00:03:20.577 --> 00:03:23.870
of the bond enthalpies
of the bonds broken.
00:03:23.870 --> 00:03:26.120
And from that you subtract the sum
00:03:26.120 --> 00:03:29.400
of the bond enthalpies
of the bonds formed.
00:03:29.400 --> 00:03:31.240
The minus sign is in there because energy
00:03:31.240 --> 00:03:33.920
is given off when bonds form.
00:03:33.920 --> 00:03:35.940
A good way to remember this equation
00:03:35.940 --> 00:03:40.020
is to remember that B comes
before F in the alphabet.
00:03:40.020 --> 00:03:42.700
So B before F therefore it's bonds broken
00:03:42.700 --> 00:03:44.860
minus bonds formed.
00:03:44.860 --> 00:03:47.100
Let's use bond enthalpies to estimate
00:03:47.100 --> 00:03:50.400
the enthalpy of reaction for
the following reaction here,
00:03:50.400 --> 00:03:54.380
methane with chlorine gas
to form chloro methane
00:03:54.380 --> 00:03:56.950
and hydrogen chloride gas.
00:03:56.950 --> 00:03:59.040
It's often helpful to draw dot structures
00:03:59.040 --> 00:04:00.690
for these kinds of problems.
00:04:00.690 --> 00:04:03.330
If we look at the methane dot structure,
00:04:03.330 --> 00:04:07.670
we would need to break one
carbon-hydrogen single bond
00:04:07.670 --> 00:04:09.350
in order to get to our products.
00:04:09.350 --> 00:04:13.220
We would also need to break a
chlorine-chlorine single bond.
00:04:13.220 --> 00:04:18.130
Next, one of the chlorine
goes over to the CH3
00:04:18.130 --> 00:04:19.200
to form CH3Cl.
00:04:19.200 --> 00:04:21.920
So therefore we are forming
00:04:21.920 --> 00:04:24.830
one carbon-chlorine single bonds,
00:04:24.830 --> 00:04:27.480
and the other Cl goes with the hydrogen.
00:04:27.480 --> 00:04:32.090
So we also need to form one
hydrogen-chlorine single bond.
00:04:32.090 --> 00:04:35.150
The next step is to
sum the bond enthalpies
00:04:35.150 --> 00:04:37.200
of the bonds broken.
00:04:37.200 --> 00:04:38.330
So let's think about this.
00:04:38.330 --> 00:04:40.430
For our reactants we're breaking bonds.
00:04:40.430 --> 00:04:42.170
So we have one mole of methane
00:04:42.170 --> 00:04:45.170
reacting with one mole of chlorine.
00:04:45.170 --> 00:04:48.840
And since we're breaking one
carbon-hydrogen single bond
00:04:48.840 --> 00:04:51.000
for every one molecule of methane,
00:04:51.000 --> 00:04:53.670
since we have one mole
of methane molecules,
00:04:53.670 --> 00:04:58.330
we're breaking one mole of
carbon-hydrogen single bonds.
00:04:58.330 --> 00:05:00.070
Therefore we can write down here,
00:05:00.070 --> 00:05:03.660
one mole of carbon-hydrogen bonds,
00:05:03.660 --> 00:05:07.720
and the bond enthalpy for a
carbon-hydrogen single bond
00:05:07.720 --> 00:05:12.323
is 413 kilojoules per mole.
00:05:14.510 --> 00:05:17.520
Since there's one
chlorine-chlorine single bond
00:05:17.520 --> 00:05:19.540
for every Cl2 molecule,
00:05:19.540 --> 00:05:22.630
and we have one mole
of chlorine molecules,
00:05:22.630 --> 00:05:26.120
we're breaking one mole of
chlorine-chlorine single bonds.
00:05:26.120 --> 00:05:28.830
So to this we're gonna add one mole
00:05:28.830 --> 00:05:31.170
of chlorine-chlorine single bonds.
00:05:31.170 --> 00:05:34.860
And the bond enthalpy for a
chlorine-chlorine single bond
00:05:34.860 --> 00:05:39.363
is 242 kilojoules per mole.
00:05:40.550 --> 00:05:43.700
Moles cancel out and we get that the sum
00:05:43.700 --> 00:05:46.050
of the bond enthalpies of the bonds broken
00:05:46.050 --> 00:05:51.050
is equal to 655 kilojoules.
00:05:51.240 --> 00:05:53.081
Next, we need to sum the bond enthalpies
00:05:53.081 --> 00:05:54.950
of the bonds formed.
00:05:54.950 --> 00:05:58.150
So we're forming one
mole of chloro methane
00:05:58.150 --> 00:06:01.970
and one mole of hydrogen chloride gas.
00:06:01.970 --> 00:06:05.840
And since we're forming one
carbon-chlorine single bond
00:06:05.840 --> 00:06:08.620
for every molecule of chloro methane,
00:06:08.620 --> 00:06:10.900
since we're forming one
mole of chloral methane,
00:06:10.900 --> 00:06:15.070
we're reforming one mole of
carbon-chlorine single bonds.
00:06:15.070 --> 00:06:17.640
So let's write down here,
we're forming one mole
00:06:17.640 --> 00:06:21.014
of carbon-chlorine bonds
and the bond enthalpy
00:06:21.014 --> 00:06:23.550
for a carbon-chlorine single bond
00:06:23.550 --> 00:06:28.550
is equal to 328 kilojoules per mole.
00:06:30.980 --> 00:06:34.112
And since we form one
hydrogen-chlorine single bond
00:06:34.112 --> 00:06:36.760
for every molecule of hydrogen chloride,
00:06:36.760 --> 00:06:39.370
since we're making one
mole of hydrogen chloride,
00:06:39.370 --> 00:06:43.310
we're forming one mole of
hydrogen-chlorine single bonds.
00:06:43.310 --> 00:06:46.140
So to this we add one mole
00:06:46.140 --> 00:06:50.120
of hydrogen-chlorine single
bonds and the bond enthalpy
00:06:50.120 --> 00:06:52.080
for a hydrogen-chlorine single bond
00:06:52.080 --> 00:06:57.063
is 431 kilojoules per mole.
00:06:58.660 --> 00:07:02.530
Moles cancel and we get that
the sum of the bond enthalpies
00:07:02.530 --> 00:07:07.530
of the bonds formed is
equal to 759 kilojoules.
00:07:09.690 --> 00:07:11.966
Next, we're ready to find
the change in enthalpy
00:07:11.966 --> 00:07:14.720
for our chemical reaction.
00:07:14.720 --> 00:07:18.020
The sum of the enthalpy
of the bonds broken,
00:07:18.020 --> 00:07:21.670
we found that was equal to 655 kilojoules.
00:07:21.670 --> 00:07:24.049
And from that we subtract the
sum of the bond enthalpies
00:07:24.049 --> 00:07:29.049
of the bonds formed, which
we found was 759 kilojoules.
00:07:29.420 --> 00:07:34.420
So 655 minus 759 gives -104 kilojoules.
00:07:37.430 --> 00:07:40.710
Sometimes we see kilojoules
or kilojoules per mole
00:07:40.710 --> 00:07:43.330
or kilojoules per mole of reaction.
00:07:43.330 --> 00:07:45.460
Kilojoules per mole of reaction just means
00:07:45.460 --> 00:07:48.180
how the balanced equation is written.
00:07:48.180 --> 00:07:50.170
And let's see how we can look at the units
00:07:50.170 --> 00:07:52.570
to get kilojoules per mole of reaction
00:07:52.570 --> 00:07:54.680
when we do the calculations.
00:07:54.680 --> 00:07:56.190
If you go back to breaking
00:07:56.190 --> 00:08:00.200
the carbon hydrogen bond over here,
00:08:00.200 --> 00:08:03.780
we've seen there's one mole
of carbon-hydrogen bonds
00:08:03.780 --> 00:08:06.950
that we need to break for
how the equation is written.
00:08:06.950 --> 00:08:09.030
Therefore, we can write
a conversion factor
00:08:09.030 --> 00:08:11.320
of one mole of carbon-hydrogen bonds
00:08:11.320 --> 00:08:14.160
per one mole of reaction as it's written.
00:08:14.160 --> 00:08:16.900
And then we multiply
that by the bond enthalpy
00:08:16.900 --> 00:08:21.190
as 413 kilojoules per mole
for a carbon-hydrogen bond,
00:08:21.190 --> 00:08:24.120
this cancels out moles
of carbon-hydrogen bonds
00:08:24.120 --> 00:08:27.010
and this gives us kilojoules
per mole of reaction
00:08:27.010 --> 00:08:28.480
as our units.
00:08:28.480 --> 00:08:30.530
So it's more time consuming
to write it this way
00:08:30.530 --> 00:08:31.860
but we could do that for all
00:08:31.860 --> 00:08:33.540
of our different bond enthalpies
00:08:33.540 --> 00:08:35.450
to get kilojoules per mole of reaction
00:08:35.450 --> 00:08:37.600
for the units for our final answer.
00:08:37.600 --> 00:08:39.300
When everything is under
standard conditions,
00:08:39.300 --> 00:08:41.400
we need to add a superscript of note.
00:08:41.400 --> 00:08:44.770
So this would be the
standard change in enthalpy
00:08:44.770 --> 00:08:46.930
for a chemical reaction.
00:08:46.930 --> 00:08:48.740
So for the value we just calculated,
00:08:48.740 --> 00:08:52.520
- 140 kilojoules per mole of reaction,
00:08:52.520 --> 00:08:53.870
this is under standard of conditions.
00:08:53.870 --> 00:08:56.330
So this is actually the
standard change in enthalpy
00:08:56.330 --> 00:08:58.850
for this chemical reaction.
00:08:58.850 --> 00:09:01.950
Remember that bond
enthalpies are only averages.
00:09:01.950 --> 00:09:05.340
And so this value that we
calculated is only an estimate
00:09:05.340 --> 00:09:07.050
for the standard change in enthalpy
00:09:07.050 --> 00:09:08.950
for this chemical reaction.
00:09:08.950 --> 00:09:11.350
A more accurate way of
finding this standard change
00:09:11.350 --> 00:09:13.580
in enthalpy for a chemical reaction
00:09:13.580 --> 00:09:16.476
is to use standard
enthalpies of formation.
00:09:16.476 --> 00:09:19.580
And when you use standard
enthalpies of formation
00:09:19.580 --> 00:09:21.460
to find the standard change in enthalpy
00:09:21.460 --> 00:09:23.330
for this particular chemical reaction,
00:09:23.330 --> 00:09:28.330
you get -99.8 kilojoules
per mole of reaction.
00:09:28.560 --> 00:09:32.413
So -104 is pretty close to -99.8.
|
Enthalpy of formation | https://www.youtube.com/watch?v=TNwGNHqwHxc | vtt | https://www.youtube.com/api/timedtext?v=TNwGNHqwHxc&ei=5VWUZfHKL9nWxN8PoKaHyAQ&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=4A8AB4333AAFA29804CECDF0856BAA3DB605E332.36D8FEA60FDC753A04CB806B1E2EB6899C52A6CD&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.910 --> 00:00:01.890
- [Instructor] Enthalpy of a formation
00:00:01.890 --> 00:00:03.830
refers to the change in enthalpy
00:00:03.830 --> 00:00:06.400
for the formation of one mole
00:00:06.400 --> 00:00:09.320
of a substance from the most stable form
00:00:09.320 --> 00:00:11.870
of its constituent elements.
00:00:11.870 --> 00:00:13.380
Change in enthalpy is symbolized
00:00:13.380 --> 00:00:17.060
by delta H and the f stands for formation.
00:00:17.060 --> 00:00:20.670
And the superscript
nought refers to the fact
00:00:20.670 --> 00:00:23.440
that everything is under
standard state conditions,
00:00:23.440 --> 00:00:25.600
which refers to atmospheric pressure
00:00:25.600 --> 00:00:28.830
of one atmosphere and
a specified temperature
00:00:28.830 --> 00:00:33.240
that is usually 25 degrees Celsius.
00:00:33.240 --> 00:00:36.490
So when we're thinking about
standard enthalpy of formation,
00:00:36.490 --> 00:00:38.100
we're thinking about the elements
00:00:38.100 --> 00:00:40.730
and the state that they exist
under standard conditions.
00:00:40.730 --> 00:00:43.880
So the elements have to be
in their standard states.
00:00:43.880 --> 00:00:48.420
So let's think about forming
one mole of carbon dioxide.
00:00:48.420 --> 00:00:51.370
So carbon dioxide is
composed of the elements
00:00:51.370 --> 00:00:53.680
carbon and oxygen.
00:00:53.680 --> 00:00:55.610
And under standard conditions,
00:00:55.610 --> 00:01:00.200
the most stable form
of carbon is graphite.
00:01:00.200 --> 00:01:02.710
So we're gonna write
carbon in the solid state
00:01:02.710 --> 00:01:05.590
and we're gonna write graphite over here.
00:01:05.590 --> 00:01:08.900
And next, when you think
about the most stable form
00:01:08.900 --> 00:01:11.910
of oxygen under standard conditions.
00:01:11.910 --> 00:01:15.030
And so at one atmosphere,
so atmospheric pressure
00:01:15.030 --> 00:01:17.590
and room temperature
of 25 degrees Celsius,
00:01:17.590 --> 00:01:20.700
the most stable form of
oxygen is oxygen gas.
00:01:20.700 --> 00:01:23.403
So we can go ahead and write in here O2.
00:01:24.490 --> 00:01:27.200
And since we're forming
one mole of carbon dioxide
00:01:27.200 --> 00:01:29.920
from the elements that
make up carbon dioxide
00:01:29.920 --> 00:01:33.620
in their most stable form
under standard conditions,
00:01:33.620 --> 00:01:35.590
the change in enthalpy for this
00:01:35.590 --> 00:01:38.420
would be the standard
enthalpy of formation.
00:01:38.420 --> 00:01:39.910
So we have our subscript f
00:01:39.910 --> 00:01:43.550
and our superscript nought
indicate standard conditions.
00:01:43.550 --> 00:01:46.370
The change in enthalpy for the formation
00:01:46.370 --> 00:01:51.247
of one mole of CO2 is equal
to negative 393.5 kilojoules
00:01:54.160 --> 00:01:56.673
per one mole of carbon dioxide.
00:01:57.620 --> 00:01:59.590
Let's look at some more
equations showing the formation
00:01:59.590 --> 00:02:01.210
of one mole of a substance.
00:02:01.210 --> 00:02:02.930
For example, let's look at the equation
00:02:02.930 --> 00:02:06.030
showing the formation
of one mole of water.
00:02:06.030 --> 00:02:08.490
So water is composed
of hydrogen and oxygen
00:02:08.490 --> 00:02:10.720
and the most stable forms
of those two elements
00:02:10.720 --> 00:02:14.170
under standard conditions are
hydrogen gas and oxygen gas.
00:02:14.170 --> 00:02:17.590
And for the coefficients
to make one mole of water,
00:02:17.590 --> 00:02:21.010
we need a 1/2 as our
coefficient in front of O2.
00:02:21.010 --> 00:02:23.960
The standard change in
enthalpy of formation
00:02:23.960 --> 00:02:26.270
for the formation of one mole of water
00:02:26.270 --> 00:02:30.720
is negative 285.8 kilojoules per mole.
00:02:30.720 --> 00:02:32.850
We can do the same thing for
the formation of one mole
00:02:32.850 --> 00:02:34.800
of methane CH4.
00:02:34.800 --> 00:02:36.640
We already know that the most stable form
00:02:36.640 --> 00:02:38.210
of carbon is graphite
00:02:38.210 --> 00:02:41.470
and the most stable form of
hydrogen is hydrogen gas.
00:02:41.470 --> 00:02:44.810
And the standard change
in enthalpy of formation
00:02:44.810 --> 00:02:46.720
for the formation of one mole of methane
00:02:46.720 --> 00:02:50.770
is equal to negative
74.8 kilojoules per mole.
00:02:50.770 --> 00:02:55.160
Next, let's think about
forming one mole of oxygen gas.
00:02:55.160 --> 00:02:56.850
Well, we're forming the oxygen gas
00:02:56.850 --> 00:02:59.050
from the most stable form of oxygen
00:02:59.050 --> 00:03:00.210
under standard conditions,
00:03:00.210 --> 00:03:04.070
which is also diatomic oxygen gas, O2.
00:03:04.070 --> 00:03:06.880
So we're not changing anything
we're going from O2 to O2.
00:03:06.880 --> 00:03:09.900
And since there's no change,
there's no change in enthalpy.
00:03:09.900 --> 00:03:11.700
Therefore, the standard enthalpy
00:03:11.700 --> 00:03:15.200
of formation is equal to zero.
00:03:15.200 --> 00:03:17.940
And this is true for the most
stable form of any element.
00:03:17.940 --> 00:03:19.430
The standard enthalpy of formation
00:03:19.430 --> 00:03:22.120
of the most stable form
of any element is zero
00:03:22.120 --> 00:03:24.830
since you'd be making it from itself.
00:03:24.830 --> 00:03:27.600
Standard enthalpies of formation
and kilojoules per mole
00:03:27.600 --> 00:03:31.410
are often found in the
appendices of many textbooks.
00:03:31.410 --> 00:03:33.380
And if you look in the
appendix of a textbook,
00:03:33.380 --> 00:03:36.020
you'll see the standard
enthalpy of formation
00:03:36.020 --> 00:03:40.740
for diatomic oxygen gas,
O2, is equal to zero.
00:03:40.740 --> 00:03:44.760
Ozone, which is O3, also exists
under standard conditions.
00:03:44.760 --> 00:03:48.190
However, it's not the
most stable form of oxygen
00:03:48.190 --> 00:03:49.930
under standard conditions and therefore,
00:03:49.930 --> 00:03:54.930
its standard enthalpy formation
is not zero, it's 142.3.
00:03:56.020 --> 00:03:58.550
Graphite is the most stable form of carbon
00:03:58.550 --> 00:03:59.550
under standard conditions.
00:03:59.550 --> 00:04:01.230
Therefore, it has a standard enthalpy
00:04:01.230 --> 00:04:03.720
of formation of zero, but of course,
00:04:03.720 --> 00:04:06.500
diamond also exists
under standard conditions
00:04:06.500 --> 00:04:07.860
but it's not the most stable form.
00:04:07.860 --> 00:04:10.890
So its standard enthalpy
formation is not zero,
00:04:10.890 --> 00:04:14.050
it's 1.88 kilojoules per mole.
00:04:14.050 --> 00:04:16.610
Enthalpies of formation
can be used to calculate
00:04:16.610 --> 00:04:19.990
the change in enthalpy
for a chemical reaction.
00:04:19.990 --> 00:04:22.560
We can do this by using
the following equation.
00:04:22.560 --> 00:04:26.160
The standard change in enthalpy
for a chemical reaction
00:04:26.160 --> 00:04:31.160
is equal to the sum of the
standard enthalpies of formation
00:04:31.230 --> 00:04:34.880
of the products minus the sum
of the standard enthalpies
00:04:34.880 --> 00:04:37.580
of formation of the reactants.
00:04:37.580 --> 00:04:39.810
Let's say our goal is to
find the standard change
00:04:39.810 --> 00:04:42.960
in enthalpy for the
following chemical reaction.
00:04:42.960 --> 00:04:44.360
So we have one mole of methane
00:04:44.360 --> 00:04:46.060
reacting with two moles of oxygen
00:04:46.060 --> 00:04:50.830
to form one mole of carbon
dioxide and two moles of water.
00:04:50.830 --> 00:04:53.340
The first thing we need to do is sum
00:04:53.340 --> 00:04:57.090
all the standard enthalpies
of formation of the products.
00:04:57.090 --> 00:04:59.550
So if we look at our
two products over here
00:04:59.550 --> 00:05:02.760
and we'll start with one
mole of carbon dioxide.
00:05:02.760 --> 00:05:04.460
So let's go ahead and
write this down here.
00:05:04.460 --> 00:05:07.120
We have one mole of carbon dioxide
00:05:07.120 --> 00:05:10.760
and the standard molar
enthalpy of carbon dioxide
00:05:10.760 --> 00:05:14.340
we've already seen as
negative 393.5 kilojoules
00:05:14.340 --> 00:05:16.590
per mole of carbon dioxide.
00:05:16.590 --> 00:05:18.980
So we're gonna multiply
one mole of carbon dioxide
00:05:18.980 --> 00:05:23.980
by negative 393.5 kilojoules
per mole of carbon dioxide.
00:05:28.400 --> 00:05:31.490
Our other product is two moles of water.
00:05:31.490 --> 00:05:34.610
So we're going to add
this to the other ones.
00:05:34.610 --> 00:05:37.530
We have two moles of H2O.
00:05:37.530 --> 00:05:40.040
And the standard enthalpy
of formation of H2O
00:05:40.040 --> 00:05:42.460
is negative 285.8.
00:05:42.460 --> 00:05:43.530
So we're gonna multiply this
00:05:43.530 --> 00:05:48.530
by negative 285.8 kilojoules per mole.
00:05:51.600 --> 00:05:56.600
So moles cancel out and we
get negative 393.5 kilojoules.
00:05:57.910 --> 00:05:59.990
And then for the other one,
moles cancel out again.
00:05:59.990 --> 00:06:04.140
And this would be plus
negative 571.6 kilojoules,
00:06:07.340 --> 00:06:12.340
which is equal to
negative 965.1 kilojoules.
00:06:12.710 --> 00:06:15.550
So that's the sum of all
00:06:15.550 --> 00:06:20.540
of the standard enthalpies
of formation of our products.
00:06:20.540 --> 00:06:23.170
Next, we need to sum
the standard enthalpies
00:06:23.170 --> 00:06:24.920
of formation of our reactants.
00:06:24.920 --> 00:06:28.930
So the two reactants that we
have are methane and oxygen
00:06:28.930 --> 00:06:31.730
and we have one mole of methane.
00:06:31.730 --> 00:06:33.810
So let's go ahead and write that in here.
00:06:33.810 --> 00:06:35.650
So we have one mole of methane.
00:06:35.650 --> 00:06:38.570
The standard molar enthalpy
of formation of methane
00:06:38.570 --> 00:06:42.260
is negative 74.8 kilojoules per mole.
00:06:42.260 --> 00:06:43.430
So we're multiplying one mole
00:06:43.430 --> 00:06:48.430
by negative 74.8 kilojoules per mole.
00:06:50.860 --> 00:06:53.840
Our other reactant is oxygen.
00:06:53.840 --> 00:06:56.270
And we know that diatomic oxygen gas
00:06:56.270 --> 00:06:59.250
has a standard enthalpy
of formation of zero.
00:06:59.250 --> 00:07:00.560
So we could go ahead and write this in
00:07:00.560 --> 00:07:01.560
just to show it.
00:07:01.560 --> 00:07:03.480
So we have two moles of oxygen
00:07:03.480 --> 00:07:06.113
but we're multiplying that number by zero.
00:07:07.300 --> 00:07:12.300
Some moles cancel and give
us negative 74.8 kilojoules.
00:07:12.490 --> 00:07:14.530
And we're adding zero to that.
00:07:14.530 --> 00:07:18.300
So negative 74.8 kilojoules
00:07:18.300 --> 00:07:22.980
is the sum of all the standard
enthalpies of formation
00:07:22.980 --> 00:07:24.547
of our reactants.
00:07:25.396 --> 00:07:28.020
So to find the standard change
in enthalpy for our reaction,
00:07:28.020 --> 00:07:30.820
we take the summation of
the enthalpies of formation
00:07:30.820 --> 00:07:35.040
of our products, which was
negative 965.1 kilojoules.
00:07:35.040 --> 00:07:36.940
And from that, we subtract the sum
00:07:36.940 --> 00:07:39.160
of the standard enthalpies of
formation of the reactants,
00:07:39.160 --> 00:07:43.220
which we found was
negative 74.8 kilojoules.
00:07:43.220 --> 00:07:47.700
So negative 965.1 minus negative 74.8
00:07:47.700 --> 00:07:52.700
is equal to negative 890.3 kilojoules.
00:07:54.300 --> 00:07:56.130
For the unit, sometimes
you see kilojoules,
00:07:56.130 --> 00:07:58.610
sometimes you see kilojoules per mole,
00:07:58.610 --> 00:08:01.830
and sometimes you see
kilojoules per mole of reaction.
00:08:01.830 --> 00:08:04.080
And what kilojoules per
mole a reaction means
00:08:04.080 --> 00:08:06.480
is how the balanced equation is written.
00:08:06.480 --> 00:08:07.530
For this balanced equation,
00:08:07.530 --> 00:08:10.790
we're showing the combustion
of one mole of methane.
00:08:10.790 --> 00:08:12.570
So combusting one mole of methane
00:08:12.570 --> 00:08:17.510
releases 890.3 kilojoules of energy.
00:08:17.510 --> 00:08:19.670
So that's what kilojoules
per mole of reaction
00:08:19.670 --> 00:08:20.573
is referring to.
00:08:21.650 --> 00:08:22.730
Let's go back to the step
00:08:22.730 --> 00:08:26.090
where we summed the standard
enthalpies of formation
00:08:26.090 --> 00:08:28.880
of the products to see how we
could actually get kilojoules
00:08:28.880 --> 00:08:32.460
per mole of reaction as our units.
00:08:32.460 --> 00:08:35.040
To do this, we need to
use a conversion factor.
00:08:35.040 --> 00:08:36.500
For how the equation is written,
00:08:36.500 --> 00:08:39.340
we're producing one
mole of carbon dioxide.
00:08:39.340 --> 00:08:41.510
So we can use as a conversion factor,
00:08:41.510 --> 00:08:46.510
there's one mole of carbon
dioxide per one mole of reaction.
00:08:49.420 --> 00:08:51.800
We can do the same thing
for our other product,
00:08:51.800 --> 00:08:52.930
which is water.
00:08:52.930 --> 00:08:54.500
For how the equation is written,
00:08:54.500 --> 00:08:56.790
we're forming two moles of water.
00:08:56.790 --> 00:09:01.440
So our conversion factor can
be there are two moles of water
00:09:01.440 --> 00:09:04.803
for every one mole of reaction.
00:09:06.190 --> 00:09:09.030
Next, moles of carbon dioxide cancels out
00:09:09.030 --> 00:09:11.660
and moles of water cancel out.
00:09:11.660 --> 00:09:14.710
And this gives us kilojoules
per mole of reaction
00:09:14.710 --> 00:09:16.350
as our units.
00:09:16.350 --> 00:09:17.730
It's a little more time-consuming
00:09:17.730 --> 00:09:19.310
to write out all the units this way.
00:09:19.310 --> 00:09:21.840
So often, it's faster
to do it the first way
00:09:21.840 --> 00:09:23.933
and add in these units at the end.
|
Worked example: Measuring enthalpy of reaction using coffee-cup calorimetry | https://www.youtube.com/watch?v=pDCcRU5OGmA | vtt | https://www.youtube.com/api/timedtext?v=pDCcRU5OGmA&ei=5VWUZbaYI6aJp-oPh-OQiAY&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=DE25469684320004502432802BDB3CD22E42AB45.82DDC43799890C5D97266EFEA1330B360DA9BB52&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.680 --> 00:00:02.600
- [Instructor] A constant
pressure calorimeter
00:00:02.600 --> 00:00:04.730
can be used to find the change in entropy
00:00:04.730 --> 00:00:06.980
for a chemical reaction.
00:00:06.980 --> 00:00:08.390
Let's look at the chemical reaction
00:00:08.390 --> 00:00:10.990
between an aqueous
solution of silver nitrate
00:00:10.990 --> 00:00:13.210
and aqueous solution of sodium chloride
00:00:13.210 --> 00:00:15.470
to form a precipitate of silver chloride
00:00:15.470 --> 00:00:18.490
and an aqueous solution of sodium nitrate.
00:00:18.490 --> 00:00:20.880
Let's say we have 25.0 milliliters
00:00:20.880 --> 00:00:25.490
of a 0.100 molar solution
of silver nitrate
00:00:25.490 --> 00:00:30.080
and 25.0 milliliters of
a 0.100 molar solution
00:00:30.080 --> 00:00:31.760
of sodium chloride.
00:00:31.760 --> 00:00:34.010
Both solutions are
initially at a temperature
00:00:34.010 --> 00:00:38.710
of 25.000 degrees Celsius.
00:00:38.710 --> 00:00:41.900
Next, we add our two
solutions to our calorimeter
00:00:41.900 --> 00:00:44.270
which has made of two coffee cups.
00:00:44.270 --> 00:00:47.240
And since the top coffee
cup is loose fitting,
00:00:47.240 --> 00:00:49.630
this reaction is under
the constant pressure
00:00:49.630 --> 00:00:50.800
of the atmosphere.
00:00:50.800 --> 00:00:54.080
So this is constant pressure calorimetry.
00:00:54.080 --> 00:00:57.570
After the two aqueous solutions
mix, the reaction occurs
00:00:57.570 --> 00:01:00.490
and we watch the thermometer
in the calorimeter.
00:01:00.490 --> 00:01:04.240
In this case, the temperature
of the solution increases
00:01:04.240 --> 00:01:05.860
and the final temperature,
00:01:05.860 --> 00:01:07.700
the highest one reached in our experiment
00:01:07.700 --> 00:01:12.100
is 25.781 degrees Celsius.
00:01:12.100 --> 00:01:14.130
So the change in the
temperature of the solution
00:01:14.130 --> 00:01:15.670
would be the final temperature
00:01:15.670 --> 00:01:17.220
minus the initial temperature,
00:01:17.220 --> 00:01:22.217
which is 25.781 minus 25.0
00:01:24.510 --> 00:01:29.510
which is equal to positive
0.781 degrees Celsius.
00:01:32.350 --> 00:01:36.170
The total volume of solution
would be 25 plus 25,
00:01:36.170 --> 00:01:41.170
which is equal to 50.0
milliliters of solution.
00:01:41.800 --> 00:01:43.640
If we assume the density of the solution
00:01:43.640 --> 00:01:45.840
is one gram per milliliter,
00:01:45.840 --> 00:01:50.840
50.0 milliliters is equal to 50.0 grams.
00:01:52.410 --> 00:01:55.580
Next we need to solve for
the heat gained by the water
00:01:55.580 --> 00:01:59.600
and we can use the Q is
equal to MC delta T equation.
00:01:59.600 --> 00:02:01.190
So we're solving for the heat,
00:02:01.190 --> 00:02:03.180
which is symbolized by Q,
00:02:03.180 --> 00:02:05.000
M is the mass of our solution
00:02:05.000 --> 00:02:07.530
which we saw was 50.0 grams,
00:02:07.530 --> 00:02:09.990
So we can plug that in.
00:02:09.990 --> 00:02:12.610
We can assume that the
specific heat of the solution
00:02:12.610 --> 00:02:15.240
is the same as the specific heat of water,
00:02:15.240 --> 00:02:20.050
which is 4.18 joules
per gram degrees Celsius
00:02:20.050 --> 00:02:22.170
and the change in the
temperature of the solution
00:02:22.170 --> 00:02:24.940
was 0.781 degrees Celsius.
00:02:24.940 --> 00:02:27.593
So we can plug that in as well.
00:02:29.630 --> 00:02:33.900
Grams cancels out, degrees
Celsius cancels out
00:02:33.900 --> 00:02:38.900
and we find that Q is equal to
00:02:39.040 --> 00:02:44.040
positive 1.63 times 10
to the second joules.
00:02:47.170 --> 00:02:51.030
The positive sign means that
energy was gained by the water.
00:02:51.030 --> 00:02:52.680
But let's think about the distinction
00:02:52.680 --> 00:02:56.520
between system and surroundings.
00:02:56.520 --> 00:02:58.740
The system consists of the reactants
00:02:58.740 --> 00:03:01.320
and products for our particular reaction
00:03:01.320 --> 00:03:03.320
and the surroundings are everything else
00:03:03.320 --> 00:03:05.880
which includes the water.
00:03:05.880 --> 00:03:06.770
So in this case,
00:03:06.770 --> 00:03:09.660
since the temperature of the
surroundings increased, right?
00:03:09.660 --> 00:03:11.830
We saw an increase in the temperature,
00:03:11.830 --> 00:03:13.110
that means that heat flowed
00:03:13.110 --> 00:03:15.880
from the system to the surroundings
00:03:15.880 --> 00:03:18.190
and so the surroundings
increased in energy
00:03:18.190 --> 00:03:20.823
and that's what we see with
this positive sign here.
00:03:21.940 --> 00:03:24.440
If we assume a perfect transfer of heat
00:03:24.440 --> 00:03:26.490
from the system to the surroundings,
00:03:26.490 --> 00:03:28.530
if the surroundings gained energy,
00:03:28.530 --> 00:03:31.210
that means the system lost energy.
00:03:31.210 --> 00:03:32.450
So if we're thinking about the heat
00:03:32.450 --> 00:03:34.830
transferred for the reaction,
00:03:34.830 --> 00:03:36.260
it's the same in magnitude,
00:03:36.260 --> 00:03:40.160
1.63 times 10 to the second joules.
00:03:40.160 --> 00:03:43.040
However, we need to put
a negative sign in here
00:03:43.040 --> 00:03:47.223
which indicates that energy
was given off by the reaction.
00:03:48.130 --> 00:03:50.590
The heat that's transferred
under constant pressure
00:03:50.590 --> 00:03:52.730
is equal to the change in the entropy
00:03:52.730 --> 00:03:55.230
of the reaction, delta H.
00:03:55.230 --> 00:03:57.950
However, let's find the
change in entropy, delta H
00:03:57.950 --> 00:04:01.270
in terms of kilojoules per mole
00:04:01.270 --> 00:04:05.120
of silver chloride for our units.
00:04:05.120 --> 00:04:07.010
Since silver chloride
is one of our products,
00:04:07.010 --> 00:04:09.770
we first need to find
moles of our reactants
00:04:09.770 --> 00:04:12.650
and we're gonna do that
using the molarity equation
00:04:12.650 --> 00:04:13.770
which says that molarity
00:04:13.770 --> 00:04:16.540
is equal to moles divided by liters.
00:04:16.540 --> 00:04:19.290
For our silver nitrate solution,
00:04:19.290 --> 00:04:23.900
the concentration was 0.100 molar
00:04:23.900 --> 00:04:26.610
and trying to solve for moles so that's X.
00:04:26.610 --> 00:04:28.560
The volume of our silver nitrate solution
00:04:28.560 --> 00:04:30.710
was 25.0 milliliters
00:04:30.710 --> 00:04:35.310
which is 0.0250 liters.
00:04:35.310 --> 00:04:38.690
So we solve for X and we get 0.00250.
00:04:42.580 --> 00:04:46.140
So that's how many moles of silver nitrate
00:04:46.140 --> 00:04:48.010
that we started with
00:04:48.010 --> 00:04:50.100
and it's the exact same calculation
00:04:50.100 --> 00:04:52.230
for sodium chloride as well.
00:04:52.230 --> 00:04:56.913
So this is also how many moles
of sodium chloride we have.
00:04:57.850 --> 00:05:00.800
Next, we go back to our
balanced chemical equation
00:05:00.800 --> 00:05:03.290
and we can see we have coefficients of one
00:05:03.290 --> 00:05:04.610
in front of silver nitrate,
00:05:04.610 --> 00:05:05.820
in front of sodium chloride
00:05:05.820 --> 00:05:08.390
and in front of silver chloride.
00:05:08.390 --> 00:05:11.967
Therefore, we're also going
to produce 0.00250 moles
00:05:14.930 --> 00:05:16.710
of silver chloride.
00:05:16.710 --> 00:05:18.530
Next we're gonna calculate the change
00:05:18.530 --> 00:05:21.870
in the entropy, delta H, for our reaction.
00:05:21.870 --> 00:05:23.400
The heat that was transferred
00:05:23.400 --> 00:05:28.400
was negative 1.63 times
10 to the second joules
00:05:30.060 --> 00:05:31.650
and we're gonna divide that
00:05:31.650 --> 00:05:33.690
by the moles of silver chloride
00:05:33.690 --> 00:05:38.690
which was 0.00250 moles
of silver chlorides.
00:05:41.890 --> 00:05:45.447
This is equal to negative 65,200 joules
00:05:48.350 --> 00:05:51.050
per mole of silver chloride
00:05:51.050 --> 00:05:53.720
and we could convert that into kilojoules.
00:05:53.720 --> 00:05:58.720
And so this is equal to
negative 65.2 kilojoules
00:05:59.550 --> 00:06:02.983
per mole of silver chloride.
00:06:04.930 --> 00:06:08.030
We could stop right here and
give this as our final answer,
00:06:08.030 --> 00:06:09.020
but let's keep going
00:06:09.020 --> 00:06:13.200
and convert two kilojoules
per mole of reaction.
00:06:13.200 --> 00:06:14.560
First, let's rewrite this.
00:06:14.560 --> 00:06:19.210
We have negative 65.2 kilojoules
00:06:19.210 --> 00:06:23.590
per mole of silver chlorides
00:06:23.590 --> 00:06:26.540
and what it means by
kilojoules per mole of reaction
00:06:26.540 --> 00:06:28.590
is how the reaction is written
00:06:28.590 --> 00:06:31.660
in the balanced equation down here.
00:06:31.660 --> 00:06:33.440
So if we look at the balanced equation,
00:06:33.440 --> 00:06:37.010
there's one mole of silver chloride
00:06:37.010 --> 00:06:38.860
for how the reaction is written.
00:06:38.860 --> 00:06:41.370
So we can write a conversion factor
00:06:41.370 --> 00:06:45.340
of one mole of silver chloride
00:06:45.340 --> 00:06:49.520
per one mole of reaction
00:06:49.520 --> 00:06:52.490
and writing it this way
for the conversion factor,
00:06:52.490 --> 00:06:55.850
the moles of silver
chloride would cancel out
00:06:55.850 --> 00:07:00.850
and give us negative 65.2
kilojoules per mole of reaction.
00:07:06.100 --> 00:07:08.993
So this could also be our final answer.
00:07:11.540 --> 00:07:12.740
Finally, the negative sign
00:07:12.740 --> 00:07:15.350
means that we have an exothermic reaction.
00:07:15.350 --> 00:07:17.730
The reaction gave off energy
00:07:17.730 --> 00:07:19.720
and this value when you do
00:07:19.720 --> 00:07:21.750
a constant pressure calorimetry experiment
00:07:21.750 --> 00:07:24.520
is often a little bit
lower than the actual value
00:07:24.520 --> 00:07:27.940
because in reality there's
not always a perfect transfer
00:07:27.940 --> 00:07:31.610
of heat from the reaction to the water.
00:07:31.610 --> 00:07:35.063
Often some of the energy
is lost to the environment.
|
Enthalpy of reaction | https://www.youtube.com/watch?v=cEzN33gfgVs | vtt | https://www.youtube.com/api/timedtext?v=cEzN33gfgVs&ei=5VWUZev0Iu_6vdIPx6OPgA4&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=A135A677D1D1028F2022E7CFB01460C9AAF0EEF1.3E3774F7D4F7DE1EE5D774178B32A785A27AEEB1&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.660 --> 00:00:01.580
- [Instructor] The change in enthalpy
00:00:01.580 --> 00:00:03.500
for a chemical reaction delta H,
00:00:03.500 --> 00:00:06.240
we could even write delta
H of reaction in here
00:00:06.240 --> 00:00:08.230
is equal to the heat transferred
00:00:08.230 --> 00:00:11.100
during a chemical reaction
at constant pressure.
00:00:11.100 --> 00:00:13.963
So delta H is equal to qp.
00:00:14.930 --> 00:00:17.100
Let's say we are performing
a chemical reaction,
00:00:17.100 --> 00:00:20.710
an aqueous solution under
constant atmospheric pressure.
00:00:20.710 --> 00:00:23.060
The reactants and products
of that chemical reaction
00:00:23.060 --> 00:00:25.270
make up the system and
everything else makes
00:00:25.270 --> 00:00:27.550
up the surroundings.
00:00:27.550 --> 00:00:30.800
When heat flows from the
surroundings to the system,
00:00:30.800 --> 00:00:33.500
the system or the reaction absorbs heat
00:00:33.500 --> 00:00:35.690
and therefore the change in enthalpy
00:00:35.690 --> 00:00:38.010
is positive for the reaction.
00:00:38.010 --> 00:00:41.320
This is called an endothermic reaction.
00:00:41.320 --> 00:00:44.450
If heat flows from the
system to the surroundings,
00:00:44.450 --> 00:00:46.730
the reaction gave off energy.
00:00:46.730 --> 00:00:48.290
Therefore the change in enthalpy
00:00:48.290 --> 00:00:50.030
for the reaction is negative
00:00:50.030 --> 00:00:52.853
and this is called an exothermic reaction.
00:00:53.790 --> 00:00:57.050
As an example of a reaction,
let's look at the decomposition
00:00:57.050 --> 00:01:01.930
of hydrogen peroxide to form
liquid water and oxygen gas.
00:01:01.930 --> 00:01:04.470
The change in the
enthalpy for this reaction
00:01:04.470 --> 00:01:07.540
is equal to negative 196 kilojoules.
00:01:07.540 --> 00:01:11.330
The negative sign means
the reaction is exothermic.
00:01:11.330 --> 00:01:14.420
And for the units, sometimes
you might see kilojoules.
00:01:14.420 --> 00:01:18.320
Sometimes you might see
kilojoules per mole,
00:01:18.320 --> 00:01:22.553
and sometimes you might see
kilojoules per mole of reaction.
00:01:23.540 --> 00:01:25.150
What kilojoules per mole of reaction
00:01:25.150 --> 00:01:28.900
is referring to is how
the equation is written.
00:01:28.900 --> 00:01:31.120
So if we look at this balanced equation,
00:01:31.120 --> 00:01:33.980
there's a two as a coefficient
in front of hydrogen peroxide
00:01:33.980 --> 00:01:36.290
and therefore two moles
of hydrogen peroxide
00:01:36.290 --> 00:01:39.470
are decomposing to form two moles of water
00:01:39.470 --> 00:01:42.080
and one mole of oxygen gas.
00:01:42.080 --> 00:01:45.770
So when two moles of
hydrogen peroxide decompose,
00:01:45.770 --> 00:01:50.770
196 kilojoules of energy are given off.
00:01:50.810 --> 00:01:54.120
Next, let's calculate
how much heat is released
00:01:54.120 --> 00:01:58.580
when 5.00 grams of hydrogen
peroxide decomposes
00:01:58.580 --> 00:02:00.400
at a constant pressure.
00:02:00.400 --> 00:02:02.530
The first step is to
find out how many moles
00:02:02.530 --> 00:02:04.680
of hydrogen peroxide that we have.
00:02:04.680 --> 00:02:07.020
So we take the mass of hydrogen peroxide
00:02:07.020 --> 00:02:08.490
which is five grams
00:02:08.490 --> 00:02:12.040
and we divide that by the
molar mass of hydrogen peroxide
00:02:12.040 --> 00:02:15.530
which is 34.0 grams per mole.
00:02:15.530 --> 00:02:18.713
Grams cancels out and this gives us 0.147
00:02:21.570 --> 00:02:25.033
moles of hydrogen peroxide.
00:02:26.120 --> 00:02:29.770
Next, we take our negative 196 kilojoules
00:02:29.770 --> 00:02:32.430
per mole of reaction
00:02:32.430 --> 00:02:36.540
and we're gonna multiply
this by a conversion factor.
00:02:36.540 --> 00:02:39.130
When we look at the balanced
equation for how it's written,
00:02:39.130 --> 00:02:42.590
there are two moles of hydrogen peroxide.
00:02:42.590 --> 00:02:44.720
So for our conversion factor
00:02:44.720 --> 00:02:49.480
for every one mole of
reaction as it is written,
00:02:49.480 --> 00:02:53.590
there are two moles of hydrogen peroxide.
00:02:53.590 --> 00:02:55.743
So two moles of H2O2.
00:02:58.450 --> 00:03:01.230
Now the of reaction will cancel out
00:03:01.230 --> 00:03:06.230
and this gives us negative 98.0 kilojoules
00:03:07.730 --> 00:03:12.033
per one mole of H2O2.
00:03:13.220 --> 00:03:15.560
So two moles of hydrogen peroxide
00:03:15.560 --> 00:03:18.810
would give off 196 kilojoules of energy.
00:03:18.810 --> 00:03:21.350
And one mole of hydrogen
peroxide would give
00:03:21.350 --> 00:03:25.793
off half that amount or
98.0 kilojoules of energy.
00:03:26.690 --> 00:03:30.520
Next, we take our 0.147
moles of hydrogen peroxide.
00:03:30.520 --> 00:03:31.353
So let me just go ahead
00:03:31.353 --> 00:03:32.970
and write this down here really quickly.
00:03:32.970 --> 00:03:37.390
So we have 0.147 moles of H202.
00:03:38.710 --> 00:03:41.730
And remember, we're trying to calculate,
00:03:41.730 --> 00:03:44.930
we're trying to calculate
the amount of heat
00:03:44.930 --> 00:03:46.410
that was released.
00:03:46.410 --> 00:03:51.153
So next we multiply that
by negative 98.0 kilojoules
00:03:52.760 --> 00:03:57.760
per mole of H202, and moles
of H2O2 will cancel out
00:04:00.910 --> 00:04:03.280
and this gives us our final answer.
00:04:03.280 --> 00:04:07.100
So the heat that was
released when 5.00 grams
00:04:07.100 --> 00:04:10.440
of hydrogen peroxide decompose
at constant pressure,
00:04:10.440 --> 00:04:15.430
this turns out to be equal
to negative 14.4 kilojoules.
|
Heating curve for water | https://www.youtube.com/watch?v=MqAVc_XaIXQ | vtt | https://www.youtube.com/api/timedtext?v=MqAVc_XaIXQ&ei=5VWUZcrdL4X3xN8P_7SfiAs&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245333&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=0A64CED0EF0F3611FC4663D352C3C19B2CB6635C.39567DD15DFA5119A7EBB116CD41FEB69FC997E4&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.220 --> 00:00:02.700
- [Instructor] Let's look at
the heating curve for water.
00:00:02.700 --> 00:00:05.360
A heating curve has
temperature on the y-axis.
00:00:05.360 --> 00:00:07.730
In this case, we have
it in degrees Celsius.
00:00:07.730 --> 00:00:10.550
And heat added on the x-axis,
00:00:10.550 --> 00:00:12.780
let's say it's in kilojoules.
00:00:12.780 --> 00:00:15.740
Let's say we have 18.0 grams of ice
00:00:15.740 --> 00:00:18.090
and our goal is to
calculate the total heat
00:00:18.090 --> 00:00:21.460
necessary to convert that 18 grams of ice
00:00:21.460 --> 00:00:26.460
at -25 degrees Celsius to
steam at 125 degrees Celsius.
00:00:28.880 --> 00:00:31.890
So we're starting with
ice at -25 degrees Celsius
00:00:31.890 --> 00:00:34.010
and first we need to heat up the ice
00:00:34.010 --> 00:00:37.770
to zero degrees Celsius, which
we know is the melting point.
00:00:37.770 --> 00:00:38.950
So on our heating curve,
00:00:38.950 --> 00:00:43.110
we're going from point A to point B.
00:00:43.110 --> 00:00:44.690
To calculate the heat necessary,
00:00:44.690 --> 00:00:49.690
we need to use the equation
Q is equal to mc delta T,
00:00:50.350 --> 00:00:52.000
where q is the heat added,
00:00:52.000 --> 00:00:53.850
m is the mass of the ice.
00:00:53.850 --> 00:00:55.760
c is the specific heat of ice
00:00:55.760 --> 00:00:57.990
and delta T is the change in temperature,
00:00:57.990 --> 00:00:59.370
which is the final temperature
00:00:59.370 --> 00:01:01.520
minus the initial temperature.
00:01:01.520 --> 00:01:03.560
So we're trying to calculate q.
00:01:03.560 --> 00:01:08.147
We know the mass of our ice is 18.0 grams.
00:01:08.147 --> 00:01:10.740
The specific heat of ice
00:01:10.740 --> 00:01:15.740
is 2.03 joules per gram degrees Celsius.
00:01:18.420 --> 00:01:21.350
And for the change in temperature,
it's final minus initial.
00:01:21.350 --> 00:01:24.898
So the final temperature
would be zero degrees Celsius,
00:01:24.898 --> 00:01:27.030
initial is -25.
00:01:27.030 --> 00:01:32.030
So zero minus -25 gives
us +25 degrees Celsius.
00:01:34.730 --> 00:01:38.130
So grams will cancel out,
degrees Celsius cancels out.
00:01:38.130 --> 00:01:43.130
And this gives us q is
equal to 9.1 times 10
00:01:44.580 --> 00:01:49.070
to the second joules to
two significant figures
00:01:49.070 --> 00:01:54.070
or we could also write 0.91 kilojoules.
00:01:55.660 --> 00:01:57.620
Now that the ice is at
zero degrees Celsius,
00:01:57.620 --> 00:01:58.850
we know what's going to melt.
00:01:58.850 --> 00:02:00.520
So we're gonna go from point B
00:02:00.520 --> 00:02:03.260
on the heating curve to point C.
00:02:03.260 --> 00:02:07.020
And to calculate how much heat
is necessary to melt the ice,
00:02:07.020 --> 00:02:10.450
we need to know the heat of fusion of ice,
00:02:10.450 --> 00:02:14.200
which is equal to 6.01
kilojoules per mole.
00:02:18.213 --> 00:02:21.690
So we need to figure out how
many moles of ice we have.
00:02:21.690 --> 00:02:24.890
After starting with 18.0 grams,
00:02:24.890 --> 00:02:27.050
we divide by the molar mass of H2O
00:02:27.050 --> 00:02:31.590
which is 18.0 grams per mole.
00:02:31.590 --> 00:02:35.370
And the grams will cancel
and give us one mole.
00:02:35.370 --> 00:02:39.440
So we have 1.00 moles of ice
00:02:39.440 --> 00:02:43.520
and we multiply that by
6.01 kilojoules per mole
00:02:43.520 --> 00:02:48.040
and the moles cancel out
and give us 6.01 kilojoules.
00:02:50.940 --> 00:02:53.790
Now that all the ice is
melted, we have liquid water.
00:02:53.790 --> 00:02:54.940
And so on our heating curve,
00:02:54.940 --> 00:02:56.370
we're gonna heat that liquid water
00:02:56.370 --> 00:02:59.940
from zero degrees Celsius to 100 Celsius
00:02:59.940 --> 00:03:01.820
which is the boiling point of water.
00:03:01.820 --> 00:03:04.340
So we're going from point C to point D
00:03:04.340 --> 00:03:05.840
on the heating curve.
00:03:05.840 --> 00:03:07.430
To calculate the heat added,
00:03:07.430 --> 00:03:12.400
we use the Q is equal to
mc delta T equation again.
00:03:12.400 --> 00:03:14.880
So we're solving for Q.
00:03:14.880 --> 00:03:18.450
The mass is still 18.0 grams
00:03:18.450 --> 00:03:20.060
but the specific heat now,
00:03:20.060 --> 00:03:21.250
since we have liquid water,
00:03:21.250 --> 00:03:24.020
we need to use the specific
heat of liquid water,
00:03:24.020 --> 00:03:29.020
which is 4.18 joules per
gram degrees Celsius.
00:03:29.720 --> 00:03:31.320
And for the change in temperature,
00:03:31.320 --> 00:03:34.489
the final temperature is 100.
00:03:34.489 --> 00:03:39.489
So 100 minus zero gives
us +100 degrees Celsius.
00:03:42.870 --> 00:03:46.440
So grams cancel out,
degrees Celsius cancels out
00:03:46.440 --> 00:03:50.447
and we find that Q is
equal to 7.52 times 10
00:03:53.180 --> 00:03:57.113
to the third joules, let me
just correct three there,
00:03:57.113 --> 00:04:00.470
7.52 times 10 to the third joules,
00:04:00.470 --> 00:04:03.177
which is equal to 7.52 kilojoules.
00:04:07.170 --> 00:04:09.170
Once we reached a point
D in the heating curve,
00:04:09.170 --> 00:04:10.630
we're at the boiling point of water.
00:04:10.630 --> 00:04:12.680
So the heat that we add now is gonna go
00:04:12.680 --> 00:04:15.760
into turning the liquid
water into gaseous water.
00:04:15.760 --> 00:04:18.730
So going from point D to point E,
00:04:18.730 --> 00:04:19.820
we're doing a phase change.
00:04:19.820 --> 00:04:23.240
We need to know the heat
of vaporization of water,
00:04:23.240 --> 00:04:28.240
and that's equal to 40.7
kilojoules per mole.
00:04:31.030 --> 00:04:35.600
And we already know we
have one mole of H2O.
00:04:35.600 --> 00:04:40.040
So one mole times 40.7
moles, the moles cancel
00:04:40.040 --> 00:04:45.040
and it takes 40.7 kilojoules of energy
00:04:45.740 --> 00:04:50.350
to convert the liquid water
in to gaseous water or steam.
00:04:50.350 --> 00:04:52.130
Next we're gonna heat the gaseous water
00:04:52.130 --> 00:04:55.480
from 100 degrees Celsius
to 125 degrees Celsius.
00:04:55.480 --> 00:04:59.050
So we're going from point E to
point F on the heating curve.
00:04:59.050 --> 00:05:01.280
And to figure out how
much heat we need to add,
00:05:01.280 --> 00:05:06.010
we use the Q is equal to mc
delta T equation one more time.
00:05:06.010 --> 00:05:10.700
So we're solving for Q and
we still have 18.0 grams.
00:05:10.700 --> 00:05:13.990
This time we need to use
these specific heat of steam,
00:05:13.990 --> 00:05:18.990
which is 1.84 joules
per gram degree Celsius.
00:05:20.570 --> 00:05:24.380
The change in temperature
would be 125 minus 100
00:05:24.380 --> 00:05:28.780
or +25 degrees Celsius.
00:05:28.780 --> 00:05:31.540
So grams cancel, units cancel out
00:05:31.540 --> 00:05:36.540
and we get Q is equal to 8.3
times 10 to the second joules
00:05:40.130 --> 00:05:42.020
to two significant figures,
00:05:42.020 --> 00:05:46.823
which is equal to 0.83 kilojoules.
00:05:48.760 --> 00:05:50.700
Finally, we need to add everything up.
00:05:50.700 --> 00:05:53.960
So going from point A to
point B in the heating curve.
00:05:53.960 --> 00:05:57.060
So think about just the X
axis this time, all right?
00:05:57.060 --> 00:05:59.460
So going from point A to point B,
00:05:59.460 --> 00:06:04.460
we calculated that to be
equal to 0.91 kilojoules.
00:06:05.370 --> 00:06:08.492
And then from point B to point C,
00:06:08.492 --> 00:06:13.480
we calculated that to be 6.01 kilojoules.
00:06:13.480 --> 00:06:18.480
From C to D, so this
distance here was 7.52.
00:06:21.463 --> 00:06:24.990
From D to E, this was the big one here.
00:06:24.990 --> 00:06:29.047
This was equal to 40.7 kilojoules.
00:06:30.650 --> 00:06:32.760
And finally from E to F we calculated
00:06:32.760 --> 00:06:35.487
this was equal to 0.83 kilojoules.
00:06:39.010 --> 00:06:40.240
And when you add everything up
00:06:40.240 --> 00:06:44.870
this is equal to 56.0 kilojoules.
00:06:44.870 --> 00:06:47.360
So that's how much energy it takes
00:06:47.360 --> 00:06:52.360
to convert 18.0 grams of
ice at -25 degrees Celsius
00:06:53.450 --> 00:06:58.270
to gaseous water at 125 degrees Celsius.
00:06:58.270 --> 00:06:59.970
Next, let's think about the slopes
00:06:59.970 --> 00:07:02.540
of the different lines
on our heating curve.
00:07:02.540 --> 00:07:06.770
So let's look at the
line going from B to C
00:07:06.770 --> 00:07:11.770
and also the line going
from point D to point E.
00:07:12.170 --> 00:07:14.110
Both of these lines
represent phase changes,
00:07:14.110 --> 00:07:16.280
going from point B to point C
00:07:16.280 --> 00:07:18.420
was going from a solid to a liquid
00:07:18.420 --> 00:07:20.370
and going from point D to E
00:07:20.370 --> 00:07:22.938
was going from a liquid to a gas.
00:07:22.938 --> 00:07:26.270
And since the slope of both
of these lines is zero,
00:07:26.270 --> 00:07:29.930
that means as you add heat on the x-axis,
00:07:29.930 --> 00:07:32.207
the temperature doesn't change.
00:07:32.207 --> 00:07:34.070
So during a phase change,
00:07:34.070 --> 00:07:36.490
all the energy goes into disrupting
00:07:36.490 --> 00:07:39.660
the intermolecular forces that are present
00:07:39.660 --> 00:07:42.500
and they don't go into
increasing the temperature.
00:07:42.500 --> 00:07:44.410
So there is no increase in temperature
00:07:44.410 --> 00:07:46.190
during a phase change.
00:07:46.190 --> 00:07:48.740
Think about going from point D to point E,
00:07:48.740 --> 00:07:52.160
this was converting our liquid
water into gaseous water.
00:07:52.160 --> 00:07:54.470
So as the heat is being added,
00:07:54.470 --> 00:07:59.100
all that energy goes into
breaking the intermolecular forces
00:07:59.100 --> 00:08:01.470
between water molecules and pulling apart
00:08:01.470 --> 00:08:02.790
those liquid water molecules
00:08:02.790 --> 00:08:06.400
and turning them into
gaseous water molecules.
00:08:06.400 --> 00:08:09.190
So it's only after all of
the liquid water molecules
00:08:09.190 --> 00:08:11.720
are converted into
gaseous water molecules,
00:08:11.720 --> 00:08:14.000
that's when we see the
temperature increase again.
00:08:14.000 --> 00:08:16.730
So talking about from point E to point F,
00:08:16.730 --> 00:08:19.160
everything is now in the gaseous state
00:08:19.160 --> 00:08:22.050
and then we see the
increase in temperature.
00:08:22.050 --> 00:08:25.700
Finally, let's compare the
slope of the line from A to B
00:08:25.700 --> 00:08:29.284
to the slope of the line from C to D.
00:08:29.284 --> 00:08:31.080
If we look at it, the slope of the line
00:08:31.080 --> 00:08:34.330
from A to B is a little bit steeper
00:08:34.330 --> 00:08:37.600
than the slope of the line from C to D.
00:08:37.600 --> 00:08:39.090
The reason for the different slopes
00:08:39.090 --> 00:08:41.671
has to do with the
different specific heats.
00:08:41.671 --> 00:08:45.270
From A to B, we used the
specific heat for ice
00:08:45.270 --> 00:08:49.060
which is 2.03 joules per
gram degrees Celsius.
00:08:49.060 --> 00:08:51.840
From C to D in our calculation,
00:08:51.840 --> 00:08:53.910
we used the specific heat for water
00:08:53.910 --> 00:08:57.800
which is 4.1 joules per
gram degrees Celsius.
00:08:57.800 --> 00:09:00.160
The higher the value
for the specific heat,
00:09:00.160 --> 00:09:02.410
the more energy it takes to raise
00:09:02.410 --> 00:09:06.030
the temperature of a
substance by a certain amount.
00:09:06.030 --> 00:09:07.660
So if we think about comparing these two,
00:09:07.660 --> 00:09:09.290
let's say we try to raise the temperature
00:09:09.290 --> 00:09:11.850
of ice by 25 degrees Celsius.
00:09:11.850 --> 00:09:15.460
So lets think about this
distance here on the y-axis.
00:09:15.460 --> 00:09:18.560
We would have to put in only
a small amount of energy
00:09:18.560 --> 00:09:20.700
to get ice to increase its temperature
00:09:20.700 --> 00:09:23.200
by 25 degrees Celsius.
00:09:23.200 --> 00:09:26.160
We think about that same
temperature change on liquid water.
00:09:26.160 --> 00:09:28.820
So if we tried to increase the
temperature of liquid water
00:09:28.820 --> 00:09:31.690
by that same amount, 25 degrees,
00:09:31.690 --> 00:09:34.280
we would have to put in more energy.
00:09:34.280 --> 00:09:37.440
So on the x-axis, we have
to put in more energy
00:09:37.440 --> 00:09:40.020
to accomplish the same
change in temperature.
00:09:40.020 --> 00:09:44.820
And that's because liquid water
has a higher specific heat.
00:09:44.820 --> 00:09:47.100
Since it might be a little bit
hard to see on that diagram,
00:09:47.100 --> 00:09:50.870
let's think about putting some
heat into a substance here.
00:09:50.870 --> 00:09:52.590
So I'm gonna draw a horizontal line,
00:09:52.590 --> 00:09:54.050
and then we're trying to accomplish
00:09:54.050 --> 00:09:55.420
a certain temperature change.
00:09:55.420 --> 00:09:57.200
So I'll draw a vertical line.
00:09:57.200 --> 00:10:02.060
Those two give me a line with a slope.
00:10:02.060 --> 00:10:03.790
So let's say we're trying to accomplish
00:10:03.790 --> 00:10:06.060
the same change in temperature.
00:10:06.060 --> 00:10:09.182
So I'll draw this Y
distance the same as before
00:10:09.182 --> 00:10:11.450
but we have a higher specific heat.
00:10:11.450 --> 00:10:14.190
So it takes more energy.
00:10:14.190 --> 00:10:17.370
Therefore this X distance
is going to increase.
00:10:17.370 --> 00:10:19.740
And when we increase the X distance,
00:10:19.740 --> 00:10:23.230
we see that the slope decreases.
00:10:23.230 --> 00:10:26.780
So the greater the value
for the specific heat,
00:10:26.780 --> 00:10:30.033
the lower the slope on the heating curve.
|
Enthalpy and phase changes | https://www.youtube.com/watch?v=jCKvxH5mXR4 | vtt | https://www.youtube.com/api/timedtext?v=jCKvxH5mXR4&ei=6VWUZYTCDdCehcIP-q-EOA&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245337&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=0DC4C4875CA1BA3612FAB96E4D915A8F0F7D429D.5496286D6E8465AC9670BB569D87357A57F3D68F&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.030 --> 00:00:01.720
- [Instructor] Let's say
that we have some solid water
00:00:01.720 --> 00:00:04.860
or ice and we want to melt the ice
00:00:04.860 --> 00:00:09.170
and turn the solid
water into liquid water.
00:00:09.170 --> 00:00:10.900
This phase change of solid water
00:00:10.900 --> 00:00:13.010
to liquid water is called melting
00:00:13.010 --> 00:00:16.460
and it takes positive 6.01 kilojoules
00:00:16.460 --> 00:00:20.010
per one mole to melt ice.
00:00:20.010 --> 00:00:23.970
This change in enthalpy
is symbolized by delta H
00:00:23.970 --> 00:00:27.090
with a subscript fus,
which stands for fusion.
00:00:27.090 --> 00:00:29.913
So this is called the heat of fusion.
00:00:31.020 --> 00:00:32.580
Next let's think about the phase change
00:00:32.580 --> 00:00:35.630
of converting liquid
water into gaseous water.
00:00:35.630 --> 00:00:38.040
This phase change is called vaporization
00:00:38.040 --> 00:00:40.810
and it also takes energy
to convert liquid water
00:00:40.810 --> 00:00:42.860
into gaseous water.
00:00:42.860 --> 00:00:46.970
Specifically for water
it takes 40.7 kilojoules
00:00:46.970 --> 00:00:50.700
per one mole of liquid
water to vaporize it.
00:00:50.700 --> 00:00:54.490
And so this change in energy
is called the enthalpy
00:00:54.490 --> 00:00:59.140
of vaporization or simply
the heat of vaporization.
00:00:59.140 --> 00:01:01.600
Let's go back and think
about the structure of ice.
00:01:01.600 --> 00:01:05.790
Ice has water molecules in a
repeating crystal structure
00:01:05.790 --> 00:01:10.270
and the water molecules are
held together by hydrogen bonds.
00:01:10.270 --> 00:01:12.690
So between these two water molecules here,
00:01:12.690 --> 00:01:16.810
when we add energy, we
increase the freedom of motion,
00:01:16.810 --> 00:01:19.300
so over here is a picture of liquid water.
00:01:19.300 --> 00:01:22.100
So this is still held
together by hydrogen bonds.
00:01:22.100 --> 00:01:23.850
These water molecules
are still held together
00:01:23.850 --> 00:01:26.940
by hydrogen bonds but we no
longer have a crystal structure.
00:01:26.940 --> 00:01:29.490
So we have increased freedom of motion
00:01:29.490 --> 00:01:33.690
and it takes energy to disrupt
that crystal structure.
00:01:33.690 --> 00:01:35.680
And next, let's think about
converting liquid water
00:01:35.680 --> 00:01:38.320
into gaseous water or steam.
00:01:38.320 --> 00:01:39.790
When water is in the gaseous state,
00:01:39.790 --> 00:01:42.240
there are no more intermolecular forces
00:01:42.240 --> 00:01:43.450
between the molecules.
00:01:43.450 --> 00:01:45.450
There's nothing holding them together.
00:01:45.450 --> 00:01:48.170
And so it takes a lot
of energy to pull these
00:01:48.170 --> 00:01:49.600
two water molecules apart.
00:01:49.600 --> 00:01:52.610
It takes a lot of energy to
overcome these hydrogen bonds.
00:01:52.610 --> 00:01:55.950
And that's the reason why
we have such a large value
00:01:55.950 --> 00:01:58.730
for the heat of vaporization.
00:01:58.730 --> 00:02:01.703
So it takes a lot more
energy to completely pull
00:02:01.703 --> 00:02:05.190
these molecules apart
than it did to simply
00:02:05.190 --> 00:02:06.500
increase the freedom of motion.
00:02:06.500 --> 00:02:11.500
So 40.7 is a much bigger number than 6.01.
00:02:12.060 --> 00:02:15.070
If it takes positive
40.7 kilojoules per mole
00:02:15.070 --> 00:02:18.030
of energy to go from the liquid
state to the gaseous state.
00:02:18.030 --> 00:02:19.090
If we go in reverse
00:02:19.090 --> 00:02:21.730
from the gaseous state
back to the liquid state
00:02:21.730 --> 00:02:24.390
that same amount of energy is given off.
00:02:24.390 --> 00:02:28.930
So we can write 40.7 kilojoules per mole.
00:02:28.930 --> 00:02:31.110
However, since the energy is given off,
00:02:31.110 --> 00:02:33.870
we need to include a negative sign,
00:02:33.870 --> 00:02:35.130
going from the gaseous state
00:02:35.130 --> 00:02:37.900
to the liquid state is
called condensation.
00:02:37.900 --> 00:02:39.410
So we could call this value
00:02:39.410 --> 00:02:42.260
of negative 40.7 kilojoules per mole,
00:02:42.260 --> 00:02:44.453
the heat of condensation.
00:02:45.470 --> 00:02:48.900
And if it takes positive 6.01
kilojoules per mole to go
00:02:48.900 --> 00:02:50.970
from the solid state to the liquid state.
00:02:50.970 --> 00:02:52.080
If we go in reverse
00:02:52.080 --> 00:02:54.880
from the liquid state
back to the solid state
00:02:54.880 --> 00:02:59.880
we would give off 6.01
kilojoules per mole of energy.
00:03:00.690 --> 00:03:03.020
And so we need to write
a negative sign here
00:03:03.020 --> 00:03:05.250
to indicate the energy is given off.
00:03:05.250 --> 00:03:08.770
When we go from a liquid to
a solid, that's freezing.
00:03:08.770 --> 00:03:12.543
So this value is called the
heat of freezing for water.
|
Constant-volume calorimetry | https://www.youtube.com/watch?v=1NueJQpqkuc | vtt | https://www.youtube.com/api/timedtext?v=1NueJQpqkuc&ei=6VWUZZfuDvu5mLAPrLWO8AM&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245337&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=7C5003DD3D45C2DDB4F76E989DE86723C24A0C28.D565C29F65E913A9EC2D6569ABE8FBA880B230A5&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.690 --> 00:00:03.170
- [Instructor] Calorimetry
refers to the measurement
00:00:03.170 --> 00:00:04.370
of heat flow.
00:00:04.370 --> 00:00:07.060
And there are many different
types of calorimeters.
00:00:07.060 --> 00:00:10.970
In this case, we're looking at
a constant volume calorimeter
00:00:10.970 --> 00:00:14.460
which is also called a bomb calorimeter.
00:00:14.460 --> 00:00:17.190
Let's look at how a
bomb calorimeter works.
00:00:17.190 --> 00:00:20.490
First, the sample to
be combusted is placed
00:00:20.490 --> 00:00:23.220
in a container that has some oxygen.
00:00:23.220 --> 00:00:25.750
And then there's some
ignition wires that go into
00:00:25.750 --> 00:00:29.690
this little container here,
and the sample is ignited
00:00:29.690 --> 00:00:33.440
and heat is given off by
the combustion reaction.
00:00:33.440 --> 00:00:37.460
So heat is being
transferred from our sample
00:00:37.460 --> 00:00:41.460
to the water in our containers.
00:00:41.460 --> 00:00:43.530
Let me go ahead and
draw some water in here.
00:00:43.530 --> 00:00:45.600
So imagine we have some water,
00:00:45.600 --> 00:00:49.560
and it's important to know
that the container is rigid.
00:00:49.560 --> 00:00:54.560
So the walls are very,
very solid and cannot move.
00:00:55.350 --> 00:00:57.550
There's also something to stir the water
00:00:57.550 --> 00:00:59.400
and since heat is being transferred
00:00:59.400 --> 00:01:02.110
from the combustion reaction to the water,
00:01:02.110 --> 00:01:04.480
the temperature of the water will increase
00:01:04.480 --> 00:01:07.980
which we can see on the thermometer.
00:01:07.980 --> 00:01:11.270
Now that we understand how
a bomb calorimeter works,
00:01:11.270 --> 00:01:12.610
let's think about that heat
00:01:12.610 --> 00:01:15.420
that's being transferred
from the combustion reaction
00:01:15.420 --> 00:01:19.980
to the water, so that heat is q.
00:01:19.980 --> 00:01:22.780
Let's go back to the first
law of thermodynamics,
00:01:22.780 --> 00:01:25.220
which says that the change
in the internal energy
00:01:25.220 --> 00:01:28.210
of the system is equal to q plus w,
00:01:28.210 --> 00:01:30.890
where q is the heat that's transferred
00:01:30.890 --> 00:01:33.840
and w is the work done.
00:01:33.840 --> 00:01:37.020
Let's say we do this combustion
reaction in a container
00:01:37.020 --> 00:01:39.070
with a movable piston.
00:01:39.070 --> 00:01:41.830
And the combustion reaction is performed
00:01:41.830 --> 00:01:45.080
under the constant
pressure of the atmosphere.
00:01:45.080 --> 00:01:47.971
So this time, when we do
the combustion reaction,
00:01:47.971 --> 00:01:50.590
we will transfer some heat.
00:01:50.590 --> 00:01:53.640
So heat is being transferred
from the combustion reaction
00:01:53.640 --> 00:01:57.060
and we would also produce some
gases, which would push up
00:01:57.060 --> 00:02:00.200
on the piston and so the
piston would move up,
00:02:00.200 --> 00:02:01.960
and since the piston's moving,
00:02:01.960 --> 00:02:06.130
work is being done by
the combustion reaction.
00:02:06.130 --> 00:02:08.960
In this case, the heat
that's transferred q
00:02:08.960 --> 00:02:11.090
is done under constant pressure,
00:02:11.090 --> 00:02:14.935
and so we can write qp
here and by definition,
00:02:14.935 --> 00:02:17.395
the heat that's transferred
at constant pressure,
00:02:17.395 --> 00:02:20.895
that's the change in the enthalpy delta H.
00:02:23.150 --> 00:02:25.399
So for this example with the container
00:02:25.399 --> 00:02:26.918
with the movable piston,
00:02:26.918 --> 00:02:29.385
when we did our combustion reaction,
00:02:29.385 --> 00:02:31.706
the heat that's transferred
at constant pressure is equal
00:02:31.706 --> 00:02:35.401
to the enthalpy delta H, the
change in enthalpy delta H,
00:02:35.401 --> 00:02:40.012
and as the gases expand and
pushing the piston work is done.
00:02:40.012 --> 00:02:42.236
Let's compare the example
with the movable piston
00:02:42.236 --> 00:02:44.293
to our bomb calorimeter.
00:02:44.293 --> 00:02:46.513
Our bomb calorimeter has rigid walls
00:02:46.513 --> 00:02:49.013
and therefore no work can be done.
00:02:49.013 --> 00:02:51.846
So the work done is equal to zero.
00:02:52.751 --> 00:02:55.841
When we plugged that into the
first law of thermodynamics,
00:02:55.841 --> 00:03:00.038
we find that the change in
the internal energy delta E
00:03:00.038 --> 00:03:02.955
is equal to the heat transferred q.
00:03:03.861 --> 00:03:06.617
And since this is a constant volume
00:03:06.617 --> 00:03:10.369
calorimeter right, the walls are rigid.
00:03:10.369 --> 00:03:12.536
We can write q sub v here.
00:03:13.406 --> 00:03:17.665
So this heat that's transferred
from our combustion reaction
00:03:17.665 --> 00:03:20.782
in this case is not equal to
the change in the enthalpy.
00:03:20.782 --> 00:03:25.782
It's equal to the change in
the internal energy delta E.
00:03:26.209 --> 00:03:27.280
So the heat that's transferred
00:03:27.280 --> 00:03:30.210
at constant pressure
is equal to the change
00:03:30.210 --> 00:03:32.180
in the enthalpy delta H,
00:03:32.180 --> 00:03:35.140
while the heat that's
transferred at constant volume
00:03:35.140 --> 00:03:38.453
is equal to the change in
the internal energy delta E.
00:03:39.330 --> 00:03:42.100
To do a constant volume
calorimetry problem,
00:03:42.100 --> 00:03:44.650
we need to know the heat
capacity of the calorimeter
00:03:44.650 --> 00:03:49.090
which is symbolized by
C with a subscript cal.
00:03:49.090 --> 00:03:51.190
To find the heat capacity
of the calorimeter,
00:03:51.190 --> 00:03:54.380
we need to combust something
that we know the exact amount
00:03:54.380 --> 00:03:55.250
of heat for them.
00:03:55.250 --> 00:03:58.510
For example, if you
combust exactly one gram
00:03:58.510 --> 00:04:00.170
of benzoic acid,
00:04:00.170 --> 00:04:05.170
you'll get 26.38 kilojoules
released of energy.
00:04:05.500 --> 00:04:10.220
So let's say we have a 0.2350
gram sample of benzoic acid.
00:04:10.220 --> 00:04:13.080
And we put that in our calorimeter
00:04:13.080 --> 00:04:16.400
and we go ahead and
combust the benzoic acid.
00:04:16.400 --> 00:04:18.610
And we find that the temperature increases
00:04:18.610 --> 00:04:22.793
by positive 1.642 degrees Celsius.
00:04:23.730 --> 00:04:25.870
To find the heat capacity
for the calorimeter,
00:04:25.870 --> 00:04:27.210
first we take our known amount
00:04:27.210 --> 00:04:32.210
which is 26.38 kilojoules per gram
00:04:32.820 --> 00:04:35.820
and we multiply that by
how much benzoic acid
00:04:35.820 --> 00:04:40.820
we used in our calorimeter
which was 0.2350 grams.
00:04:41.430 --> 00:04:43.570
And so the grams will cancel out
00:04:43.570 --> 00:04:48.000
and this is equal to 6.199 kilojoules.
00:04:50.580 --> 00:04:53.090
Next we divide this by
our temperature change
00:04:53.090 --> 00:04:56.467
which was positive 1.642 degrees Celsius.
00:04:59.070 --> 00:05:01.240
And this gives us the heat capacity
00:05:01.240 --> 00:05:06.240
of our calorimeter, which turns
out to be 3.3775 kilojoules
00:05:11.590 --> 00:05:14.083
per degree Celsius.
00:05:15.060 --> 00:05:16.960
Now that we know the heat capacity
00:05:16.960 --> 00:05:19.340
for our specific calorimeter,
00:05:19.340 --> 00:05:21.610
we can use this value
to calculate the heat
00:05:21.610 --> 00:05:24.500
of combustion for another substance.
00:05:24.500 --> 00:05:27.230
So the heat of combustion
for another substance
00:05:27.230 --> 00:05:30.030
or just q would be equal to the negative
00:05:30.030 --> 00:05:32.650
of the heat capacity of the calorimeter
00:05:32.650 --> 00:05:35.740
times the change in the
temperature of the water
00:05:35.740 --> 00:05:37.113
in that calorimeter.
00:05:38.320 --> 00:05:40.030
Let's say our goal is
to calculate the heat
00:05:40.030 --> 00:05:43.760
of combustion of caffeine
in kilojoules per mole.
00:05:43.760 --> 00:05:46.650
So we take 0.265 grams of caffeine.
00:05:46.650 --> 00:05:50.100
We put that in our
calorimeter, we combust it
00:05:50.100 --> 00:05:52.510
and we find the temperature
of the water increases
00:05:52.510 --> 00:05:57.510
by positive 1.525 degrees Celsius.
00:05:57.510 --> 00:06:00.530
So to calculate q, q is
equal to the negative
00:06:00.530 --> 00:06:02.570
of the heat capacity of the calorimeter,
00:06:02.570 --> 00:06:07.570
which is 3.775 kilojoules
per degree Celsius.
00:06:09.270 --> 00:06:11.580
And we multiply that by
the temperature change
00:06:11.580 --> 00:06:15.880
which has 1.525 degrees Celsius.
00:06:15.880 --> 00:06:18.400
So degrees Celsius cancels out
00:06:18.400 --> 00:06:23.400
and this gives us
negative 5.757 kilojoules.
00:06:26.830 --> 00:06:28.323
And technically this is the heat transfer
00:06:28.323 --> 00:06:32.640
to a constant volume so we could
even write q sub v in here,
00:06:32.640 --> 00:06:35.130
and remember this is equal to the change
00:06:35.130 --> 00:06:37.970
in the internal energy of our system.
00:06:37.970 --> 00:06:41.690
So this is qv is equal to delta E.
00:06:41.690 --> 00:06:43.670
Since our goal is to find
the heat of combustion
00:06:43.670 --> 00:06:46.270
of caffeine in kilojoules per mole,
00:06:46.270 --> 00:06:48.660
next we need to take
our grams of caffeine,
00:06:48.660 --> 00:06:51.390
which is 0.265 grams, and divide that
00:06:51.390 --> 00:06:53.200
by the molar mass of caffeine.
00:06:53.200 --> 00:06:57.740
And so grams will cancel out
and give us moles of caffeine.
00:06:57.740 --> 00:07:00.450
So this calculation is equal to 1.36
00:07:01.930 --> 00:07:06.930
times 10 to the negative
third moles of caffeine.
00:07:08.800 --> 00:07:10.810
Now, all we have to do is divide our heat,
00:07:10.810 --> 00:07:15.810
which is negative 5.757
kilojoules by our moles
00:07:17.340 --> 00:07:22.340
of 1.36 times 10 to the
negative third moles,
00:07:23.620 --> 00:07:26.830
to give us a final value of negative 4.23
00:07:28.289 --> 00:07:33.289
times 10 to the third kilojoules per mole
00:07:33.740 --> 00:07:36.713
with a negative sign,
meaning heat is given off.
00:07:37.800 --> 00:07:39.490
So we can say that this is the value,
00:07:39.490 --> 00:07:41.890
this is the change in the internal energy
00:07:41.890 --> 00:07:44.920
for our reaction in kilojoules per mole.
00:07:44.920 --> 00:07:48.180
And often the change in
enthalpy is about the same
00:07:48.180 --> 00:07:50.250
as the change in the internal energy.
00:07:50.250 --> 00:07:52.640
So we can say that this
is approximately equal
00:07:52.640 --> 00:07:57.023
to the change in the enthalpy
for the reaction as well.
|
Worked example: Measuring the energy content of foods using soda-can calorimetry | https://www.youtube.com/watch?v=1Zx71Il5jaM | vtt | https://www.youtube.com/api/timedtext?v=1Zx71Il5jaM&ei=6VWUZeyCHui2mLAP48ehsA0&caps=asr&opi=112496729&xoaf=5&hl=en&ip=0.0.0.0&ipbits=0&expire=1704245337&sparams=ip%2Cipbits%2Cexpire%2Cv%2Cei%2Ccaps%2Copi%2Cxoaf&signature=849CDBF96EA0863595B429434E82B9EF1A1B8BC1.AE7D0886476EDDB85EE8982D4E80A2A632FE9EE7&key=yt8&lang=en&name=Default&fmt=vtt | en | WEBVTT
Kind: captions
Language: en
00:00:00.252 --> 00:00:01.450
- [Instructor] Calorimetry refers
00:00:01.450 --> 00:00:04.040
to the measurement of heat flow.
00:00:04.040 --> 00:00:05.550
And in this worked example,
00:00:05.550 --> 00:00:07.850
we're going to burn a marshmallow
00:00:07.850 --> 00:00:11.820
and find the energy
content of the marshmallow.
00:00:11.820 --> 00:00:15.320
First, let's look at the setup
for our soda can calorimeter.
00:00:15.320 --> 00:00:17.800
So our soda can has some water in it.
00:00:17.800 --> 00:00:19.970
So here's the water in our soda can.
00:00:19.970 --> 00:00:23.720
And then we also have a
thermometer in the soda can
00:00:23.720 --> 00:00:26.950
to measure the change in the
temperature of the water.
00:00:26.950 --> 00:00:29.560
If you take a stir rod
and you put the stir rod
00:00:29.560 --> 00:00:31.840
through the tab on the soda can,
00:00:31.840 --> 00:00:35.290
you can attach the soda can to a stand.
00:00:35.290 --> 00:00:37.480
Next, we can put our marshmallow on a pin
00:00:37.480 --> 00:00:39.650
that's attached to a piece of cork.
00:00:39.650 --> 00:00:40.900
Before we start the experiment,
00:00:40.900 --> 00:00:43.360
we need to take the
mass of the marshmallow
00:00:43.360 --> 00:00:44.470
with the cork and the pin,
00:00:44.470 --> 00:00:47.553
so we'll call that the initial mass.
00:00:47.553 --> 00:00:51.464
And we also need the initial
temperature of the water.
00:00:51.464 --> 00:00:53.297
So we'll call that Ti.
00:00:54.990 --> 00:00:57.210
Next, we'd light the marshmallow on fire.
00:00:57.210 --> 00:01:00.190
As the marshmallow burns heat is given off
00:01:00.190 --> 00:01:04.290
and that heat is transferred
to the water in the soda can.
00:01:04.290 --> 00:01:05.910
Therefore the water and the soda can
00:01:05.910 --> 00:01:07.520
will increase in temperature,
00:01:07.520 --> 00:01:10.370
which we can see on the thermometer.
00:01:10.370 --> 00:01:12.170
After the marshmallow
burns for a little while,
00:01:12.170 --> 00:01:14.614
we can stop the burning process.
00:01:14.614 --> 00:01:17.700
And once we stop that, we
wanna look at the thermometer
00:01:17.700 --> 00:01:20.576
for the maximum temperature reached.
00:01:20.576 --> 00:01:22.870
And when we find that maximum temperature
00:01:22.870 --> 00:01:24.230
we can go ahead and record it.
00:01:24.230 --> 00:01:26.230
So we have our final temperature
00:01:26.230 --> 00:01:28.350
and once the marshmallow
with the cork and the pin
00:01:28.350 --> 00:01:31.313
cools down we can find our final mass.
00:01:33.430 --> 00:01:34.790
Let's say the initial mass
00:01:34.790 --> 00:01:39.130
of our marshmallow pin cork was 6.08 grams
00:01:39.130 --> 00:01:42.371
and the final mass was 6.00 grams.
00:01:42.371 --> 00:01:45.000
The initial temperature of
the water in the soda can
00:01:45.000 --> 00:01:48.180
was 25.0 degrees Celsius
and the final temperature
00:01:48.180 --> 00:01:52.080
was 30.0 degrees Celsius.
00:01:52.080 --> 00:01:57.080
Also, let's say that we
started with 50.0 grams
00:01:57.240 --> 00:01:59.253
of water in the soda can.
00:02:00.360 --> 00:02:03.830
Let's calculate the heat
gained by the water.
00:02:03.830 --> 00:02:07.850
To do that we can use the Q is
equal to mc delta T equation
00:02:07.850 --> 00:02:11.527
where Q is equal to the heat transferred,
00:02:11.527 --> 00:02:16.527
m is the mass of the
water which is 50.0 grams,
00:02:17.410 --> 00:02:20.160
c is the specific heat of water
00:02:20.160 --> 00:02:25.160
which is 4.18 joules per
gram degrees Celsius,
00:02:27.153 --> 00:02:29.710
and delta T is the change in temperature
00:02:29.710 --> 00:02:31.780
which should be the final temperature
00:02:31.780 --> 00:02:35.640
minus the initial temperature of the water
00:02:35.640 --> 00:02:40.640
which is 30.0 minus 25.0
00:02:43.160 --> 00:02:48.160
which is equal to 5.0 degrees Celsius.
00:02:50.300 --> 00:02:53.240
Grams cancels out, degrees
Celsius cancels out
00:02:53.240 --> 00:02:57.593
and we find that Q is
equal to +1.0 times 10
00:03:00.973 --> 00:03:02.983
to the third joules.
00:03:02.983 --> 00:03:05.816
That's to two significant figures.
00:03:07.338 --> 00:03:09.304
The positive sign here means
00:03:09.304 --> 00:03:11.839
that heat was gained by the water
00:03:11.839 --> 00:03:15.154
which is why we saw an
increase in the temperature.
00:03:15.154 --> 00:03:17.215
If we assume a perfect transfer of heat,
00:03:17.215 --> 00:03:19.394
so all the heat that was
given off by the burning
00:03:19.394 --> 00:03:21.572
of the marshmallow was
transferred to the water,
00:03:21.572 --> 00:03:25.342
if we think about Q for the
burning of the marshmallow,
00:03:25.342 --> 00:03:27.592
it should be equal in magnitudes.
00:03:27.592 --> 00:03:30.341
So we can write Q is equal to,
00:03:30.341 --> 00:03:31.817
this time we're gonna write a negative
00:03:31.817 --> 00:03:34.886
since heat was given off by
the burning of the marshmallow,
00:03:34.886 --> 00:03:37.636
1.0 times 10 to the third joules.
00:03:41.930 --> 00:03:43.940
So assuming a perfect transfer of heat,
00:03:43.940 --> 00:03:46.800
the magnitude of these
two numbers is equal.
00:03:46.800 --> 00:03:49.260
However, there's no way that
all of the heat was transferred
00:03:49.260 --> 00:03:51.320
from the combustion of the marshmallow
00:03:51.320 --> 00:03:53.954
to the soda can with our simple setup.
00:03:53.954 --> 00:03:56.200
So definitely not all
of it was transferred.
00:03:56.200 --> 00:03:58.120
For example, some of
it could have been lost
00:03:58.120 --> 00:03:59.743
simply to the environment.
00:04:00.820 --> 00:04:02.670
And since the soda can is open
00:04:02.670 --> 00:04:06.390
to the atmospheric pressure
of the environment,
00:04:06.390 --> 00:04:08.960
so I'll go ahead and write
atmospheric pressure in here,
00:04:08.960 --> 00:04:11.330
this soda can calorimeter is an example
00:04:11.330 --> 00:04:14.210
of constant pressure calorimetry.
00:04:14.210 --> 00:04:16.070
And since this is the heat
00:04:16.070 --> 00:04:18.360
that's transferred
under constant pressure,
00:04:18.360 --> 00:04:20.970
I can go ahead and write
QP here to indicate
00:04:20.970 --> 00:04:23.510
the heat transferred
under constant pressure.
00:04:23.510 --> 00:04:27.863
That's the definition of the
change in enthalpy delta H.
00:04:30.920 --> 00:04:34.240
So burning the marshmallow gave off energy
00:04:34.240 --> 00:04:36.850
which is an exothermic reaction,
00:04:36.850 --> 00:04:40.383
therefore, the sign for
delta H is negative.
00:04:41.470 --> 00:04:46.240
Finally, let's relate this soda
can calorimetry experiments
00:04:46.240 --> 00:04:49.010
to calories in everyday life.
00:04:49.010 --> 00:04:51.250
And so let's find the energy content
00:04:51.250 --> 00:04:54.870
of the marshmallow in calories per gram.
00:04:54.870 --> 00:04:58.370
A food calorie has a capital C
00:04:58.370 --> 00:05:02.100
and in chemistry, there's
also a unit of energy
00:05:02.100 --> 00:05:05.260
with calorie with a lowercase C.
00:05:05.260 --> 00:05:07.925
So one food calorie with a capital C
00:05:07.925 --> 00:05:12.925
is equal to one kilocalorie
or 1000 calories
00:05:13.260 --> 00:05:14.533
with a lowercase C.
00:05:15.830 --> 00:05:17.510
When we burned the marshmallow,
00:05:17.510 --> 00:05:20.360
we started off with a mass of 6.08 grams
00:05:20.360 --> 00:05:22.660
for the marshmallow pin cork.
00:05:22.660 --> 00:05:25.780
And the final mass was 6.00 grams,
00:05:25.780 --> 00:05:29.473
which means we burned 0.08
grams of marshmallows.
00:05:30.595 --> 00:05:31.610
And when we burned the marshmallow,
00:05:31.610 --> 00:05:32.830
we found there was a transfer
00:05:32.830 --> 00:05:37.830
of 1.0 times 10 to the
third joules of energy.
00:05:38.460 --> 00:05:40.790
So first, let's convert that
00:05:40.790 --> 00:05:44.190
into calories with a lowercase C.
00:05:44.190 --> 00:05:46.950
So if we multiply by the conversion factor
00:05:46.950 --> 00:05:51.560
of there is one calorie with a lowercase C
00:05:51.560 --> 00:05:54.507
for every 4.184 joules.
00:05:57.530 --> 00:05:59.440
Joules will cancel out
00:05:59.440 --> 00:06:04.440
and this gives us 239
calories with a lowercase C.
00:06:08.040 --> 00:06:12.680
Next, let's convert 239
calories into food calories.
00:06:12.680 --> 00:06:16.760
So first let's take 239 calories,
00:06:16.760 --> 00:06:20.150
and we can multiply by
the conversion factor of,
00:06:20.150 --> 00:06:24.430
there are 1000 calories
with the lowercase C
00:06:24.430 --> 00:06:26.768
for every one kilocalorie.
00:06:26.768 --> 00:06:31.768
And that's gonna give
us 0.239 kilocalories.
00:06:33.142 --> 00:06:35.780
And going back up here to our chart,
00:06:35.780 --> 00:06:40.020
remember, one kilocalorie
is equal to one food calorie
00:06:40.020 --> 00:06:41.920
with a capital C.
00:06:41.920 --> 00:06:46.250
Therefore we have 0.239 kilocalories
00:06:46.250 --> 00:06:51.250
or 0.239 Calories with a capital
C which is a food calorie.
00:06:54.340 --> 00:06:56.270
To find the answer
content of the marshmallow
00:06:56.270 --> 00:06:59.170
in calories per gram,
we just need to divide
00:06:59.170 --> 00:07:02.850
our food calories by how many
grams of marshmallows we use
00:07:02.850 --> 00:07:06.060
which was 0.08 grams in our combustion.
00:07:06.060 --> 00:07:09.410
So dividing by 0.08 grams
00:07:09.410 --> 00:07:14.240
gives us approximately
three calories per gram
00:07:14.240 --> 00:07:15.840
of marshmallows.
00:07:15.840 --> 00:07:16.700
And that's useful
00:07:16.700 --> 00:07:20.940
because let's say we had one
serving size of marshmallows
00:07:20.940 --> 00:07:23.630
which is about 30 grams.
00:07:23.630 --> 00:07:25.688
So therefore, if we
know the energy content
00:07:25.688 --> 00:07:27.891
is three calories per gram,
00:07:27.891 --> 00:07:31.690
we can simply multiply
our four marshmallows
00:07:31.690 --> 00:07:36.660
approximately by three calories per gram
00:07:36.660 --> 00:07:38.660
and grams would cancel out.
00:07:38.660 --> 00:07:41.210
And we would find that
those four marshmallows
00:07:41.210 --> 00:07:45.023
that we wanted to eat are
about 90 food calories.
|