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- [Instructor] We talk about
fluid pressure all the time,
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for example, blood pressure
or pressure inside our tires,
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but what exactly are these numbers?
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What does 120 mean over here?
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Or what does 40 mean over here?
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So the big question over here
is what exactly is pressure?
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That's what we're gonna
find out in this video,
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so let's begin.
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To make sense of this,
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let's hang a perfectly cubicle wooden box
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and think about all the forces.
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We know that there's gravitational
force acting downwards,
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which is perfectly balanced
by the tension force,
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but there is another
set of force over here.
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Remember that there are
air molecules in our room,
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and so these air molecules
are constantly bumping
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and exerting tiny forces.
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But how do we model these forces?
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There are billions of air molecules around
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and they're constantly bumping,
so how do we model this?
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Well, we can model them to be continuous,
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that simplifies things,
but more importantly,
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if you think about the surface area,
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since this is the perfect cube,
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and the surface areas
are exactly the same,
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that means the number of
molecules bumping per second
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on each surface is pretty much the same,
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and therefore, we could model these forces
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to be pretty much the same
from all the directions,
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and that's why these
forces together cancel out
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and they do not accelerate
the box or anything like that.
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But these forces, look,
are pressing on the box
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from all the direction,
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so it's these forces that
are related to pressure.
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But how exactly?
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Well, to answer that question,
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let's think of a bigger box.
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Let's imagine that the
surface area over here
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was twice as much as the
surface area over here.
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Then what would be the amount of force
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that the air molecules
would be putting here
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compared to over here?
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Pause the video and think about this.
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Okay, since we have twice the area,
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if you take any surface,
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if you consider, for
example, the top surface,
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the number of molecules bumping per second
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would be twice as much
compared to over here,
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because you have twice the area,
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and there are air molecules everywhere.
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So can you see just from that logic,
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the amount of force over here
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must be twice as much as over here.
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If the surface area was
three times as much,
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the amount of force
must be thrice as much.
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In other words, you can see
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the force that the air molecules
are exerting on the box
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is proportional to the surface area.
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Or in other words, the force
per area is a constant.
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That is the key characteristics
of the force exerted by air
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or, in general, any fluid.
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And that ratio, force per area,
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is what we call, in general, stress, okay?
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But what exactly is pressure?
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Well, in our example, notice that
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the forces are not in
some random direction.
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All the forces are perpendicular
to the surface area,
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but how can we be so sure, you ask?
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I mean, these are random
molecules bumping into it, right?
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Well, if you zoom in, what do you notice?
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You notice that when the molecules bump
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and they sort of collide,
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and they reflect off of the
walls of our cubicle box,
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what you notice is the acceleration
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is always perpendicular to the box,
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and therefore, the force that
the box is exerting on them
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is also perpendicular to the box.
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And therefore, from Newton's Third Law,
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the force that the molecules
are exerting on the box
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will also be equal and opposite
perpendicular to the box.
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And that's why the forces over here
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are always perpendicular.
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And so look, there's a special
kind of stress over here.
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It's not just any force,
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the force there are always perpendicular,
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and that particular special kind of stress
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where the forces are perpendicular,
that is called pressure.
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So you can think of pressure
as a special kind of stress
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where the forces are
perpendicular to the area.
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But wait, this raises another question.
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Is it possible for fluids to exert forces
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which are paddle to the area as well?
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Yes.
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Consider the air molecules
again, they're all moving,
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but they're all moving in
random direction, isn't it?
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But now, imagine that
there was some kind of wind
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that could happen if the
block itself is moving down,
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or there is wind blowing
upwards, whatever that is,
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there's some kind of a relative motion.
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Now, if there is a wind,
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let's say the air molecules
are moving upwards
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along with the random motion
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that they're doing along with that,
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then because these molecules also interact
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with the molecules of the box,
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they will also exert force on them,
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pulling them upwards.
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This force is called the viscous force,
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and at the heart of it comes from the fact
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that molecules can
interact with each other
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and as a result, look,
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this total viscous force is parallel
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to the surface area,
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and this force tends to shear our cube.
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It's kind of like this deck of cards.
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If you press it
perpendicular to the surface,
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then the stress is just the pressure.
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But if you press at an angle,
then there's a pedal component
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which shears the deck of cards.
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And shearing stresses
can be quite complicated,
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but we don't have to worry about it
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because in our model, we
are considering ideal fluids
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and ideal fluids do
not have any viscosity.
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And we're also going to
assume that we are dealing
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with static fluids, which
means no viscus forces,
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no relative motion, and therefore,
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we can completely ignore shearing stress.
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And therefore, in our model,
we only have pressure.
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Forces will always be only perpendicular
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to the surface area.
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All right, so let's try
to understand pressure
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a little bit better.
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What about its units?
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Well, because it's force per area,
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the unit of force is Newtons
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and the unit of area is meters squared,
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so the unit of pressure,
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at least a standard unit of pressure,
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becomes Newtons per meters squared,
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which we also call pascals.
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So over an area of one meter squared,
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if there's one Newton of force
acting perpendicular to it,
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then we would say that the
pressure is one pascal.
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And that is a very tiny pressure.
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One Newton exerted over one meter squared
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is incredibly tiny.
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So the big question is,
what is the pressure
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over here in a room?
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What is the atmospheric pressure?
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Pressure that the air
molecules are pushing
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on the sides of this cube with?
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Well, turns out that pressure
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is about 10 to the power of five pascals.
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In other words, that is a 100,000 pascals.
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That is insanely huge.
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A 100,000 Newtons of force is exerted
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by the air molecules per square meter.
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That is insanely high. I
wouldn't have expected.
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That is the amount of
pressure we are all feeling
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just sitting in our room
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due to the air molecules over there.
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But that was an important question.
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Why don't things get
crushed under that pressure?
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I mean, sure, this cube
is not getting crushed
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because the internal forces
are able to balance that out.
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But what if I take a plastic bag
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and there's nothing inside it,
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then because there's so much air pressure
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over from the outside,
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shouldn't the plastic bag just get crushed
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due to the air pressure?
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Well, the reason it doesn't get crushed
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is because there's air inside as well.
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And that air also has
the exact same pressure,
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which means it is able to
balance out the pressure
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from the outside.
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But what if you could
somehow suck that air out?
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Ooh, then the balance will be lost
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because the pressure drops
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and then we would see the
plastic bag collapsing,
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getting crushed under the
pressure from the outside.
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That all makes sense, right?
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Okay, before moving forward,
let's also quickly talk
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about a couple of other units of pressure
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that we usually use in our daily life.
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For example, when it
comes to tire pressure,
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we usually talk in terms
of pounds per square inch.
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And just to give some feeling for numbers,
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10 to the power of five
pascals happens to be close
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to 14.7 pounds per square inch.
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So that is the atmospheric pressure
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in pounds per square inch.
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Another unit is millimeters of mercury,
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and 10 to the power of five
pascals happens to be close
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to 760 millimeters of mercury.
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In other words, the atmospheric
pressure can pull up
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the mercury up to 760
millimeters in a column.
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Anyways, let's focus on Pascals for now.
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And the big question
now, is pressure a scalar
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or a vector quantity, what do you think?
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Well, my intuition says it's vector
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because there's force in one over here,
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but let's think a little
bit more about it.
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In fact, think about
pressure at a specific point.
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How do we do that?
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Well, one way to do that
is you take this box
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and shrink it down.
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Let's say we shrink the size of the box.
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Well, now, the area has
become, let's say half,
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but the number of air molecules
will also become half,
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and therefore, the
force also becomes half,
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making sure force per area stays the same.
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So the pressure stays the same.
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We'll keep shrinking it, keep shrinking,
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and keep shrinking it.
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Now shrink it all the way
to an extremely tiny point.
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We call that as an infinitesimal.
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Now, the areas are incredibly tiny,
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the forces are incredibly tiny,
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yet the force per area stays the same.
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That is the pressure
at a particular point.
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And now the question is,
should we assign a direction
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to this number, to this pressure?
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Well, not really, because
all I need is a number,
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because what this number is
saying is that if you zoom in
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and if you have any area,
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then there will always be
forces perpendicular to the area
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that is exerted by the fluid,
and that force per area
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will be 10 to the power of five pascals.
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And that is valid from any direction.
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It doesn't matter how
your area is oriented,
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that will always be the case.
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Which means, look, all I need is a number.
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I don't need a direction
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to communicate the idea of pressure,
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and therefore, pressure
is a scalar quantity.
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And because the number of air molecules
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bumping per square meter is
pretty much the same everywhere
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and their speeds are pretty
much the same anywhere you take,
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therefore, the pressure
now is the same everywhere.
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But if we zoom out and look
at the entire atmosphere,
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for example, that's not the case.
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In fact, that 10 to the
power of five we said
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is the pressure close to the sea level,
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but if you were to go
a little bit above it,
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say at 10 kilometers, which
is the cruising altitude
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of commercial airplanes,
you would now find
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that the pressure is about one fourth
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is what we'd find over here.
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Why is the pressure different over here
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compared to over here?
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Well, that's because
the molecules over here
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are carrying the weight
of the entire atmosphere
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on top of it.
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That entire weight is pushing down,
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pressing the molecules over here.
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However, if you consider
the molecules at this level,
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they're not carrying the entire weight,
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they're carrying the
weight only on top of them.
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They're not carrying the
weight of this amount
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of air molecules.
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And that's why the pressure
over here is slightly lower,
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which means the pressure depends
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on the height if you zoom out.
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And so now, the next
obvious question would be,
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is there a relationship between
the pressure and the height?
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Well, there is, and it's
harder to think about that
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for air molecules because air molecules
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are very compressible, so
it's a little hard over there.
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But let's consider
non-compressible fluids,
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like water, for example.
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So here's a specific question.
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If we know the pressure
at some level over here,
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what is the pressure at
some depth, say h, below?
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So let's say the pressure at the top is PT
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and the pressure at the bottom is PB.
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Well, we know that the pressure
at the bottom is higher
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than the pressure at the top.
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So we could say pressure at the bottom
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equals pressure at the top,
plus some additional pressure
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due to this weight of the water.
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But how do we figure that out?
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Well, for that, let's just
draw a cuboidal surface,
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having the surface area A.
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Now, the additional pressure
that we are getting over here
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is due to the weight of
this cuboidal column.
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To be precise, it's going
to be the weight per area.
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So this term over here is
gonna be weight per area.
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But what exactly is the
weight of this cubital column?
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Well, weight is just the force of gravity,
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so it's gonna be MG, where
M is the mass of the water
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in this column divided
by the area, which is A,
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but how do we figure out what is the mass
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of the column of this water?
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Well, we know that density
is mass per volume.
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So mass can written as
density times volume,
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and that's because we know
the density of a fluid.
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So we can write this as
density of the fluid,
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density of water, times
the volume of the column
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times GD divided by A.
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But the final question is what
is the volume of this column?
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Hey, we know the volume of the column.
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Volume of this cuboidal column
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is just going to be area times the height.
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And so we can plug that in over here,
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and if we cancel out the areas,
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we finally get our expression.
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The pressure at the bottom will equal
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the pressure at the top plus
this additional pressure
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due to the weight of this column.
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And this equation will work anywhere
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as long as you're dealing
with a non-compressible fluid
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because we are assuming
the density to be the same.
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If you consider a
compressible fluid, like air,
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the density varies and this
calculation becomes harder,
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and so you'll get a considerably
different expression.
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But what I find really
surprising about this
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is that for a given
non-compressible fluid,
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which means it has a specific density,
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the pressure difference between two points
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only depends on their
height, nothing else.
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In other words, this means
the pressure difference
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between two points, say
10 centimeter apart,
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whether you consider that in an ocean
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or a tiny test tube, it's the same.
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It doesn't matter how much
water you're dealing with,
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it's just the height that matters.
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Anyways, now we can introduce
two kinds of pressure.
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The pressure that we have
over here, these two,
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they're called absolute pressures.
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For example, if this was
the atmospheric pressure,
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then that is the absolute pressure.
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The absolute pressure of the atmosphere
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close to the sea level
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is about 10 to the power of five pascals.
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But now, look at this term.
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What does that term represent?
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That represents the extra pressure
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that you have at this point
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over and above the atmospheric pressure.
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That extra pressure is what
we call the gauge pressure.
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And most of the time when
we're talking about pressure
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in our day-today life,
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we are not talking about
the absolute pressure,
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we're talking about the gauge pressure.
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So for example, when we talk
about the blood pressure,
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we say it's 120 millimeters of mercury.
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What does that even mean?
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Well, remember that the
atmospheric pressure
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is 760 millimeters of mercury.
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This is the pressure over and above that.
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So the pressure in the arteries, or veins,
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during a cysto for example,
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is 760 millimeters plus
120 millimeters of mercury.
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That's what it really means.
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So this is the additional pressure
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above the atmospheric pressure,
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so this is the gauge pressure.
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The same as the case with our tires.
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For example, if you look at
the pressure inside the tire,
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you can see it's about 40 PSI,
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but that is a gauge pressure,
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meaning it's over and above
the atmospheric pressure.
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Remember, the atmospheric
pressure is 14.7 PSI.
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So the pressure in the tire is 40 PSI
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above the atmospheric pressure.
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So most of the time, we're
dealing with gauge pressures.
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Okay, finally. coming back over here,
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suppose we were to draw a
graph of the gauge pressure
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versus the depth.
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Okay, what do you think the
graph would look like for,
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say, a lake and for the ocean?
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Why don't you pause it and
have a think about this?
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Okay, let's consider the lake.
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Right at the surface, the
gauge pressure is zero
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because the pressure
over there is the same
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as the atmospheric pressure,
so we start from zero,
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and then you can see that the
gauge pressure is proportional
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to the height, it's proportional to it,
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so we get a straight line.
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And so we'd expect the
pressure to increase linearly.
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That's what we would get for
the lake. What about the ocean?
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Well, ocean is also water,
so it has the same density,
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or does it?
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Remember, ocean has salt water,
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so the density is slightly higher.
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So for the ocean, we expect
the line to be steeper,
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having slightly higher slope.
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Finally, before wrapping up the video,
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if you were to submerge
a cube inside water,
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earlier, we said that the
pressure is gonna be the same
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from all directions,
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but now we know that the
pressure on the bottom
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is slightly higher than
the pressure on the top,
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which means the forces on the bottom
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would be slightly higher
than the force on the top
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because the area is the same.
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So wouldn't that produce
a net upward force?
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Yes, it would, and that's
called the buoyant force,
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which is responsible for
making certain things float.
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And that's something we'll
talk about in a future video.