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