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Today, we're going to talk about pressure in fluids. Can anyone tell me what they know about pressure?
Isn't pressure just the force applied on an area?
That's correct! But remember, pressure is a scalar quantity. This means it has magnitude but no direction. It's defined as the normal force acting per unit area. Can anyone think of an example where this concept plays a role?
Like when I use a needle to draw blood? It hurts less if I use a bigger object, right?
Exactly! A smaller area leads to higher pressure. This principle helps us understand many everyday phenomena.
To remember the concept of pressure, think of the acronym 'POS': Pressure Over Surface.
Got it! It makes sense that the smaller the area, the more pressure is exerted!
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Great! Now, let's discuss fluid equilibrium. When we have a fluid at rest, does anyone know why the pressures on different faces of a fluid element must balance?
So that it stays still? It won't move if the forces are equal.
Exactly! This leads us to the hydrostatic pressure equation P = Pa + Οgh. Can anyone explain what each term in this equation represents?
Pa is the atmospheric pressure, Ο is the density of the fluid, g is the acceleration due to gravity, and h is the height of the fluid column above the point you're measuring, right?
Spot on! This equation helps us understand why pressure increases with depth in a fluid. Can someone share a real-world example where this applies?
Pressure underwater! The deeper you go, the more pressure you're under because of all that water above.
Perfect example! Keep in mind that this equation applies well to incompressible fluids, which is nearly true for liquids.
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Now, letβs clarify the difference between gauge pressure and absolute pressure. Who can explain what gauge pressure is?
Isn't it the pressure relative to atmospheric pressure?
That's correct! Gauge pressure is measured above atmospheric pressure. So any pressure reading from a gauge subtracts the atmosphere? Can anyone give an example?
Like a car tire pressure gauge, right? It shows how much pressure is in the tire above the atmospheric pressure.
Exactly! Now, absolute pressure includes atmospheric pressure. Remember, the formula is P = Pg + Pa. To recap: Gauge pressure is what you read from the gauge, and absolute pressure is gauge plus atmospheric.
So if it reads zero, it doesn't mean there's no pressure, it just means itβs measuring pressure relative to the air?
Exactly! And this distinction is critical in many engineering applications.
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The Points to Ponder section emphasizes the intricacies of fluid behavior, such as scaling pressure, the variations in pressure due to height, and distinguishing between gauge and absolute pressure. Additionally, it clarifies the nature of pressure as a scalar quantity and elaborates on the significance of hydrostatic pressure in various contexts.
In this section, we explore several important concepts about fluid properties that require careful consideration. It starts with the understanding that pressure, despite being derived from a force, is a scalar quantity. The definition, often misconstrued as implying a vector nature, focuses strictly on the normal force acting on an area. Furthermore, pressure exists throughout a fluid at varying depths, and the equilibrium state of a fluid element is maintained by equal pressures acting on different surfaces. This leads to the realization that the formula for pressure gradients, P = Pa + Οgh, holds for incompressible liquids, supporting the analysis of real-world scenarios like atmospheric pressure variations. The section also touches on gauge versus absolute pressure, providing clarity on how these concepts are utilized in practical applications, such as pressure measurement in different gauges.
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Pressure is a scalar quantity. The definition of the pressure as 'force per unit area' may give one false impression that pressure is a vector. The 'force' in the numerator of the definition is the component of the force normal to the area upon which it is impressed. While describing fluids as a concept, shift from particle and rigid body mechanics is required. We are concerned with properties that vary from point to point in the fluid.
Pressure is essentially a measure of how much force is distributed over a specific area. Since pressure does not have a direction like force, we classify it as a scalar quantity. In formulas, we often represent force as a vector, but when calculating pressure, we need only the part of the force that acts directly perpendicular (normal) to the surface. This understanding is crucial, especially when we move from studying solid bodies to the more fluid-like behavior where pressure can vary throughout the material.
Consider a soft pillow. When you press down on it, the pillow compresses and the pressure on the surface is felt evenly, no matter where you press. If you press hard with a small point (like a pencil), you feel a sharper pressure on that spot. Here, the overall pressure is scalar, but the localized force can act differently depending on how hard you press or the area you apply it to.
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One should not think of pressure of a fluid as being exerted only on a solid like the walls of a container or a piece of solid matter immersed in the fluid. Pressure exists at all points in a fluid. An element of a fluid (such as the one shown in Fig. 9.4) is in equilibrium because the pressures exerted on the various faces are equal.
Pressure is not something that only impacts the walls of a container or solid objects submerged in it; it permeates all of the fluid itself. Each tiny element of fluid experiences pressure from all sides equally, creating an equilibrium state. This means that if you were to take a small piece of fluid out of a larger body, it would still maintain this balance of pressure, acting uniformly without any directionality.
Think of a balloon filled with water. When you squeeze the balloon, you feel the pressure of the water pushing back against your hands regardless of where you press. This is because the water inside exerts equal pressure in all directions. If the balloonβs fabric stretches in one spot, itβs still contained and balanced by the pressure of the water pushing from the other areas.
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The expression for pressure P = Pa + Οgh holds true if fluid is incompressible. Practically speaking it holds for liquids, which are largely incompressible and hence is a constant with height.
In the equation P = Pa + Οgh, P represents the pressure at a certain depth in a fluid, Pa is the atmospheric pressure above the fluid, Ο is the fluid's density, g is the acceleration due to gravity, and h is the depth. This equation assumes the fluid is incompressible, which is a good approximation for liquids. This means that, for very small changes in the pressure, the density remains nearly constant, even as you calculate changes in pressure with depth.
Imagine diving into a pool. As you dive deeper, you might feel the water pressure increasing with each meter you descend. The equation demonstrates that this increase in pressure directly corresponds to the depth and the constant density of the water. Itβs similar to how the pressure in a balloon increases when it is filled with air and compressed β the air density changes very little even as the pressure changes with volume.
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The gauge pressure is the difference of the actual pressure and the atmospheric pressure. P β Pa = Pg. Many pressure-measuring devices measure the gauge pressure. These include the tyre pressure gauge and the blood pressure gauge (sphygmomanometer).
Gauge pressure is the measurement of pressure relative to atmospheric pressure. When you measure how much pressure is in your car tires, you are measuring gauge pressure, not absolute pressure. This means that the guage subtracts the atmospheric pressure from its reading to show how much pressure is above the atmospheric level. This can be important because only the pressure above the atmospheric pressure affects the behavior of fluids in many practical situations.
When you inflate a bicycle tire, the pressure gauge tells you how much air is inside it relative to the atmospheric pressure outside. If the gauge shows 30 psi, it means the tire pressure is higher than the surrounding atmospheric pressure by 30 pounds per square inch. This is important because if you only consider absolute pressure, you might not realize the tire is not inflated enough to support your weight or ride comfortably.
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A streamline is a map of fluid flow. In a steady flow two streamlines do not intersect as it means that the fluid particle will have two possible velocities at the point.
Streamlines visually represent the flow of fluid in a steady state. In a well-defined flow, each fluid particle has a specific path it follows. If two streamlines were to intersect, it would imply that at that point, a particle of fluid could be moving in two different directions at once, which is not physically possible. Therefore, in a steady flow, streamlines never cross.
Think of traffic flowing on a road. Each car has a designated lane, and no two cars occupy the same spot at the same time. If cars crossed lanes at the same time, chaos would ensue. Similarly, streamlines represent the orderly flow of fluid particles; they each follow a specific path without crossing one another.
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Bernoulliβs principle does not hold in presence of viscous drag on the fluid. The work done by this dissipative viscous force must be taken into account in this case, and P2 will be lower than the value given by Eq. (9.12).
Bernoulliβs principle is based on the assumption that there are no losses in energy due to friction or viscosity while fluid flows. However, in real-world scenarios, fluids encounter resistance due to viscous forces, which means some of the energy is converted to heat and reduces the total mechanical energy available in the fluid flow. Therefore, in such cases, the pressure calculated using Bernoulli's equation would not be accurate.
When you slide a book on the table, a certain amount of energy is lost due to friction. If you expect the book to slide across the table without stopping, you will realize it slows down too quickly, not due to forces directly acting on it but rather the invisible forces of friction. In fluid dynamics, similar losses occur and thus the ideal calculations using Bernoulli's principle need adjusting.
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As the temperature rises the atoms of the liquid become more mobile and the coefficient of viscosity, Ξ· falls. In a gas the temperature rise increases the random motion of atoms and Ξ· increases.
In liquids, increasing the temperature gives molecules more kinetic energy, allowing them to move past one another more easily, this results in a lower viscosity. Conversely, in gases, increased temperature heightens the random movement of gas molecules, contributing to a higher viscosity as they collide more frequently. This behavior is critical to understanding fluid dynamics and managing different fluids under varying temperatures.
Consider how honey flows thicker and slower when cold, but becomes much thinner and runs quickly when warmed. A similar effect happens with gas β the warm air inside a balloon expands and causes it to rise, illustrating how changes in temperature directly affect the viscosity of these materials.
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Surface tension arises due to excess potential energy of the molecules on the surface in comparison to their potential energy in the interior. Such a surface energy is present at the interface separating two substances at least one of which is a fluid. It is not the property of a single fluid alone.
Surface tension is a phenomenon that describes how the surface of a liquid behaves differently from its interior. Because molecules on the surface of a liquid experience imbalance due to having fewer neighboring molecules to pull them inward, these surface molecules possess more energy. This excess energy leads to surface tension, making liquids bead up and resist external forces trying to break the surface.
Think about how small insects like water striders can walk on the surface of water without sinking. Their legs spread out, distributing weight over the surface tension; the water is trying to pull its surface down into itself, and effectively 'supporting' the insect, thanks to the physics of surface tension.
Learn essential terms and foundational ideas that form the basis of the topic.
Key Concepts
Pressure: A scalar quantity defined as force per unit area.
Hydrostatic Pressure: Pressure variation due to fluid weight and height.
Gauge Pressure: Measurement of pressure above atmospheric pressure.
Absolute Pressure: Total pressure measured including atmospheric influence.
Fluid Equilibrium: Condition where pressures are balanced, preventing fluid flow.
See how the concepts apply in real-world scenarios to understand their practical implications.
When a scuba diver goes deeper underwater, they experience increased pressure due to the water column above them.
A tire pressure gauge displays the pressure inside the tire, which is gauge pressure, not accounting for the atmospheric pressure.
Use mnemonics, acronyms, or visual cues to help remember key information more easily.
Pressure's how force does play, on areas big and small, every day.
Imagine a deep-sea diver who feels the weight of the ocean above. The deeper they go, the pressure builds; it's as if the water's hugging them tighter.
P = Pa + Οgh: Think of 'Pigs Are Great Huggers' for remembering hydrostatic pressure relationship.
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Review the Definitions for terms.
Term: Pressure
Definition:
The force applied per unit area, measured in pascals (Pa).
Term: Gauge Pressure
Definition:
Pressure relative to atmospheric pressure, typically read from a gauge.
Term: Absolute Pressure
Definition:
Total pressure measured, including atmospheric pressure.
Term: Hydrostatic Pressure
Definition:
Pressure exerted by a fluid due to its weight when at rest.
Term: Fluid Equilibrium
Definition:
State where forces and pressures in a fluid are balanced, leading to no movement.