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Today, we're going to discuss pressure in fluids when they are at rest. Can anyone tell me what happens to shear stresses in this scenario?
I think shear stress becomes zero when the fluid is not moving.
That's correct! So when fluids are at rest, only normal stresses, which we relate to pressure, act on the fluid. This is key to understanding static fluid behavior.
What do we mean by normal stress acting on the surface?
Normal stress refers to the pressure acting perpendicular to the surface. Think of it like a force that pushes directly inward without causing any sliding. We often express this as P = P(x, y, z), which signifies how pressure varies in three dimensions.
Let’s consider a simple control volume in fluid mechanics. Can anyone describe what this includes?
It would include the fluid itself and the surfaces where forces act, like pressure.
Exactly! We have two main forces: surface forces from pressure and body forces from gravity. Can anyone remember how we express force components in our equations?
We calculate them based on the unit weight and volume of the fluid.
Correct! The pressure applies normal to surfaces, and through our calculations, we can derive how pressure gradients relate to these forces. Who remembers how this relates to gravity?
The pressure gradient has to balance against gravitational forces for fluids at rest!
Now, let’s talk about measuring pressure. What are the main types of pressure we encounter in fluid systems?
There's absolute pressure and gauge pressure, right?
Exactly! Absolute pressure is measured from a perfect vacuum, while gauge pressure is measured relative to atmospheric pressure. Can anyone explain when we would use gauge pressure?
In most practical scenarios, like measuring pressure in pipelines, we often care more about gauge pressure because it's relative to the air around us.
Great point! It's vital to understand these differences, especially when dealing with problems in hydrostatics.
Finally, let’s explore applications. How do we apply our understanding of pressure to real-world situations like barometers?
Barometers measure atmospheric pressure using mercury, right? They show how pressure decreases at higher altitudes.
Exactly! That concept connects to how we can measure altitude as well. What can you tell me about capillary action?
Capillary action happens when surface tension interacts with fluid, causing it to rise in narrow tubes!
Yes! This interplay of forces is essential for various applications in biology, engineering, and physics.
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The conclusion addresses the fundamental aspects of pressure in fluids at rest, explaining hydrostatic pressure distributions, the importance of control volumes, and differentiating between absolute, gauge, and vacuum pressures. Additionally, it introduces the relationship of pressure to the gravitational field and summarizes core equations governing these principles.
In this section, we delve into the behavior of pressure within fluid systems, particularly when the fluid is at rest. The discussion centers on how we can describe pressure fields as functions of three spatial coordinates (P = P(x, y, z)). When a fluid is at rest, shear stresses are non-existent, meaning that only normal stresses (pressure) affect the control surfaces of the fluid. This leads to the understanding that pressure acts perpendicularly to the surface in fluid mechanics, confirming Pascal's Law.
We utilize a control volume to analyze forces acting on a fluid element, including surface forces due to pressure and body forces like gravity. The unit weight and volume of the fluid control element are critical in determining force components along the x, y, and z directions. The resultant equations derived from these force components summarize the equilibrium conditions necessary for fluids at rest: the gradient of pressure is linked to the gravitational field.
Moreover, we distinguish between absolute and gauge pressures, emphasizing how local atmospheric conditions can dictate measurements of pressure. Knowledge of both types of pressure is essential for understanding real-world applications such as manometry and how pressure varies with changes in fluid states or environmental conditions. The significance of these equations extends to practical applications, including calculating pressures in situations like capillarity and barometric measurements.
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Now the point is what we are going to discuss is that gauge pressure and vacuum pressure. Components now is coming it what is your datum to measure the pressure. Whether you have to make a absolute zero pressure, that means you have a vacuum. From there you are measuring the pressure, or you consider as local atmosphere, to measure the pressure.
In this chunk, we discuss two primary methods of measuring pressure: gauge pressure and vacuum pressure. Gauge pressure measures the pressure relative to the surrounding atmospheric pressure, while vacuum pressure refers to pressures below atmospheric pressure. The key aspect is the 'datum'—the reference point used to gauge the pressure. Absolute pressure measurements use a vacuum as a reference point, where the pressure is zero. On the other hand, in most practical situations, particularly near the Earth's surface, atmospheric pressure serves as the datum.
Imagine you are at the beach, and you have a balloon filled with air. If you take that balloon to the bottom of the ocean, the water pressure increases, and your balloon compresses. If you were measuring this pressure with a gauge, it would tell you how much higher the pressure is compared to the atmospheric pressure at the surface, hence it's gauge pressure. However, if you measure it in an absolute sense (i.e., from a complete vacuum), you would include the atmospheric pressure acting on the balloon as well.
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If you need to compute it what will be the absolute pressure, then it is a very easy. You just use whether the gauge pressure or this vacuum pressure that difference what we can get it that what you just add with atmospheric pressure to get the absolute pressure.
To find the absolute pressure, one must consider the gauge pressure and the atmospheric pressure. If you have a gauge pressure that is above atmospheric pressure, you would simply add the atmospheric pressure. Conversely, if you have vacuum pressure (pressure below atmospheric), you would subtract that value from atmospheric pressure. This is essential for many engineering calculations, as absolute pressure provides a consistent reference across varying conditions.
Think about a tire gauge that measures how inflated your car tires are. When it reads 32 psi, it is displaying gauge pressure. If atmospheric pressure is approximately 14.7 psi, then the absolute pressure is simply 32 + 14.7 = 46.7 psi. This means the total pressure inside your tire is actually 46.7 psi when you consider both the tire’s pressure and atmospheric pressure.
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Now as we derive pressure distribution equations which in vector forms and let we simplify that equations which earlier we consider the acceleration due to gravity is a vector which will have, …and that field what we will get it this part and is finally the ∇ρg.
In this section, we discuss hydrostatic equations and how they relate to fluid pressure distributions. The gravitational force acting on a fluid can be defined in vector form, accounting for varying directions of force. When the fluid is at rest, the sum of forces acting on it must equal zero, leading us to conclude that a pressure gradient exists in the direction of gravitational pull. Thus, the change in pressure in a fluid is directly related to the height and density of the fluid, alongside gravitational acceleration.
Consider a tall glass of water. The water at the bottom of the glass experiences a higher pressure than the water at the top due to the weight of the water above it. Just like the hydrostatic equation describes, the pressure difference depends on how deep you go into the glass, highlighting how gravity affects fluid pressure.
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Now let me consider the capillary effect as you could have seen some of the books if any of the class 12th levels. What do we do it we just coming the two force components, the force due to the surface tensions and the gravity force of the capillary part.
The capillary effect refers to the ability of a liquid to flow in narrow spaces without the assistance of external forces. This phenomenon occurs due to the interplay of cohesive forces (between the liquid molecules) and adhesive forces (between the liquid and another surface). In smaller tubes, the surface tension of the liquid can cause it to rise higher against gravity. We analyze this effect and derive equations governing how high the liquid will rise based on factors such as tube diameter and liquid properties.
Think of a sponge soaking up water. The small holes in the sponge act like tiny capillary tubes. When you place the sponge in water, the water climbs up into the sponge against gravity because of the adhesive forces holding the water to the sponge and the cohesive forces within the water itself. This is very similar to how water rises in a thin straw.
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Now let me come it to the mercury barometer case with a very simplified same capability concept what we used to measure the atmospheric pressure.
Mercury barometers use a simple principle to measure atmospheric pressure. They consist of a tube filled with mercury that is inverted in a reservoir of mercury, creating a vacuum at the top of the tube. The height of the mercury column is used to determine the atmospheric pressure; the higher the mercury column, the greater the atmospheric pressure. The key aspect is that the atmospheric pressure forces the mercury up the tube from the reservoir. This method is a practical application of hydrostatic principles.
Imagine holding a straw in a glass of water. If you put your thumb over the end of the straw while it's submerged and lift it out, the water stays in the straw because of the atmospheric pressure pushing up from below. Similarly, in a mercury barometer, the atmospheric pressure pushes the mercury column up against gravity, allowing us to measure that pressure accurately.
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Key Concepts
Pressure acts normally to surfaces in fluid mechanics.
Hydrostatic pressure can be calculated with respect to fluid height and weight.
Gauge pressure relates to atmospheric pressure, while absolute pressure relates to vacuum.
See how the concepts apply in real-world scenarios to understand their practical implications.
A mercury barometer is used to measure atmospheric pressure by balancing the weight of mercury against the atmospheric pressure.
In a connected liquid system, such as a lake and reservoir, the pressure remains constant across horizontal surfaces when the fluid is at rest.
Use mnemonics, acronyms, or visual cues to help remember key information more easily.
In fluid at rest, pressure is best, no shear, just normal, it's the test.
Imagine a fluid sitting still in a glass. The pressure from the fluid pushes against the walls equally, just like when you press your hand against a flat surface.
PAG, stands for Pressure And Gravity which reflects the key relationship in hydrostatics.
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Review the Definitions for terms.
Term: Pressure Field
Definition:
A map of pressure within a defined area of fluid, expressed as a function of Cartesian coordinates.
Term: Control Volume
Definition:
A designated volume in fluid mechanics used to analyze physical quantities such as mass, momentum, and energy.
Term: Absolute Pressure
Definition:
Pressure measured relative to a perfect vacuum where the pressure is zero.
Term: Gauge Pressure
Definition:
Pressure measurement relative to the atmospheric pressure surrounding the measurement point.
Term: Hydrostatic Pressure
Definition:
Pressure exerted by a fluid at rest due to the weight of the fluid above it.