Hydrostatic Paradox
The hydrostatic paradox explains the very interesting concept in fluid mechanics that pressure exerted by a fluid at rest at any depth is determined by only the height of the fluid column above that point and does not depend on the shape or volume of the container. The whole idea clashes with our general notion about how pressure behaves in various containers.
1.0What is the Hydrostatic Paradox?
The meaning of the Hydrostatic Paradox is that pressure at any depth is independent of the size, shape, and aspect of the container, with the liquid's height being at par. This paradoxical-looking result indicates that the shape and volume of the containing vessel do not affect the pressure at a particular depth.
2.0Principle of Hydrostatic Paradox
The Hydrostatic Paradox is based on the idea that hydrostatic pressure is determined by the height of the liquid column, its density, and gravitational force and does not depend on the shape of the container used. Mathematically, the pressure at any given depth is described by the formula:
Here:
- 𝑃 = pressure at the point,
- 𝜌 = density of the fluid,
- 𝑔 = acceleration due to gravity and
- ℎ = height of the fluid column above the point.
S.I. unit of pressure is Pascal (Pa).
Key Takeaway
- The difference in pressure between two points at different depths in a fluid, you can use the following formula: . Here, P is the difference in pressure, and h is the different depths in a fluid.
- The formula for pressure can also be written as: . This formula is used to calculate the pressure of the fluid on an open surface like an ocean or lake. Here, P0 is the atmospheric pressure.
- The formula is used to calculate the pressure in a fluid at rest in a closed column where the atmospheric pressure is assumed to be zero.
3.0Hydrostatic Law
The law states that in a stationary fluid, Hydrostatic pressure due to liquid on the vertical wall of the container increases with the increase in depth and has a direct relation with its corresponding column height.
In simpler words the deeper you go into the fluid, the greater pressure the fluid will exert. It happens primarily due to the weight of the fluid increases with the depth. This expresses why pressure becomes greater by sinking deeper into a fluid. The expression for pressure at hydrostatic is:
This law is an important concept in fluid dynamics to understand why containers of different shapes filled with the same height exert the same hydrostatic pressure at the bottom.
4.0Gauge Pressure and Atmospheric pressure
As mentioned earlier, Hydrostatic law is the concept used only for stationary fluids. In real-life scenarios, the gauge pressure gives the actual pressure exerted by the fluid on an object, relative to the atmospheric pressure. This is the actual pressure experienced by the object submerged in a fluid.
The gauge pressure does not include the effect of atmospheric pressure, which is assumed to be constant and acting uniformly on all surfaces. Hence, gauge pressure represents the real, effective pressure exerted by the fluid, which is critical for understanding fluid dynamics in systems like tanks, pipes, and machinery.
Mathematically the Gauge pressure with respect to atmospheric pressure is represented as:
5.0Examples of Hydrostatic Paradox
Problem 1: A U-tube manometer contains mercury (ρHg=13600 kg/m3) and water (ρwater=1000 kg/m3). The difference in the height of mercury columns in the two arms of the U-tube is 0.1 meters. Calculate the pressure difference between the two arms.
Solution: It is given that:
ρHg=13600 kg/m3, h = 0.1m, g = 9.8 m/s2
The pressure difference(P) due to the height difference(h) in a fluid of density p is given by:
Problem 2: A rectangular gate in a dam is 2 meters high and 4 meters wide. The gate is submerged in water such that the top edge of the gate is 3 meters below the water surface. Calculate the hydrostatic force acting on the gate. Use the density of water ρ=1000 kg/m3 and g=9.8 m/s2.
Solution:
Hydrostatic Pressure at the top and bottom of the Gate:
- Top of the gate:
- Bottom of the gate:
Average Pressure on the gate:
Hydrostatic force
Now the area of Gate =
Problem 3: A solid cube with a side length of 0.5 meters and density ρcube=500 kg/m3 is completely submerged in a container with three immiscible fluids: oil (ρoil=800 kg/m3, water (ρwater=1000 kg/m3), and mercury (ρHg=13600 kg/m3). The cube is half submerged in oil, with the remaining part in water and mercury. Determine the hydrostatic pressure acting on the top and bottom faces of the cube and calculate the net buoyant force acting on the cube. Assume g=9.8 m/s2.
Solution: According to the question
The total height of the cube is 0.5m
The cube is half submerged in oil, so the depth in oil is 0.25m
The remaining 0.25m is submerged in water and mercury.
Hydrostatic Pressure on the top face: The top face is at the interface between the oil and air.
Depth of the top face htop in oil = 0.25 meters.
Hydrostatic pressure at the top face due to oil: Ptop = ρoilghtop = 800×9.8×0.25 = 1960 Pa
Hydrostatic Pressure on the Bottom Face: The bottom face is submerged in water and mercury.
Depth of the bottom face hbottom in oil + water: 0.25 meters (oil) + 0.25 meters (water) = 0.5 meters.
Pressure due to oil: Poil = 800×9.8×0.25 = 1960 Pa
Pressure due to water: Pwater = 1000×9.8×0.25 = 2450 Pa
Total pressure at the bottom face: Pbottom = Poil +Pwater = 1960+2450 = 4410 Pa
The buoyant force is the weight of the displaced fluid.
The volume of the cube Vcube = 0.5×0.5×0.5=0.125 m3
Weight of displaced oil: Woil = ρoilgVoil = 800×9.8×(0.5×0.5×0.25) = 490 N
Weight of displaced water: Wwater = ρwatergVwater = 1000×9.8×(0.5×0.5×0.25)= 613.5 N
Total buoyant force:
Fbyoyant = Woil + Wwater = 490 + 613.5 = 1102.5N
Table of Contents
- 1.0What is the Hydrostatic Paradox?
- 2.0Principle of Hydrostatic Paradox
- 2.1Key Takeaway
- 3.0Hydrostatic Law
- 4.0Gauge Pressure and Atmospheric pressure
- 5.0Examples of Hydrostatic Paradox
Frequently Asked Questions
Applications include the designing of dams, water towers, and submarines, also the understanding of the change in pressure in the atmosphere and oceans.
Hydrostatic pressure explains that atmospheric pressure is due to the weight column of air above a given point, which at altitude decreases.
The pressure is directly proportional to the fluid's density. The denser the fluid, the more intense hydrostatic pressure at a specific depth is produced.
There is no negative hydrostatic pressure because it is given as the pressure exerted by a fluid on any given object. Negative pressure involves suction or vacuum.
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