Fluid pressure

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The pressure to the red area is the same, in all three cases, even though the containers are different. This is known as hydrostatic paradox.

Fluid pressure is a measurement of the force per unit area. Fluid pressure can be caused by gravity, acceleration, or forces in a closed container. Since a fluid has no definite shape, its pressure applies in all directions. Fluid pressure can also be amplified through hydraulic mechanisms and changes with the velocity of the fluid.

In a fluid column, as the depth increases, the pressure increases as well. Pressure (P) increases because as you go deeper, fluid at a lower depth has to support fluid above it as well. Therefore to define fluid pressure, we can say that it is the pressure at a point within a fluid arising due to the weight of the fluid.

Pressure in liquids is equally divided in all directions, therefore if a force is applied to one point of the liquid, it will be transmitted to all other points within the liquid.

The pressure in fluids can be calculated using the following relation:

P = hρg (Pressure = Height or Depth of the liquid × Density of the liquid × Gravitational pull (9.81m/s)).

Pressure is a scalar quantity. The SI Unit (International System of Unit) of pressure is the Pascal, or Newton per meter squared (N/m^2).

Points along the same depth will have the same pressure, while points at different depths will have different pressure.

An object that is partly, or completely submerged in fluid experiences a greater pressure on its bottom surface than on its top surface. This causes a resultant force upwards. This force is called upthrust, and is also known as buoyancy

For moving containers, the pressure changes,(Acceleration is the acceleration of the container)-.

For a vertical acceleration in the upward direction, the pressure in fluids= P = ρh (g+a)

For a vertical acceleration downward, the pressure in fluids= P = ρh (g-a)

For a horizontal acceleration, the pressure in fluids= tan θ

For any random angle of acceleration, the pressure in fluids= ρh (g + a sinθ)

Pascal's law for pressure at a point[change | change source]

The pressure at a point for a fluid at rest is the same in all directions.[1] This is Pascal's law. However, it is only valid under the continuum medium assumption, i.e, the point must be small but large enough in order that the hypothesis of continuum medium to be valid. If the point is smaller, then thermal fluctuations become important and the pressure (if can be defined at such a level) becomes anything but fluctuation (Brownian motion). [2]

References[change | change source]

  1. Bloomfield, Louis (2006). How Things Work: The Physics of Everyday Life (Third ed.). John Wiley & Sons. p. 153. ISBN 0-471-46886-X.
  2. Francisco J Arias (April 2022). "The demonstration of isotropic pressure at a point in fluid mechanics". HAL. Archived from the original on 23 October 2022. Retrieved 20 October 2022.{{cite web}}: CS1 maint: bot: original URL status unknown (link)