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Hydrostatic Pressure Formula

Describes the pressure exerted by a fluid at a given depth, where \rho is density, g is acceleration due to gravity, and h is depth.
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The statement of the theorem

The hydrostatic pressure P(h)P(h) at a depth hh within a fluid of constant density ρ\rho under gravitational acceleration g\vec{g} is derived from the condition of mechanical equilibrium. Consider a fluid element of height dhdh and cross-sectional area AA. The pressure gradient P\nabla P must balance the body force per unit volume, fb=ρg\vec{f}_b = \rho \vec{g}. Since the fluid is static, the pressure gradient is purely vertical: Ph=ρg\frac{\partial P}{\partial h} = -\rho g. Integrating this differential equation from the surface (h=0h=0) to an arbitrary depth hh, and assuming the surface pressure P0P_0 is the reference pressure, yields the scalar relationship for the gauge pressure Pgauge(h)P_{gauge}(h): \n\nPgauge(h)=0hρgdh=ρghP_{gauge}(h) = \int_{0}^{h} \rho g \, d h' = \rho g h
Source: Wikipedia