Equations · equation
Hydrostatic Pressure
Fluid Dynamics · 1653
- Equation
- p = p₀ + ρ g h
- Field
- Fluid Dynamics
- Symbols
- p pressure at depth h · p₀ pressure at the surface · ρ fluid density · g gravitational acceleration · h depth below the surface
- Year
- 1653
Significance
Pressure in a still fluid rises with depth by the weight of the column above — about one atmosphere per ten metres of water. Stevin had it in 1586, Pascal made it precise in 1653. It is the load on a tailings dam's face, the pressure a diver feels, the metallostatic head that fills a sand mould, and the p in every fluid equation that follows.
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