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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From the Equations database in Notion, last edited 2026-08-18. This page is the row, rendered by the build; nothing on it is written by hand.