Pressure (p)

Pressure is force distributed over an area - how much push, per unit of surface.

Static fluid pressure follows p = p0 + ρgh (hydrostatic pressure increasing with depth); flowing-fluid pressure trades off against velocity and elevation along the Bernoulli relation. Base SI unit is the pascal (Pa); engineering and gas work commonly use kPa, bar, atm, or psi instead.

A frequent point of confusion: pressure increases with depth regardless of the shape or total volume of the container - a narrow deep tank and a wide shallow-but-equally-deep pool exert the same pressure at the same depth. It's h (depth), not the total amount of fluid, that drives p = ρgh.

Typical Pressures by Context

ContextkPapsi / other
Standard atmosphere (sea level)101.32514.7 psi
Car tire (gauge)220–24032–35 psi
Municipal water main400–80058–116 psi
Human systolic blood pressure (~120 mmHg)~16~120 mmHg
Mariana Trench (deepest ocean point)~108,000~1,080 atm

Frequently Asked Questions

What's the difference between gauge and absolute pressure?

Gauge pressure is measured relative to atmospheric pressure (what most pressure gauges read, including tire gauges - 0 gauge means "same as the surrounding air"). Absolute pressure is measured relative to a true vacuum: absolute = gauge + atmospheric. The Hydrostatic Pressure Calculator's absolute mode adds that atmospheric term explicitly.

Does the shape of a container affect the pressure at the bottom?

No - this is often called the hydrostatic paradox. Pressure at a given depth depends only on the fluid's density, gravity, and that depth (p = ρgh), not on the container's shape or the total volume of fluid above it. A thin tall tube and a wide tank filled to the same depth exert identical pressure at the bottom.

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