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Pressure in still fluids

Pressure is force spread over area, and in a fluid it grows with depth — nothing else about the container matters.

Pressure

Pressure is force per area, P = F/A, measured in pascals (1 Pa = 1 N/m^2). Fluid pressure pushes perpendicular to every surface it touches, equally in all directions. Gauge pressure is what a tire gauge reads — the amount above atmospheric — while absolute pressure adds the 1.01e5 Pa of the atmosphere on top.

P = \frac{F}{A}

Hydrostatic pressure

In a liquid at rest, pressure grows linearly with depth: P = P0 + rho*g*h, where rho is the fluid density and h is the depth below the surface. The pressure depends only on depth and fluid — not on the container's shape or the total volume of water — which is why connected tanks of any geometry fill to the same height.

P = P_0 + \rho g h

Worked example

A diver descends 10 m in fresh water (rho = 1000 kg/m^3). The gauge pressure is rho*g*h = (1000)(9.8)(10) = 98,000 Pa, about 98 kPa — roughly one atmosphere. Adding the air's 1.01e5 Pa, the absolute pressure is about 2.0e5 Pa: two atmospheres total at 10 m down.

P = P_0 + \rho g h \approx 1.0\times 10^5 + 9.8\times 10^4 = 2.0\times 10^5\ \text{Pa}

Flashcard

P = \frac{F}{A}

Pressure equals force per unit area

One pascal is one newton spread over one square meter. Doubling the contact area halves the pressure for the same push, which is why snowshoes keep you on top of the drift.

Check your understanding

What gauge pressure does a swimmer feel 5.0 m below the surface of a lake?

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