Pour oil or kerosene into a water U-tube — or water on top of mercury — and watch the levels settle: columns of different height balance each other, ρ₁h₁ = ρ₂h₂. In vessels of different shapes the water stands at one level, and the pressure on the bottom is the same, although they hold different amounts of water. Drag the pressure probe: it shows the pressure p = ρgh at any point, and the rings mark where the pressure is the same.
The colour of the liquid shows the pressure (scale at the bottom left). Force arrows are not to scale (∝ ∛F); the numbers are exact.
Pressure without the atmosphere: p = ρgh, h is the depth below the surface of the same liquid. The arms of the U-tube have equal cross-sections, so the lower liquid drops on the left by as much as it rises on the right. The oscillations after pouring die out; the numbers in Measurements are for equilibrium.
The fountains of Peterhof near St Petersburg have been playing since 1721 without a single pump. Water collects in ponds on the Ropsha heights and runs down a conduit more than 20 kilometres long to the parks, where it rises in the fountains by itself — like in communicating vessels, towards the level it came from. Water towers, the plumbing of tall buildings, locks on rivers and canals that carry ships from one water level to another, gauge glasses on boilers and an ordinary kettle all work the same way: the water in the spout always stands at the same level as in the kettle.
ρ is the density of the liquid, kg/m³; g ≈ 9.8 m/s²; h is the depth below the free surface, m
h₁, h₂ are the heights of the liquid columns above the interface level, m; ρ₁, ρ₂ are the densities, kg/m³
h₁, h₂ are the heights of the liquid levels in the vessels above the connecting tube, m
p is the pressure on the bottom, Pa; S is the area of the bottom, m²; h is the height of the liquid level above the bottom, m
Pressure inside a liquid. Each layer of a liquid presses with its weight on the layers below, so pressure grows with depth: p = ρgh, where h is the depth below the free surface. In water the pressure rises by about 10 kPa for every metre: at a depth of 10 m it is 98 kPa — almost one more atmosphere. Mercury is 13.6 times denser than water, and the pressure in it grows 13.6 times faster. At the same depth in the same liquid the pressure is the same in all directions.
Pressure does not depend on the shape of the vessel. The pressure on the bottom is set only by the height of the column and the density of the liquid. In vessels of different shapes with equal bottoms, filled to the same level, the pressure on the bottom is the same, and so is the force F = pS — although the wide vessel holds several times more water than the narrow one. This is called the hydrostatic paradox. The walls of a widening vessel carry the 'extra' water themselves, while in a narrowing vessel the walls press down on the water.
Communicating vessels. These are vessels joined at the bottom. A single liquid settles in them at the same level, whatever their shape. If the levels differed, the pressures on the two sides at the bottom of the connecting tube would be different, and the liquid would flow across until they were equal. In the simulator the probe shows it: in one liquid, points with the same pressure always lie at the same height.
Two different liquids. If oil is poured into one arm of a water U-tube, the pressures are compared at the level of the interface: below it both arms contain the same water, and the pressures are equal. Above that level there is a column of oil h₁ on the left and a column of water h₂ on the right, so ρ₁gh₁ = ρ₂gh₂, or ρ₁h₁ = ρ₂h₂. The heights are inversely proportional to the densities: 15 cm of oil (900 kg/m³) balances 13.5 cm of water, and 30 cm of water balances only 2.2 cm of mercury. A liquid manometer works this way: pressure is measured by the difference of levels in a U-tube.
Try it yourself. Start with an empty left arm (h₁ = 0) — the levels are equal. Add oil and watch the interface go down while the water on the right goes up. Put the probe at the interface — the ring in the right arm is at the same height. Raise the probe into the oil — the point with the same pressure in the water is lower. Choose 'mercury + water': with the same column of water the mercury shifts only a little. In 'Different shapes' add water and compare the volumes in Measurements: the vessels hold different amounts of water, yet the pressure on the bottom is one and the same.
First come simulators and problems from this very chapter, then closely related topics of the section.
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Mechanics · Motion
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Mechanics · Energy