A fluid is anything that can flow — both liquids and gases. Unlike a solid, a fluid cannot sustain a shearing stress at rest, so it takes the shape of its container. The single most useful idea for fluids at rest is pressure.
Pressure is the normal (perpendicular) force exerted by a fluid per unit area of the surface in contact with it:
- $P=\frac{F}{A}$, where $F$ is the force acting perpendicular to a surface of area $A$.
- The SI unit of pressure is the pascal, $1\ \text{Pa}=1\ \text{N/m}^2$. Pressure is a scalar — it has no direction, even though force does.
- At a point inside a fluid the pressure acts equally in all directions; this is why a balloon inflates evenly.
Pressure due to a liquid column (pressure at depth). Consider a point at depth $h$ below the free surface of a liquid of density $\rho$. The weight of the liquid column above it pushes down, so the pressure increases with depth:
- $P=P_0+\rho gh$, where $P_0$ is the atmospheric (or surface) pressure and $\rho gh$ is the gauge pressure due to the liquid.
- Pressure depends only on the depth, density and $g$ — not on the shape or cross-sectional area of the container. This is the hydrostatic paradox: liquid stands at the same level in connected vessels of different shapes.
Pascal's law states that a change in pressure applied to an enclosed incompressible fluid is transmitted undiminished to every part of the fluid and to the walls of the container. This principle is the heart of all hydraulic machines.
Hydraulic lift and brakes. In a hydraulic lift two pistons of areas $A_1$ (small) and $A_2$ (large) are connected by fluid. A force $F_1$ on the small piston creates a pressure $P=\frac{F_1}{A_1}$, transmitted to the large piston, which then experiences $F_2=P\,A_2=F_1\frac{A_2}{A_1}$. Because $A_2>A_1$, a small input force lifts a large load — a force multiplier. Hydraulic brakes use the same idea to apply equal braking force at all wheels.
Atmospheric pressure and the barometer. The atmosphere exerts pressure because of the weight of air above us; at sea level $P_0\approx1.013\times10^5\ \text{Pa}=1\ \text{atm}$. Torricelli's mercury barometer measures it: atmospheric pressure supports a column of mercury about $76\ \text{cm}$ high, so $P_0=\rho_{Hg}\,g\,h$. A height of $76\ \text{cm}$ of mercury equals 1 atm.