1.8 Pressure

Syllabus
0625–2026–2027
Topic
1.8
Level

Learning objectives

Calculate pressure from force and area

Pressure is the perpendicular force acting per unit area of a surface. The same force produces different pressures when it is spread over different contact areas.

p=FAp=\frac{F}{A}

Symbol Meaning SI unit
pp pressure pascal (Pa)
FF force perpendicular to the surface newton (N)
AA area over which that force acts square metre (m2\text{m}^2)

One pascal is one newton per square metre: 1Pa=1N/m21\,\text{Pa}=1\,\text{N}/\text{m}^2. Convert areas before dividing: 1cm2=104m21\,\text{cm}^2=10^{-4}\,\text{m}^2.

Identify the force acting on the named surface, identify its actual contact area, convert to SI units, then divide. Rearrangements are F=pAF=pA and A=F/pA=F/p.

For an object resting on a horizontal surface with no other vertical forces, the contact force equals its weight, not its mass. If mass is given, first find weight using F=mgF=mg.

Area means the area in contact with the surface, not total surface area. Pressure is not force: two surfaces can transmit the same force but experience different pressure because their areas differ.

Control pressure by changing force or contact area

Use p=F/Ap=F/A qualitatively: pressure increases with force and decreases with contact area. Hold one quantity constant before judging the effect of changing the other.

Change Effect on pressure
double the force, same area pressure doubles
halve the force, same area pressure halves
double the area, same force pressure halves
halve the area, same force pressure doubles
double both force and area pressure stays the same
Design Pressure idea
sharp pin or knife edge small area gives large pressure, helping penetration or cutting
skis, snowshoes or lying on thin ice large area gives smaller pressure, reducing sinking or cracking
wide tyres or foundations the load is spread over a larger area, reducing pressure on soft ground
turning the same block onto a larger face weight is unchanged but contact area grows, so pressure falls

A complete explanation names what stays constant, states how the contact area or force changes, and concludes how pressure changes. For example: the person's weight is unchanged, lying down increases contact area, so pressure on the ice decreases.

A sharp point does not create a larger transmitted force by itself. With the same force, its smaller area creates the larger pressure.

Predict how liquid pressure varies

Pressure caused by a liquid increases with vertical depth beneath its surface and increases with the liquid's density.

Comparison Pressure due to the liquid
same liquid, deeper point greater pressure
same depth, denser liquid greater pressure
same liquid and same vertical depth same pressure, whatever the container shape or width
uniform liquid, depth doubled pressure difference from the surface doubles

A deeper point has a taller column of liquid above it, so a greater liquid weight acts per unit area. A denser liquid has more mass—and therefore more weight—in the same volume, so its pressure rises more rapidly with depth.

For one uniform liquid at constant gravitational field strength, pressure due to the liquid rises as a straight line with depth. In layered liquids, the graph remains continuous but becomes steeper in the denser layer.

At the same horizontal level in a connected liquid at rest, pressure is the same. Container volume, base area and sloping sides do not by themselves change pressure at a specified depth.

Pressure due to the liquid is not always total pressure. If the surface is exposed to the atmosphere, total pressure equals atmospheric pressure plus the pressure caused by the liquid column.

Calculate changes in liquid pressure

For a liquid of uniform density, the pressure change between two levels depends on density, gravitational field strength and their vertical separation.

Δp=ρgΔh\Delta p=\rho g\Delta h

Symbol Meaning SI unit
Δp\Delta p change in pressure Pa
ρ\rho liquid density kg/m3\text{kg}/\text{m}^3
gg gravitational field strength N/kg\text{N}/\text{kg}
Δh\Delta h vertical depth difference m

Choose the two levels, measure their vertical separation, convert density and height to SI units, then multiply. Rearrangements are ρ=Δp/(gΔh)\rho=\Delta p/(g\Delta h) and Δh=Δp/(ρg)\Delta h=\Delta p/(\rho g).

If the reference is the liquid surface, pressure due to the liquid at depth hh is p=ρghp=\rho gh. If total pressure is requested and the surface pressure is known, add it: ptotal=psurface+ρghp_{\text{total}}=p_{\text{surface}}+\rho gh.

For several unmixed layers, calculate ρgΔh\rho g\Delta h for each layer crossed and add the pressure changes. The container's cross-sectional area is not part of the equation.

Use vertical depth, not the length of a tilted tube or the distance along a container. The equation gives a pressure difference; do not add atmospheric pressure unless total pressure is explicitly required.