Explain why (a) The blood pressure in humans is greater at the feet than at the brain (b) Atmospheric pressure at a height of about 6 km decreases to nearly half of its value at the sea level, though the height of the atmosphere is more than 100 km (c) Hydrostatic pressure is a scalar quantity even though pressure is force divided by area.
Hint. For (a) and (b), think about the weight of the column of fluid above the point. For (b), ask whether air has the same density all the way up. For (c), ask whether pressure at a point picks out any particular direction.
Step 1 — (a) Blood pressure at the feet. Pressure in a fluid at rest increases with depth as p = p₀ + ρgh. The feet lie roughly 1.5 m below the brain, so the blood there carries the extra weight of that whole column above it. Since the additional pressure is ρgh with ρ ≈ 1060 kg m⁻³, this comes to around 1.5 × 10⁴ Pa more at the feet than at the brain.
Step 2 — (b) Atmospheric pressure halving in 6 km. A liquid is very nearly incompressible, so its density stays constant with depth. Air is not — it is compressible, and the layers near the ground are squeezed by the weight of everything above them.
The density of air therefore falls off as you rise, so the upper 94 km of atmosphere contains far less mass than the lowest 6 km. Because pressure counts the weight above you rather than the height above you, most of the atmosphere's weight sits in that first few kilometres, which is why half the pressure is gone by 6 km.
Step 3 — (c) Why hydrostatic pressure is a scalar. Force is a vector and area has an orientation, so the ratio looks as though it should be a vector. But in a fluid at rest, the pressure at a point is the same in every direction — turn a tiny test surface any way you like and the force per unit area on it is unchanged.
A quantity that has no preferred direction cannot be a vector, since a vector must point somewhere. Pressure has magnitude only, so it is a scalar.
✦ (a) the extra weight of the blood column, ρgh; (b) air is compressible so most of its mass lies low down; (c) pressure at a point is the same in all directions, so it has no direction to be a vector.
Where students slip. Answering (b) with "gravity gets weaker with height". Gravity changes negligibly over 6 km. The real cause is the compressibility of air, which packs most of the atmosphere's mass into the lowest few kilometres.
