A diver at the surface of a lake feels only atmospheric pressure. As the diver descends vertically to 25 m, the weight of the water column above increases and the pressure rises. The diver then swims 10 m horizontally at the same depth; the lecturer says "the depth remains constant, I don't expect a change in the pressure".
The lecturer then asks: we have seen that the diver feels more pressure going deeper, but how can we model this pressure mathematically? (Answer on the slide: by a balance of forces.)
Formulas you may need
- Differential hydrostatic equation: for measured upwards, equivalently for measured downwards (depth); (on the formula sheet, derived in slides 12-13: be able to derive it)
- Pressure at depth: (on the formula sheet)
- Gauge pressure: (learn this)
- (a)[4]By a force balance on a small vertical cylinder of fluid at rest (cross-sectional area , height ), derive the differential equation for the variation of pressure in the vertical direction. State your sign convention for .
- (b)[2]By a force balance on a small horizontal cylinder of fluid at rest, show that pressure does not vary in the horizontal direction.
- (c)[2]Integrate your result from (a), assuming constant density, to find the pressure at a depth below a free surface at atmospheric pressure . State the hypothesis this needs.
- (d)[2][Added, to put numbers on the diver] Take , and . Calculate the absolute and gauge pressure on the diver at 25 m, and the absolute pressure after swimming 10 m horizontally at that depth.