Question
A gas in equilibrium has uniform density and pressure throughout its volume. This is strictly true only if there are no external influences. A gas column under gravity, for example, does not have uniform density (and pressure). As you might expect, its density decreases with height. The precise dependence is given by the so-called law of atmospheres
n2=n1exp[−mg(h2−h1)/kBT]
where n2,n1 refer to number density at heights h2 and h1 respectively. Use this relation to derive the equation for sedimentation equilibrium of a suspension in a liquid column:
n2=n1exp[−mgNA(ρ−ρ′)(h2−h1)/(ρRT)]
where ρ is the density of the suspended particle and ρ′ that of surrounding medium. [NA is Avogadro's number, and R the universal gas constant.][Hint : Use Archimedes principle to find the apparent weight of the suspended particle.]