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: $\text{n}_2=\text{n}_1\text{exp}\Big[\frac{-\text{mg}}{\text{k}_\text{B}\text{T}}(\text{h}_2-\text{h}_1)\Big]$ where $n_2, n_1$ refer to number density at heights $h_2$ and $h_1$respectively. Use this relation to derive the equation for sedimentation equilibrium of a suspension in a liquid column: $\text{n}_2=\text{n}_1\text{exp}\Big[\frac{-\text{mgN}_\text{A}(\rho-\rho')(\text{h}_2-\text{h}_1)}{(\rho\text{RT})}\Big]$ where $\rho$ is the density of the suspended particle, and $\rho'$ 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]


