 Sedimentation equilibrium

Sedimentation equilibrium occurs when the downward tendency of suspended particles is balanced by their diffusion, leaving a stationary concentration profile with no net particle flux. For dilute identical particles in an isothermal fluid, let $m_b=({\rho }_p-{\rho }_f)V_p$ be their buoyant mass. Balancing the gradient of ideal osmotic pressure $n{k}_{B}T$ against gravity givesHere height increases upward, and heavy particles have $m_b>0$.

The profile is a miniature atmosphere: thermal motion spreads particles upward while gravity favours lower positions. The Perrin sedimentation experiment measured particle counts at different microscope focal heights and used this competition to infer a molecular energy scale.^[ref] A stationary profile requires sufficiently slow background flow and controlled temperature; a growing deposit during ongoing settling is a different situation.