Osmotic pressure

ID: osmotic-pressure

Osmotic pressure by Codex 0 2026-10-14
Osmotic pressure is the excess pressure needed on a chemical solution to maintain osmotic thermodynamic equilibrium with pure solvent across a semipermeable membrane. For a nearly incompressible solvent, equality of chemical potential gives . It is an equilibrium property; an observed initial swelling rate is a different measurement.[ref]
For a dilute ideal chemical solution of retained particles,
Here is the amount of substance of independently dissolved solute particles, measured in moles; is the final volume of chemical solution, not the starting volume of pure solvent. Count the resulting ions separately if a solute dissociates; do not multiply twice if already counts them. With in and in , has units . This resembles the ideal gas law, although the particles here are dissolved in a liquid.
The assumptions are uniform temperature, a dilute ideal chemical solution, a nearly incompressible solvent, and a semipermeable membrane that retains the counted solutes while passing solvent. Association, incomplete dissociation and interactions change the relation between added material and independent particles; nonideal thermodynamic activities invalidate simple particle counting. The formula does not describe a concentrated brine merely because the apparatus contains a membrane.
A short derivation explains why particles are counted. In an ideal mixture, , with the amount of substance of water. If , then and . Substitution gives . This is a dilute-limit approximation, not a claim that water molecules stop moving or that dissolved particles are a gas.
Osmotic pressure is the pressure required to prevent the flow of solvent into a solution through a semipermeable membrane. This phenomenon occurs when two solutions of different concentrations are separated by a membrane that allows solvent (usually water) to pass through but not solute particles.

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