Osmotic pressure is the force exerted by a solution across a semipermeable membrane separating it from a pure solvent. This phenomenon arises from solvent molecule migration from regions of lower solute concentration to those of higher concentration. Osmotic pressure is favored for ascertaining macromolecule molar masses due to its colligative nature, meaning it is contingent on the number of solute particles, not their identity. This technique is especially beneficial for large molecules like proteins and polymers, which may pose challenges for alternative analytical methods.