Osmotic pressure is related to the effect of solutes on water movement across a semi-permeable membrane, similar to hydrostatic pressure. The van't Hoff equation, π = nRT, describes this relationship, where π represents osmotic pressure, n is the number of moles of solute, R is the gas constant, and T is the temperature. The discussion explains the chemical potential of water and how it relates to osmotic pressure through the equilibrium of two compartments with different solute concentrations. The equation incorporates variables such as the mole fraction of water and hydrostatic pressure. Overall, the exchange of information clarified the concept of osmotic pressure and its mathematical representation.