1. Introduction
Osmosis is the process of movement of solvent molecules from a region of lower solute
concentration to a region of higher solute concentration through a semipermeable membrane. This
process continues until equilibrium is reached.
Osmotic pressure is the pressure required to stop the osmosis process. It is a colligative property
that depends on the concentration of solute particles, not their identity.
2. Definition and Explanation
**Osmosis:** The spontaneous movement of solvent molecules across a semipermeable membrane
toward a higher solute concentration.
**Osmotic Pressure:** The minimum pressure needed to prevent the net movement of solvent
molecules through a semipermeable membrane.
3. Formula and Derivation
Osmotic pressure (Pi) is given by Van't Hoff's equation:
Pi = nRT / V
or in terms of molarity (C):
Pi = CRT
where:
- Pi = Osmotic pressure
- C = Molar concentration of the solution (mol/L)
- R = Universal gas constant (0.0821 L atm mol-¹ K-¹)
- T = Temperature in Kelvin