Osmosis is the net diffusion of water molecules from a dilute solution into a more concentrated solution through a semi-permeable membrane due to a concentration gradient. Osmotic pressure is the excess pressure that must be applied to a solution to prevent the passage of solvent into the solution, and it is measured in units called osmoles. Osmotic pressure follows two laws: πV = nRT and π = cRT, where π is osmotic pressure, V is volume, n is moles of solute, R is the gas constant, T is temperature, and c is molarity. Applications of osmosis include water desalination through reverse osmosis, measuring