When a pure solvent freezes, its molecules arrange into an orderly lattice, strengthening intermolecular forces. In water, this results in a hexagonal hydrogen‑bond network that defines ice’s unique properties.
Introducing a solute disrupts the solvent’s ordered structure. The solvent molecules can no longer align perfectly, so more energy must be removed for freezing to occur. In practice, this means the freezing point of the mixture is lower than that of the pure solvent—a phenomenon known as freezing point depression.
The decrease in freezing temperature is directly proportional to the solute’s molality:
\(\Delta T_f = K_f \times m \times i\)
Where:
Freezing point depression is also expressed as the difference between the pure solvent’s freezing point (Tf⁰) and that of the solution (Tf):
\(\Delta T_f = T_f^{\circ} - T_f\)
Two everyday applications demonstrate its importance:
Calculate the freezing point of a solution containing 100 g of NaCl in 1 kg of water.
Thus, adding 100 g of salt to 1 kg of water depresses the freezing point to –6.4 °C.
Adding a solute like salt lowers a solvent’s freezing point. The more solute present, the greater the depression—explaining antifreeze and road salting.