Depression of Freezing Point
Imagine a cold winter morning. You see water on the road turning to ice at 0°C. But if you sprinkle salt on that ice, it melts — even though the temperature is still below zero. That’s the same phenomenon that keeps roads safe in snowy countries and makes ice cream freeze in a churn. The salt lowers the freezing point of water.
That is the core idea: when you dissolve a non-volatile solute (like salt, sugar, or urea) in a solvent (like water), the freezing point of the solution becomes lower than that of the pure solvent. This drop is called the depression of freezing point, denoted by ΔTf.
Why does this happen? The intuition
In a pure liquid, molecules at the surface escape into the solid (freeze) when the temperature is low enough — the solid and liquid are in equilibrium at the freezing point. Now add a solute. The solute particles sit between solvent molecules, getting in the way. For the solvent to freeze, its molecules must arrange themselves into an orderly crystal lattice. The solute particles disrupt this order — they make it harder for the solvent to solidify.
Think of it like trying to pack a suitcase full of neatly stacked blocks. If you throw in a few marbles, the blocks can’t settle as tightly. You’d need to cool the system further (lower the temperature) to force the blocks into place. That extra cooling is the depression.
The solute must be non-volatile (it doesn’t evaporate) and non-electrolyte (it doesn’t break into ions) for the simplest formula to work. If the solute dissociates (like NaCl → Na⁺ + Cl⁻), the effect is larger — but that’s a refinement you’ll meet later.
The precise statement
For a dilute solution, the depression in freezing point is directly proportional to the molality of the solution (moles of solute per kilogram of solvent).
ΔTf=Kf⋅m
Where:
- ΔTf=Tf∘−Tf (pure solvent freezing point minus solution freezing point)
- Kf = cryoscopic constant or molal freezing point depression constant — a property of the solvent alone (units: K kg mol⁻¹)
- m = molality of the solution
ΔTf=Kf⋅m
Each solvent has its own Kf. For water, Kf=1.86 K kg mol−1. That means: a 1 molal aqueous solution freezes at −1.86∘C (instead of 0∘C).
How it helps find molar mass
If you dissolve a known mass w2 of an unknown solute in a known mass w1 of solvent, measure the freezing point depression ΔTf, you can calculate the molar mass M2 of the solute.
Start from the definition of molality:
m=kg of solventmoles of solute=w1/1000w2/M2
Substitute into ΔTf=Kf⋅m:
ΔTf=Kf⋅M2×w1w2×1000
Rearrange for M2:
M2=ΔTf⋅w1Kf⋅w2⋅1000
This is the most common exam formula. Remember: w1 is in grams, w2 in grams, and the factor 1000 converts grams of solvent to kilograms.
A quick example
You dissolve 5.00 g of a non-electrolyte in 100 g of water. The freezing point drops to −0.93∘C. Find the molar mass.
Given: Kf=1.86, ΔTf=0.93, w2=5.00, w1=100. …