Chemistry Tools

Colligative Properties Calculator

Colligative properties depend on how many solute particles are dissolved, not what they are. Find ΔT, molality, the van 't Hoff factor, or osmotic pressure.

ΔT = i × K × m — fill in every field except the one you want; the empty field is solved for.

Solvent constant (°C·kg/mol):
°C·kg/mol
mol/kg

Change in boiling or freezing point (ΔT) = 1.86 °C

  1. Rearrange: ΔT = i × K × m
  2. Substitute: (2) × (1.86 °C·kg/mol) × (0.5 mol/kg) = 1.86 K

How it works

For boiling and freezing points, ΔT = i × K × m, where m is molality (mol of solute per kg of solvent) and K is the solvent's ebullioscopic (K_b) or cryoscopic (K_f) constant. The result is the size of the change: add it to the pure solvent's boiling point, or subtract it from the freezing point.

Osmotic pressure uses Π = iMRT with molarity and R = 0.082057 L·atm/(mol·K). The van 't Hoff factor i is the number of particles per formula unit: 1 for sugar, close to 2 for NaCl and 3 for CaCl₂ in dilute solution (slightly less in practice because ions pair up).

Frequently asked questions

How much does salt lower the freezing point of water?
For 1.00 mol of NaCl per kg of water: ΔT = 2 × 1.86 × 1.00 = 3.72 °C, so the solution freezes at about −3.7 °C.
Why is molality used instead of molarity?
Molality is based on mass of solvent, so it doesn't change with temperature — important when the temperature itself is what you're measuring.
How are colligative properties used to find molar mass?
Measure ΔT for a known mass of solute in a known mass of solvent, solve for molality, then divide the grams of solute by the moles.

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