Chemistry

Freezing Point Depression Calculator

Calculate how much a solute lowers a solvent's freezing point.


Freezing Point Depression Calculator

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Calculates how much a dissolved solute lowers a solvent’s freezing point — the same colligative-property principle behind road salt melting ice.

How it works

The number of particles the solute dissociates into is multiplied by the solvent’s cryoscopic constant and the solution’s molality.

What this does not include

This does not include the opposite effect on boiling point — for that, use this site’s boiling point elevation calculator instead, which uses the same underlying principle applied to the other phase transition.

How to use this calculator

  1. Enter the Van’t Hoff factor, the solvent’s cryoscopic constant (water’s value is pre-filled), and the molality.

A worked example

A solute with van’t Hoff factor 2 (like a salt that dissociates into two ions), Kf = 1.86, molality 0.5: freezing point depression = i×Kf×m = 2×1.86×0.5 = 1.86°C.

A non-dissociating solute (i=1), Kf = 1.86, molality 1: depression is also 1.86°C.

What the variables mean

Variable Meaning
i (van’t Hoff factor) Number of particles the solute dissociates into
Kf The solvent’s freezing point depression constant
Molality Moles of solute per kg of solvent

Edge cases worth knowing

A dissociating solute like salt depresses the freezing point more than a non-dissociating one at the same molality — each ion it splits into contributes separately, which is exactly why road salt (which dissociates into two ions) works better than an equal molar amount of sugar (which doesn’t dissociate at all).

A negative van’t Hoff factor has no physical meaning, so the calculator declines to show a result for one.

Frequently asked questions

Why does salting roads melt ice?

Dissolved salt lowers the freezing point of the water on the road below the ambient temperature, so ice that would normally stay frozen instead melts.

Does antifreeze work the same way?

Yes — antifreeze lowers a car radiator’s freezing point using the same colligative-property principle, just with a different solute (typically ethylene glycol) than table salt.

Why is the cryoscopic constant different from the ebullioscopic constant?

They’re both properties of the solvent, but they describe different physical processes (freezing vs. boiling) and are measured independently — for water they happen to be different numbers (1.86 vs. 0.512).

Sources

  1. Water's cryoscopic constant (Kf = 1.86 °C·kg/mol) — standard physical-chemistry reference value
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Written by

P. Nakamura

Chemistry writer

P. Nakamura writes the chemistry calculators, covering solution concentration, stoichiometry, gas laws and colligative properties. Each page separates the definitional part of a formula from the reference constants it depends on, and leaves those constants adjustable where a different solvent or condition would change them. Worked chemistry is only as good as the assumptions stated alongside it.

Reviewed by

D. Petrov

Calculator reviewer — chemistry and environmental science

D. Petrov reviews the chemistry and environmental-science calculators, verifying that reference constants match their stated values and that they remain adjustable wherever a different substance or condition would change them. Review also checks that definitional relationships are not presented as though they required a citation, and that non-definitional values always carry one.

How we write and review

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