Clausius-Clapeyron relation Created 2026-09-24 Updated 2026-10-14
The Clapeyron equation connects the slope of a phase coexistence curve to the latent heat and the change in volume during a first-order phase transition. A steep boundary can indicate a large latent heat, a small change in volume, or both. This lets a measured boundary constrain caloric properties and predicts how changing pressure shifts a melting temperature.
For a pure substance in bulk phase coexistence, label the initial and final thermodynamic phases and . Both have the same absolute temperature , pressure , and chemical potential. With , , and denoting entropy, enthalpy, and volume on one common basis, define , , and . Then
The derivative follows the phase coexistence curve; it is not a partial derivative within one thermodynamic phase. Use molar volume with molar latent heat in , or specific volume with latent heat in . Both give in . For molar mass , and , so the predicted slope is independent of the chosen basis. This formulation assumes a simple compressible system, fixed composition, and negligible interface contributions; a curved interface can instead require the Young–Laplace equation.
For positive latent heat in the stated conversion direction, the sign of the slope is the sign of . Converting liquid to gas normally increases volume and gives a positive slope. The negative melting-point slope of water illustrates the opposite sign. At a thermodynamic critical point, the coexisting gas and liquid merge: both and vanish, so their ratio needs a limiting analysis rather than substitution of zero into the Clapeyron equation.[ref]
A short derivation uses the molar Gibbs free energy , equal to the chemical potential for a pure substance. Equality persists along the boundary, so with . Therefore . Equality of also gives . Eliminating yields the Clapeyron equation.