The Clausius-Clapeyron equation was initially proposed by German physicist Rudolf Clausius in 1834 and further developed by French physicist Benoît Clapeyron in 1850. This equation is extremely useful in characterizing a discontinuous phase transition between two phases of a single constituent.
We know from fundamental thermodynamics that the total variation of Gibbs free energy ($G$) is expressed as:
Let us consider a single-constituent equilibrium containing two balancing state phases:
$\text{Phase-1} \rightleftharpoons \text{Phase-2}$
Where Phase-1 may be solid, liquid, or gas, and Phase-2 may be liquid or vapor, depending upon the nature of the phase transformation (melting, vaporization, or sublimation).
For Phase-1, the differential change in free energy is given by:
And for Phase-2, the corresponding change in free energy is:
At equilibrium, the system exhibits zero net change in free energy ($dG_1 = dG_2$, i.e., $\Delta G = 0$). Equating Equation 2 and Equation 3 yields:
If $\Delta H$ is the latent heat of phase transformation taking place at transition temperature ($T$), then the entropy change ($\Delta S$) is defined as:
Substituting the expression for $\Delta S$ from Equation 5 into Equation 4 yields the Clapeyron Equation:
Equation 6 is applicable to all closed phase transitions taking place at constant pressure.
Application to Fusion and Vaporization Systems
If Phase-1 is solid while Phase-2 is liquid ($\text{solid} \rightleftharpoons \text{liquid}$), Equation 6 frames the fusion curve:
Where $\Delta_{\text{fus}}H$ is the latent heat of fusion and $T_f$ is the melting point.
For liquid-vapor equilibrium ($\text{liquid} \rightleftharpoons \text{vapor}$):
Assuming the gas phase behaves ideally, the molar volume of the vapor can be written using the ideal gas law ($V_v = \frac{RT}{P}$). Substituting this approximation alters the expression:
Using calculus identity $\frac{1}{P}dP = d(\ln P)$, we get the standard differential Clausius-Clapeyron Equation:
Integrated Form of the Clausius-Clapeyron Equation
Rearranging Equation 11 to solve across changing state variables:
Integrating between definite temperature boundaries ($T_1$ to $T_2$) and corresponding vapor pressures ($P_1$ to $P_2$):
Evaluating this yields the integrated form in terms of natural logarithm ($\ln$):
Converting the expression to a common logarithm (base 10) for standard scientific calculations: