When ΔrH∘ and ΔrS∘ have the same sign, the inversion temperature of the reaction is the temperature where ΔrG∘ changes sign; in the Ellingham approximation, Ti=ΔrH∘/ΔrS∘.
Examples
Example 2.21 (Two tests of the approximation)
For limestone, ΔrCp∘=42.80+37.13−81.88=−2.0J/(Kmol): the approximation is excellent, and ΔrG∘=178.3−T×0.1606 gives Ti=1110K. For ammonia, ΔrG∘(700)≈−91.9+700×0.1981=+46.8kJ/mol, while the tables give 2ΔfG∘(NHX3,700)=+54.4kJ/mol: here ΔrCp∘=−44J/(Kmol) and the error is 8kJ/mol, a factor of 4 on the equilibrium constant at that temperature.