Clapeyron's Equation States:
dP/dT = ΔtrsS/ΔtrsV
According to the text book I am reading, in order to determine the slope of the phase boundaries on the phase diagram we use
ΔtrsS = ΔtrsH/T
and substitute it in to the Clapeyron's Equation.
However, this equation for the entropy of a phase transition is only true under a constant pressure (dP=0). How then can we use it in our situation where pressure is not constant?
Am I missing something?