Abstract
The free energy change accompanying martensite formation at the Ms temperature of steels ∆FM1γ→α′ is evaluated using various thermodynamic methods together with relatively accurate and recent thermodynamic data. ∆FM1γ→α′ has been found to be rather less than was originaliy believed, and varies between −900 and −1400 J mol−1 as a function of the carbon content; however, the variation is not monotonic.