“…In other words, the partial derivative of the interaction energy with respect to the fraction of the martensite, døaM/dZ, represents the TDF during the martensitic transformation. As for the TDF, there exists a positive value, AGOM, at which both the austenitic and the martensitic phase are stable and the phase transformation proceeds along the two-phase equilibrium state Matsuzaki, 1996, and1997a), that is, (*PaM g1 -g2 + ce0 = i\GOM for the martensitic transformation. (13) Similarly, the TDF of the reverse transformation is given by a positive value of AGOA: (1) and (1 1), we obtain (e 2) = 01 -02 (*Pa…”