“…As mentioned earlier in the paper, the volume fraction of strain induced martensite as a function of strain can be calculated by using Olson‐Cohen model as follows: where n is constant and α and β are parameters depending on strain rate, temperature, and composition. However, Olson‐Cohen model is not sensitive to the stress state, and as such, it has been modified to incorporate the effect of stress state on the kinetics of martensite phase transformation. According to the modified Olson‐Cohen model, quite contrary to the α , two parameters of β and n are functions of stress state, as can be seen in the following equations: where , A , , B and C are constant, is the absolute value of normalized Lode angle parameter and is stress triaxiality.…”