“…That is, f 0 ¼ M 0 ðT R Þ=M 0 0 ðT R Þ, where M 0 ðT R Þ and M 0 0 ðT R Þ are the spontaneous magnetization of the specimen and that of the 0 -phase, respectively, at T R . 8) Here, the magnetizations of -phase and " 0 -martensite are neglected because they are nonmagnetic. 9,10) The value of M 0 0 ðT R Þ is approximated to be the value at 0 K, M 0 0 ð0Þ, although it is a rough approximation.…”