Abstract
The low chromium Fe−C−Cr phase equilibria pertinent to the eutectoid transformation of austenite have been modeled and calculated from published thermodynamic information and verified through a series of selected equilibration experiments. In particular, α-γ, α-cm and γ-cm partition coefficients have been measured within the range 700 to 770°C and compared with austenite and carbide models proposed by Hillert and coworkers. While the theoretical-empirical closure is not perfect, the models are proven to be completely adequate for incorporation within the kinetic description of the corresponding ternary pearlite reaction.
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R. C. SHARMA, formerly with McMaster University
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Sharma, R.C., Purdy, G.R. & Kirkaldy, J.S. Thermodynamics and phase equilibria for the Fe−C−Cr system in the vicinity of the eutectoid temperature. Metall Trans A 10, 1119–1127 (1979). https://doi.org/10.1007/BF02811657
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DOI: https://doi.org/10.1007/BF02811657