Experimental evidence for bainite formation below Ms in Fe–0.66C
作者： S.M.C. van Bohemen , M.J. Santofimia , J. Sietsma
DOI: 10.1016/J.SCRIPTAMAT.2007.10.045
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摘要: The isothermal decomposition of austenite in the temperature range 220–300 °C Fe–0.69Mn–0.66C has been studied using dilatometry and scanning electron microscopy (SEM). Analysis curves shows that after athermal martensite formation is interrupted below Ms = 264 °C, continues to decompose isothermally at a certain rate, which agreement with kinetics bainite above Ms. This strongly indicates formed Ms, supported by SEM images showing mixed martensite–bainite microstructure.
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