Abstract
The transformation of a ductile iron at 410 °C for different times, after austenitization for 30 minutes at 900 °C, is analyzed in detail. Upper bainite and a high volume fraction of austenite are formed for intermediate annealing times. A certain amount of martensite is observed after quenching not only for short transformation times but also for intermediate times. The formation of the martensite on cooling after intermediate transformation times is due to the decrease in carbon concentration of the retained austenite because of the homogeneous precipitation of epsilon carbides within. This homogeneous precipitation of epsilon carbide inside austenite is unambiguously observed. The epsilon carbide, pre-precipitated in austenite, which transforms to martensite on cooling, continues growing in the martensite after transformation. For long times of austempering at 410 °C, some complex large carbides or silicocarbides are formed, probably from the epsilon carbide, which result in the total decomposition of austenite.
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Gutierrez, I., Aranzabal, J., Castro, F. et al. Homogeneous formation of epsilon carbides within the austenite during the isothermal transformation of a ductile iron at 410 °C. Metall Mater Trans A 26, 1045–1060 (1995). https://doi.org/10.1007/BF02670600
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DOI: https://doi.org/10.1007/BF02670600