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- W2023104413 abstract "Abstract The morphology and crystallography of the isothermal transformation of Fe–N austenite at 225 °C were characterized by transmission electron microscopy and scanning electronic microscope. Fe–N austenite was produced by through-nitriding thin pure iron sheets at 640 °C. Lath-shaped and periodically distributed (γ-austenite + γ′-Fe4N + α-Fe) microstructures formed at the prior austenite grain boundaries, this kind of microstructure was shown to be bainite in nature and kept a Greninge–Troiano orientation relationship between the γ-austenite (γ´-Fe4N) and α-ferrite. The formation mechanism of the grain boundary microstructure was shown to be the preferential precipitation of the proeutectoid γ′-Fe4N at the grain boundary, followed by the transformation of the N-depleted austenite into α-ferrite and γ′-Fe4N, thus forming a periodic γ-γ′-α-γ′-γ-γ′-α-γ′-γ-γ′ arrangement." @default.
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- W2023104413 date "2012-01-01" @default.
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- W2023104413 title "Grain boundary transformation character in Fe–N austenite" @default.
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- W2023104413 doi "https://doi.org/10.1016/j.matlet.2011.08.010" @default.
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