ON THE STRUCTURE OF IRON-CARBON MARTENSITE

Abstract
Spectra of Fe-1.5~7 at % C alloys without and 50 kOe longitudinal external magnetic field were measured to clarify the structure of iron-carbon martensite. The spectra of freshly quenched martensite were decomposed into three magnetic hyperfine splittings having different fields, and three additional components were found in the aged specimen. Derived Mössbauer parameters are discussed in connection with the structure of martensite

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