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 Mossbauer parameters are discussed in connection with the structure of martensite.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
