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dc.contributor.authorTuan, Yi Hsuanen_US
dc.contributor.authorLin, Chih Lungen_US
dc.contributor.authorChao, Chuen Guangen_US
dc.contributor.authorLiu, Tzeng Fengen_US
dc.date.accessioned2014-12-08T15:11:13Z-
dc.date.available2014-12-08T15:11:13Z-
dc.date.issued2008-07-01en_US
dc.identifier.issn1345-9678en_US
dc.identifier.urihttp://dx.doi.org/10.2320/matertrans.MRA2008060en_US
dc.identifier.urihttp://hdl.handle.net/11536/8614-
dc.description.abstractThe as-quenched microstructure of the Fe-30%Mn-9%Al-5%Cr-0.7%C (in mass%) alloy was single-phase austenite. When the as-quenched alloy was aged at 550 degrees C-750 degrees C, fine (Fe,Mn)(3)AlC carbides were formed within the austenite matrix. In addition, as the aging temperature increased, a M7C3 carbide + D0(3) -> M7C3 carbide + B-2 -> M7C3 carbide + alpha (ferrite) phase transition had occurred on the grain boundaries. This grain boundary precipitation behavior has never before been observed in FeMnAlC and FeMnAlCrC alloy systems.en_US
dc.language.isoen_USen_US
dc.subjecttransmission electron microscopyen_US
dc.subjectcarbidesen_US
dc.subjectorderingen_US
dc.subjectaustenitic iron aluminum manganese chromium carbon alloyen_US
dc.titleGrain boundary precipitation in Fe-30Mn-9Al-5Cr-0.7C alloyen_US
dc.typeArticleen_US
dc.identifier.doi10.2320/matertrans.MRA2008060en_US
dc.identifier.journalMATERIALS TRANSACTIONSen_US
dc.citation.volume49en_US
dc.citation.issue7en_US
dc.citation.spage1589en_US
dc.citation.epage1593en_US
dc.contributor.department材料科學與工程學系zh_TW
dc.contributor.departmentDepartment of Materials Science and Engineeringen_US
dc.identifier.wosnumberWOS:000258810900016-
dc.citation.woscount3-
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