完整後設資料紀錄
DC 欄位語言
dc.contributor.authorWU, CCen_US
dc.contributor.authorLIU, TFen_US
dc.date.accessioned2014-12-08T15:05:13Z-
dc.date.available2014-12-08T15:05:13Z-
dc.date.issued1991-06-01en_US
dc.identifier.issn0360-2133en_US
dc.identifier.urihttp://dx.doi.org/10.1007/BF02660673en_US
dc.identifier.urihttp://hdl.handle.net/11536/3767-
dc.description.abstractA new type of precipitate (designated L phase) was observed within the ferrite matrix in an Fe-9.0Al-29.5Mn-1.2Si alloy after being aged at 550-degrees-C. Transmission electron microscopy examinations indicated that the L-phase precipitate has a monoclinic structure with lattice parameters a = 0.656 nm, b = 0.797 nm, c = 0.637 nm, and beta = 109.4 deg, and the orientation relationship between the L-phase precipitate and the ferrite matrix could be stated as follows: (1BAR01)alpha-parallel-to (001)L-phase (1BAR10)alpha-parallel-to (1BAR11)L-phase with a deviation of 0.3 deg (011)alpha-parallel-to (131)L-phase with a deviation of 1.5 deg The L phase has never been observed in various Fe-Al-Mn, Fe-Mn-Si, Fe-Al-Si, and Mn-Al-Si alloy systems before.en_US
dc.language.isoen_USen_US
dc.titleA NEW PHASE IN AN FE-9.0AL-29.5MN-1.2SI ALLOYen_US
dc.typeArticleen_US
dc.identifier.doi10.1007/BF02660673en_US
dc.identifier.journalMETALLURGICAL TRANSACTIONS A-PHYSICAL METALLURGY AND MATERIALS SCIENCEen_US
dc.citation.volume22en_US
dc.citation.issue6en_US
dc.citation.spage1417en_US
dc.citation.epage1423en_US
dc.contributor.department機械工程學系zh_TW
dc.contributor.department材料科學與工程學系zh_TW
dc.contributor.departmentDepartment of Mechanical Engineeringen_US
dc.contributor.departmentDepartment of Materials Science and Engineeringen_US
dc.identifier.wosnumberWOS:A1991FQ38700030-
dc.citation.woscount5-
顯示於類別:期刊論文