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dc.contributor.authorMandal, Hasan
dc.contributor.authorThompson, D. P.
dc.date.accessioned2019-10-20T07:59:53Z
dc.date.available2019-10-20T07:59:53Z
dc.date.issued1997
dc.identifier.issn1013-9826
dc.identifier.urihttps://hdl.handle.net/11421/15812
dc.identifier.urihttps://doi.org/10.4028/www.scientific.net/KEM.132-136.798en_US
dc.description.abstractIn-situ ??ß sialon transformation in rare earth sialon systems, which occurs when dense ?- and ?/ß-sialon samples are heat-treated at temperatures in the range 1300-1600°C was first observed five years ago, and has generated a considerable level of research activity aimed at defining the reason(s) why the transformation occurs. A mass of experimental data is now available, and many factors have been identified which influence the reaction. However, the exact reason for the transformation is still not entirely clear, and in the present paper, various explanations which have been suggested during the last five years are discussed and the current position evaluateden_US
dc.language.isoengen_US
dc.relation.isversionof10.4028/www.scientific.net/KEM.132-136.798en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectTransformationen_US
dc.subjectRare Earth ?-Sialonsen_US
dc.subjectSialonsen_US
dc.titleThe driving force for ??ß transformation in rare earth ? sialon ceramicsen_US
dc.typearticleen_US
dc.relation.journalKey Engineering Materialsen_US
dc.contributor.departmentAnadolu Üniversitesi, Fen Bilimleri Enstitüsü, Seramik Mühendisliği Anabilim Dalıen_US
dc.identifier.issue136 PART 2en_US
dc.identifier.startpage798en_US
dc.identifier.endpage801en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.contributor.institutionauthorMandal, Hasan


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