dc.contributor.author | Camuşcu, N. | |
dc.contributor.author | Thompson, DP | |
dc.contributor.author | Mandal, Hasan | |
dc.date.accessioned | 2019-10-19T21:03:55Z | |
dc.date.available | 2019-10-19T21:03:55Z | |
dc.date.issued | 1997 | |
dc.identifier.issn | 0955-2219 | |
dc.identifier.uri | https://dx.doi.org/10.1016/S0955-2219(96)00112-4 | |
dc.identifier.uri | https://hdl.handle.net/11421/15701 | |
dc.description | WOS: A1997WG29500013 | en_US |
dc.description.abstract | Five different alpha-beta sialon and alpha-sialon compositions have been prepared using different rare earth oxide additives namely, neodymium, samarium, dysprosium and ytterbium., Post-sintering heat treatments have been carried out at 1450 degrees C for up to 720 h (one month) to observe alpha --> beta sialon transformation. A combination of X-ray and microstructural observations has shown that the high-temperature stability of the alpha-sialon phase depends on the starting composition, the type of rare earth sintering additives, the amount and viscosity of the liquid phase, and the presence or absence of beta-sialon grains in the initial sintered material | en_US |
dc.language.iso | eng | en_US |
dc.publisher | Elsevier Sci LTD | en_US |
dc.relation.isversionof | 10.1016/S0955-2219(96)00112-4 | en_US |
dc.rights | info:eu-repo/semantics/closedAccess | en_US |
dc.title | Effect of starting composition, type of rare earth sintering additive and amount of liquid phase on alpha reversible arrow beta sialon transformation | en_US |
dc.type | article | en_US |
dc.relation.journal | Journal of the European Ceramic Society | en_US |
dc.contributor.department | Anadolu Üniversitesi, Fen Bilimleri Enstitüsü, Seramik Mühendisliği Anabilim Dalı | en_US |
dc.identifier.volume | 17 | en_US |
dc.identifier.issue | 4 | en_US |
dc.identifier.startpage | 599 | en_US |
dc.identifier.endpage | 613 | en_US |
dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | en_US] |
dc.contributor.institutionauthor | Mandal, Hasan | |