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dc.contributor.authorAlptekin, Sebahaddin
dc.contributor.authorDurandurdu, Murat
dc.date.accessioned2019-11-24T20:37:49Z
dc.date.available2019-11-24T20:37:49Z
dc.date.issued2009
dc.identifier.issn0038-1098
dc.identifier.urihttps://dx.doi.org/10.1016/j.ssc.2008.12.025
dc.identifier.urihttps://hdl.handle.net/20.500.12513/2424
dc.descriptionWOS: 000263493600002en_US
dc.description.abstractA constant pressure ab initio technique is used to study the pressure-induced phase transition in BeO. A first order phase transition from the wurtzite structure to a rocksalt structure at 700.0 GPa is successfully observed in the constant pressure simulation. The wurtzite-to-rocksalt transformation is based on two fivefold coordinated intermediate states with space groups P6(3)/mmc and Cmcm, similar to what has been observed or proposed in various wurtzite structured materials. This phase transition should occur around 70 GPa from the enthalpy calculations. (C) 2008 Elsevier Ltd. All rights reserved.en_US
dc.language.isoengen_US
dc.publisherPERGAMON-ELSEVIER SCIENCE LTDen_US
dc.relation.isversionof10.1016/j.ssc.2008.12.025en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectOxidesen_US
dc.subjectPhase transformationen_US
dc.subjectHigh pressureen_US
dc.subjectAb initio molecular dynamicsen_US
dc.titlePressure-induced phase transition of BeOen_US
dc.typearticleen_US
dc.relation.journalSOLID STATE COMMUNICATIONSen_US
dc.contributor.departmentKırşehir Ahi Evran Üniversitesi, Fen-Edebiyat Fakültesi, Fizik Bölümüen_US
dc.identifier.volume149en_US
dc.identifier.issue9.Ekien_US
dc.identifier.startpage345en_US
dc.identifier.endpage348en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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