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dc.contributor.authorPatabendige, Chami Nilasha Kahakachchi
dc.contributor.authorAzad, Abul Kalam
dc.contributor.authorConnor, Paul Alexander
dc.contributor.authorRolle, Aurélie
dc.contributor.authorIrvine, John Thomas Sirr
dc.date.accessioned2013-03-26T14:01:02Z
dc.date.available2013-03-26T14:01:02Z
dc.date.issued2013-03-21
dc.identifier.citationPatabendige , C N K , Azad , A K , Connor , P A , Rolle , A & Irvine , J T S 2013 , ' Remarkable transition from rocksalt/perovskite layered structure to fluorite/rocksalt layered structure in rapidly cooled Ln 2 CuO 4 ' , Scientific Reports , vol. 3 , 1504 . https://doi.org/10.1038/srep01504en
dc.identifier.issn2045-2322
dc.identifier.otherPURE: 48764868
dc.identifier.otherPURE UUID: 4e94a30f-86d4-4237-9069-84e314624e48
dc.identifier.otherWOS: 000316541300001
dc.identifier.otherScopus: 84875768582
dc.identifier.otherORCID: /0000-0002-1492-7590/work/60427196
dc.identifier.otherORCID: /0000-0002-8394-3359/work/68280682
dc.identifier.urihttp://hdl.handle.net/10023/3426
dc.descriptionThis work was supported by EPSRCen
dc.description.abstractLanthanide cuprates of formula Ln2CuO4 exist in two principal forms, T and T′ which are renowned for their exhibition at low temperatures of hole and electronic types of superconductivity, respectively. These structures differ primarily in the arrangement of oxygen between the perovskite layers and also in nature of the copper oxygen planes. The Cu-O distance in the T structure (~1.90 Å) is much shorter than the T′ (1.97Å), reflecting a transition between partial Cu+ and partial Cu3+ character. In seeking to find compositions that bridge these two structure/electron carrier types, we observed the transition from a T structure to a T′ type structure, resulting in the metastable form T″ with slightly larger volume but similar character to T′. This transition from T to T″ is associated with 5% increase in a and a 5% decrease in c parameters of the tetragonal unit cells, which results in disintegration of ceramic bodies.
dc.format.extent5
dc.language.isoeng
dc.relation.ispartofScientific Reportsen
dc.rightsThis work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/en
dc.subjectZIRCONIAen
dc.subjectSUPERCONDUCTIVITYen
dc.subjectCU-O SYSTEMen
dc.subjectPHASEen
dc.subjectCOPPER OXIDESen
dc.subjectOXYGENen
dc.subjectCRYSTAL-CHEMISTRYen
dc.subjectCOMPOUNDen
dc.subjectQD Chemistryen
dc.subject.lccQDen
dc.titleRemarkable transition from rocksalt/perovskite layered structure to fluorite/rocksalt layered structure in rapidly cooled Ln2CuO4en
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews.School of Chemistryen
dc.contributor.institutionUniversity of St Andrews.EaSTCHEMen
dc.identifier.doihttps://doi.org/10.1038/srep01504
dc.description.statusPeer revieweden


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