Show simple item record

FieldValueLanguage
dc.contributor.authorAvdeev, Maxim
dc.contributor.authorMohamed, Zakiah
dc.contributor.authorLing, Chris D
dc.date.accessioned2022-08-09T04:22:39Z
dc.date.available2022-08-09T04:22:39Z
dc.date.issued2014en_AU
dc.identifier.urihttps://hdl.handle.net/2123/29381
dc.description.abstractThe magnetic structure and properties of the candidate lithium-ion battery cathode materials Pbn21(≡Pna21) Li2CoSiO4 and P21/n Li2MnSiO4 have been studied experimentally using low-temperature neutron powder diffraction and magnetometry. Both materials undergo long-range antiferromagnetic ordering, at 14 K and 12 K respectively, due to super-super-exchange mediated by bridging silicate groups. Despite having different crystal structures (wurtzite- vs. “dipolar”-type), Li2CoSiO4 and Li2MnSiO4 have the same topology in terms of magnetic interactions, and adopt collinear magnetic structures of the same type with the propagation vectors (0,1/2,1/2) and (1/2,0,1/2) respectively. The magnetic moments in the two materials are aligned perpendicular-ly and obliquely to the distorted closed-packed layers of oxygen atoms. The experimentally observed values of the ordered magnetic moments, 2.9 μB and 4.6 μB, are close to those expected for d7 Co2+ and d5 Mn2+ re-spectively.en_AU
dc.language.isoenen_AU
dc.publisherElsevieren_AU
dc.relation.ispartofJournal of Solid State Chemistryen_AU
dc.titleMagnetic structures of βI-Li2CoSiO4 and γ0-Li2MnSiO4: crystal structure type vs. magnetic topologyen_AU
dc.typeArticleen_AU
dc.subject.asrc0302 Inorganic Chemistryen_AU
dc.identifier.doi10.1016/j.jssc.2014.04.028
dc.type.pubtypeAuthor accepted manuscripten_AU
dc.relation.arcDP110102662
usyd.facultySeS faculties schools::Faculty of Science::School of Chemistryen_AU
usyd.citation.volume216en_AU
usyd.citation.spage42en_AU
usyd.citation.epage48en_AU
workflow.metadata.onlyNoen_AU


Show simple item record

Associated file/s

Associated collections

Show simple item record

There are no previous versions of the item available.