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dc.contributor.authorAvdeev, Maxim
dc.contributor.authorBarpanda, P
dc.contributor.authorMohamed, Zakiah
dc.contributor.authorLing, Chris D
dc.contributor.authorLu, J
dc.contributor.authorYamada, A
dc.date.accessioned2022-07-21T06:33:06Z
dc.date.available2022-07-21T06:33:06Z
dc.date.issued2013en_AU
dc.identifier.urihttps://hdl.handle.net/2123/29306
dc.description.abstractThe magnetic structure and properties of polycrystalline NaFePO4 polymorphs, maricite and triphylite, both derived from the olivine structure type, have been investigated using magnetic susceptibility, heat capacity, and low-temperature neutron powder diffraction. These NaFePO4 polymorphs assume orthorhombic frameworks (space group #62, Pnma), built from FeO6 octahedral and PO4 tetrahedral units having corner-sharing and edge-sharing arrangements. Both polymorphs demonstrate antiferromagnetic ordering below 13 K for maricite and 50 K for triphylite. The magnetic structure and properties are discussed considering super and super-super exchange interactions in comparison to those of triphylite-LiFePO4.en_AU
dc.language.isoenen_AU
dc.publisherAmerican Chemical Societyen_AU
dc.relation.ispartofInorganic Chemistryen_AU
dc.titleMagnetic structures of NaFePO4 marićite and triphylite polymorphs for sodium-ion batteriesen_AU
dc.typeArticleen_AU
dc.subject.asrc0302 Inorganic Chemistryen_AU
dc.identifier.doi10.1021/ic400870x
dc.type.pubtypeAuthor accepted manuscripten_AU
dc.relation.arcDP110102662
usyd.facultySeS faculties schools::Faculty of Science::School of Chemistryen_AU
usyd.citation.volume53en_AU
usyd.citation.spage8685en_AU
usyd.citation.epage8693en_AU
workflow.metadata.onlyNoen_AU


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