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dc.contributor.authorBarpanda, P
dc.contributor.authorLing, Chris D
dc.contributor.authorOyama, G
dc.contributor.authorYamada, A
dc.date.accessioned2022-08-09T03:54:36Z
dc.date.available2022-08-09T03:54:36Z
dc.date.issued2013en_AU
dc.identifier.urihttps://hdl.handle.net/2123/29378
dc.description.abstractThe crystal structure of the NaMnSO4F fluorosulphate phase prepared by low-temperature solid-state synthesis has been solved and refined by the Rietveld analysis of synchrotron X-ray powder diffraction data. Isostructural to the naturally occurring triplite family of minerals, this compound crystallizes in monoclinic C2/c symmetry (#15) with unit cell parameters of a = 13.77027(17), b = 6.63687(8), c = 10.35113(14) Å,  = 121.4795(3) and V = 806.78(2) Å3. Its structure is built of edge-sharing chains of distorted MO4F2 octahedra, which are interconnected by constituent SO4 tetrahedra to form a robust three-dimensional polyanionic framework. MO4F2 octahedra are randomly occupied by Na and Mn with close to 1:1 occupancy. This random mixing of cations among polyhedral building blocks means that there are no channels for Na-ion conduction, rendering it electrochemically inactive. The structure is discussed and compared to other known alkali metal fluorosulphates as well as to naturally occurring triplite-type minerals.en_AU
dc.language.isoenen_AU
dc.publisherInternational Union of Crystallographyen_AU
dc.relation.ispartofActa Crystallographica Section B – Structural Scienceen_AU
dc.titleSodium manganese fluorosulphate with a triplite structureen_AU
dc.typeArticleen_AU
dc.subject.asrc0302 Inorganic Chemistryen_AU
dc.identifier.doi10.1107/S2052519213024093
dc.type.pubtypeAuthor accepted manuscripten_AU
dc.relation.arcDP110102662
usyd.facultySeS faculties schools::Faculty of Science::School of Chemistryen_AU
usyd.citation.volume69en_AU
usyd.citation.spage584en_AU
usyd.citation.epage588en_AU
workflow.metadata.onlyNoen_AU


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