Please use this identifier to cite or link to this item: http://cmuir.cmu.ac.th/jspui/handle/6653943832/59469
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dc.contributor.authorBunlawee Yotnoien_US
dc.contributor.authorSanchai Luachanen_US
dc.contributor.authorTimothy J. Prioren_US
dc.contributor.authorApinpus Rujiwatraen_US
dc.date.accessioned2018-09-10T03:15:41Z-
dc.date.available2018-09-10T03:15:41Z-
dc.date.issued2009-07-27en_US
dc.identifier.issn16005368en_US
dc.identifier.issn16005368en_US
dc.identifier.other2-s2.0-67650832072en_US
dc.identifier.other10.1107/S160053680902251Xen_US
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=67650832072&origin=inwarden_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/59469-
dc.description.abstractIn an attempt to synthesize new cobalt(II) sulfate framework structures using 1,4-diazabicyclo[2.2.2]octane as a template, crystals of poly[0.35-[hexaaquacobalt(II)] [tri-μ-hydroxido-μ-sulfato-dicobalt(II)]], {[Co(H2O)6]0.35[Co2(OH) 3(SO4)]}n, were obtained as a mixture with [Co(H2O)6]SO4 crystals. The crystal structure can be described as being constructed from discrete brucite-type [Co 4(OH)6(SO4)2] layers, each of which is built up from edge-shared [Co(OH)6] and [Co(OH) 4-(OSO3)2] octahedra, with partial intercalation by [Co(H2O)6]2+ ions. The absence of ca 30% of the [Co(H2O)6]2+ cations indicates partial oxidation of cobalt(II) to cobalt(III) within the layer.en_US
dc.subjectChemistryen_US
dc.subjectMaterials Scienceen_US
dc.subjectPhysics and Astronomyen_US
dc.titleIntercalated brucite-type layered cobalt(II) hydroxysulfateen_US
dc.typeJournalen_US
article.title.sourcetitleActa Crystallographica Section E: Structure Reports Onlineen_US
article.volume65en_US
article.stream.affiliationsChiang Mai Universityen_US
article.stream.affiliationsUniversity of Hullen_US
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