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dc.contributor.authorCarroll, Dale
dc.contributor.authorRichmond, William
dc.date.accessioned2017-01-30T12:25:39Z
dc.date.available2017-01-30T12:25:39Z
dc.date.created2009-02-16T18:02:32Z
dc.date.issued2008
dc.identifier.citationCarroll, Dale and Richmond, William. 2008. Incorporation of Molybdate Anion into -FeOOH. American Mineralogist 93: pp. 1641-1646.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/21523
dc.description.abstract

An analogue of -FeOOH (akaganite) containing structurally-incorporated molybdate has beensynthesized and the conditions for its formation have been studied in the presence of chloride, sulfateand nitrate anions. The incorporation of molybdate into the -FeOOH structure has been shown togreatly increase the stability of this phase with respect to its transformation to hematite at elevatedtemperature. Molybdate incorporation has also been shown to change the particle morphology, withincreasing amounts of molybdate causing the rod-shaped nanoparticles to become progressively shorteruntil spherical nanocrystals are observed. The combined observations of increased stability, morphologychanges and measured levels of incorporated molybdenum suggest that although inclusion of molybdateanions into the -FeOOH tunnel sites is possible, it is unlikely to be the only mode of molybdateincorporation.

dc.publisherMineralogical Society of America
dc.titleIncorporation of Molybdate Anion into -FeOOH
dc.typeJournal Article
dcterms.source.volume93
dcterms.source.startPage1641
dcterms.source.endPage1646
dcterms.source.issn0003004X
dcterms.source.titleAmerican Mineralogist
curtin.departmentNanochemistry Research Institute (Research Institute)
curtin.accessStatusFulltext not available


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