Phase evolution of vanadium oxides obtained through temperature programmed calcinations of ammonium vanadate in hydrogen atmosphere and their humidity sensing properties

dc.contributor.authorAkande, A.A.
dc.contributor.authorLinganiso, E.C.
dc.contributor.authorDhonge, B.P.
dc.contributor.authorRammutla, K.E.
dc.contributor.authorMachatine, Augusto Gonçalo Jose
dc.contributor.authorPrinsloo, Linda Charlotta
dc.contributor.authorKunert, Herbert W.
dc.contributor.authorMwakikunga, B.W.
dc.date.accessioned2015-03-05T09:02:45Z
dc.date.available2015-03-05T09:02:45Z
dc.date.issued2015-02
dc.description.abstractThe possibility of obtaining vanadium dioxide (VO2) [wherein the vanadium ionic state is 4þ] from a precursor of ammonium metavanadate (NH4VO3) bearing the ion V5þ is investigated. The reduction is carried out by calcining the NH4VO3 powders in similar concentrations of H2 flow at varying temperatures. The resulting powders have been studied by several techniques including XRD, Raman spectroscopy, FTIR, TEM, BET and DSC. It is found that remnants of bright yellow V5þ still exist up to calcination temperatures of 100 C after which the sky-blue VO2 dominates at calcination temperatures of 150 C e250 C. There is a population surge of metastable dark-blue V6O13 (where V is in between V4þ and V5þ ionic states) between 250 C and 300 C. However above 350 C the material reverts to the stable V5þ in the yellow-orange V2O5. XPS/EDS and VSM confirm the order of appearance to be VO2(150 C) / V6O13(200 C) / V2O5 (350 C).en_ZA
dc.description.librarianhb2015en_ZA
dc.description.sponsorshipIndia-Brazil-South Africa trilateral cooperation under the National Research Foundation (NRF) grant number HGER24X.en_ZA
dc.description.urihttp://www.elsevier.com/locate/matchemphysen_ZA
dc.identifier.citationAkande, AA, Linganiso, EC, Dhonge, BP, Rammutla, KE, Machatine, AGJ, Prinsloo, LC, Kunert, HW & Mwakikunga, BW 2014, 'Phase evolution of vanadium oxides obtained through temperature programmed calcinations of ammonium vanadate in hydrogen atmosphere and their humidity sensing properties', Materials Chemistry and Physics, vol. 151, no. 206-2015.en_ZA
dc.identifier.issn0254-0584
dc.identifier.other10.1016/j.matchemphys.2014.11.055
dc.identifier.urihttp://hdl.handle.net/2263/43873
dc.language.isoenen_ZA
dc.publisherElsevieren_ZA
dc.rights© 2014 Elsevier B.V. All rights reserved. Notice : this is the author’s version of a work that was accepted for publication in Materials Chemistry and Physics. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Materials Chemistry and Physics, vol. 151, pp. 206-215, 2015. doi : 10.1016/j.matchemphys.2014.11.055.en_ZA
dc.subjectAnnealingen_ZA
dc.subjectOxidationen_ZA
dc.subjectPhase transitionen_ZA
dc.subjectThermogravimetric analysisen_ZA
dc.subjectX-ray diffraction (XRD)en_ZA
dc.subjectTopologyen_ZA
dc.subjectAdsorptionen_ZA
dc.subjectDesorptionen_ZA
dc.subjectDifferential scanning calorimetry (DSC)en_ZA
dc.subjectX-ray photo-electron spectroscopy (XPS)en_ZA
dc.subjectVibrating sample magnetometer (VSM)en_ZA
dc.titlePhase evolution of vanadium oxides obtained through temperature programmed calcinations of ammonium vanadate in hydrogen atmosphere and their humidity sensing propertiesen_ZA
dc.typePostprint Articleen_ZA

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