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Seok, Sang Il
Laboratory for Energy Harvesting Materials and Systems
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dc.citation.endPage 3787 -
dc.citation.number 28 -
dc.citation.startPage 3783 -
dc.citation.title MATERIALS LETTERS -
dc.citation.volume 59 -
dc.contributor.author Pramanik, Nimai Chand -
dc.contributor.author Bhuiyan, Tarequl Islam -
dc.contributor.author Nakanishi, Makoto -
dc.contributor.author Fujii, Tatsuo -
dc.contributor.author Takada, Jun -
dc.contributor.author Seok, Sang Il -
dc.date.accessioned 2023-12-22T10:10:16Z -
dc.date.available 2023-12-22T10:10:16Z -
dc.date.created 2016-02-15 -
dc.date.issued 2005-12 -
dc.description.abstract Fine particles of cerium substituted hematite with different compositions were prepared by the sol-gel method from the aqueous solution of their corresponding metal salts. Mixed hydroxides of Fe3+ and Ce4+ were obtained by reacting aqueous NH3 with the aqueous solution of FeCl3 and Ce(NH3)(2)(NO3)(6) at pH 2.5-3.0) and they were heat treated at different temperatures between 400 and 1200 degrees C in air for 2 h to get the mixed oxide product. Thermal analysis and X-ray diffraction studies revealed the coexistence of Fe2O3 and CeO2 phase separately up to 900 degrees C, and covalent interaction between them above 1000 degrees C, which was evidenced by the shifting of the XRD peaks. Unit cell parameters and the cell volumes (V) of the samples derived between 1000 and 1200 degrees C were found to be in the range a=5.045-5.048 +/- 0.007 angstrom, c=13.774-13.815 +/- 0.041 angstrom and V=303.608-304.874 angstrom(3) respectively. It was observed that both the lattice parameters and the cell volumes were higher than that of the pure alpha-Fe2O3 (a =5.036 angstrom, c = 13.749 angstrom, V=301.976 angstrom(3)) system. The expansion of lattice parameters further supported the incorporation of the large Ce4+ ion into the alpha-Fe2O3 matrix. The lattice parameter increased with increasing Ce4+ ion loading. FESEM studies showed the growth of the particles with increasing temperature though it was suppressed due to the presence of Ce4+ ions as compared to the pure system. (C) 2005 Elsevier B.V. All rights reserved -
dc.identifier.bibliographicCitation MATERIALS LETTERS, v.59, no.28, pp.3783 - 3787 -
dc.identifier.doi 10.1016/j.matlet.2005.06.056 -
dc.identifier.issn 0167-577X -
dc.identifier.scopusid 2-s2.0-27144457644 -
dc.identifier.uri https://scholarworks.unist.ac.kr/handle/201301/18688 -
dc.identifier.url http://www.sciencedirect.com/science/article/pii/S0167577X05006713 -
dc.identifier.wosid 000232514200052 -
dc.language 영어 -
dc.publisher ELSEVIER SCIENCE BV -
dc.title Synthesis and characterization of cerium substituted hematite by sol-gel method -
dc.type Article -
dc.description.journalRegisteredClass scopus -
dc.subject.keywordAuthor cerium substituted Fe2O3 -
dc.subject.keywordAuthor sol-gel method -
dc.subject.keywordAuthor XRD -
dc.subject.keywordAuthor crystal growth -
dc.subject.keywordPlus ALKALINE MEDIA -
dc.subject.keywordPlus COLOR -
dc.subject.keywordPlus FERRIHYDRITE -
dc.subject.keywordPlus TRANSFORMATION -
dc.subject.keywordPlus GOETHITE -
dc.subject.keywordPlus PRODUCTS -

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