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dc.contributor.author김동수*
dc.date.accessioned2016-08-27T02:08:20Z-
dc.date.available2016-08-27T02:08:20Z-
dc.date.issued1999*
dc.identifier.issn0253-2964*
dc.identifier.otherOAK-173*
dc.identifier.urihttps://dspace.ewha.ac.kr/handle/2015.oak/215288-
dc.description.abstractThe partitionings of NiO and of NiO and TiO2 between hematite and Na2O 2B(2)O(3) melts were studied by the flux growth method as a function of solute concentration. The substitution mechanisms of NiO and/or TiO2 in -Fe2O3 lattice were discussed based on the concentration dependence of the distribution coefficients. The substitution of Ni2+ ion for Fe3+ was accompanied by the charge compensating oxygen ion vacancies, while the coupled substitution of Ni2+ and Ti4+ ions for Fe3+ was accompanied by the formation of Fe2+ ion, which was confirmed by chemical analysis.*
dc.languageEnglish*
dc.publisherKOREAN CHEMICAL SOC*
dc.titleCoupled substitution of NiO and TiO2 in hematite*
dc.typeArticle*
dc.relation.issue2*
dc.relation.volume20*
dc.relation.indexSCI*
dc.relation.indexSCIE*
dc.relation.indexSCOPUS*
dc.relation.indexKCI*
dc.relation.startpage195*
dc.relation.lastpage198*
dc.relation.journaltitleBULLETIN OF THE KOREAN CHEMICAL SOCIETY*
dc.identifier.wosidWOS:000079139600016*
dc.author.googlePark, BH*
dc.author.googleKim, DS*
dc.contributor.scopusid김동수(57218545867)*
dc.date.modifydate20240322131352*
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공과대학 > 환경공학과 > Journal papers
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