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dc.creatorNikolić, Violeta N.
dc.creatorVasić, Milica M.
dc.creatorMilić, Mirjana M.
dc.date.accessioned2018-10-22T10:07:18Z
dc.date.available2018-10-22T10:07:18Z
dc.date.issued2018
dc.identifier.issn0272-8842
dc.identifier.issn1873-3956
dc.identifier.urihttps://vinar.vin.bg.ac.rs/handle/123456789/7876
dc.description.abstractSamples containing CuFe2O4 and CuO nanoparticles were synthesized by coprecipitation method and subjected to thermal treatment at 300 °C, 500 °C, 700 °C, 900 °C and 1100 °C. Depending on the synthesis conditions, high-temperature treatment of the prepared samples brought to the formation of CuFe2O4 with a tetragonal or cubic structure, which was confirmed by X-ray diffraction analysis. The influence of formation mechanism onto the crystallite sizes of nanoparticles and structural transformation of CuFe2O4 is discussed. For the first time it was shown that variations of the initial amount of Fe3+ and Cu2+ ions precursors resulted in the formation of low- and high-temperature CuFe2O4 phase at the same annealing temperature, 1100 °C. © 2018en
dc.relationinfo:eu-repo/grantAgreement/MESTD/Integrated and Interdisciplinary Research (IIR or III)/45015/RS//
dc.relationMinistry of Education, Science and Technological Development of the Republic of Serbia (Grant no. OI 1710)
dc.rightsrestrictedAccess
dc.sourceCeramics International
dc.subjectCoprecipitationen
dc.subjectCuFe2O4en
dc.subjectCrystallite sizeen
dc.subjectStructural transformationen
dc.titleObservation of low- and high-temperature CuFe2O4 phase at 1100 °C: The influence of Fe3+ ions on CuFe2O4 structural transformationen
dc.typearticleen
dc.rights.licenseARR
dcterms.abstractНиколић, Виолета Н; Милић, Мирјана М; Васић, Милица;
dc.rights.holder© 2018 Elsevier Ltd and Techna Group S.r.l.
dc.citation.volume44
dc.citation.issue17
dc.citation.spage21145
dc.citation.epage21152
dc.identifier.wos000448226900072
dc.identifier.doi10.1016/j.ceramint.2018.08.157
dc.citation.rankaM21
dc.type.versionpublishedVersion
dc.identifier.scopus2-s2.0-85051663135


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