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dc.creatorNikolić, Violeta N.
dc.creatorMilić, Mirjana M.
dc.creatorZdravković, Jelena D.
dc.creatorSpasojević, Vojislav
dc.date.accessioned2019-08-26T10:57:28Z
dc.date.accessioned2023-02-24T12:22:20Z
dc.date.available2019-08-26T10:57:28Z
dc.date.available2023-02-24T12:22:20Z
dc.date.issued2019
dc.identifier.issn0036-0244
dc.identifier.issn1531-863X
dc.identifier.urihttp://TechnoRep.tmf.bg.ac.rs/handle/123456789/5903
dc.description.abstractOrigin of the intrinsic coercivity field variations observed by hysteretic measurements established by Nikolic et al. was investigated in detail by ZFC/FC measurements. In this study, magnetic behavior of the samples is further examined by calculation of the ZFC Mn(T) and Mn(H) first derivatives. Performed study showed that the main contribution to the measured coercivity comes from the ε-Fe2O3 particles, characterized by Hci = 24 kOe, although both samples posses SPM ε-Fe2O3 fraction. As a result, Hci values of the samples are differed dependent on the quantity of the SPM ε-Fe2O3 particles in the sample. Mechanism of the intrisic coercivity field variations is discussed. © 2019, Pleiades Publishing, Ltd.en
dc.language.isoen
dc.relationinfo:eu-repo/grantAgreement/MESTD/Integrated and Interdisciplinary Research (IIR or III)/45015/RS//
dc.rightsrestrictedAccess
dc.sourceRussian Journal of Physical Chemistry A
dc.subjectepsilon-Fe2O3en
dc.subjectsol-gelen
dc.subjectintrinsic coercivity fielden
dc.titleOrigin of the Intrinsic Coercivity Field Variations and Magnetic Study of ε-Fe2O3en
dc.typearticleen
dc.rights.licenseARR
dc.rights.holder© 2019, Pleiades Publishing, Ltd.
dc.citation.epage593
dc.citation.issue3
dc.citation.rankM23
dc.citation.spage588
dc.citation.volume93
dc.identifier.doi10.1134/S0036024419030130
dc.identifier.scopus2-s2.0-85066139624
dc.identifier.wos000468852500032
dc.type.versionpublishedVersion


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