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dc.contributor.authorKöseoğlu R.
dc.contributor.authorKöksal F.
dc.contributor.authorAkkurt M.
dc.contributor.authorÇiftçi E.
dc.date.accessioned2020-06-21T09:23:12Z
dc.date.available2020-06-21T09:23:12Z
dc.date.issued2006
dc.identifier.issn0932-0784
dc.identifier.urihttps://hdl.handle.net/20.500.12712/3446
dc.description.abstractNatural sepiolite minerals and their ?-irradiated forms were investigated by electron paramagnetic resonance (EPR) at room temperature and at 113 K. The EPR signals in powders of natural sepiolite were observed due to clusters of Fe3+ ions. The paramagnetic centers produced by ?-irradiation of natural sepiolite minerals were attributed to the ?H3 at room temperature and ?O2- and ?O3- radicals at 113 K. These centers were found to be perfectly observable above 20 mW microwave power. The g values of all paramagnetic centers have been measured and the A values of some of them have been reported. The results were consistent with the literature data for similar paramagnetic centers. © 2006 Verlag der Zeitschrift für Naturforschung.en_US
dc.description.sponsorshipThis work was supported by the Erciyes University Research Fund, Project No. FBA-04-24.en_US
dc.language.isoengen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subject?-Irradiationen_US
dc.subjectEPRen_US
dc.subjectParamagnetic Centersen_US
dc.subjectSepiolite Mineralsen_US
dc.titleElectron paramagnetic resonance of organic and inorganic centers in ?-irradiated natural sepiolite mineralsen_US
dc.typearticleen_US
dc.contributor.departmentOMÜen_US
dc.identifier.volume61en_US
dc.identifier.issue07.Augen_US
dc.identifier.startpage413en_US
dc.identifier.endpage417en_US
dc.relation.journalZeitschrift fur Naturforschung - Section A Journal of Physical Sciencesen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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