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dc.contributor.authorKoseoglu, Rahmi
dc.contributor.authorKoksal, Fevzi
dc.contributor.authorAkkurt, Mehmet
dc.contributor.authorCiftci, Emin
dc.date.accessioned2020-06-21T15:28:38Z
dc.date.available2020-06-21T15:28:38Z
dc.date.issued2006
dc.identifier.issn0932-0784
dc.identifier.issn1865-7109
dc.identifier.urihttps://doi.org/10.1515/zna-2006-7-816
dc.identifier.urihttps://hdl.handle.net/20.500.12712/20563
dc.descriptionWOS: 000240769000016en_US
dc.description.abstractNatural sepiolite minerals and their gamma-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 gamma-irradiation of natural sepiolite minerals were attributed to the CH3 at room temperature and SO2- and SO3- 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.en_US
dc.language.isoengen_US
dc.publisherWalter De Gruyter Gmbhen_US
dc.relation.isversionof10.1515/zna-2006-7-816en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectEPRen_US
dc.subjectparamagnetic centersen_US
dc.subjectgamma-irradiationen_US
dc.subjectsepiolite mineralsen_US
dc.titleElectron paramagnetic resonance of organic and inorganic centers in gamma-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-A Journal of Physical Sciencesen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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