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dc.contributor.authorKoseoglu, R
dc.contributor.authorKoksal, F
dc.contributor.authorCiftci, E
dc.contributor.authorAkkurt, M
dc.date.accessioned2019-08-01T13:38:39Z
dc.date.available2019-08-01T13:38:39Z
dc.date.issued2005
dc.identifier.issn0022-2860
dc.identifier.urihttps://dx.doi.org/10.1016/j.molstruc.2004.08.005
dc.identifier.urihttps://hdl.handle.net/11480/5615
dc.descriptionWOS: 000225487000021en_US
dc.description.abstractIn this study, gamma-irradiated natural diatomite minerals were investigated by electron paramagnetic resonance (EPR) spectroscopy at ambient temperature. The paramagnetic radicals produced by gamma-irradiation in natural diatomite minerals at ambient temperature were free radicals. These centers were found to be perfectly attributed to CH3, PO42-, CO2-, organic (probably, humic or fluvic acid), SO2- and SO3- observable at below 20 mW microwave power. The g values of all the paramagnetic centers were obtained, and some of their a values were reported. The results were found to be consistent with the existing literature data and theoretical predictions for similar paramagnetic centers. (C) 2004 Elsevier B.V. All rights reserved.en_US
dc.language.isoengen_US
dc.publisherELSEVIER SCIENCE BVen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectEPRen_US
dc.subjectdiatomiteen_US
dc.subjectgamma-irradiationen_US
dc.subjectfree radicalsen_US
dc.titleIdentification of paramagnetic radicals in gamma-irradiated natural diatomite minerals by electron paramagnetic resonanceen_US
dc.typearticleen_US
dc.relation.journalJOURNAL OF MOLECULAR STRUCTUREen_US
dc.departmentNiğde ÖHÜen_US
dc.identifier.volume733en_US
dc.identifier.issue1.Maren_US
dc.identifier.startpage151en_US
dc.identifier.endpage154en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.contributor.institutionauthor[0-Belirlenecek]
dc.identifier.doi10.1016/j.molstruc.2004.08.005


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