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dc.contributor.authorKöksal F.
dc.contributor.authorUcun F.
dc.date.accessioned2020-06-21T09:16:22Z
dc.date.available2020-06-21T09:16:22Z
dc.date.issued1998
dc.identifier.issn0932-0784
dc.identifier.urihttps://doi.org/10.1515/zna-1998-1204
dc.identifier.urihttps://hdl.handle.net/20.500.12712/2903
dc.description.abstractActivated and non-activated states of the zeolites NH4NaY and NH4CaA, and their NH+4 forms were prepared with an (NH4)2SO4 solution and were investigated by EPR after ?-irradiation. The formed radicals were attributed to O-2 supposed to be trapped near a trigonally coordinated framework of 27A1 (I = 5/2). Anisotropic O-2 spectra were observed, consisting of hyperfine structure due to the 27A1 framework, even at room temperature. This was attributed to the scarceness of NH+4 sites or trap sites because of the preparation of the NH+4 forms of the zeolites with an (NH4)2SO4 solution. The crystal field splittings were found and interpreted.en_US
dc.language.isoengen_US
dc.publisherVerlag der Zeitschrift fur Naturforschungen_US
dc.relation.isversionof10.1515/zna-1998-1204en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectEPRen_US
dc.subjectNH4NaYen_US
dc.subjectNH4CaAen_US
dc.subjectO-2en_US
dc.subjectZeolitesen_US
dc.titleEPR of O2-radicals in the zeolites NH4NaY and NH4CaAen_US
dc.typearticleen_US
dc.contributor.departmentOMÜen_US
dc.identifier.volume53en_US
dc.identifier.issue12en_US
dc.identifier.startpage951en_US
dc.identifier.endpage954en_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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