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dc.contributor.authorAssemi, S.en_US
dc.contributor.authorErten H.N.en_US
dc.date.accessioned2016-02-08T10:53:03Z
dc.date.available2016-02-08T10:53:03Z
dc.date.issued1994en_US
dc.identifier.issn2365731en_US
dc.identifier.urihttp://hdl.handle.net/11693/25966
dc.description.abstractBatch method was used to investigate the sorption behavior of radioiodine on organic rich soil, alumina, chlorite-illite clay mixture and bentonite.131I was used as tracer. The grain sizes of the samples used were all below 38 μm. A rather slow kinetics was observed for the adsorption of radioiodine on organic rich soil. The distribution ratio increased with increasing solution/solid (V/m) ratio, and the contact time. The pH of the synthetic groundwater did not change the distribution ratio appreciably. The soil biomass however, showed a striking effect on the adsorption of radioiodine. Among the clay minerals, the highest distribution ratio value was found for chlorite-illite clay mixture. All the values were however well below those of the organic rich soil. The sorption data were fitted to Freundlich and Dubinin-Radushkevich types isotherms. Means energies of adsorption, as well as the affinity ratios of the sorption sites to iodine and chlorine were calculated. © 1994 Akadémiai Kiadó.en_US
dc.language.isoEnglishen_US
dc.source.titleJournal of Radioanalytical and Nuclear Chemistry Articlesen_US
dc.relation.isversionofhttp://dx.doi.org/10.1007/BF02068670en_US
dc.subjectiodine 131en_US
dc.subjectradioactive iodineen_US
dc.subjectadsorptionen_US
dc.subjectarticleen_US
dc.subjectmethodologyen_US
dc.titleSorption of radioiodine on organic rich soil, clay minerals and aluminaen_US
dc.typeResearch Paperen_US
dc.departmentDepartment of Chemistryen_US
dc.citation.spage193en_US
dc.citation.epage204en_US
dc.citation.volumeNumber178en_US
dc.citation.issueNumber1en_US
dc.identifier.doi10.1007/BF02068670en_US
dc.publisherKluwer Academic Publishersen_US


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