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dc.contributor.authorErten, H. N.en_US
dc.contributor.authorAksoyoglu, S.en_US
dc.contributor.authorHatipoglu, S.en_US
dc.contributor.authorGöktürk, H.en_US
dc.date.accessioned2016-02-08T10:57:29Z
dc.date.available2016-02-08T10:57:29Z
dc.date.issued1988en_US
dc.identifier.issn0033-8230
dc.identifier.urihttp://hdl.handle.net/11693/26278
dc.description.abstractSorption characteristics of Cs+ and Sr++on montmorillonite and kaolinite type clays and soil fractions from various regions of Turkey were studied using the batch method. 137Cs and 90Sr were used as tracers. Concentrations of Cs+ and Sr++ ions ranged from 10-8to 10-2 mol/1; natural groundwater was used and the grain size of the solid particles was < 20 yμm. Equilibrium was reached in 4 - 7 days for Cs+and 7 - 11 days for Sr++. The distribution coefficient, RD, increased with decreasing grain size, suggesting mainly a surface phenomenon. The sorption isotherms were non-linear suggesting at least two different sorption processes. The sorption was found to be predominantly reversible. Cs+ was sorbed much stronger than Sr++in all samples. © 1988, Walter de Gruyter. All rights reserved.en_US
dc.language.isoEnglishen_US
dc.source.titleRadiochimica Actaen_US
dc.relation.isversionofhttp://dx.doi.org/10.1524/ract.1988.4445.1.147en_US
dc.subjectBatch methoden_US
dc.subjectClaysen_US
dc.subjectDistribution ratiosen_US
dc.subjectFission productsen_US
dc.subjectSorptionen_US
dc.subjectturkey (republic)en_US
dc.titleSorption of cesium and strontium on montmorillonite and kaoliniteen_US
dc.typeArticleen_US
dc.departmentDepartment of Chemistryen_US
dc.citation.spage147en_US
dc.citation.epage152en_US
dc.citation.volumeNumber44-45en_US
dc.citation.issueNumber1en_US
dc.identifier.doi10.1524/ract.1988.4445.1.147en_US
dc.publisherDe Gruyter Oldenbourgen_US


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