Sorption of barium on kaolinite, montmorillonite and chlorite

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dc.citation.epage353en_US
dc.citation.issueNumber3en_US
dc.citation.spage351en_US
dc.citation.volumeNumber114en_US
dc.contributor.authorEylem, C.en_US
dc.contributor.authorErten, H. N.en_US
dc.contributor.authorGöktürk, H.en_US
dc.date.accessioned2016-02-08T10:56:54Z
dc.date.available2016-02-08T10:56:54Z
dc.date.issued1989en_US
dc.departmentDepartment of Chemistryen_US
dc.description.abstractThe sorption characteristics of the Ba2+ ion on kaolinite, montmorillonite and chloritetype clays were studied using the batch method. Barium-133 was used as a tracer. The Ba2+ ion concentrations ranged from 10-8 to 10-5 mol l-1; synthetic groundwater was used and the grain size of all the solid particles was <40 μm. About 6, 8 and 12 d of shaking were necessary to reach equilibrium for chlorite, kaolinite and montmorillonite, respectively. The sorption isotherms were described best by Freundlich and Dubinin - Radushkevich type isotherms. Sorption was predominantly reversible for kaolinite and partly reversible for montmorillonite and chlorite.en_US
dc.identifier.doi10.1039/AN9891400351en_US
dc.identifier.issn0003-2654
dc.identifier.urihttp://hdl.handle.net/11693/26240
dc.language.isoEnglishen_US
dc.publisherRoyal Society of Chemistryen_US
dc.relation.isversionofhttp://dx.doi.org/10.1039/AN9891400351en_US
dc.source.titleThe Analysten_US
dc.subjectBariumen_US
dc.subjectBatch methoden_US
dc.subjectClaysen_US
dc.subjectIsothermsen_US
dc.subjectSorption - Desorptionen_US
dc.titleSorption of barium on kaolinite, montmorillonite and chloriteen_US
dc.typeArticleen_US

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