Sorption of barium on kaolinite, montmorillonite and chlorite
dc.citation.epage | 353 | en_US |
dc.citation.issueNumber | 3 | en_US |
dc.citation.spage | 351 | en_US |
dc.citation.volumeNumber | 114 | en_US |
dc.contributor.author | Eylem, C. | en_US |
dc.contributor.author | Erten, H. N. | en_US |
dc.contributor.author | Göktürk, H. | en_US |
dc.date.accessioned | 2016-02-08T10:56:54Z | |
dc.date.available | 2016-02-08T10:56:54Z | |
dc.date.issued | 1989 | en_US |
dc.department | Department of Chemistry | en_US |
dc.description.abstract | The 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.description.provenance | Made available in DSpace on 2016-02-08T10:56:54Z (GMT). No. of bitstreams: 1 bilkent-research-paper.pdf: 70227 bytes, checksum: 26e812c6f5156f83f0e77b261a471b5a (MD5) Previous issue date: 1989 | en |
dc.identifier.doi | 10.1039/AN9891400351 | en_US |
dc.identifier.issn | 0003-2654 | |
dc.identifier.uri | http://hdl.handle.net/11693/26240 | |
dc.language.iso | English | en_US |
dc.publisher | Royal Society of Chemistry | en_US |
dc.relation.isversionof | http://dx.doi.org/10.1039/AN9891400351 | en_US |
dc.source.title | The Analyst | en_US |
dc.subject | Barium | en_US |
dc.subject | Batch method | en_US |
dc.subject | Clays | en_US |
dc.subject | Isotherms | en_US |
dc.subject | Sorption - Desorption | en_US |
dc.title | Sorption of barium on kaolinite, montmorillonite and chlorite | en_US |
dc.type | Article | en_US |
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