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dc.contributor.authorDyer, Alan
dc.contributor.authorChimedtsogzol, Anaad
dc.contributor.authorCampbell, Linda
dc.contributor.authorWilliams, Craig D.
dc.date.accessioned2008-06-23T15:14:34Z
dc.date.available2008-06-23T15:14:34Z
dc.date.issued2006
dc.identifier.citationMicroporous and Mesoporous Materials, 95(1-3): 172-175
dc.identifier.issn13871811
dc.identifier.doi10.1016/j.micromeso.2006.05.013
dc.identifier.urihttp://hdl.handle.net/2436/30338
dc.description.abstractMongolian clinoptilolite-rich tuffs were examined for their ability to take up 137-Cs and 90-Sr/90-Y in the presence of competing cations (Na+, K+, Cs+, Ca2+, Mg2+, Sr2+), as nitrate salts, in the concentration range 10−1–10−3 M. Experiments were carried out by the batch technique and expressed as distribution coefficients. Clear differences were seen in Sr and Cs uptakes and those for Sr did not follow the trends expected from simple ion exchange theory. Results are discussed in relationship to the Si/Al framework compositions and cation contents of the zeolites, and suggestions made for the anomalies observed. It is concluded that the presence of some cations, potentially present in aqueous nuclear wastes, cause effects which can affect the use of clinoptilolite in the treatment of these wastes.
dc.language.isoen
dc.publisherAmsterdam: Elsevier
dc.relation.urlhttp://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6TH4-4KBVX47-2&_user=10&_rdoc=1&_fmt=&_orig=search&_sort=d&view=c&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=4deb24fa491e741cdea4635f63acd8ca
dc.subjectGeochemistry
dc.subjectZeolites
dc.subjectCaesium
dc.subjectStrontium
dc.subjectMongolia
dc.subjectClinoptilolite
dc.subjectRadioisotopes
dc.subjectNuclear waste
dc.subjectCations
dc.titleUptake of caesium and strontium radioisotopes by natural zeolites from Mongolia.
dc.typeJournal article
dc.identifier.journalMicroporous and Mesoporous Materials
html.description.abstractMongolian clinoptilolite-rich tuffs were examined for their ability to take up 137-Cs and 90-Sr/90-Y in the presence of competing cations (Na+, K+, Cs+, Ca2+, Mg2+, Sr2+), as nitrate salts, in the concentration range 10−1–10−3 M. Experiments were carried out by the batch technique and expressed as distribution coefficients. Clear differences were seen in Sr and Cs uptakes and those for Sr did not follow the trends expected from simple ion exchange theory. Results are discussed in relationship to the Si/Al framework compositions and cation contents of the zeolites, and suggestions made for the anomalies observed. It is concluded that the presence of some cations, potentially present in aqueous nuclear wastes, cause effects which can affect the use of clinoptilolite in the treatment of these wastes.


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