Journal
APPLIED CLAY SCIENCE
Volume 44, Issue 1-2, Pages 15-20Publisher
ELSEVIER SCIENCE BV
DOI: 10.1016/j.clay.2008.12.015
Keywords
K-depleted biotite; K-depleted muscovite; Cation exchange; Radioactive species
Funding
- Chemical and Transport Systems, Division of the National Science Foundation [CTS-0242285]
- College of Agricultural Sciences [PEN03963]
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Cation exchange selectivity for Cs+ and Sr2+ with K-depleted biotite (Na-biotite) and K-depleted muscovite (Na-muscovite) was determined with equilibration for 4 weeks at room temperature. The cation exchange isotherms and Kielland plots indicated that both K-depleted micas show high selectivity for Cs+ at low equivalent fraction of Cs+ on solid. The K-depleted micas took up Cs up to approximately 50% of their theoretical cation exchange capacities. The XRD patterns after Na+ -> Cs+ exchange reactions with K-depleted biotite showed that the d(001)-spacings collapsed from similar to 12.2 to similar to 11.2 angstrom with high Cs+ concentrations. This collapse suggests that K-depleted biotite is able to immobilize or fix Cs ions in the interlayers. In case of 2Na(+) -> Sr2+ exchange, K-depleted biotite showed high selectivity for Sr ions at low equivalent fraction of Sr2+ on solid. The XRD patterns showed that the main d(001)-spacing of the K-depleted biotite slightly increased from 12.16 angstrom to similar to 12.3 angstrom after the exchange reactions with the high Sr2+ concentrations. These results suggest that K-depleted biotite could be used as an ion exchanger to remove radioactive Cs-137 as well as Sr-90 from groundwater. (C) 2008 Elsevier B.V. All rights reserved.
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