Cation exchange equilibria of cesium and strontium with K-depleted biotite and muscovite

被引:42
作者
Cho, Yunchul [3 ,4 ]
Komarneni, Sridhar [1 ,2 ]
机构
[1] Penn State Univ, Mat Res Lab 205, Dept Crop & Soil Sci, University Pk, PA 16802 USA
[2] Penn State Univ, Mat Res Inst, University Pk, PA 16802 USA
[3] Univ Calif Davis, Peter A Rock Thermochem Lab, Davis, CA 95616 USA
[4] Univ Calif Davis, NEAT ORU, Davis, CA 95616 USA
基金
美国国家科学基金会;
关键词
K-depleted biotite; K-depleted muscovite; Cation exchange; Radioactive species; ION-EXCHANGE; ALKALI-METAL; SELECTIVITY; PHLOGOPITE; SILICATE; PHILLIPSITE; KAOLINITE; NA-2-MICA; REMOVAL; MICA;
D O I
10.1016/j.clay.2008.12.015
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
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.
引用
收藏
页码:15 / 20
页数:6
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