Uptake of Cs+ on poorly crystalline layered manganese oxide (Na birnessite) is reported. Distribution coefficients (Kd) showed significant uptake of Cs+ under acidic (pH 2.4) or basic conditions (pH 10.2). The uptake of Cs+ takes place with release of Na+ into the solution confirming ion exchange. The maximum uptake of Cs+ was 2.0 mmol g−1 at pH 10.2.
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Chitrakar et al. (2011) studied this question.
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