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論文

Sorption behavior of selenide on montmorillonite

杉浦 佑樹; 戸村 努*; 石寺 孝充; 土井 玲祐; Francisco, P. C. M.; 塩飽 秀啓; 小林 徹; 松村 大樹; 高橋 嘉夫*; 舘 幸男

Journal of Radioanalytical and Nuclear Chemistry, 324(2), p.615 - 622, 2020/05

 被引用回数:4 パーセンタイル:45.45(Chemistry, Analytical)

Batch sorption experiments were performed to investigate the sorption mechanism of Se on montmorillonite under reducing conditions in deep geological environments. Based on Eh-pH diagrams and ultraviolet-visible spectra, Se was dissolved as selenide (Se(-II)) anions under the experimental conditions. The distribution coefficients ($$K_{rm d}$$; m$$^{3}$$ kg$$^{-1}$$) of Se(-II) indicated ionic strength independence and slight pH dependence. The $$K_{rm d}$$ values of Se(-II) were higher than those of Se(IV), which also exists as an anionic species. X-ray absorption near edge spectroscopy showed that the oxidation state of Se-sorbed on montmorillonite was zero even though selenide remained in the solution. These results suggest that Se(-II) was oxidized and precipitated on the montmorillonite surface. Therefore, it is implied that a redox reaction on the montmorillonite surface contributed to high $$K_{rm d}$$ values for Se(-II).

口頭

Evaluation of sorption behavior of selenide onto montmorillonite

杉浦 佑樹; 戸村 努*; 土井 玲祐; 石寺 孝充; 舘 幸男

no journal, , 

We carried out batch sorption and XAFS experiments in various solution conditions identifying the aqueous species to evaluate the sorption behavior of Se(-II) onto montmorillonite. The ${it K$_{d}$}$ values were independent of ionic strength. The ${it K$_{d}$}$ values were nearly constant between pH 8-11, while the value decreased around pH 12. The aqueous species of Se(-II) were stable in 7d, and hydroselenide (HSe$$^{-}$$) was the dominant species at pH 8; whereas, polyselenide (Se$$_{3}$$$$^{2-}$$, Se$$_{4}$$$$^{2-}$$) increased with the increase of pH. These behavior implies that Se(-II) sorption onto the edge site of montmorillonite by complexation is not a dominant sorption mechanism. The XANES spectra indicate that Se in the collected solid phase exists as Se(0). These results suggest that the ${it K$_{d}$}$ values were independence of ionic strength and pH due to the oxidation and precipitation of Se by contacting montmorillonite in this work.

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