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Weathering promotes the sorption of radiocesium in mafic minerals of river sediments in the Fukushima Prefecture, Japan

Hagiwara, Hiroki  ; Watanabe, Yusuke  ; Konishi, Hiromi*; Funaki, Hironori ; Fujiwara, Kenso ; Iijima, Kazuki 

Radiocesium ($$^{134}$$Cs and $$^{137}$$Cs) was sorbed on minerals and transported to river systems due to the Fukushima Daiichi Nuclear Power Plant accident. Recently, the authors have reported that mafic minerals sorb $$^{137}$$Cs equally or more strongly than micaceous minerals in fine sands. We characterized mafic minerals and elucidated their weathering using electron microscopy to determine whether they can sorb $$^{137}$$Cs. The surface of hornblende particles is weathered and altered to vermiculite. The surface of micas is less weathered than that of hornblende, indicating the $$^{137}$$Cs activity concentrations of highly weathered mafic minerals are higher than those of micas in part of sampling site. The results indicate that the effects of $$^{137}$$Cs sorption for hornblende depend on the weathering product at the surface.

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Category:Geochemistry & Geophysics

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