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Evaluation of labile $$^{137}$$Cs in Fukushima rivers by diffusive gradients in thin films (DGT), 3; Relations between geochemical parameters

Tanaka, Takuro*; Saito, Takumi*; Toda, Kanako*; Fujiwara, Kenso ; Terashima, Motoki  ; Nakanishi, Takahiro   ; Kobayashi, Natsuko*; Tanoi, Keitaro*; Kato, Hiroaki*

$$^{137}$$Cs dispersed by the Fukushima Daiichi Nuclear Power Plant accident deposited in Fukushima area, that are not decontaminated in mountainous areas, may migrate through river water to animals and plants. Most of $$^{137}$$Cs in river are fixed in clay minerals, but there are some Cs that can be easily desorbed, named as labile components. It has been suggested that labile components affect the bioavailability of $$^{137}$$Cs. In this study, the labile $$^{137}$$Cs was sampled in situ from upstream to downstream in several rivers of Fukushima using a passive sampler called diffusive gradients in thin films (DGT). The desorption behavior of the labile component and factors affecting it will be discussed by examining the relationship with particulate $$^{137}$$Cs and geochemical parameters in river water.

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