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Assessment of suspended sediment and $$^{137}$$Cs sources during the flood event in the Fukushima river using $$^{13}$$C and $$^{14}$$C

Nakanishi, Takahiro   ; Tsuruta, Tadahiko  ; Funaki, Hironori 

In this study, the radiocarbon isotope ratio, $$Delta$$$$^{14}$$C, was used to identify the sources of suspended sediment and $$^{137}$$Cs discharged into rivers after the Fukushima nuclear accident. Suspended sediments were collected during the flood event and under normal water conditions to determine $$^{137}$$Cs concentrations, $$Delta$$$$^{14}$$C, and stable carbon isotope ratios. The results indicated that the contribution of forest surface soil runoff increased during the flood peak. Furthermore, the distribution of $$^{137}$$Cs deposition in the watershed was reflected in temporal changes in suspended $$^{137}$$Cs concentration during the flood event. This approach provides a comprehensive understanding of both $$^{137}$$Cs and carbon dynamics.

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