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Ten-year temporal changes in the supply source of $$^{137}$$Cs released by the Fukushima Daiichi Nuclear Power Plant to the coastal area

Sato, Shun ; Wakiyama, Yoshifumi*; Takahashi, Fumiaki  ; Takata, Hyoe*

We compared the ongoing direct release of $$^{137}$$Cs from the Fukushima Daiichi Nuclear Power Plant (FDNPP) and riverine inputs of $$^{137}$$Cs that have contributed to the persistent elevated $$^{137}$$Cs in coastal waters around the plant since 2012. The direct release of $$^{137}$$Cs clearly decreased from 17.5 TBq during 2012$$sim$$2014 to 0.6 TBq during 2019$$sim$$2021 because of measures implemented by the FDNPP. The riverine input decreased slightly from 2.2 TBq during 2012$$sim$$2014 to 2.0 TBq during 2019$$sim$$2021. The ratio of direct release to the total $$^{137}$$Cs flux into the coastal water around the FDNPP decreased from 89% during 2012$$sim$$2014 to 23% during 2019$$sim$$2021. This change resulted in part from a lowering of the limit of detection of $$^{137}$$Cs activities to avoid overestimation of Cs fluxes from the facility, but also from installation of an impermeable seaside wall. The trend of decreasing riverine $$^{137}$$Cs input might have been due entirely to environmental remediation. Our results indicate that the contribution of riverine input to the coastal waters will continue for a long time. Precise prediction of the long-term distribution of $$^{137}$$Cs in the marine environment will require consideration of a variety of environmental factors and anthropogenic effects.

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