Radiocesium in North Pacific coastal and offshore areas of Japan within several months after the Fukushima accident

Publication date: March 2019

Source: Journal of Environmental Radioactivity, Volume 198

Author(s): Yuichiro Kumamoto, Masatoshi Yamada, Michio Aoyama, Yasunori Hamajima, Hideki Kaeriyama, Hisao Nagai, Takeyasu Yamagata, Akihiko Murata, Yukio Masumoto

Abstract

We measured activity concentrations of radiocesium (¹³⁴Cs and ¹³⁷Cs) in seawater samples collected in North Pacific coastal and offshore areas of Japan within several months after the Fukushima Dai-ichi Nuclear Power Plant (FNPP1) accident in March 2011, including archived seawater samples whose radiocesium concentrations were previously reported to be below detection limits. By merging 329 new data with published results, we succeeded in reconstructing the temporal changes in activity concentrations and inventories of FNPP1-derived radiocesium in the coastal and offshore areas within several months after the accident for the first time. ¹³⁷Cs directly-discharged from the FNPP1 was transported eastward within the coastal area about 250 km from the FNPP1 during two months after the accident due to complex movements of coastal surface currents. The eastward speed was calculated to be about 5 cm s⁻¹. Eastward transport of ¹³⁷Cs to the offshore area more than 600 km away from the FNPP1 along the north flank of the Kuroshio Extension Current was faster (about 9 cm s⁻¹) and probably more dominant in the eastward transport. The total inventory of directly-discharged ¹³⁷Cs in early April 2011 was estimated to be 3–6 PBq approximately, which agrees with the smaller estimates in previous studies (2–6 PBq).

Graphical abstract

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