微粒
沉积物
羽流
环境科学
河口
铯
福岛核事故
环境化学
放射性核素
海洋学
生物群
海水
地质学
核电站
化学
生态学
生物
核物理学
有机化学
古生物学
物理
热力学
量子力学
作者
Hikaru Miura,Takashi Ishimaru,Yukari Ito,Yuichi Kurihara,Shigeyoshi Otosaka,Aya Sakaguchi,Kazuhiro Misumi,Daisuke Tsumune,Atsushi Kubo,Shogo Higaki,Jota Kanda,Yoshio Takahashi
标识
DOI:10.1038/s41598-021-85085-w
摘要
Abstract A part of the radiocaesium from the Fukushima Daiichi Nuclear Power Plant (FDNPP) accident was emitted as glassy, water-resistant caesium-bearing microparticles (CsMPs). Here, we isolated and investigated seven CsMPs from marine particulate matter and sediment. From the elemental composition, the 134 Cs/ 137 Cs activity ratio, and the 137 Cs activity per unit volume results, we inferred that the five CsMPs collected from particulate matter were emitted from Unit 2 of the FDNPP, whereas the two CsMPs collected from marine sediment were possibly emitted from Unit 3, as suggested by (i) the presence of calcium and absence of zinc and (ii) the direction of the atmospheric plume during the radionuclide emission event from Unit 3. The presence of CsMPs can cause overestimation of the solid–water distribution coefficient of Cs in marine sediments and particulate matter and a high apparent radiocaesium concentration factor for marine biota. CsMPs emitted from Unit 2, which were collected from the estuary of a river that flowed through a highly contaminated area, may have been deposited on land and then transported by the river. By contrast, CsMPs emitted from Unit 3 were possibly transported eastward by the wind and deposited directly onto the ocean surface.
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