Discovery of radiocesium-bearing microparticles in river water and their influence on the solid-water distribution coefficient (Kd) of radiocesium in the Kuchibuto River in Fukushima
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- Miura Hikaru
- Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo
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- Kurihara Yuichi
- Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo
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- Sakaguchi Aya
- Center for Research in Isotopes and Environmental Dynamics, University of Tsukuba
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- Tanaka Kazuya
- Advanced Science Research Center, Japan Atomic Energy Agency
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- Yamaguchi Noriko
- Institute for Agro-Environmental Sciences, NARO
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- Higaki Shogo
- Isotope Science Center, The University of Tokyo
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- Takahashi Yoshio
- Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo
書誌事項
- タイトル別名
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- Discovery of radiocesium-bearing microparticles in river water and their influence on the solid-water distribution coefficient (<i>K</i><sub>d</sub>) of radiocesium in the Kuchibuto River in Fukushima
- Discovery of radiocesium-bearing microparticles in river water and their influence on the solid-water distribution coefficient (Kd) of radiocesium in the Kuchiboso River in Fukushima
- 公開日
- 2018
- 資源種別
- journal article
- DOI
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- 10.2343/geochemj.2.0517
- 公開者
- 一般社団法人日本地球化学会
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説明
<p>We found four radiocesium-bearing microparticles (CsMPs) with high cesium (Cs) radioactivity in suspended particles collected from the Kuchibuto River in Fukushima by filtering water during 2011–2016. The CsMPs were identified by autoradiography and subsequently were separated from other suspended particles by the “multiple wet separation method” using a NaI scintillation counter. The present four CsMPs contained 0.426–2.827 Bq of 137Cs and had a chemical composition similar to that of particles released during the accident at the Fukushima Daiichi Nuclear Power Plant (FDNPP). The activity ratio of Cs (134Cs/137Cs) suggests that they originated from Unit 2 or 3 of the FDNPP. The ratio of the radioactivity of the separated CsMPs to the total radiocesium on the filters ranged from 0 to 46%. Moreover, we calculated the radioactivities of CsMPs with lower radioactivity (0.1 to 0.4 Bq 137Cs) determined by autoradiography. When smaller CsMPs were included, the ratio of the radioactivity of the CsMPs to the total radioactivity of radiocesium on the filters ranged from 1.3 to 67%. It has been previously suggested that the solid-water distribution coefficient (Kd) of radiocesium in rivers is apparently increased due to the possible presence of CsMPs in the solid phase because the water solubility of radiocesium in CsMPs is small. However, this study reveals that higher Kd values in rivers in Fukushima compared with those in Chernobyl cannot be explained by the contribution of CsMPs alone. The temporal variation of the ratio of radioactivity of CsMPs to the total radioactivity of radiocesium in river water after the FDNPP accident is also discussed.</p>
収録刊行物
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- GEOCHEMICAL JOURNAL
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GEOCHEMICAL JOURNAL 52 (2), 145-154, 2018
一般社団法人日本地球化学会
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詳細情報 詳細情報について
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- CRID
- 1390282679528840448
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- NII論文ID
- 130006708588
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- NII書誌ID
- AA00654975
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- ISSN
- 18805973
- 00167002
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- NDL書誌ID
- 028933174
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- 本文言語コード
- en
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- 資料種別
- journal article
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