Changes in radioactive cesium concentrations from 2011 to 2017 in Fukushima coastal sediments and relative contributions of radioactive cesium-bearing microparticles

Sedimentary cesium-137 concentrations around the Fukushima Daiichi Nuclear Power Plant (FDNPP) were measured from 2011 to 2017 at eight stations. Although high values were observed until 2013, decreasing trends were observed at the surface sediments of seven stations. We isolated 25 radioactive Cs-b...

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Veröffentlicht in:Marine pollution bulletin 2020-12, Vol.161 (Pt B), p.111769, Article 111769
Hauptverfasser: Kubo, Atsushi, Tanabe, Kai, Ito, Yukari, Ishimaru, Takashi, Otsuki, Mayumi, Arakawa, Hisayuki, Watanabe, Yutaka W., Miura, Hikaru, Tsumune, Daisuke, Kanda, Jota
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Sprache:eng
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Zusammenfassung:Sedimentary cesium-137 concentrations around the Fukushima Daiichi Nuclear Power Plant (FDNPP) were measured from 2011 to 2017 at eight stations. Although high values were observed until 2013, decreasing trends were observed at the surface sediments of seven stations. We isolated 25 radioactive Cs-bearing microparticles (CsMPs; 1.0–5385 Bq per particle). The contribution ratio of CsMPs to each sample ranged from 4.1% to 99.5% (median 58.8%), with the contribution ratio of the CsMPs in the southern part of the FDNPP was low compared to that from the northern part. In the southern part of the FDNPP, small CsMPs that could not be isolated in this study were present in large quantities immediately after the accident, and gradually diffused away and/or were dissolved over time. In contrast, the CsMPs in the northern part of the FDNPP have most likely accumulated over time, as suggested by the silty nature of the sediments there. •Sedimentary 137Cs concentrations around FDNPP were measured from 2011 to 2017.•We isolated 25 CsMPs (1.0–5385 Bq per particle) in the sediment samples.•The contribution ratio of CsMPs to each sample ranged from 4.1 to 99.5%.•These at the southern part of FDNPP were low relative to the northern part.•The source of CsMPs was derived from Unit3.
ISSN:0025-326X
1879-3363
DOI:10.1016/j.marpolbul.2020.111769