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Remobilisation of radiocaesium from bottom sediments to water column in reservoirs in Fukushima, Japan.

Authors :
Funaki H
Tsuji H
Nakanishi T
Yoshimura K
Sakuma K
Hayashi S
Source :
The Science of the total environment [Sci Total Environ] 2022 Mar 15; Vol. 812, pp. 152534. Date of Electronic Publication: 2021 Dec 23.
Publication Year :
2022

Abstract

Reservoir sediments generally act as a sink for radionuclides derived from nuclear accidents, but under anaerobic conditions, several radionuclides remobilise in bioavailable form from sediments to water columns, which may contribute to the long-term contamination of aquatic products. This study systematically investigated the <superscript>137</superscript> Cs activities of sediment-pore water, providing a direct evidence of the remobilisation of bioavailable <superscript>137</superscript> Cs from sediments in two highly contaminated reservoirs affected by the Fukushima Dai-ichi Nuclear Power Plant (FDNPP) accident. We observed that the dissolved <superscript>137</superscript> Cs activity concentration of pore water (3.0-65.8 Bq L <superscript>-1</superscript> ) was one to two orders of magnitude higher than that of reservoir water. Moreover, the distribution coefficient (K <subscript>d</subscript> ) values for the <superscript>137</superscript> Cs of sediment-pore water (2.6-14 × 10 <superscript>3</superscript>  L kg <superscript>-1</superscript> ) decreased with depth. The K <subscript>d</subscript> values were significantly and negatively correlated with the concentration of the major <superscript>137</superscript> Cs competing cation NH <subscript>4</subscript> <superscript>+</superscript> . Our results strongly indicate a competitive ion exchange process between <superscript>137</superscript> Cs and NH <subscript>4</subscript> <superscript>+</superscript> via a highly selective interaction with the frayed edge sites of phyllosilicate minerals, which is the major reason for the variability of K <subscript>d</subscript> values of sediment-pore water, even in the Fukushima case. Additionally, the sediment accumulation rates were relatively high, and the annual depositional rate of exchangeable <superscript>137</superscript> Cs prevailed over the annual diffusive flux of <superscript>137</superscript> Cs from the sediment to the overlying water. This finding indicates that even after 10 years since the FDNPP accident, the bioavailable <superscript>137</superscript> Cs is still continuously supplied from the catchment covered by mountainous forests, and reservoir sediments are a long-term important source of bioavailable <superscript>137</superscript> Cs in the riverine system. Our findings provide important parameter values for mid- and long-term assessments of the radiation impact of radionuclide discharges to freshwater environments.<br />Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.<br /> (Copyright © 2021 Elsevier B.V. All rights reserved.)

Details

Language :
English
ISSN :
1879-1026
Volume :
812
Database :
MEDLINE
Journal :
The Science of the total environment
Publication Type :
Academic Journal
Accession number :
34954177
Full Text :
https://doi.org/10.1016/j.scitotenv.2021.152534