期刊
SCIENCE OF THE TOTAL ENVIRONMENT
卷 447, 期 -, 页码 301-314出版社
ELSEVIER SCIENCE BV
DOI: 10.1016/j.scitotenv.2012.12.087
关键词
Radiocesium (Cs-137 and Cs-134); Fukushima Daiichi nuclear power plant; Rainfall; Relaxation length; Sequential extraction; Clay minerals
资金
- Ministry of Education, Culture, Sports, Science and Technology (MEXT)
Effect of intense rainfall on the distribution of Fukushima-accident-derived Cs-137 in soil was examined. Inventories and vertical distributions of Cs-137 in soils were determined at 15 locations (including croplands, grasslands, and forests) in Fukushima city in the post-rainy season, approximately 4.5 months after the accident, and were compared with those in the pre-rainy season determined in our former study. The Cs-137 inventory levels scarcely changed between points in time spanning the first rainy season after the accident. Moreover, the majority of Cs-137 remained stored in the aboveground vegetation and in the upper 5 cm of soil layer at undisturbed locations in the post-rainy season. A more quantitative analysis with the characterization of the vertical profile of Cs-137 using the relaxation length confirmed that the vertical profile was almost unchanged at most locations. Accordingly, it is concluded that rainfall during the rainy season had a limited effect on Cs-137 distribution in the soil, indicating the very low mobility. Chemical extraction of Cs-137 from selected soil samples indicated that Cs-137 in the soil was barely water soluble, and even the fraction extracted with I M ammonium acetate was only approximately 10%. This further supports the low mobility of Cs-137 in our soils. Soil mineralogical analyses, which included the identification of clay minerals, suggested that smectite and mica could lower the exchangeable fraction of Cs-137. However, no direct relationship was obtained between mineral composition and Cs-137 retention in the upper soil layer. In contrast, positive correlations were observed between Cs-137 extractability and soil properties such as pH, organic matter content, finer-sized particle content, and cation-exchange capacity. These results suggest that the mineralogical effect on the firm fixation of Cs-137 on soil constituents may be masked by the non-specific adsorption offered by the physicochemical properties of the soils. (C) 2013 Elsevier B.V. All rights reserved.
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