Factors affecting vertical distribution of Fukushima accident-derived radiocesium in soil under different land-use conditions

被引:149
作者
Koarashi, Jun [1 ]
Atarashi-Andoh, Mariko [1 ]
Matsunaga, Takeshi [1 ]
Sato, Tsutomu [2 ]
Nagao, Seiya [3 ]
Nagai, Haruyasu [1 ]
机构
[1] Japan Atom Energy Agcy, Nucl Sci & Engn Directorate, Tokai, Ibaraki 3191195, Japan
[2] Hokkaido Univ, Grad Sch Engn, Div Sustainable Resources Engn, Sapporo, Hokkaido 0608628, Japan
[3] Kanazawa Univ, Inst Nat & Environm Technol, Low Level Radioact Lab, Kanazawa, Ishikawa 9231224, Japan
关键词
Radiocesium (Cs-137 and Cs-134); Fukushima Dai-ichi nuclear power plant; Vertical distribution; Soil physicochemical properties; Soil organic matter; Land-use types; PARTICLE-SIZE FRACTIONS; ORGANIC-MATTER; CHERNOBYL ACCIDENT; FOREST; CS-137; DYNAMICS; AVAILABILITY; ADSORPTION; RETENTION; MIGRATION;
D O I
10.1016/j.scitotenv.2012.05.041
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Fukushima Dai-ichi nuclear power plant accident in Japan, triggered by a big earthquake and the resulting tsunami on 11 March 2011, caused a substantial release of radiocesium (Cs-137 and Cs-134) and a subsequent contamination of soils in a range of terrestrial ecosystems. Identifying factors and processes affecting radiocesium retention in these soils is essential to predict how the deposited radiocesium will migrate through the soil profile and to other biological components. We investigated vertical distributions of radiocesium and physicochemical properties in soils (to 20 cm depth) at 15 locations under different land-use types (croplands, grasslands, and forests) within a 2 km x 2 km mesh area in Fukushima city. The total Cs-137 inventory deposited onto and into soil was similar (58.4 +/- 9.6 kBq m(-2)) between the three different land-use types. However, aboveground litter layer at the forest sites and herbaceous vegetation at the non-forested sites contributed differently to the total Cs-137 inventory. At the forest sites, 50-91% of the total inventory was observed in the litter layer. The aboveground vegetation contribution was in contrast smaller (<35%) at the other sites. Another remarkable difference was found in vertical distribution of Cs-137 in mineral soil layers: Cs-137 penetrated deeper in the forest soil profiles than in the non-forested soil profiles. We quantified Cs-137 retention at surface soil layers, and showed that higher Cs-137 retention can be explained in part by larger amounts of silt- and clay-sized particles in the layers. More importantly, the Cs-137 retention highly and negatively correlated with soil organic carbon content divided by clay content across all land-use types. The results suggest that organic matter inhibits strong adsorption of Cs-137 on clay minerals in surface soil layers, and as a result affects the vertical distribution and thus the mobility of Cs-137 in soil, particularly in the forest ecosystems. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:392 / 401
页数:10
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