Depth profiles of radioactive cesium in soil using a scraper plate over a wide area surrounding the Fukushima Dai-ichi Nuclear Power Plant, Japan

被引:103
作者
Matsuda, Norihiro [1 ]
Mikami, Satoshi [1 ]
Shimoura, Susumu [2 ]
Takahashi, Junko [3 ]
Nakano, Masakazu [1 ]
Shimada, Kiyotaka [1 ]
Uno, Kiichiro [1 ]
Hagiwara, Shigetomo [1 ]
Saito, Kimiaki [1 ]
机构
[1] Japan Atom Energy Agcy, Chiyoda Ku, Tokyo 1008577, Japan
[2] Univ Tokyo, Ctr Nucl Study, Bunkyo Ku, Tokyo 1130033, Japan
[3] Univ Tsukuba, Ctr Res Isotopes & Environm Dynam, Tsukuba, Ibaraki 3058572, Japan
关键词
Depth profile; Radioactive; Cesium; Relaxation mass depth; EROSION RATES; MIGRATION; CS-137; RADIOCESIUM; CATCHMENTS; CHERNOBYL; CALABRIA;
D O I
10.1016/j.jenvrad.2014.10.001
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
During the Fukushima Dai-ichi Nuclear Power Plant (NPP) accident, radioactive cesium was released in the environment and deposited on the soils. Depth profiles of radioactive cesium in contaminated soils provide useful information not only for radiation protection and decontamination operations but also for geoscience and radioecology studies. Soil samples were collected using a scraper plate three times between December 2011 and December 2012 at 84 or 85 locations within a 100-km radius of the Fukushima Dai-ichi NPR In most of the obtained radioactive cesium depth profiles, it was possible to fit the concentration to a function of mass depth as either an exponential or hyperbolic secant function. By using those functions, following three parameters were estimated: (i) relaxation mass depth beta (g cm(-2)), (ii) effective relaxation mass depth beta(eff) (g cm(-2)), which is defined for a hyperbolic secant function as the relaxation mass depth of an equivalent exponential function giving the same air kerma rate at 1 m above the ground as the inventory, and (iii) 1/10 depth L-1/10 (cm), at which the soil contains 90% of the inventory. The average beta value (wet weight) including ones by hyperbolic secant function in December 2012, was 1.29 times higher than that in December 2011. In fact, it was observed that depth profiles at some study sites deviated from the typical exponential distributions over time. These results indicate the gradual downward migration of radioactive cesium in the soils. The L-1/10 values in December 2012 were summarized and presented on a map surrounding the Fukushima Dai-ichi NPP, and the average value of L-1/10 was 3.01 cm (n = 82) at this time. It was found that radioactive cesium remained within 5 cm of the ground surface at most study sites (71 sites). The sech function can also be used to estimate the downward migration rate V (kg m(-2) y(-1)). The V values in December 2012 (n = 25) were in good agreement with those found by a realistic approach using a diffusion and migration model. Almost all values ranged between 1.7 and 9.6 kg m(-2) y(-1) in this study. (C) 2014 The Authors. Published by Elsevier Ltd.
引用
收藏
页码:427 / 434
页数:8
相关论文
共 31 条
[1]   THE BEHAVIOR OF CHERNOBYL CS-137, CS-134 AND RU-106 IN UNDISTURBED SOIL - IMPLICATIONS FOR EXTERNAL RADIATION [J].
ANDERSSON, KG ;
ROED, J .
JOURNAL OF ENVIRONMENTAL RADIOACTIVITY, 1994, 22 (03) :183-196
[2]  
[Anonymous], 2006, WORLD SOIL RESOURCE
[3]  
[Anonymous], 2006, ENV CONSEQUENCES CHE
[4]   Changes with time in the migration of radiocesium in the soil, as observed near Chernobyl and in Germany, 1986-1994 [J].
Bunzl, K ;
Schimmack, W ;
Krouglov, SV ;
Alexakhin, RM .
SCIENCE OF THE TOTAL ENVIRONMENT, 1995, 175 (01) :49-56
[5]  
Burkart W., 2002, HDB ASSESSMENT SOIL, pvii
[6]  
DMCM (Decision by the Monitoring Coordination Meeting),, 2011, COMPR MON PLAN PROV
[7]  
Genuchten M.T., 1979, SOIL CHEM B, P349
[8]   The distribution of fallout Cs-137 and Pb-210 in undisturbed and cultivated soils [J].
He, Q ;
Walling, DE .
APPLIED RADIATION AND ISOTOPES, 1997, 48 (05) :677-690
[9]   In situ gamma-spectrometry several years after deposition of radiocesium .1. Approximation of depth distributions by the Lorentz function [J].
Hillmann, U ;
Schimmack, W ;
Jacob, P ;
Bunzl, K .
RADIATION AND ENVIRONMENTAL BIOPHYSICS, 1996, 35 (04) :297-303
[10]  
HND (Headquarters against Nuclear Disasters), 2011, ENF PLAN ENV MON