首页> 外文期刊>Journal of Environmental Radioactivity >The Cs-137 activity concentration of suspended and dissolved fractions in irrigation waters collected from the 80 km zone around TEPCO's Fukushima Daiichi Nuclear Power Station
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The Cs-137 activity concentration of suspended and dissolved fractions in irrigation waters collected from the 80 km zone around TEPCO's Fukushima Daiichi Nuclear Power Station

机译:东京电力公司福岛第一核电站周围80公里区域收集的灌溉水中悬浮和溶解部分的Cs-137活性浓度

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Fifty-four samples of irrigation water were collected in 2014 from agricultural ponds, rivers, and dams within the 80 km zone around TEPCO's Fukushima Daiichi Nuclear Power Station (FDNPS). The samples were filtered with a 0.45 gm pore-size membrane filter to produce suspended and dissolved fractions. The Cs-137 activity concentration of the suspended fraction varied from 1.5 to 300 Bq g(-1) dry weight and was significantly higher than that in the soil around each sampling site. The range of 137Cs activity concentrations in the dissolved fraction varied over three orders of magnitude at 0.0075-6.7 Bq I-1, which was a larger range than that of the suspended fraction; the higher values for samples were from within the 20 km zone. In the dissolved fraction 87 +/- 9% of the Cs-137 (n = 37) was in a monovalent cationic form (Cs+) and therefore potentially mobile. The distribution coefficient (Kd) ranged from 4100 to 2,100,000; the geometric mean value (110,000) was higher than that reported by the IAEA (2010). The geometric mean Kd of samples collected from the 20 km zone was 61,000 (n = 27), which was significantly lower than that collected from 20 to 80 km zone (200,000, n = 27). The Kd-value was negative correlated with the concentration of stable Cs-133 and the electric conductivity in the dissolved fraction. This shows relatively higher mobility of radiocaesium in irrigation waters may occur when there are higher contents of cations present. (c) 2017 Elsevier Ltd. All rights reserved.
机译:2014年,在东京电力公司福岛第一核电站(FDNPS)周围80公里区域内的农业池塘,河流和水坝中收集了五十四份灌溉水样本。用0.45 gm孔径的膜滤器过滤样品,以产生悬浮和溶解的馏分。悬浮部分的Cs-137活性浓度从1.5到300 Bq g(-1)干重变化,并且显着高于每个采样点周围土壤中的Cs-137活性浓度。溶解级分中137Cs活性浓度的范围在0.0075-6.7 Bq I-1范围内变化了三个数量级,这比悬浮级分的范围大。较高的样品值来自20 km区域内。在溶解的馏分中,Cs-137的87 +/- 9%(n = 37)为一价阳离子形式(Cs +),因此具有潜在的移动性。分配系数(Kd)在4100至2,100,000之间;几何平均值(110,000)高于国际原子能机构(2010)的报告。从20 km区域采集的样品的几何平均Kd为61,000(n = 27),大大低于从20至80 km区域采集的几何平均Kd(200,000,n = 27)。 Kd值与稳定Cs-133的浓度和溶解级分中的电导率呈负相关。这表明当存在更高含量的阳离子时,放射性铯在灌溉水中的迁移率可能相对较高。 (c)2017 Elsevier Ltd.保留所有权利。

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