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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Radionuclide pollution inside the Fukushima Daiichi exclusion zone, part 2: Forensic search for the 'Forgotten' contaminants Uranium-236 and plutonium
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Radionuclide pollution inside the Fukushima Daiichi exclusion zone, part 2: Forensic search for the 'Forgotten' contaminants Uranium-236 and plutonium

机译:放射性核素污染在福岛Daiichi排除区内,第2部分:法医检索“被遗忘的”污染物铀-236和钚

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In the course of the Fukushima Daiichi nuclear accident (March 2011), large quantities of radionuclides, mainly of the volatile elements such as cesium and iodine were released to the environment. In small amounts non-volatile elements such as plutonium and uranium have also been released. For this study vegetation, litter and soil drill core samples were taken in 2013 and 2015 in the contaminated area in Fukushima prefecture. In 2015 the samples were taken as close to the sampling locations of the 2013 campaign as possible. To investigate the origin of plutonium and uranium the isotopic ratios Pu-240/Pu-239 and U-236/U-238 were measured using accelerator mass spectrometry. While the determined Pu-240/Pu-239 ratios indicate global fallout as the plutonium source for most samples, reactor plutonium of the reactors of Fukushima Daiichi is identified unambiguously in some vegetation and litter samples. This assumption is corroborated by the detection of U-236. None of the samples contained higher plutonium activity concentrations than in the rest of Japan, caused by global fallout. This holds even for the samples where the reactors were identified as the source from the isotope ratios. This and the strong localization, even for neighboring sampling sites, indicate that the overall small quantities of plutonium were most likely released in the form of particulate matter. (C) 2017 Elsevier Ltd. All rights reserved.
机译:在福岛Daiichi核事故(2011年3月)的过程中,大量放射性核素,主要是挥发性元素如铯和碘被释放到环境中。在少量的情况下,也释放了钚和铀等非挥发性元素。对于这项研究,植被,垃圾和土壤钻孔核心样本于2013年和2015年在福岛县的污染区域进行。 2015年,按照尽可能靠近2013年活动的采样地点进行样品。为了研究钚和铀的起源,使用促进剂质谱法测量同位素率PU-240 / PU-239和U-236 / U-238。虽然确定的PU-240 / PU-239比率表明全球辐射作为大多数样品的钚源,但福岛Daiichi反应器的反应堆钚在一些植被和垃圾样本中明确鉴定。通过检测U-236来证实该假设。没有一个样品含有比全球辐射的其他地区更高的钚活动浓度浓度高于日本其余的浓度。即使对于从同位素比被鉴定为源的样品,也保持了反应器的样品。即使是相邻的抽样网站,这也是强烈的本地化表明整体少量钚最容易以颗粒物质的形式释放。 (c)2017 Elsevier Ltd.保留所有权利。

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