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从福岛第一核电站附近采集的土壤样本中放射性铯微粒的分离、特性描述和来源分析。

Isolation, characterization and source analysis of radiocaesium micro-particles in soil sample collected from vicinity of Fukushima Dai-ichi nuclear power plant.

机构信息

Institute for Integrated Radiation and Nuclear Science, Kyoto University, Osaka, Japan.

Institute for Integrated Radiation and Nuclear Science, Kyoto University, Osaka, Japan; Egypt Second Research Reactor, Egyptian Atomic Energy Authority, Cairo, Egypt.

出版信息

J Environ Radioact. 2020 Nov;223-224:106388. doi: 10.1016/j.jenvrad.2020.106388. Epub 2020 Aug 29.

DOI:10.1016/j.jenvrad.2020.106388
PMID:32868095
Abstract

Radioactive caesium was released during the accident of Fukushima Dai-ichi nuclear power plant (FDNPP) into the surrounding environment. In the current work, radiocaesium micro-particles (CsMPs) and radiocaesium-rich soil particles were selectively separated from soil particles as well as from each other using autoradiography-based procedure. The applied separation scheme is based on water dilution followed by drying of the soil sample prior to imaging plate autoradiography. The SEM/EDS investigation of the individual CsMPs showed that these particles have a silicate glass structure and vary in shape with a diameter less than 10 μm. For the first time, a two-stage formation mechanism was suggested for a CsMP based on shape and structure heterogeneity of its two parts. Perfect spherical core might be formed in the first stage with a remarkable lower content of Al, and relatively higher concentrations of Si and K than an outer angulated structure, which might be attached to the core sphere during a late stage. The radiocaesium-rich soil particles have bigger size than CsMPs and have a plate-like structure with cleavages inside the grains, which suggest that these particles might be a weathered biotite. The average radioactivity ratio of Cs/Cs (dated March 11, 2011) in the investigated particles was found to be 1.05 ± 0.01, which confirmed that the radiocaesium in CsMPs and in the contaminated soil particles has the same source of origin, which could be unite 3 of FDNPP.

摘要

福岛第一核电站(FDNPP)事故期间,放射性铯释放到周围环境中。在当前的工作中,使用基于放射性自显影的程序,从土壤颗粒以及彼此之间选择性地分离放射性铯微颗粒(CsMPs)和富含放射性铯的土壤颗粒。所应用的分离方案基于水稀释,然后在成像板放射性自显影之前干燥土壤样品。对单个 CsMPs 的 SEM/EDS 研究表明,这些颗粒具有硅酸盐玻璃结构,形状各异,直径小于 10μm。首次提出了基于 CsMP 形状和结构异质性的两阶段形成机制。第一阶段可能形成完美的球形核心,其 Al 含量显著降低,Si 和 K 的浓度相对较高,而外部棱角结构可能在后期附着在核心球体上。富含放射性铯的土壤颗粒比 CsMPs 更大,具有板状结构,颗粒内部有劈裂,表明这些颗粒可能是风化的黑云母。在所研究的颗粒中,Cs/Cs(2011 年 3 月 11 日测定)的平均放射性比为 1.05±0.01,这证实了 CsMPs 和污染土壤颗粒中的放射性铯具有相同的起源,可能来自 FDNPP 的 3 号机组。

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