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从福岛第一核电站中提取的球形放射性含铯微颗粒中的铀和铯的同位素比值。

Isotopic ratios of uranium and caesium in spherical radioactive caesium-bearing microparticles derived from the Fukushima Dai-ichi Nuclear Power Plant.

机构信息

Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo (UT), 7-3-1 Hongo, Bunkyo-ku, Tokyo, 113-0033, Japan.

Ningyo-toge Environmental Engineering Centre, Japan Atomic Energy Agency (JAEA), 1550 Kamisaibara, Kagamino-cho, Tomata-gun, Okayama, 708-0698, Japan.

出版信息

Sci Rep. 2020 Feb 24;10(1):3281. doi: 10.1038/s41598-020-59933-0.

Abstract

Spherical radioactive caesium (Cs)-bearing microparticles (CsMPs) were emitted during the Fukushima Dai-ichi Nuclear Power Plant (FDNPP) accident in March, 2011. The emission source (timing) and formation process of these particles remain unclear. In this study, the isotopic ratios of uranium (U and U) and caesium (Cs, Cs, Cs, and Cs) isotopes in the five spherical CsMPs (ca. 2 μm in size) sampled at 50 km west of the FDNPP were determined using secondary ion mass spectrometry and laser ablation-ICPMS, respectively. Results showed that the U/U ratios of CsMPs were homogeneous (1.93 ± 0.03, N = 4) and close to those estimated for the fuel cores in units 2 and 3, and that the Cs isotopic ratios of CsMP were identical to those of units 2 and 3. These results indicated that U and Cs in the spherical CsMPs originated exclusively from the fuel melt in the reactors. Based on a thorough review of literatures related to the detailed atmospheric releases of radionuclides, the flow of plumes from the FDNPP reactor units during the accident and the U and Cs isotopic ratio results in this study, we hereby suggest that the spherical CsMPs originate only from the fuel in unit 2 on the night of 14 March to the morning of 15 March. The variation range of the analysed U/U isotopic ratios for the four spherical particles was extremely narrow. Thus, U may have been homogenised in the source through the formation of fuel melt, which ultimately evaporating and taken into CsMPs in the reactor and was released from the unit 2.

摘要

球形放射性铯(Cs)载入微球(CsMPs)于 2011 年 3 月福岛第一核电站(FDNPP)事故中释放。这些颗粒的排放源(时间)和形成过程仍不清楚。在这项研究中,使用二次离子质谱法和激光烧蚀 ICPMS 分别测定了取自 FDNPP 以西 50km 处的 5 个球形 CsMPs(约 2μm 大小)中铀(U 和 U)和铯(Cs、Cs、Cs 和 Cs)同位素的同位素比值。结果表明,CsMPs 的 U/U 比值均匀(1.93±0.03,N=4),接近 2 号和 3 号机组燃料芯块的估算值,并且 CsMP 的 Cs 同位素比值与 2 号和 3 号机组相同。这些结果表明,球形 CsMPs 中的 U 和 Cs 仅源自反应堆中的燃料熔融物。基于对与放射性核素详细大气释放相关的文献的全面回顾,事故期间 FDNPP 反应堆单元的羽流流动以及本研究中的 U 和 Cs 同位素比值结果,我们建议这些球形 CsMPs 仅源自 3 月 14 日夜间至 3 月 15 日早晨的 2 号机组的燃料。四个球形颗粒的分析 U/U 同位素比值的变化范围非常狭窄。因此,U 可能在源中通过燃料熔融物的形成而均匀化,最终蒸发并进入反应堆中的 CsMPs,并从 2 号机组中释放。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3b84/7039901/8a45c5e72379/41598_2020_59933_Fig1_HTML.jpg

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