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[周一午餐交流会]第二十八讲:应用新的地球化学示踪剂识别福岛核事故释放的钚和铯及其长期的环境行为

发布时间:2015/01/13     浏览次数:
时间:2015-1-19 (星期一) 11:40-13:30(12:20开讲)
地点:周隆泉楼一楼多功能厅
主讲人:郑建研究员 Prof.
来访单位:Research Center for Radiation Protection, National Institute of Radiological Sciences,日本 Japan
邀请人:MEL周午餐会
联系人:施薇

下周一的午餐交流会,将由戴民汉老师邀请的,来自日本国立放射线医学综合研究所的郑建研究员主讲。详情如下:

主题:第二十八讲——New geochemical tracers for source identification and long-term environmental behavior studies of plutonium and radiocesium released from the Fukushima nuclear accident新地球化学示踪方法研究福岛核事故释放的放射性钚和铯的源识别和长期环境行为

主讲人:Prof. Jian Zheng, Research Center for Radiation Protection, National Institute of Radiological Sciences

时间:2014119日(星期一)11:40-13:3012:20开讲)

地点:周隆泉楼一楼多功能厅

郑建老师个人简历请见附件。

讲座摘要:The Fukushima Daiichi Nuclear Power Plant (FDNPP) accident released large amounts of radionuclides into the environment. In addition to the atmospheric releases, the release of highly contaminated water from the damaged reactor buildings resulted in the direct discharges of radionuclides into the sea. It has been estimated that the total amount of 137Cs released from the FDNPP accident to the atmosphere ranged from 15-35 PBq. For the refractory actinides, although in a tiny amount, the release of Pu isotopes has been detected in various environmental samples, such as soil, litter, aerosol, black substance and river sediment. The released radioactive materials posed radiation threat to human society. Thus, source identification of radioactive contamination and long-term environmental behavior of released radioactive materials are important issues of study after the FDNPP accident.

Since the FDNPP accident, intensive studies on the distribution of released fission products, in particular 134Cs and 137Cs, in the environment have been conducted, and the activity ratio of 134Cs/ 137Cs has been widely used as a tracer for contamination source identification. However, due to the short half-life of 134Cs (2.06 y), this tracer will become unavailable in the near future. Thus, for long-term environmental behavior studies of the released radionuclides, new tracers which can be used in a time scale of several tens-years or hundred years are highly required. In this work, we discuss new geochemical tracers, such as Pu isotope ratios (240Pu / 239Pu and 241Pu/239Pu) and radioactive Cs isotope ratios (135Cs/137Cs and 135Cs/ 133Cs) for contamination source identification and long-term environmental studies of Pu and Cs released from the FDNPP accident. To establish the feasibility of the proposed tracers, we identified the isotopic compositions of radioactive Cs and Pu isotopes released from the FDNPP accident, and estimated the released amounts of 135Cs and Pu isotopes. The potential applications of the obtained FDNPP-sourced Cs and Pu fingerprints in the study of long-term environmental behavior of the released radioactive materials will be discussed.

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