日本地球惑星科学連合2015年大会

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セッション記号 M (領域外・複数領域) » M-AG 応用地球科学

[M-AG38] 福島原発事故により放出された放射性核種の環境動態

2015年5月26日(火) 11:00 〜 12:45 301B (3F)

コンビーナ:*北 和之(茨城大学理学部)、恩田 裕一(筑波大学アイソトープ環境動態研究センター)、中島 映至(東京大学大気海洋研究所)、五十嵐 康人(気象研究所 環境・応用気象研究部)、山田 正俊(弘前大学被ばく医療総合研究所)、竹中 千里(名古屋大学大学院生命農学研究科)、山本 政儀(金沢大学環低レベル放射能実験施設)、篠原 厚(大阪大学理学系研究科)、座長:加藤 弘亮(筑波大学アイソトープ環境動態研究センター)

12:30 〜 12:45

[MAG38-14] 福島第一原発周辺で採取した土壌から分離した放射性微粒子の同定

*佐藤 志彦1末木 啓介1笹 公和1足立 光司2五十嵐 康人2 (1.筑波大学大学院数理物質科学研究科、2.気象研究所)

キーワード:福島第一原発事故, 放射性微粒子, 元素組成, 同位体比

The Fukushima Dai-ichi Nuclear Power Plant (FDNPP) disaster in 2011 discharged a large amount of radionuclides to the environment. Previous studies already disclosed the source term and inventory of radionuclides. However, physical and chemical states of radionuclides in the environment have yet to be revealed. Numerous environmental samples have been analyzed to investigate distribution of radionuclides by digital autoradiography using an imaging plate (IP). These studies pointed out that the spot-type contaminations were appeared and very common not only for the samples collected during the early stage (collecting until April 2011) of the FDNPP disaster but also for those collected later. In the FDNPP disaster, major forms of radioactive materials have been assumed to be gaseous. This is because the disaster underwent no reactor explosion nor fire of the reactor core, which is quite different from the situation in the Chernobyl NPP (ChNPP) disaster in 1986. In addition, it has been revealed that the emitted nuclear fuel (uranium) and 90Sr was very low. Therefore, elucidation of the cause of the spot-type contamination is crucial, which could contribute to know about physical and chemical state of radionuclides in the environment, as well as disclose their release processes from the FDNPP. Present study thus aiming at elucidation what makes the spot-type contamination in the IP analysis.
Surface soil samples were collected in the area about 20 km northwest from the FDNPP in June 2013. Spot-type contaminations were detected by IP analysis. Then, the radioactive particles were isolated by repeated sorting process and measured by the γ-spectroscopy with the high purity germanium semiconductor detector. The particles isolated were finally observed by SEM-EDS to determine the elemental composition and the morphology.
So far identified are four particles, and determined radionuclides by γ-spectroscopy were 134Cs and 137Cs. The morphology of the particles exhibited two types; spherical and fragmental. Thus, the spot-type contamination was characterized as due to such specific radioactive particles. The particles consist of Si, O, Zn, Fe, etc. and Cs (of which activity matched with the results by γ-spectroscopy) were also easily detected by SEM-EDS, suggesting glassy molten material. However, other fission products were not found in the particles. Tremendous amount of radioactive particles were collected around the ChNPP, and they were termed hot particle. Dominant components of the hot particle are nuclear fuel and typical fission products such as 90Sr, 153Eu as well as 134Cs and 137Cs. In contrast elemental composition of the present particles were dominated by Si. Uranium was found for only one of the present particles, but its concentration was very low and localized within the particle. In conclusion, characteristics of the present particles are quite different from the Chernobyl hot particles, but very similar to those reported for the particles isolated from HV filter samples in Tsukuba (Adachi et al., 2013, Abe et al., 2014).