Japan Geoscience Union Meeting 2015

Presentation information

Oral

Symbol M (Multidisciplinary and Interdisciplinary) » M-AG Applied Geosciences

[M-AG38] Dynamics of radionuclides emitted from Fukuchima Dai-ichi Nuclear Power Plant in the environment

Tue. May 26, 2015 11:00 AM - 12:45 PM 301B (3F)

Convener:*Kazuyuki Kita(Faculty of Science, Ibaraki University), Yuichi Onda(Center for Research on Isotopes and Environmental Dynamics, University of Tsukuba), Teruyuki Nakajima(Atmosphere and Ocean Research Institute), Yasuhito Igarashi(Atmospheric Environment and Applied Meteorology Research Department, Meteorological Research Institute), Masatoshi Yamada(Institute of Radiation Emergency Medicine, Hirosaki University), Chisato Takenaka(Graduate school of bioagricultural sciences, Nagoya University), masayoshi yamamoto(Low Level Radioactivity Laboratory, Kanazawa University), Atsushi Shinohara(Graduate school of science, Osaka University), Chair:Hiroaki Kato(Center for Research in Isotopes and Environmental Dynamics, University of Tsukuba)

12:30 PM - 12:45 PM

[MAG38-14] Identification of radioactive microparticles in the vicinity of the Fukushima Dai-ichi Nuclear Power Plant

*Yukihiko SATOU1, Keisuke SUEKI1, Kimikazu SASA1, Kouji ADACHI2, Yasuhito IGARASHI2 (1.Graduate School of Pure and Applied Sciences, University of Tsukuba, Japan, 2.Meteorological Research Institute, Japan)

Keywords:FDNPP disaster, Radioactive particle, Consist elements, Isotope ratio

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).