*Kazuhiko Ninomiya1, Kazuyuki Kita2, Atsushi Shinohara1, Kencho Kawatsu3, Haruka Minowa4, Nobufumi Fujita1, Tsutomu Ohtsuki5, Koichi Takamiya5, Yasushi Kino6, Kazuma Koarai6, Takashi Saito7, Yukihiko Satou8, Keisuke Sueki9, Yukio Takeuchi10, Taeko Doi10, Kazuhiko Chimura10, Yoshinari Abe11, Yuki Inai1, Yasuhiro Iwamoto12, Masaki Uesugi13, Satoru Endo14, Hiroshi Okochi12, Syoya Katsumi12, Kenya Kubo19, Yuya Koike15, Akinori Sueoka12, Masatoshi Suzuki6, Taketsugu Suzuki3, Tsugiko Takase3, Masaomi Takahashi1, zi jian zhang1, Izumi Nakai11, Seiya Nagao13, Yuichi Moriguchi16, Akiyo Yatagai17, Akihiko Yokoyama13, Go Yoshida18, Takashi Yoshimura1, Akira Watanabe3
(1.Osaka University, 2.Ibaraki University, 3.Fukushima University, 4.The Jikei University School of Medicine, 5.Kyoto University, 6.Tohoku University, 7.Shokei Gakuin University, 8.Japan Atomic Energy Agency, 9.Tsukuba University, 10.National Institute for Environmental Studies, 11.Tokyo University of Science, 12.Waseda University, 13.Kanazawa University, 14.Hiroshima University, 15.Meiji University, 16.The University of Tokyo, 17.Hirosaki University, 18.High Energy Accelerator Research Organization, 19.International Christian University)
Keywords:Fukushima Dai-ichi Nuclear Power Plant, Cs-137, Depth Profile
A large-scale soil sampling project for radionuclides from the accident of Fukushima Daiichi Nuclear Power Plant (FDNPP) was conducted in June 2011 by a research group on the Japan Geoscience Union and the Japan Society of Nuclear and Radiochemical Sciences. Five year later, a new research project was implemented with the objective to know the transition process of radioactivity and the current contamination in 2016. The air dose rate measurement and collection of soil samples for over 105 locations near the FDNPP was conducted [1], and 27 core soil samples were also obtained. In this presentation, we will show the results of depth-profiling of radioactive cesium concentration in the soil samples. The core soil samples were collected using the dedicated soil sampling tool with the depth of 20-30 cm. Each sample was divided into parts with every 2.5 cm depth at the sampling location and filled into polyethylene bag. After drying the soil samples in the room temperature, the soil samples was filled into a U-8 container, and radiocesium was quantified using gamma ray spectrometry with Ge detectors. At least one sample in each sampling location, long-time measurement was conducted to obtain radiocesium ratio (Cs-134/Cs-137). From the depth-profile of the soil, the radioactivities becomes to move deeper side with time passing. On the other hand, the medium concentration of depth was varied with the sampling point. The results were very consistent with the reported values obtained from the soil analysis up to 5 cm depth [1]. [1] K. Ninomiya et. al., Proceedings of the 13th Workshop on Environmental Radioactivity 2017-6 (2017) 31-34.