@misc{oai:repo.qst.go.jp:00071489,
 author = {青野, 辰雄 and 福田, 美保 and 吉田, 聡 and SOHTOME, Tadahiro and MIZUNO, Takuji and IGARASHI, Satoshi and ITO, Yukari and KANDA, Jota and ISHIMARU, Takashi and 青野 辰雄 and 福田 美保 and 吉田 聡},
 month = {Sep},
 note = {The accident of TEPCO's Fukushima Daiichi Nuclear Power Station (FDNPS) has caused the release of the huge quantities of radionuclide by the 2011 Great East Japan Earthquake and Tsunami, and then the serious problems gave rise to pollution in marine environment widely in the coast area off Fukushima. Monitoring of radioactivity in seawater and biota are important for understanding the dispersion of radionuclides and the effects of radioecology in the marine environment around the coast of Fukushima and the Pacific. The activities of Cs-134 and Cs-137 in seawater decreased exponentially and then were almost same levels before the accident around off Fukushima after about three years from the accident. However, the high activities of radio casesium(Cs) have been monitored in marine biota off Fukushima. The aims of the present study were to examine the temporal changes in radioactivity and to clarify the variation factor and the effect of radioecology in marine biota. Cs-134 and Cs-137, and Ag-110m, were released by this accident, determined in biota sample such as the plankton, fish and benthos, although it is well-known that mollusca and crustacea concentrate silver in visceral parts. However, Sr-90 was not detected and the activities of plutonium were almost same level before this accident in the marine biota around off Fukushima. Concentration ratios of Cs (CR-Cs) in marine organism were from 2.6E+1 in the muscle part of squid to 1.0E+4 in the viscera of clam. The large differences in CR-Cs by the parts of marine organism were not observed. It is suggested that rapid change in the activities of radio Cs and silver in seawater, resuspension of particles from sediments and food chain effects led to high radionuclide activities in marine biota after this accident. CR-Cs in plankton was also calculated with the activities in seawater, which were collected around sampling area during this monitoring period. These resulting values ranged from 5.8E+1 to 7.8E+2, were higher than the CR-Cs values (2.0E+1~4.0E+1) and also similar with the Cs-Kd value in TRS-422. It was considered that the CR fluctuations in plankton were not only the activities in seawater, but also the sediment resuspension., ICRER 2014 - Third International Conference on Radioecology and Environmental Radioactivity},
 title = {Activities of radionuclides in the coast area off Fukushima after TEPCO's Fukushima Daiichi Nuclear Power Station accident},
 year = {2014}
}