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      Activity concentrations of environmental samples collected in Fukushima Prefecture immediately after the Fukushima nuclear accident

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          Abstract

          Radionuclide concentrations in environmental samples such as surface soils, plants and water were evaluated by high purity germanium detector measurements. The contribution rate of short half-life radionuclides such as 132I to the exposure dose to residents was discussed from the measured values. The highest values of the 131I/ 137Cs activity ratio ranged from 49 to 70 in the environmental samples collected at Iwaki City which is located to the south of the F1-NPS. On the other hand, the 132I/ 131I activity ratio in the same environmental samples had the lowest values, ranging from 0.01 to 0.02. By assuming that the 132I/ 131I activity ratio in the atmosphere was equal to the ratio in the environmental samples, the percent contribution to the thyroid equivalent dose by 132I was estimated to be less than 2%. Moreover, the contribution to the thyroid exposure by 132I might be negligible if 132I contamination was restricted to Iwaki City.

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          Thyroid doses for evacuees from the Fukushima nuclear accident

          A primary health concern among residents and evacuees in affected areas immediately after a nuclear accident is the internal exposure of the thyroid to radioiodine, particularly I-131, and subsequent thyroid cancer risk. In Japan, the natural disasters of the earthquake and tsunami in March 2011 destroyed an important function of the Fukushima Daiichi Nuclear Power Plant (F1-NPP) and a large amount of radioactive material was released to the environment. Here we report for the first time extensive measurements of the exposure to I-131 revealing I-131 activity in the thyroid of 46 out of the 62 residents and evacuees measured. The median thyroid equivalent dose was estimated to be 4.2 mSv and 3.5 mSv for children and adults, respectively, much smaller than the mean thyroid dose in the Chernobyl accident (490 mSv in evacuees). Maximum thyroid doses for children and adults were 23 mSv and 33 mSv, respectively.
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            Radioiodine and radiocesium in Thessaloniki, Northern Greece due to the Fukushima nuclear accident.

            Radioiodine ((131)I) in air and rainwater as high as 497 μBq m(-3) and 0.7 Bq L(-1), respectively, as well as (137)Cs and (134)Cs in air as high as 145 μBq m(-3) and 126 μBq m(-3), respectively were recorded in Thessaloniki, Northern Greece (40°38'N, 22°58'E) from March 24, 2011 through April 09, 2011, after a nuclear accident occurred at Fukushima, Japan (37°45'N, 140°28'E) on March 11, 2011. Copyright © 2011 Elsevier Ltd. All rights reserved.
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              Numerical reconstruction of high dose rate zones due to the Fukushima Dai-ichi Nuclear Power Plant accident.

              To understand how the high dose rate zones were created during the Fukushima Dai-ichi Nuclear Power Plant (FNPP1) accident on March 2011, the atmospheric dispersion of radionuclides during the period from 15 to 17 March was reproduced by using a computer-based nuclear emergency response system, WSPEEDI-II. With use of limited environmental monitoring data, prediction accuracy of meteorological and radiological fields by the system was improved to obtain best estimates of release rates, radiation dose maps, and plume movements. A large part of current high dose rate zones in Fukushima was explained by simulated surface deposition of radionuclides due to major releases of radionuclides on 15 March. In the simulation, the highest dose rate zones to the northwest of FNPP1 were created by a significant deposition of radionuclides discharged from FNPP1 during the afternoon. The results indicate that two environmental factors, i.e., rainfall and topography, strongly affected the spatial patterns of surface deposition of radionuclides. The wet deposition due to rainfall particularly played an important role in the formation of wide and heterogeneous distributions of high dose rate zones. The simulation also demonstrated that the radioactive plume flowed along the valleys to its leeward, which can expand the areas of a large amount of surface deposition in complex topography. Copyright © 2011 Elsevier Ltd. All rights reserved.
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                Author and article information

                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group
                2045-2322
                26 July 2013
                2013
                : 3
                : 2283
                Affiliations
                [1 ]Department of Radiological Life Sciences, Hirosaki University Graduate School of Health Sciences 66-1 Hon-cho , Hirosaki, Aomori 036-8564, Japan
                [2 ]Institute of Radiation Emergency Medicine, Hirosaki University 66-1 Hon-cho , Hirosaki, Aomori 036-8564, Japan
                [3 ]Department of Radioecology, Institute for Environmental Sciences 1-7 Ienomae , Obuchi, Rokkasho, Aomori 039-3212, Japan
                [4 ]Research Center for Radiation Protection, National Institute of Radiological Sciences 4-9-1 Anagawa , Inage, Chiba 263-8555, Japan
                [5 ]Institute of Radiochemistry and Radioecology, University of Pannonia Egyetem St. 10 , Veszprem, H-8200, Hungary
                Author notes
                Article
                srep02283
                10.1038/srep02283
                3724182
                23887080
                06c5f341-3d16-4572-9b12-e2557a9b20e0
                Copyright © 2013, Macmillan Publishers Limited. All rights reserved

                This work is licensed under a Creative Commons Attribution-NonCommercial-ShareALike 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/3.0/

                History
                : 04 July 2013
                : 09 July 2013
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