Distribution of radionuclides in surface seawater obtained by an aerial radiological survey

被引:11
作者
Inomata, Yayoi [1 ]
Aoyama, Michio [2 ]
Hirose, Katsumi [3 ]
Sanada, Yukihisa [4 ]
Torii, Tatsuo [4 ]
Tsubono, Takaki [5 ]
Tsumune, Daisuke [5 ]
Yamada, Masatoshi [6 ]
机构
[1] Asia Ctr Air Pollut Res, Nishi Ku, Niigata 9512144, Japan
[2] Meteorol Res Inst, Tsukuba, Ibaraki 3050052, Japan
[3] Sophia Univ, Fac Sci & Technol, Chiyoda Ku, Tokyo 1018554, Japan
[4] Japan Atom Energy Agcy, Chiyoda Ku, Tokyo 1008577, Japan
[5] Cent Res Inst Elect Power Ind, Abiko, Chiba 2701194, Japan
[6] Hirosaki Univ, Grad Sch Hlth Sci, Hirosaki, Aomori 0368564, Japan
关键词
aerial radiological survey; gamma-ray count rates; radionuclides; surface seawater; nuclear accidents; model simulation; CS-137; INTERPOLATION; SYSTEM;
D O I
10.1080/00223131.2014.914451
中图分类号
TL [原子能技术]; O571 [原子核物理学];
学科分类号
0827 ; 082701 ;
摘要
We investigated the distribution in seawater of anthropogenic radionuclides from the Fukushima Daiichi Nuclear Power Plant (FNPP1) as preliminary attempt using a rapid aerial radiological survey performed by the U. S. Department of Energy National Nuclear Security Administration on 18 April 2011. We found strong correlations between in-situ activities of I-131, Cs-134, and Cs-137 measured in surface seawater samples and gamma-ray peak count rates determined by the aerial survey (correlation coefficients were 0.89 for I-131, 0.96 for(134)Cs, and 0.92 for(137)Cs). The offshore area of high radionuclide activity extended south and southeast from the FNPP1. The maximum activities of I-131, Cs-134, and Cs-137 were 329, 650, and 599 Bq L-1, respectively. The I-131/Cs-137 ratio in surface water of the high-activity area ranged from 0.6 to 0.7. Considering the radioactive decay of I-131 (half-life 8.02 d), we determined that the radionuclides in this area were directly released from FNPP1 to the ocean. We confirm that aerial radiological surveys can be effective for investigating the surface distribution of anthropogenic radionuclides in seawater. Our model reproduced the distribution pattern of radionuclides derived from the FNPP1, although results simulated by a regional ocean model were underestimated.
引用
收藏
页码:1059 / 1063
页数:5
相关论文
共 12 条
[2]   Surface pathway of radioactive plume of TEPCO Fukushima NPP1 released 134Cs and 137Cs [J].
Aoyama, M. ;
Uematsu, M. ;
Tsumune, D. ;
Hamajima, Y. .
BIOGEOSCIENCES, 2013, 10 (05) :3067-3078
[3]   Assessment of the amount of cesium-137 released into the Pacific Ocean after the Fukushima accident and analysis of its dispersion in Japanese coastal waters [J].
Estournel, C. ;
Bosc, E. ;
Bocquet, M. ;
Ulses, C. ;
Marsaleix, P. ;
Winiarek, V. ;
Osvath, I. ;
Nguyen, C. ;
Duhaut, T. ;
Lyard, F. ;
Michaud, H. ;
Auclair, F. .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2012, 117
[4]   Optimum interpolation analysis of basin-scale 137Cs transport in surface seawater in the North Pacific Ocean [J].
Inomata, Y. ;
Aoyama, M. ;
Tsumune, D. ;
Motoi, T. ;
Nakano, H. .
JOURNAL OF ENVIRONMENTAL MONITORING, 2012, 14 (12) :3146-3155
[5]   AERIAL MEASURING SYSTEM IN JAPAN [J].
Lyons, Craig ;
Colton, David .
HEALTH PHYSICS, 2012, 102 (05) :509-515
[6]  
Ministry of Education Culture Sports Science and Technology Japan, 1993, GAMM RAY SPECTR GERM
[7]   US DOE'S RESPONSE TO THE FUKUSHIMA DAIICHI REACTOR ACCIDENT: ANSWERS AND DATA PRODUCTS FOR DECISION MAKERS [J].
Reed, Alexis L. .
HEALTH PHYSICS, 2012, 102 (05) :557-562
[8]   The regional oceanic modeling system (ROMS): a split-explicit, free-surface, topography-following-coordinate oceanic model [J].
Shchepetkin, AF ;
McWilliams, JC .
OCEAN MODELLING, 2005, 9 (04) :347-404
[9]  
Torii T., 2012, J ATOM ENERGY SOC JP, V54, P160, DOI [10.3327/jaesjb.54.3_160, DOI 10.3327/JAESJB.54.3_160]
[10]   ENHANCED ANALYSIS METHODS TO DERIVE THE SPATIAL DISTRIBUTION OF 131I DEPOSITION ON THE GROUND BY AIRBORNE SURVEYS AT AN EARLY STAGE AFTER THE FUKUSHIMA DAIICHI NUCLEAR POWER PLANT ACCIDENT [J].
Torii, Tatsuo ;
Sugita, Takeshi ;
Okada, Colin E. ;
Reed, Michael S. ;
Blumenthal, Daniel J. .
HEALTH PHYSICS, 2013, 105 (02) :192-200