Long-term simulations of the 137Cs dispersion from the Fukushima accident in the world ocean

被引:86
作者
Nakano, Masanao [1 ]
Povinec, Pavel P. [2 ]
机构
[1] Japan Atom Energy Agcy, Tokai, Ibaraki 3191194, Japan
[2] Comenius Univ, Fac Math Phys & Informat, Dept Nucl Phys & Biophys, Bratislava 84248, Slovakia
关键词
Ocean general circulation model; LAMER; Fukushima accident; Marine modeling; Dose assessment; Pacific Ocean; WIND STRESS-FIELDS; CIRCULATION; RADIONUCLIDES; PACIFIC;
D O I
10.1016/j.jenvrad.2011.12.001
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The LAMER calculation code was used for simulation of the distribution of Cs-137 released after the Fukushima accident into the Pacific and Indian Oceans. The maximum Cs-137 concentration predicted for surface waters of the open NW Pacific Ocean in 2012 (21 Bq/m(3) at 38 degrees N, 164 degrees E) will be comparable to that observed during the early 1960s after atmospheric nuclear weapons tests. The Cs-137 in surface waters of the Pacific Ocean will reach the US coast 4-5 y after the accident, however, the levels will be low (<3 Bq/m(3)). All the North Pacific Ocean will be labeled with Fukushima Cs-137 10 y after the accident with concentrations below 1 Bq/m(3). Thirty years after the accident the Cs-137 levels in the Pacific and Indian Oceans will be below 0.1 Bq/m(3), i.e. undetectable on the present global fallout background. The effective dose commitment with ingestion of marine biota found in 2012 in the open NW Pacific Ocean was estimated to be 1.7 mu Sv/y, mostly delivered by Cs-134,Cs-137. The estimated dose is by about a factor of 500 lower than the present dose limit for the public. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:109 / 115
页数:7
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