Fukushima radionuclides in the marine environment from coastal region of Japan to the Pacific Ocean through the end of 2016

M. Aoyama, Y. Inomata, D. Tsumune, Y. Tateda
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引用次数: 13

Abstract

The authors present total amount of released radiocaesium from FNPP1 accident which satisfy mass balance in all components of the environment. The authors also present consensus values of Fukushima Dai-ichi Nuclear Power Plant (FNPP1) derived 137Cs in the environment. Total amount of atmospheric release was 15-20 PBq and direct discharge to the ocean was 3-6 PBq, respectively. 12-15 PBq was deposited in the North Pacific and 3-6 PBq was deposited on land, respectively. Therefore 15-18 PBq was injected as sum of atmospheric deposition and direct discharge in the North Pacific Ocean. The authors also present temporal variation of 137Cs in coastal region close to FNPP1 site. Based on radiocaesium activity concentration and 134Cs/137Cs activity ratios decay corrected to 11 March 2011 in surface water, major source of radiocaesium is still FNPP1 site and contribution from global fallout 137Cs increased at Tomioka and Hasaki depending on the distances from FNPP1 site. A part of radiocaesium in the Sub Tropical Mode Water (STMW) in the Pacific Ocean is already obducted from ocean interior and enter into northern part of East China sea and in Japan Sea.
到2016年底,从日本沿海地区到太平洋的海洋环境中的福岛放射性核素
作者给出了FNPP1事故中满足环境各组分质量平衡的放射性铯释放总量。作者还提出了福岛第一核电站(FNPP1)环境中137Cs的共识值。大气释放总量为15 ~ 20 PBq,直接向海洋排放总量为3 ~ 6 PBq。12 ~ 15 PBq沉积于北太平洋,3 ~ 6 PBq沉积于陆地。因此,在北太平洋注入15-18 PBq作为大气沉降和直接排放的总和。作者还分析了靠近FNPP1站点的沿海地区137Cs的时间变化。根据2011年3月11日修正的地表水放射性铯活度浓度和134Cs/137Cs活度比衰减,放射性铯的主要来源仍然是FNPP1站点,富冈和Hasaki的全球沉降物137Cs的贡献随着与FNPP1站点的距离而增加。太平洋副热带模态海水(STMW)中的一部分放射性铯已经从海洋内部外溢进入东海北部和日本海。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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