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2014年7月朝鲜半岛西部和南部海域镭-226、镭-228、铯-134和铯-137浓度的空间变化。

Spatial variations of Ra, Ra, Cs, and Cs concentrations in western and southern waters off the Korean Peninsula in July 2014.

作者信息

Inoue M, Shirotani Y, Nagao S, Aramaki T, Kim Y I, Hayakawa K

机构信息

Institute of Nature and Environmental Technology, Kanazawa University, Nomi, Ishikawa 923-1224, Japan.

Institute of Nature and Environmental Technology, Kanazawa University, Nomi, Ishikawa 923-1224, Japan.

出版信息

J Environ Radioact. 2018 Feb;182:151-156. doi: 10.1016/j.jenvrad.2017.11.020. Epub 2017 Dec 8.

Abstract

We examined the spatial distributions of Ra, Ra, Cs, and Cs concentrations (activities) in seawater off the western and southern Korean Peninsula in July 2014. Radium-228 (and Ra) concentrations in water samples varied widely from 5 to 14 mBq/L (2-4 mBq/L), showing a negative correlation with salinity, particularly at the surface off the western Korean Peninsula. This indicates that the seawaters in this area are fundamentally comprised of Ra-poor and high-saline Kuroshio Current water and Ra-rich and low-saline water (e.g., continental shelf water), with various mixing ratios. Although Fukushima Dai-ichi Nuclear Power Plant (FDNPP)-derived Cs was below the detection limit (<0.08 mBq/L) in waters off the western Korean Peninsula, low level Cs (0.1-0.2 mBq/L) was detected in waters off the southern Korean Peninsula accompanied by higher Cs concentrations (1.6-1.9 mBq/L) relative to that off the western Korean Peninsula. Combined with the lower radium concentrations, the detection of Cs is explained by mixing of FDNPP-derived radiocesium-contaminated Kuroshio Current water.

摘要

2014年7月,我们对朝鲜半岛西部和南部海域海水中镭-228、镭-226、铯-137和铯-134的浓度(活度)空间分布进行了研究。水样中镭-228(和镭-226)的浓度变化范围很大,为5至14毫贝克勒尔/升(2至4毫贝克勒尔/升),与盐度呈负相关,特别是在朝鲜半岛西部近海表层。这表明该区域海水基本上由贫镭且高盐的黑潮海水以及富镭且低盐的水(如大陆架水)以不同混合比例组成。尽管朝鲜半岛西部海域来自福岛第一核电站(FDNPP)的铯低于检测限(<0.08毫贝克勒尔/升),但在朝鲜半岛南部海域检测到了低水平的铯(0.1至0.2毫贝克勒尔/升),且相对于朝鲜半岛西部海域,其铯浓度更高(1.6至1.9毫贝克勒尔/升)。结合较低的镭浓度,铯的检测结果可以用受FDNPP污染的含放射性铯的黑潮海水混合来解释。

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