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亚洲沙尘对放射性铯(¹³⁷Cs)大气沉降的贡献。

Contribution of Asian dust to atmospheric deposition of radioactive cesium ((137)Cs).

作者信息

Fukuyama Taijiro, Fujiwara Hideshi

机构信息

National Institute for Agro-Environmental Sciences, Tsukuba, Ibaraki, Japan.

出版信息

Sci Total Environ. 2008 Nov 1;405(1-3):389-95. doi: 10.1016/j.scitotenv.2008.06.037. Epub 2008 Aug 8.

Abstract

Both Asian dust (kosa) transported from the East Asian continent and locally suspended dust near monitoring sites contribute to the observed atmospheric deposition of (137)Cs in Japan. To estimate the relative contribution of these dust phenomena to the total (137)Cs deposition, we monitored weekly deposition of mineral particles and (137)Cs in spring. Deposition of (137)Cs from a single Asian dust event was 62.3 mBq m(-2) and accounted for 67% of the total (137)Cs deposition during the entire monitoring period. Furthermore, we found high (137)Cs specific activity in the Asian dust deposition sample. Although local dust events contributed to (137)Cs deposition, their contribution was considerably smaller than that of Asian dust. We conclude that the primary source of atmospheric (137)Cs in Japan is dust transported from the East Asian continent.

摘要

从东亚大陆输送来的亚洲沙尘(黄沙)以及监测站点附近的本地悬浮沙尘,都对日本观测到的大气中(137)铯的沉降有所贡献。为估算这些沙尘现象对总(137)铯沉降的相对贡献,我们在春季每周监测矿物颗粒和(137)铯的沉降情况。单次亚洲沙尘事件造成的(137)铯沉降为62.3毫贝克勒尔每平方米,占整个监测期总(137)铯沉降的67%。此外,我们在亚洲沙尘沉降样本中发现了高(137)铯比活度。尽管本地沙尘事件对(137)铯沉降有贡献,但其贡献远小于亚洲沙尘。我们得出结论,日本大气中(137)铯的主要来源是从东亚大陆输送来的沙尘。

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