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重新构建并更新我们对全球武器试验中铯-137沉降物的认识。

Re-construction and updating our understanding on the global weapons tests 137Cs fallout.

作者信息

Aoyama Michio, Hirose Katsumi, Igarashi Yasuhito

机构信息

Geochemical Research Department, Meteorological Research Institute, 305-0052, Japan.

出版信息

J Environ Monit. 2006 Apr;8(4):431-8. doi: 10.1039/b512601k. Epub 2006 Mar 9.

Abstract

Global nuclear weapons tests fallout of 137Cs in the northern hemisphere has been documented in the UNSCEAR (United Nations Scientific Committee on the Effect of Atomic Radiation) reports. However, many questions have arisen during the past three to four decades; e.g. the water column inventory of 137Cs in the North Pacific Ocean was two to three time higher than the cumulative decay corrected fallout at the same latitude as stated in the UNSCEAR reports. Here we show more precise spatial distribution of global 137Cs fallout primarily on the basis of global measurements in rain, seawater and soil, as data from 10 degrees x 10 degrees grids. A typical feature of geographical distribution is that two high global 137Cs fallout areas exist in the northern hemisphere, where the highest 137Cs fallout was observed in the globe. These areas correspond to crossovers of areas where larger precipitation amounts were expected and where higher stratosphere-troposphere exchange was expected. Our new estimate of 765 +/- 79 PBq as global 137Cs fallout for the northern hemisphere is 1.4 times higher than that of 545 PBq in the UNSCEAR reports.

摘要

联合国原子辐射影响科学委员会(UNSCEAR)的报告记录了北半球全球核武器试验产生的137Cs沉降物。然而,在过去三四十年间出现了许多问题;例如,北太平洋137Cs的水柱存量比UNSCEAR报告中所述的同一纬度经累积衰变校正后的沉降物高出两到三倍。在此,我们主要基于全球范围内对雨水、海水和土壤的测量数据(以10度×10度网格数据为准),展示了全球137Cs沉降物更精确的空间分布。地理分布的一个典型特征是,北半球存在两个全球137Cs沉降物高值区,全球观测到的137Cs沉降物最高值出现在这些区域。这些区域对应于预期降水量较大以及平流层 - 对流层交换较高区域的交叉地带。我们对北半球全球137Cs沉降物的新估计值为765±79 PBq,比UNSCEAR报告中的545 PBq高出1.4倍。

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