首页> 外文期刊>Journal of Environmental Radioactivity >Variation in airborne Cs-134, Cs-137, particulate I-131 and Be-7 maximum activities at high-altitude European locations after the arrival of Fukushima-labeled air masses
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Variation in airborne Cs-134, Cs-137, particulate I-131 and Be-7 maximum activities at high-altitude European locations after the arrival of Fukushima-labeled air masses

机译:福岛标记的空气质量到达后,欧洲高空地区的机载Cs-134,Cs-137,I-131和Be-7颗粒最大活动量的变化

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The Fukushima-labeled air mass arrival, and later the cesium-134 (Cs-134), cesium-137 (Cs-137) and particulate iodine-131 (hereafter noted I-131(p)) maximum levels were registered in Europe at different dates depending on the location. Most of those data were obtained at low-altitude sampling areas. Here, we compare the airborne levels registered at different high-altitude European locations (from 850 m to about 3500 m). The integrated Cs-137 activity concentration was not uniform with, regard to the altitude even after a long travel time/distance from Japan. Moreover, the relation of integrated Cs-137 vs. altitude showed a linear decrease up to an altitude of about 3000 m. A similar trend was noticed for I-131(p) (particulate fraction) while it increased above 3000 m. Comparison with Be-7 activity concentration showed that, as far as the high altitude location is concerned, the Cs-137 and Cs-134 maximum concentrations corresponded to the 7Be maximum, suggesting downdraft movements from high tropospheric or stratospheric layers to be responsible for (CS)-C-137,134 increase and peak values. This was also confirmed by high potential vorticity and low relative humidity registered during the peak values. (C) 2016 Elsevier Ltd. All rights reserved.
机译:福岛标记的空气质量到达,后来在欧洲记录了铯134(Cs-134),铯137(Cs-137)和微粒碘131(以下称为I-131(p))的最大水平。不同的日期,取决于位置。这些数据大多数是在低空采样区获得的。在这里,我们比较了在欧洲不同高海拔位置(从850 m到约3500 m)所记录的空中水位。即使在距离日本很长的旅行时间/距离之后,关于海拔的综合Cs-137活性浓度也不均匀。此外,Cs-137积分与海拔的关系显示出线性下降,直至海拔约3000 m。当I-131(p)(颗粒分数)增加到3000 m以上时,也注意到了类似的趋势。与Be-7活性浓度的比较表明,就高海拔位置而言,Cs-137和Cs-134的最大浓度对应于7Be的最大值,表明来自高对流层或平流层的向下气流是造成( CS)-C-137,134的增加和峰值。峰值期间记录的高潜在涡度和低相对湿度也证实了这一点。 (C)2016 Elsevier Ltd.保留所有权利。

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