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福岛第一核电站事故后波兰中部上空的气溶胶停留时间以及放射性碘 - 131I 和放射性铯 - 137Cs 活度的变化

Aerosol residence times and changes in radioiodine-131I and radiocaesium-137 Cs activity over Central Poland after the Fukushima-Daiichi Nuclear reactor accident.

作者信息

Długosz-Lisiecka Magdalena, Bem Henryk

机构信息

Technical University of Lodz, Zeromskiego Street 116, 90-024 Lodz, Poland.

出版信息

J Environ Monit. 2012 May;14(5):1483-9. doi: 10.1039/c2em00014h. Epub 2012 Apr 5.

Abstract

The first detectable activities of radioiodine (131)I, and radiocaesium (134)Cs and (137)Cs in the air over Central Poland were measured in dust samples collected by the ASS-500 station in the period of 21(st) to 24(th) of March, 2011. However, the highest activity of both fission products, (131)I and (137)Cs: 8.3 mBq m(-3) and 0.75 mBq m(-3), respectively, were obtained in the samples collected on 30(th) March, i.e.∼18 days after the beginning of the fission products' discharge from the damaged units of the Fukushima Daiichi Nuclear Power Plant. The simultaneously determined corrected aerosol residence time for the same samples by (210)Pb/(210)Bi and (210)Pb/(210)Po methods was equal to 10 days. Additionally, on the basis of the activity ratio of two other natural cosmogenic radionuclides, (7)Be and (22)Na in these aerosol samples, it was possible to estimate the aerosol residence time at ∼150 days for the solid particles coming from the stratospheric fallout. These data, as well as the differences in the activity size distribution of (7)Be and (131)I in the air particulate matter, show, in contrast to the Chernobyl discharge, a negligible input of stratospheric transport of Fukushima-released fission products.

摘要

2011年3月21日至24日期间,通过ASS - 500监测站收集的灰尘样本,测定了波兰中部空气中首次可检测到的放射性碘(131)I、放射性铯(134)Cs和(137)Cs的活度。然而,两种裂变产物(131)I和(137)Cs的最高活度分别为8.3 mBq m(-3)和0.75 mBq m(-3),是在3月30日采集的样本中测得的,即福岛第一核电站受损机组开始排放裂变产物约18天后。通过(210)Pb/(210)Bi和(210)Pb/(210)Po方法同时测定的同一样本的校正气溶胶停留时间为10天。此外,根据这些气溶胶样本中另外两种天然宇宙成因放射性核素(7)Be和(22)Na的活度比,有可能估计平流层沉降的固体颗粒的气溶胶停留时间约为150天。与切尔诺贝利核事故排放情况相比,这些数据以及空气中颗粒物中(7)Be和(131)I活度大小分布的差异表明,福岛释放的裂变产物平流层传输的输入量可忽略不计。

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