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利用福岛第一核电站事故后陆地地区总累积沉降物估算 137Cs 和 131I 的大气释放量。

Backward Estimation of Atmospheric Release of 137Cs and 131I Using Total Cumulative Deposition in Terrestrial Areas Following the Fukushima Daiichi Nuclear Power Plant Accident.

机构信息

Japan Atomic Energy Agency (JAEA), 2-4 Shirakata, Tokai-mura, Naka-gun, Ibaraki 319-1195, Japan.

出版信息

Health Phys. 2021 Dec 1;121(6):587-596. doi: 10.1097/HP.0000000000001480.

DOI:10.1097/HP.0000000000001480
PMID:34570050
Abstract

The Fukushima Daiichi Nuclear Power Plant (FDNPP) accident caused a significant release of radionuclides into the environment. It is important to explore the timing and amount of radioactive release to terrestrial areas in order to clarify the consequences of the accident, including the dose received by the population living in the areas affected by the accident. In general, backward estimations are performed using air concentrations of radionuclides, but they are difficult to measure when radioactive plumes are passing through, and only spatially and temporally limited measurements are available. Therefore, a new method of backward estimation was developed based on the total cumulative deposition density, which can provide sufficient data in the environment by combining the atmospheric transport, dispersion, and deposition model calculations. Consequently, our estimations show that a major release of 137Cs and 131I occurred on 15, 20, 21, 22, 25, and 30 March 2011, after the accident. The amounts of release estimated by our new method for 137Cs and 131I were 4.9 × 1015 Bq and 120 × 1015 Bq, respectively. These results have no significant contradiction with the estimated results by the previous studies that were based on air concentrations and air dose rates that were measured in terrestrial areas. It was found that our new method is applicable for backward estimation oriented to the dose assessment for the people living in terrestrial areas.

摘要

福岛第一核电站(FDNPP)事故导致放射性核素大量释放到环境中。为了阐明事故的后果,包括受事故影响地区居民所受的剂量,探索放射性物质向陆地环境释放的时间和数量非常重要。通常,通过空气中放射性核素的浓度进行回溯估计,但在放射性烟云穿过时很难进行测量,并且只能获得空间和时间有限的测量结果。因此,基于总累积沉积密度开发了一种新的回溯估计方法,该方法可以通过结合大气传输、扩散和沉积模型计算,在环境中提供足够的数据。因此,我们的估计表明,在事故发生后的 2011 年 3 月 15 日、20 日、21 日、22 日、25 日和 30 日发生了 137Cs 和 131I 的主要释放。我们的新方法估计的 137Cs 和 131I 的释放量分别为 4.9×1015 Bq 和 120×1015 Bq。这些结果与基于空气中放射性核素浓度和陆地地区测量的空气剂量率的先前研究的估计结果没有明显矛盾。结果表明,我们的新方法适用于针对居住在陆地地区的人们的剂量评估的回溯估计。

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