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福岛第一核电站事故期间氚向大气释放的建模及其在估算事故后水系统传输时间中的应用。

Modeling tritium release to the atmosphere during the Fukushima Daiichi Nuclear Power Plant accident and application to estimating post-accident water system transit times.

作者信息

Cauquoin Alexandre, Gusyev Maksym, Bong Hayoung, Okazaki Atsushi, Yoshimura Kei

机构信息

Institute of Industrial Science (IIS), The University of Tokyo, 5-1-5 Kashiwanoha, Kashiwa City, 277-8575, Chiba, Japan.

Institute of Environmental Radioactivity (IER), Fukushima University, 1 Kanayagawa, Fukushima City, 960-1296, Fukushima, Japan.

出版信息

Environ Sci Pollut Res Int. 2025 Feb;32(7):3649-3663. doi: 10.1007/s11356-025-35919-1. Epub 2025 Jan 16.

Abstract

During the Fukushima Daiichi Nuclear Power Plant (FDNPP) accident on March 11, 2011, radionuclides such as tritium were released into the environment across Japan, obscuring the natural background signal of tritium in precipitation. This anthropogenic component was rapidly washed out by precipitation according to measurements in Japan. However, the impact of the accident on the natural tritium-based estimation of water system transit times in Fukushima and other prefectures in Japan remains uncertain. For the first time, anthropogenic tritium from the FDNPP accident together with natural tritium were simulated in an atmospheric general circulation model with a good ability to represent tritium variations in daily and monthly precipitation. For the FDNPP accident, we estimate the maximum tritium atmospheric emission of 0.815 PBq with a tritium in precipitation peak of 68.7 Bq/L (582 tritium units) on March 2011 at Fukushima, which are consistent with previous estimations. Using our modeled outputs with tritium measurements, we improve tritium-tracer application for estimating mean transit times of Fukushima surface and groundwater systems impacted by the anthropogenic tritium from the FDNPP accident. While the anthropogenic impact of the FDNPP accident was limited compared to the tritium peak due to the thermonuclear testing, globally modeled tritium in precipitation is useful to apply for other areas of tritium-tracer studies.

摘要

在2011年3月11日福岛第一核电站事故期间,氚等放射性核素在日本各地释放到环境中,掩盖了降水中氚的自然本底信号。根据日本的测量,这种人为成分很快被降水冲刷掉。然而,该事故对日本福岛及其他县基于天然氚的水系统过境时间估算的影响仍不确定。首次在一个能够很好地反映日降水和月降水中氚变化的大气环流模型中,对福岛第一核电站事故产生的人为氚和天然氚进行了模拟。对于福岛第一核电站事故,我们估计最大氚大气排放量为0.815 PBq,2011年3月福岛降水中氚峰值为68.7 Bq/L(582个氚单位),这与先前的估计一致。利用我们模拟的输出结果和氚测量数据,我们改进了氚示踪剂在估算受福岛第一核电站事故人为氚影响的福岛地表水和地下水系统平均过境时间方面的应用。虽然与热核试验导致的氚峰值相比,福岛第一核电站事故的人为影响有限,但全球模拟的降水中的氚可用于其他氚示踪剂研究领域。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66e7/11835976/050fcb61a051/11356_2025_35919_Fig1_HTML.jpg

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