近地表土壤氡通量波动:与强降水的关系

Kazuhide Nemoto, Kojima Haruna, C. Yoshino, Shu Kaneko, Akitsugu Kitade, K. Hattori, T. Mogi, Toshiharu Konishi
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引用次数: 0

摘要

我们正在利用千叶茨城县的α射线探测器进行地下和大气氡观测,以研究地震与地面氡排放之间的关系。本文研究了土壤氡通量(SRF)与强降水的关系,发现持续2 h的20 mm及以上的强降水显著增加土壤氡通量(SRF)。我们提出了两种模型,雨水荷载模型和雨水入渗模型,两种模型都适用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soil radon flux fluctuation near the ground surface:Relationship with heavy precipitation
We are developing underground and atmospheric radon observations using an α-ray detector in Chiba-Ibaraki to investigate the relationship between earthquakes and radon emissions from the ground. In this paper, we investigated the relationship between soil radon flux (SRF) and heavy precipitation, and found that SRF was significantly increased by heavy precipitation of 20 mm or more in total for 2 hours. We proposed two types of models, a rainwater load model and a rainwater infiltration model, and it is appropriate for both models to work.
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