Sakoda Akihiro, Hanamoto Katsumi, Ishimori Yuu, Kataoka Takahiro, Kawabe Atsushi, Yamaoka Kiyonori
Graduate School of Health Sciences, Okayama University, 5-1 Shikata-cho, 2-chome, Kita-ku, Okayama 700-8558, Japan.
Appl Radiat Isot. 2010 Jun;68(6):1169-72. doi: 10.1016/j.apradiso.2009.11.070. Epub 2009 Dec 3.
The present model represents an improvement on previous models of radon emanation from soil by incorporating soil grain size in addition to moisture. Monte Carlo simulation was employed in the calculation since it was difficult to mathematically express the radon emanation fraction for the present soil model. Grain size is one of the most important factors in describing the properties of soil. Grain size was demonstrated to affect the radon emanation fraction, depending on moisture content. Although the emanation fraction is generally considered to be proportional to grain size, the result of the model calculation suggested that the effect of grain size is not so simple. This study should serve as an initial step toward improving the modeling of this radon emanation.
本模型在以往土壤中氡析出模型的基础上进行了改进,除了考虑土壤湿度外,还纳入了土壤颗粒大小因素。由于难以用数学方法表达当前土壤模型的氡析出率,因此采用蒙特卡罗模拟进行计算。颗粒大小是描述土壤性质的最重要因素之一。结果表明,颗粒大小对氡析出率有影响,且这种影响取决于土壤湿度。虽然一般认为析出率与颗粒大小成正比,但模型计算结果表明颗粒大小的影响并非如此简单。本研究应作为改进这种氡析出建模的第一步。