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Radon migration from deep soil to the earth's surface is investigated numerically using a developed Finite Element numerical model. The objectives of this study are: to predict the radon profile variation with the soil depth, the radon diffusion coefficients in multi-layer soils, the surface radon concentrations and the soil-air radon fluxes. The flexibility of the Finite Element Method allows for accommodating varying diffusion coefficients in multi-layer soils and expressing convective-typedoi:10.1080/23311940.2016.1254859 fatcat:ebld6pxijfekdf7zuj4jqpts6i