摘要
建立了一个非饱和土中水分流动的二维数值计算模型 ,用以模拟地下水位埋藏很深 ,且在不同的初始条件与边界条件下 ,土体中的水分运动。
In this paper, a planar numeric calculation model about the moisture variety in non saturated soil is built.The model can simulate the moisture variety in soil when the water table is chindeep in all kind of initial condition and boundary condition.The soil moisture variety is calculated with the program when the rainfall is a constant.
出处
《石家庄铁道学院学报》
2000年第4期43-46,共4页
Journal of Shijiazhuang Railway Institute