The infiltration process of the water on the surface is analysized under rainfall conditions, the two-dimensional mathematical model and its boundary conditions are presented.
分析了降雨条件下地表水入渗的过程，提出了降雨条件下非饱和渗流的二维数学模型及边界条件。
This paper deals with an infiltration model in which rainfall or sprinkling intensity are known but it is less than the infiltrability of soil.
本文研究均质土壤、表面供水强度已知但未超过土壤入渗能力的入渗模型。
The mathematical model of rainfall infiltration on the rock slope and the numerical simulation method for this model is discussed.
对岩质边坡降雨入渗的数学模型及模拟方法进行了探讨。
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