采用窄缝槽物理模型来模拟地下水运动，具有形象、直观的优点。
The physical model of narrow slit has been adopted to simulate groundwater movement and it has many excellences in visualization and intuition.
基于土壤水运动的物理过程，提出了降雨入渗补给地下水的计算模型。
Based on the physical process of soil water transfer, a calculated model estimating the precipitation recharge is proposed.
单元水文模型涉及到冠层截留、融雪、蒸散发、坡面流、非饱和土壤水运动和地下水出流等水文物理过程。
The former concerns with hydrological processes such as canopy interception, snowmelt, evapotranspiration, slope flow, soil flow and ground flow.
单元水文模型涉及到冠层截留、融雪、蒸散发、坡面流、非饱和土壤水运动和地下水出流等水文物理过程。
The former concerns with hydrological processes such as canopy interception, snowmelt, evapotranspiration, slope flow, soil flow and ground flow.
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