... 降水入渗补给系数 coefficient of precipitation recharge 地表水补给 surface water recharge 凝结水补给 condensation recharge ...
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地表水来自于上游，地下水主要受地表水补给。
Surface water from upstream mainly by the surface water and groundwater recharge.
井灌区地下水主要靠地表水、降雨和潜流补给，平原井灌区主要靠地表水和降雨补给。
The surface water, precipitation and undercurrent are main to the groundwater in well irrigated area while in plain area surface water and rainfall are main replenishment.
地表水资源量的变化是随着补给源补给量的变化而变化的，人类活动可以改变地表水的补给源。
Surface water resources is changed with water supply sources, but water supply sources can be changed by human activity.
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