河流补给有雨水补给、冰川融水、积雪融水、湖泊水、沼泽水和地下水补给等多种形式。
沿运河一带运河水补给孔隙水，运河以南孔隙水与裂隙喀斯特水互为补排关系，而运河水与裂隙喀斯特水无直接水力联系。
Along the canal, pore water and fissure-karst water have a recharge-discharge re lation, while in south of the canal, canal water and fissure-karst water have no direct water power relation.
随着人们对河水的取用的速度超过了水的补给速度，到2005年原本蜿蜒深邃的水库水量降至库容能力的33%。
As people’s demands on the river outpaced the rate of recharge, the deep, meandering reservoir dropped to only 33 percent of capacity in 2005.
利用环境同位素技术追踪傍河水源地开采条件下的河水激发补给过程和补给强度。
With the environmental isotope technique, the induced recharge of river water under pumping condition in water source site adjacent to the river has been probed.
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