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.
在印度、中国、美国等地，地下含水层被抽离的速度比自然补给还要快。
Groundwater aquifers are being pumped down faster than they are naturally replenished in parts of India, China, the USA and elsewhere.
地下水的渗透速度影响着其与岩石的反应速度，而地质构造、岩层厚度、岩石破碎程度及地下水的补给状况等则是影响地下水运动的重要因素。
Infiltration velocity of groundwater influences its reaction rates with rocks. Geological structure, strata depth, rupture degree and supply of groundwater are major influence factors.
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