The effect of the relative aquitard layers on the ground water flow in layered slopes is discussed in this paper.
本文研究了层状结构边坡体中，相对弱透水层对其中地下水运动的作用。
An aquitard stores water and transmits enough water to be regionally significant but not enough to supply individual Wells.
弱透水层存水且区域性地传导大量水，但不能充分供给每个井。
For porous aquifer system separated by aquitard, the precipitation recharge possesses delay effect on the medium-deep aquifers.
对于中间以弱透水层相隔的孔隙含水系统，降雨补给中深层水具有延迟作用。
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