研究结果表明，在以浅地下水位为主要特征的河套灌区，农田间“五水”转化频繁而复杂。

The results indicate that five related water commute complex and frequent in Hetao irrigation area which have unique characteristics of its shallow groundwater.

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这样的结果，对地下水位映震条件、映震特征与映震机制的深入研究，提供了有益的启示。

These results will be useful in the further studies on conditions, features and mechanism of ground water reflection to earthquakes.

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这种影响特征具有典型的周期性和滞后性，通过对坡体地下水位的动态模拟，取得了边坡稳定性随时间而变化的规律认识。

The characteristics of the effects have typic period and delay features. We obtained the law of slope stability with changing time by dynamic simulation to groundwater level of the slope.

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