The groundwater system of karst spring is a nonlinear and dynamic system influenced by factors such as hydrology, geology, landform, vegetation and human's activities.

岩溶水系统是受水文、地质、地形地貌、植被、人类活动等多种因素影响的非线性动力系统。

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It is called "the geological museum" by the geological expert because of complicated hydrology geological condition, especially the karst water in the tunnel.

其因复杂的水文地质条件，被地质专家堪称为“地质博物馆”，尤其是隧道岩溶涌水。

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The main controls on karst reservoirs are : lithology, depositional environments, hydrology, ancient landform, fractures and weathering time and so on.

控制岩溶发育的主要因素有：岩性及沉积环境、水动力条件、古地形因素、断裂与裂缝发育情况和风化淋滤时间等。

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