1. 主要的供源为中奥陶统碳酸盐类岩石中的裂隙-喀斯特
The main water source is fracture-karst water in Middle Ordovician carbonate rocks.

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2. 喀斯特动力剖面模式反映各类文地质结构中喀斯特的埋藏、迳流条件和动力特点。
The hydrodynamical section of karst reflects the conditions of karst water bury and runoff in var-ious hydrogeological structures as well as hydrodynamical characteristics.

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3. 沿运河一带运河补给孔隙,运河以南孔隙与裂隙喀斯特互为补排关系,而运河与裂隙喀斯特水无直接力联系。
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.

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4. 沿运河一带运河补给孔隙,运河以南孔隙与裂隙喀斯特互为补排关系,而运河与裂隙喀斯特水无直接力联系。
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.

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