Water resources systems of irrigation district are composed with surface water system and groundwater system.
灌区水资源系统由地表水系统与地下水系统构成。
The groundwater allocation in red beds is controlled by environment factors such as climate, geomorphology, surface water system, lithology and tectonics.
红层地下水水量受控于气候、地形地貌、地表水文网、岩性、构造运动等环境因素。
If no drainage system exists, the water table rises, bringing dissolved salts to the surface.
如果没有排水系统,地下水位就会上升,把溶解的盐带到地表。
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