地下水分水岭
- 网络groundwater divide
地下水分水岭-
水均衡分析法原理是根据岩溶系统径流反推补给面积，进而确定地下水分水岭的位置。
The principle for water balance analysis is to reversely derive the area of water supply according to runoff amount in the karst system , further to determine the position of the groundwater divide .
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关于白于山是否存在完全地下水分水岭的探讨
Confirmation of Absolute Groundwater Divide in Baiyu Mountain
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关于鄂尔多斯盆地白垩系地下水分水岭的探讨
Research on the watershed of the groundwater of Cretaceous in Erdos Basin
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而岩溶区域内的地下水分水岭非但不一定贫水，有的还可成为重要的水源地。
In fact , the dividing area of ground water catchments in karst area isn 't necessarily deficient in water , on the other hand , some parts of dividing area are important water-source bases .