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槐子水库位于高桥向斜与九坝背斜之间的单斜构造带。水库库区内河流类型以横谷为主,岩溶地层分布广泛,存在右岸条塘河低邻谷与白盐井区域性断裂,水库正常蓄水后极可能产生严重的渗漏问题。文章将库区分成库首、库区中部、库尾三段,利用岩溶泉点、地下分水岭、地层岩性等分析论证了水库的成库条件,可为同类工程提供一些参考。
The Huaizi Reservoir is a monocline structural belt located between the Takahashi syncline and the Jiuba anticline. The river type in the reservoir area is mainly Yokogawa, and the karst strata are widely distributed. There is a regional fault between the lower banks of the Right Bank and the Lower Salt Valleys and the Baiyan Well. After the reservoir is normally impounded, serious leakage problems are likely to occur. The article divides the reservoir into the first reservoir, the middle reservoir area and the third reservoir tail. Based on the analysis of karst springs, underground watersheds and stratigraphic lithologies, the conditions of reservoir formation are demonstrated, which can provide some references for similar projects.