摘要
本文在研究区域水文地质条件的基础上,分析了珠琳地区岩溶水的分布规律,认为新构造运动的间歇性和持续上升、弱透水层的存在是造成自分水岭至排泄区岩溶水的富水性由弱到强及岩溶发育均匀程度由高到低,地下水埋深呈阶梯状降低的主要因素。总结提出了高原斜坡地带岩溶石山区找水要在古溶蚀台面上接近分水岭的地段、溶蚀洼地的扬起端寻找表层带岩溶水,以及悬托的弱透水层之上寻找滞水型岩溶水;不宜在强迳流区、负地形最低部位布井。
To discuss the exploitation and ulilization of karst water in Zhulin area, we analysize the hydrogeological conditions and the occurrence of the karst water in detail. The results suggest that due to the intermittence and the sustainable rising of neotectonic movement and to the existence of aquifards, from the water divide to the dischange areas, abundance of the karst water is from poor to rich and the uniformity of the development of karst is from high to low, and the karst water level is of the shape of stairs.
出处
《水文地质工程地质》
CAS
CSCD
2003年第1期73-75,87,共4页
Hydrogeology & Engineering Geology
