六盘山东麓岩溶水系统分析  

Analysis on Karst Water System of the Eastern Foot of Liupan Mountain

作　　者：吴孔军[1] 朱玉娟[2] 周斌 

机构地区：[1]中国地质大学研究生院,湖北武汉430074 [2]河南省地矿局第二水文地质工程地质队,河南郑州450053 [3]甘肃省地质环境监测院,甘肃兰州730050

出　　处：《人民黄河》2011年第8期78-79,82,共3页Yellow River

基　　金：中国地质调查局地质调查项目(1212010535205)

摘　　要：六盘山东麓地区岩溶出露状态、形成模式等受构造作用控制,各个岩溶水系统之间无水力联系,成为各自独立的水文地质单元,无统一的水动力场,具有多区补给、多途径流和多级排泄的水流特征。根据六盘山东麓地区岩溶特征对该区岩溶水系统进行了初步划分,并对岩溶水系统的形成模式,补、径、排条件和动态特征进行了探讨。As the exposed state and the formative model of karst water is being controlled by the tectonic function in the eastern foot of Liupan Mountain,there are no hydraulic relations between the various karst water system.The various karst water systems are independent hydrogeological units,no uniform hydrodynamic field and have characteristics of multi-zone supply,multi-channel flow and multi-level excretion.According to karst features in this region,it divides the karst water system and discusses the formation model of karst water system,recharge conditions,runoff conditions,discharge conditions,and dynamic character.

关 键 词：岩溶水系统 地下水补给 地下径流 六盘山东麓 

分 类 号：P641.134[天文地球—地质矿产勘探]