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.
出处
《人民黄河》
CAS
北大核心
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)
关键词
岩溶水系统
地下水补给
地下径流
六盘山东麓
karst water system
groundwater recharge
groundwater runoff
eastern foot of Liupan Mountain
