摘要
大量的抗旱打井找水开发深层岩溶地下水资源实例证明,黔南岩溶石山区不同岩溶形态富水电测深法异常类型及成因有一定规律可循,单支电测深曲线异常类型可划分为缓升型、缓降型、低阻平台型、低阻V型、低阻平升型、低阻降尾型,富水地段电测深视电阻率断面等值线异常类型可划分为低阻U型、低阻O型、低阻梯度带型、低阻台阶型。
The large examples of against drought and development of deep water wells to prove that karst groundwater resources show different South Guizhou karst region of water-rich sounding abnormal type and causes of certain rules to follow,single abnorma type sounding curve can be divided for the slow rise,slow down type,platform type low resistance,low resistance V-type,low resistance level rise type,low resistivity drop tail type,abnormal type of water-rich sections of apparent resistivity section sounding contour can be divided into low resistance U-type,low resistance O-type,low resistivity gradient banding,step-type low resistance.
出处
《水文地质工程地质》
CAS
CSCD
北大核心
2012年第3期17-22,共6页
Hydrogeology & Engineering Geology
基金
西南严重缺水地区地下水勘查(010730)
关键词
岩溶石山区
电测深异常
类型及成因
黔南黔西南
karst region
sounding anomaly
types and causes
South Guizhou and Southwest Guizhou