榆次源涡水源地裂隙含水系统地下水位持继下降的原因分析及供水对策

Reason on groundwater level lasting decrease and countermeasure ou fissure aquifer system of Yuanwo water-supply field of Yue Ci city

源涡水源地含水层为一层间和裂隙混合的半开放含水系统,水位持续下降的原因是系统内大量增加开采井、过量超采所致。为此,在研究课题提出了榆次市主要供水对策。

The aquifer of Yuauwo water-supply field is a sem-open water-bearing systen combining layer and fissure The reason of water level lasting decrease is due to over pamning, A countermeamre on water-supply is suggested.