摘要
裂隙岩溶含水系统较为复杂,从水位动态和水化学组份难以判断孔隙水和地表水对其影响程度的主次性。本文通过水位和水化学组份的灰色关联度分析,结合水文地质特征,将二者对裂隙岩溶含水系统的影响程度的主次性进行量化比较,进一步验证了水文地质条件。
Fissurekarst waterbearing system is relatively complex. It is difficult to judge the primary and secondary influence on the system from water table dynamic state and hydrochemical components of pore water and surface water. In this paper, we conduct the grey relation analysis of water table dynamic state and hydrochemistry, by considering the hydrogeologic characteristics, compare the primary and secondary influence on the system, as a result the hydrogeologic conditions are further tested and verified.
出处
《水文地质工程地质》
CAS
CSCD
2003年第3期47-50,共4页
Hydrogeology & Engineering Geology
基金
山东鲁能集团重大科研项目(GC-1997-001)
