摘要
潞安矿区奥陶系岩溶水由于埋藏深，水交替缓慢，水文地球化学条件复杂。本文在因子分析的基础上，深入分析了深部岩溶含水层中水—岩作用机理和水化学成分的成因。
The karst water of the Ordovician is buried deeply in the Luan coal mines,which makes the runoff velocity very slow and the hydrochemical conditions very complex.Based on results of factor analysis,and according to karst feature and hydrochemical field,the studies in detail mechanism of waterrock interaction and chemical action of compositions of groundwater.
出处
《煤田地质与勘探》
CAS
CSCD
北大核心
1999年第2期39-42,共4页
Coal Geology & Exploration
关键词
岩溶水
水化学
成因
因子分析
潞安矿区
Karst water
hydrochemistry
cause of formation
factor analysis
Luan mining area
