王家兵. 潞安矿区奥陶系岩溶水化学成分的成因[J]. 煤田地质与勘探, 1999, 27(2): 39-42.
引用本文: 王家兵. 潞安矿区奥陶系岩溶水化学成分的成因[J]. 煤田地质与勘探, 1999, 27(2): 39-42.
Wang Jiabing. THE CHEMICAL ACTION OF KARST WATER COMPOSITIONS OF THE ORDOVICIAN IN LUAN MINING AREA[J]. COAL GEOLOGY & EXPLORATION, 1999, 27(2): 39-42.
Citation: Wang Jiabing. THE CHEMICAL ACTION OF KARST WATER COMPOSITIONS OF THE ORDOVICIAN IN LUAN MINING AREA[J]. COAL GEOLOGY & EXPLORATION, 1999, 27(2): 39-42.

潞安矿区奥陶系岩溶水化学成分的成因

THE CHEMICAL ACTION OF KARST WATER COMPOSITIONS OF THE ORDOVICIAN IN LUAN MINING AREA

  • 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。

     

    Abstract: 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 water-rock interaction and chemical action of compositions of groundwater.

     

/

返回文章
返回