| 潞安矿区奥陶系岩溶水化学成分的成因 |
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| 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. |
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| 作者姓名： | 王家兵 |
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| 作者单位： | 天津市地质工程勘察院 |
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| 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。
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| 关 键 词： | 岩溶水 水化学 成因 因子分析 潞安矿区 |
| 收稿时间： | 1998-09-24 |
THE CHEMICAL ACTION OF KARST WATER COMPOSITIONS OF THE ORDOVICIAN IN LUAN MINING AREA |
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| 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. |
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| Authors: | Wang Jiabing |
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| Affiliation: | Tianjin Geotechnical Engineering Investigation Institute |
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| 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 waterrock interaction and chemical action of compositions of groundwater. |
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| Keywords: | Karst water hydrochemistry cause of formation factor analysis Luan mining area |
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