| 临涣矿区水文工程地质条件与井筒破裂关系探讨 |
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| 引用本文： | 李定龙,周治安.临涣矿区水文工程地质条件与井筒破裂关系探讨[J].安徽理工大学学报(自然科学版),1994(1). |
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| 作者姓名： | 李定龙 周治安 |
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| 作者单位： | 淮南矿业学院地质系 |
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| 摘 要： | 本文着重讨论了临涣矿区新生界松散层中第四含水层(以下简称四含)及其下基岩风化带的水文地质条件.于此基础上对该矿区井筒破裂原因进行了探讨,指出不良的基岩工程地质条件和矿井开采导致四含及基岩风化带水文工程地质条件恶化是井筒破裂的重要原因.
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| 关 键 词： | 风化带 井筒变形 水文地质条件 |
Relation between hydrogeologicalcondition and shaft wall damage inLinhuan mining area |
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| Li Dinglong,Zhou Zhian.Relation between hydrogeologicalcondition and shaft wall damage inLinhuan mining area[J].Journal of Anhui University of Science and Technology:Natural Science,1994(1). |
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| Authors: | Li Dinglong Zhou Zhian |
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| Institution: | Dept. of Geology |
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| Abstract: | Based on the discussion of hydrogeological condition of the fouth aquifer of Cenozoic Erath-em and the weathered zone of bedrock in Linhuan mining area, the cause of shaft wall damage is analysed. The conclusion is deduced that the main cause of the damage is the deterioration of the hydrogeology and engineering geology of the fouth aqrifer and weathered zone caused by bad condition of engineering geology of bedrock and mis-mining |
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| Keywords: | Weathered zone shaft deformation hydrogeological condition |
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