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李晓昭, 罗国煜, 陈忠胜. 地下工程突水的断裂变形活化导水机制[J]. 岩土工程学报, 2002, 24(6): 695-700.
引用本文: 李晓昭, 罗国煜, 陈忠胜. 地下工程突水的断裂变形活化导水机制[J]. 岩土工程学报, 2002, 24(6): 695-700.
LI Xiaozhao, LUO Guoyu, CHEN Zhongsheng. The mechanism of deformation and water conduction of fault due to excavation in water inrush in underground engineering[J]. Chinese Journal of Geotechnical Engineering, 2002, 24(6): 695-700.
Citation: LI Xiaozhao, LUO Guoyu, CHEN Zhongsheng. The mechanism of deformation and water conduction of fault due to excavation in water inrush in underground engineering[J]. Chinese Journal of Geotechnical Engineering, 2002, 24(6): 695-700.

地下工程突水的断裂变形活化导水机制

The mechanism of deformation and water conduction of fault due to excavation in water inrush in underground engineering

  • 摘要: 断层突水事故中,大多是原始地质条件下的非导水断层在采动影响下发生突水。借助数值模拟,并结合大量工程事例分析,对断裂变形活化与导水机制进行了分析。研究发现,断裂变形活化与导水具有明显的时空效应。对时空效应的充分认识可为科学的工程设计和施工组织以及有效的超前探测和工程监测提供依据。

     

    Abstract: Water inrushes through fault mostly produced by deformation and water conduction of the fault due to excavation, in which no water exists in initial geological condition. By means of numerical simulation and case analysis, the mechanism of deformation and water conduction of fault due to excavation has been studied in this paper. It is found that deformation and water conduction of fault due to excavation show obvious timespace effect, which is very helpful to underground engineering design, construction organization and field exploration and monitoring. 

     

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