深埋隧洞开挖过程中突水的水力劈裂研究

On Water Burst in Deep-Buried Tunnelling Based on Hydrofracturing Method

  • 摘要: 突水是隧洞工程施工过程中常遇的主要灾害之一。文章简要介绍了采用水力劈裂理论分析隧洞突水的研究进展情况,并从水力劈裂的机理入手,分析认为隧洞突水现象的水力劈裂研究应考虑多物理场耦合作用。在 Biot固结理论基础上,引入了损伤的概念,考虑了岩体渗透性的动态演化;试图通过分析掌子面推进过程中隧洞围岩力学条件变化导致的渗透性改变,来判断突水发生的可能性。研究结果表明:围岩的损伤破坏导致其渗透性发生了改变,而渗透性的改变为突水提供了通路,提高了围岩突水的可能性;裂隙带等强透水带的存在是隧洞突水的前提条件,高水力梯度则是隧洞突水的根源。

     

    Abstract: Water burst events are the chief disasters encountered during tunnel excavation. The progress of re? search on water burst in deep-buried tunnels by hydrofracturing theory is briefly introduced. In light of the mechanism of hydraulic fracturing, the role of multi-physics coupling should be considered in study of water burst disasters. Based on Biot's consolidation theory, the concept of damage is applied, and the dynamic evolution of rock mass permeability is considered. The possibility of a water burst can be assessed by analyzing permeability change as a result of changes to rock's mechanical conditions during advance of the working face. The results show that rock mass damage and failure induces permeability change, which makes way for a water burst and increases its possibility. A strong permeable zone, like the fractured zone, is a precondition of a water burst, and a high hydraulic gradient is the original source of a water burst.

     

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