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EXPERIMENTAL STUDY ON WATER-INRUSH MECHANISM OF TUNNELS IN KARST AREA

机译:岩溶地区隧道排水机理实验研究。

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摘要

The instability of karst ground water under the disturbance of external force always results in the geological hazard of water outburst and mud gushing. It is a dynamic damage phenomenon of water and mud flowing to the tunnel face with high speed. Based on the water-rock interaction mechanism in karst tunnel, the mechanism of water inrush has been analyzed by several model tests and the theory of karst geology, engineering hydraulics and rock mechanics. It is shown that the occurrence and formation of water outburst has two steps. The first step is that the karsls water and its pressure have softening and dissolution effect on rock. It has been qualitatively studied through hydraulic fracturing experiment on rocklike material. The second step is that the water flow and its pressure have passageway expanding and flowing yield controlling effect on water inrush. It has been analyzed through the similarity test. Based on the failure characteristics of water inrush experimental tests, a mechanical model of water inrush is put forward, and the analytic solution of critical protection thickness of rock mass preventing water inrush is given. This model can be used to the calculation of safety rock mass thickness.
机译:在外力的干扰下,岩溶地下水的不稳定性总是会引起突水和涌泥的地质危害。这是水和泥浆高速流向隧道工作面的动态破坏现象。基于岩溶隧道的水-岩相互作用机理,通过几种模型试验以及岩溶地质,工程水力学和岩石力学理论,对突水的机理进行了分析。结果表明,突水的发生和形成有两个步骤。第一步是岩溶水及其压力对岩石具有软化和溶解作用。通过对岩石状材料的水力压裂实验进行了定性研究。第二步是水流及其压力具有通道扩展和流量控制对冲水的作用。已经通过相似性测试对其进行了分析。根据突水试验的破坏特征,提出了突水的力学模型,给出了防止突水的岩体临界保护厚度的解析解。该模型可用于计算安全岩体厚度。

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