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断层突水非线性渗流-应力耦合研究

Study on the Mechanism of Fault Water Inrush and the Nonlinear Seepage-Stress Coupling

中文摘要英文摘要

针对断层水突出日益严重的问题,为揭示断层水突出过程中的流固耦合作用影响下突水不同时刻,不同阶段上承压水运移规律,在断层破碎带中应用非达西流动方程并考虑应力作用和孔隙水压力作用对断层带中岩石力学参数影响,应用comsol软件建立含水层-断层-工作面三个阶段的断层导通前后达西-非达西-自由流动方程,获得应力-水压力作用下断层水突出及流动机理。结果表明:非达西Forchheimer方程能有效的模拟计算高水压高流速水流在断层中的流动过程;流固耦合作用对断层中的非达西流动特性影响较大,断层破碎带作为含水层和工作面的连接部,其在应力作用下的渗透性突变是断层突水形成的根源。?????

Specific to the problem of increasingly severe inrush of water from the fault, the non-Darcy flow equation is applied to the fractured rock mass with the consideration of the effect of the stress and pore water pressure on fillings in the fault and fracture, so as to uncover the problem of fluid-solid coupling in the fault water inrush process, the water-rock interaction at different time and different stages, and the law of water flow. The Comsol Multiphysics software is adopted to establish the Darcy and non-Darcy free flow equation before and after the fault breakover in three stages, that is, the aquifer, fault and working face. Thus obtaining the fault water inrush and current flow mechanism under the effect of stress and water pressure. Results show that the non-Darcy Forchheimer equation can help to simulate and calculate the flow process of current with high water pressure and high flow rate effectively. The influence of liquid-solid coupling on the non-Darcy flow characteristics in the fault is significant. References can be provided by the research results for the prevention of fault water inrush issue in the coal mine inrush and the post-inrush treatment work. ?????

郭惟嘉、白丽扬、赵金海

矿业工程理论与方法论矿山地质、矿山测量矿山安全、矿山劳动保护

采矿工程断层破碎带流固耦合非达西流突水

mining engineeringfault fracture zonefluid-solid couplingnon-Darcy flowwater inrush

郭惟嘉,白丽扬,赵金海.断层突水非线性渗流-应力耦合研究[EB/OL].(2017-05-09)[2025-08-02].http://www.paper.edu.cn/releasepaper/content/201705-572.点此复制

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