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首页> 外文期刊>Bulletin of engineering geology and the environment >Prediction of water–mud inrush hazard from weathered granite tunnel by an improved seepage erosion model
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Prediction of water–mud inrush hazard from weathered granite tunnel by an improved seepage erosion model

机译:通过改进的渗流侵蚀模型预测风化花岗岩隧洞的水泥涌入危险

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摘要

During tunnel construction, water and mud inrush disasters from completely weathered granite usually lead to the serious casualties and economic losses. Predicting these disasters are vital to the safety construction. Considering the critical erosion condition and flow pattern variation at the three stages (Darcy, rapid, and stable flow stages), a seepage erosion model is developed to perform the coupling analysis of water and mud inrush evolution. The model is shown to have favorable accuracy in real-time predicting the erosion region, ground settlement region, and the main hydraulic parameters (i.e., permeability, water inflow, and mud inflow) by comparison with the laboratory tests and field investigations. Then, effects of the model parameters (i.e., particle diameter, erosion coefficient, and ground permeability) on the water and mud inrush are investigated. Results show that (1) with the decreasing particle diameter, the permeability and the water and mud inflow increase gradually. (2) The erosion coefficient mainly affects the evolution rate and time of the water and mud inrush disaster. (3) The water and mud inrush can be controlled when the ground permeability decreased to the 0.2 time of the initial value. The research findings and the proposed model can provide the reference for the water inrush prevention in a similar project.
机译:在隧道施工,水和泥浆涌入灾害从完全风化花岗岩通常导致严重人员伤亡和经济损失。这些预测灾害的安全建设是至关重要的。考虑到临界侵蚀条件,并在三个阶段(达西,快速,且稳定的流动阶段)流动图案的变化中,渗流侵蚀模型来执行水和泥浪涌进化的耦合分析。该模型示出了由与实验室试验和现场调查相比,具有实时有利精度预测侵蚀区域,地面沉降区,并且主液压参数(即,透气性,水的流入,和泥浆流入)。然后,将模型参数(即,粒径,侵蚀系数和接地渗透性)在水和泥的浪涌影响进行了研究。结果表明,(1)与所述减小粒径,磁导率和逐渐的水和泥流入增加。 (2)的侵蚀系数主要影响水和泥浆涌入灾难的演变速度和时间。 (3)水和泥浪涌可以当接地渗透性降低到0.2时的初始值来控制。研究结果和该模型可为突水防治的一个类似项目参考。

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