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Numerical Simulation Analysis of Karst Tunnel Water Bursting Movement

机译:岩溶隧道水爆裂运动的数值模拟分析

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The karst water is one of the main geological disasters in tunnel construction in Karst area. The disaster of water inrush in karst tunnel is studied in this paper. FLOW-3D is used to simulation movement patterns of water inrush in karst tunnel based on BaoFeng tunnel engineering. The following contents are studied. Firstly, the total duration in tunnel and the characteristics of tunnel water inrush were studied. Secondly, 140s time before the water inrush from the left tunnel discharge, the main reason for the lowest surface for the cross channel is slightly higher than that in the bottom of tunnel. But 140s after the water inrush from the left tunnel discharge, the drainage discharge by the right line, the main reason for the decrease in left line tunnel velocity, kinetic energy due to the force of gravity, resulted in the initial stage of the water began to flow of the tunnel face and the formation of turbulence. Thirdly, at the beginning stage, water gushing speed was up to 17m/s, and the waves move forward. Fourthly, the viscosity and density of water inrush has little influence on the rate of water inrush. The research will provide the basis for karst tunnel water inrush prevention theory.
机译:喀斯特水是喀斯特地区隧道建设的主要地质灾害之一。本文研究了岩溶隧道中的浪涌灾害。基于宝丰隧道工程,流动3D用于仿真岩溶隧道中的浪涌运动模式。研究了以下内容。首先,研究了隧道中的总持续时间和隧道涌入的特征。其次,在左隧道放电的水中涌入前140秒,交叉通道最低表面的主要原因略高于隧道底部的表面。但是140年代在左隧道放电后,排水放电通过右线,左线隧道速度下降的主要原因,由于重力引起的动能,导致水的初始阶段开始流动隧道面和湍流的形成。第三,在开始阶段,水涌出速度高达17米/秒,波浪向前移动。第四,水中涌入的粘度和密度对水中涌入的速度不大。该研究将为喀斯特隧道涌入预防理论提供基础。

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