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巷道突水垮塌破碎岩体运移特性与堆堵机理

Transport characteristics and blockage mechanism of fractured rock mass during water inrush process in roadway

  • 摘要: 矿井突水垮塌事故是破坏性巨大的地质灾害之一,其中流固两相流的运动与堆积行为直接决定了灾害的演化规模与治理难度。矿井突水垮塌事故中,准确预测不同地质背景条件下碎石流动与堆积特征对灾害的治理至关重要。突水垮塌事故造成垮塌散体在井下搬运和堆积,使垮塌灾情更加复杂。通过室内物理模型试验和CFD-DEM耦合数值模拟,系统研究了不同水压及巷道倾角条件下的矿井突水垮塌事故中碎石运移堆积特征。研究通过物理模型试验宏观再现了碎石从突水口涌出至最终稳定的动态过程,并结合流固耦合模拟揭示了垮塌散体宏细观力学机制。研究结果显示,碎石运移堆积过程呈现初步堆积、快速扩散与稳定堆积3个阶段,且堆积体层序与初始层序保持一致。随着水压增大,突水口下方形成“M”形双峰堆积,巷道倾角增大则使堆积体扩散距离变远、堆积更集中、横向脊更明显、堆积高度增加。在宏观分布上,颗粒粒径呈现显著分选特征,即大颗粒堆积于堆积体前端与外围,小颗粒分布于后端与底部。在细观接触特征分析上,堆积体配位数云图整体呈“四周低、中心高”的分布模式,且其峰值随水压与倾角的增大均呈现先增后降的趋势。对多因素影响下碎石堆积运移特征的研究,可为矿井突水垮塌事故中救援通道的快速构建方案优化与施工安全风险评估提供关键的数据支持和理论指导。

     

    Abstract: Mine water inrush and collapse accidents are among the most destructive geological disasters, where the movement and deposition behavior of solid–fluid two-phase flows directly determine the scale of disaster evolution and the difficulty of mitigation. In mine water inrush and collapse accidents, accurate prediction of the flow and accumulation characteristics of crushed stone under different geological conditions is crucial for disaster management. The transport and deposition of crushed stone during such incidents complicate the disaster scenario. Through physical modeling and CFD-DEM coupled numerical simulations, this research systematically investigates the transport and accumulation characteristics of debris in mine water inrush and collapse accidents under varying water pressures and roadway inclination angles. Utilizing a combined approach of physical modeling and fluid-solid coupling simulation, this research replicated the full dynamic process of debris flow and unraveled the underlying macro-meso scale mechanical mechanisms of the collapsed mass. The results reveal that the crushed stone transport and accumulation process can be divided into three distinct stages: initial deposition, rapid spreading, and stable accumulation, with the deposit sequence remaining consistent with the initial accumulation sequence. As the water pressure increases, the crushed stones form an "M"-shaped double-peak accumulation below the water inrush opening, while a steeper roadway inclination leads to longer spreading distances, more concentrated deposition, more prominent transverse ridges, and greater accumulation heights. On a macroscopic scale, the particle size exhibits significant sorting characteristics, with large particles accumulating at the front and periphery of the deposit, while small particles are distributed at the back and bottom of the deposit. In the meso-scale analysis of contact characteristics, the coordination number contour exhibits a pattern of being low at the edges and high at the center. Moreover, its peak value follows a consistent non-monotonic trend, initially increasing and then decreasing with the increase of water pressure and inclination angle. This study investigates the transport and accumulation characteristics of crushed stone under the influence of multiple factors and offers key data and theoretical guidance for optimizing the design of rapid rescue pathways construction and for assessing construction safety risks in mine water inrush and collapse incidents.

     

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