ISSN 1003-8035 CN 11-2852/P

    重庆万州椅头沟高位岩质崩滑碎屑流数值模拟分析

    Numerical simulation of a high-elevation rock avalanche–debris flow at Yitougou, Wanzhou, Chongqing

    • 摘要:
      目的 2023年7月4日重庆市万州区长滩镇椅头沟发生一起高位岩质崩滑碎屑流,威胁408人生命安全。
      方法 为深化对高位岩崩动力学机理的认知,本研究基于LPF3D数值模拟平台,采用SPH(Smoothed Particle Hydrodynamics)方法并尝试结合MJC本构模型(Modified Johnson-Cook Constitutive Model),对椅头沟崩滑碎屑流的运动过程开展了动力学模拟。
      结果 模拟结果表明,该崩滑碎屑流的运动过程可划分为四个典型阶段,依次为“外部扰动削弱-前缘牵引加速-中后部推挤破碎-能量耗散堆积”。研究进一步揭示,岩体在运动过程中发生的剪切破碎及随之而来的碎屑流化转化,是推动其形成高速、大范围运移的关键机制。
      结论 本研究不仅深化了对高位岩崩动力学机理的理论认识,也可为此类高位岩质崩滑碎屑流的危险性评估与空间预测提供定量化科技支撑。

       

      Abstract: On July 4, 2023, a high-elevation rock avalanche-debris flow occurred in Yitougou, Changtan Town, Wanzhou District, Chongqing, threatening the lives of 408 residents. To enhance the understanding of the dynamic mechanisms governing such high-altitude rock avalanches, this study conducted a numerical simulation of the event using the Smoothed Particle Hydrodynamics (SPH) method integrated with a Modified Johnson-Cook (MJC) constitutive model within the self-developed LPF3D simulation platform. The simulation results indicate that the motion process of the avalanche-debris flow can be divided into four distinct stages: (i) weakening of the slope due to external disturbances; (ii) frontal traction and initial acceleration; (iii) middle-rear compression and fragmentation; and (iv) energy dissipation and final deposition. Furthermore, the study reveals that the shear-induced fragmentation of the rock mass and its subsequent transformation into a debris flow are key mechanisms driving the high-speed and long-runout movement. This research not only deepens the theoretical insights into the dynamics of high-elevation rock avalanches but also provides quantitative support for hazard assessment and spatial prediction of similar events in mountainous regions.

       

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