ISSN 1000-3665 CN 11-2202/P

    贵州纳雍龙家岩脚高位崩塌动力过程模拟

    Depositional characteristics and dynamic process inversion of the Longjiayanjiao high-elevation rock avalanche in Nayong, Guizhou

    • 摘要: 近年来乌蒙山区高位崩塌频繁发生,致灾性极强。为进一步提升灾害风险预测能力,以2024年6月发生于贵州纳雍的龙家岩脚高位崩塌为例,综合运用野外调查和无人机图像识别手段分析灾害堆积特征,并结合自主研发的SPH-SDPH-DEM耦合计算软件LPF3D(Landslides Post Failure 3D)开展崩塌动力过程模拟。结果表明:(1)龙家岩脚崩塌的运动路径、堆积形态和粒径分布受前缘隆起和堆积区“左低右高”地形的影响,颗粒粒径沿运动方向呈现逐渐增大的趋势,大块石主要分布于堆积区中部、左侧和前缘,呈非对称的堆积结构。堆积区岩块颗粒D50值的范围为0.16~10.28 m,全区颗粒D50值为0.87 m。(2)计算结果有效还原了龙家岩脚崩塌运动堆积过程和颗粒分布特征,模拟堆积范围与实际基本吻合,模拟显示最大速度约52 m/s,平均速度11 m/s,堆积块体最大粒径约13 m。(3)龙家岩脚崩塌具有岩体—岩块—岩屑的动力学转化特征,运动堆积过程可以概化为链式启动与初始解体—碰撞破碎与能量骤降—地形控制与非对称堆积3个阶段。研究结果提高了对高位崩塌堆积特征和动力学过程的认识,可为乌蒙山区灾害风险预测提供科技支撑。

       

      Abstract: In recent years, high-elevation collapses have occurred frequently in the Wumeng Mountains, posing severe threats to lives and property in the region. It is therefore essential to enhance the understanding of the dynamic processes associated with such disasters. This study takes the Longjiayanjiao high-elevation rock collapse that occurred in June 2024 in Nayong County, Guizhou Province as a case example. We analyzed the characteristics of the collapse deposits through field investigations and UAV-based image recognition, and simulated the collapse dynamics using LPF3D (Landslides Post Failure 3D), a self-developed SPH–SDPH–DEM coupled numerical modeling software. The results show that: (1) The movement path, depositional morphology, and grain-size distribution of the Longjiayanjiao avalanche were strongly influenced by the uplifted front-edge terrain and the “low-left–high-right” topography in the depositional area. Particle size gradually increased along the movement direction, with large boulders mainly distributed in the central, left, and frontal parts of the deposit, forming an asymmetric depositional structure. The D50 values of deposited rock blocks ranged from 0.16 to 10.28 m, with an overall mean of 0.87 m. (2) The simulation accurately reproduced the movement–deposition process and particle-size distribution characteristics of the avalanche, showing good agreement between simulated and observed depositional ranges. The maximum velocity reached approximately 52 m/s, the average velocity was about 11 m/s, and the maximum block diameter was around 13 m. (3) The avalanche exhibited a dynamic transformation sequence from rock mass to rock blocks to debris. The overall movement and deposition process can be generalized into three stages: chain-type initiation and initial disintegration, collision-induced fragmentation and rapid energy attenuation, and terrain-controlled asymmetric deposition. The results of this study provide an important basis for advancing risk prevention, mitigation, and related research on high-elevation collapses in the Wumeng Mountains.

       

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