不同路径下泥石流堆积特征的物理模型试验研究

    PHYSICAL MODELING TEST STUDY ON DEBRIS FLOW ACCUMULATION CHARACTERISTICS UNDER DIFFERENT PATHS

    • 摘要: 泥石流堆积区堆积颗粒分散、堆积形态偏移等因泥石流流路变化而产生不同的演化特征,探索不同条件下堆积物动力过程、形态特征、粒径分布规律等对泥石流预防和堆积区利用具有积极意义。本文以3种不同密度的泥石流堆积物为原型材料,探究不同流路形态对泥石流堆积区特征的影响,依托自主研发的“泥石流过程模拟试验系统”,开展了直线型(I型)、单弯道型(C型)和连续弯道型(S型)3种流路条件下泥石流的室内物理模型试验。通过集成高速摄像、分布式传感与图像处理技术,同步监测泥石流运动过程中的流速、流量、堆积形态及颗粒级配等参数,并引入“偏移角”与“偏移度”指标,分析泥石流路径对偏移的影响。研究结果表明:流路形态控制堆积区形态,直线型呈条带状,单弯道型呈扇形,且连续弯道型扩散面积最大;密度与堆积范围正相关。流路形态通过调控流速流量影响颗粒分选,并为堆积区偏移行为的主控因素,直线型偏移低而稳,单弯道型偏移显著且风险期长,连续弯道型通过二次调整实现缓冲再稳定。研究说明,优化流路形态可为泥石流灾害的风险防控与工程治理提供关键依据。

       

      Abstract: Debris-flow deposition zones often exhibit evolutionary characteristics such as dispersed sediment particles and deflected morphology due to changes in flow-path configuration. Current research in this field remains insufficient, constraining hazard prevention and comprehensive utilization of deposition zones. In this study, three types of debris-flow deposits with varying densities were employed as prototype materials. Indoor physical model tests were conducted using a self-developed variable-flow-path simulation system under three channel configurations: straight (Type I), curved bend (Type C), and twist bend (Type S). By integrating high-speed photography, distributed sensing, and image processing techniques, parameters including flow velocity, discharge, deposition morphology, thickness distribution, and particle size distribution were simultaneously monitored. Deflection angle and offset distance were introduced to quantitatively analyze flow-path deviation behavior. Results show that flow-path morphology dominates deposition patterns: straight channels form strip-like deposits, while curved channels produce fan-shaped distributions. Deposited particles display longitudinal sorting, with finer grains near the flow path and coarser grains farther away; bends significantly hinder the transport of fine particles. Path deviation is primarily controlled by channel morphology, while flow velocity and material density play regulatory roles at specific stages. This study reveals the movement-deposition response mechanism of debris flows under complex flow paths, providing a scientific basis for risk assessment and mitigation engineering design of debris-flow hazards in mountainous regions.

       

    /

    返回文章
    返回