ISSN 1003-8035 CN 11-2852/P

    西北黄土山区铁路泥石流风险评估方法研究

    Study on debris flow risk assessment methods for railways in loess mountainous areas of Northwest China

    • 摘要: 泥石流是黄土山区铁路典型的水害,严重威胁铁路安全运行。本文以西北黄土山区铁路沿线典型泥石流沟为研究对象,进一步完善对黄土山区铁路泥石流灾害特征和风险评估方法的理解。基于资料收集、遥感调查和现场调查,开展泥石流动力学特征值计算、既有涵洞行洪能力检算和动力学过程数值模拟,判别泥石流形成后对铁路及周边环境的影响,提出泥石流风险评估方法。研究区陡峭的地形和丰富的松散物源为泥石流的发生提供了基础,泥石流形成存在降雨坡面侵蚀型和崩滑型两种模式。采用雨洪法计算的降雨坡面侵蚀型泥石流一次冲出量可通过涵洞排出,对明洞及周边环境威胁较小;在强降雨条件下,若坡面冲沟沟头处弃土和沟岸陡坎同时发生垮塌,形成崩滑型泥石流,将导致泥石流规模显著增大。数值计算结果表明,泥石流启动后在明洞前淤积后将越过明洞,并威胁铁路下方居民区。本文基于泥石流灾害的易发性和既有桥涵对泥石流灾害的抑制性,提出了适用于黄土山区铁路泥石流风险评估方法。研究成果可为黄土山区铁路泥石流灾害防治与风险排查提供新的思路与技术参考。

       

      Abstract: Debris flow is a typical rainfall-induced geological hazard in the Loess Mountainous Areas, posing a serious threat to the safe operation of railways. This study selects representative debris flow gullies along the railway in the northwestern loess mountainous areas as research objects to further improve the understanding of debris flow characteristics and risk assessment methods for railways in the Loess Mountainous regions. Based on data collection, remote sensing investigation, and field investigation, dynamic parameters of debris flows were calculated, flood discharge capacity of existing culverts was checked, and numerical simulations of dynamics processes were carried out to identify the impacts of debris flows on railways and surrounding areas, and a debris flow risk assessment method was proposed. The steep topography and abundant loose materials in the study area provide basic conditions for debris flow initiation. Two formation modes are identified: rainfall-induced slope erosion type and collapse-landslide type. For rainfall-slope erosion debris flows, the single-event outburst volume calculated by the rain-flood method can be discharged through the culvert, posing little threat to the open-cut tunnel and surrounding environment. Under heavy rainfall, if spoil at the gully head and steep bank collapse simultaneously to form collapse-type debris flows, the disaster scale will increase significantly. Numerical simulation results indicate that after initiation, debris flow will deposit in front of the open-cut tunnel, overtop the structure, and threaten residential areas below the railway. Based on debris flow susceptibility and the inhibition effect of existing bridges and culverts on debris flow hazards, this paper proposes a debris flow risk assessment method suitable for railways in the Loess Mountainous Areas. The results can provide new insights and technical references for the prevention and risk investigation of railway debris flow disasters in loess mountain areas. Future research should further consider the dynamic impact of debris flow impact loads on railway structures to refine the precision of debris flow risk assessment systems.

       

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