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    祁连山东段矿渣堆料对沟道侵蚀的灾害放大作用——以西宁市金跃沟为例

    The Erosion of Ravine by Slag Heap in the Eastern Section of Qilian Mountains Disaster Amplification Effect: A Case Study of Jinyue Ravin, Xining

    • 摘要: 摘 要:目的 以2024年“9·03”西宁市金跃沟矿渣泥石流过程为例,揭示极端降雨条件下矿产开发矿渣堆料对沟道侵蚀的灾害放大作用与链生机制。方法 通过开展野外实地勘察与室内实验,综合运用Iverson泥石流启动模型、水动力分析模型以及FLO-2D模型,对祁连山东段金跃沟有无矿渣两种情境进行对比分析,探究各自的成灾过程,结合祁连山东段多个典型矿区案例,揭示祁连山东段由矿渣堆料诱发的链生灾害放大机制。结果 金跃沟废弃硅矿堆料体结构松散、抗剪强度低、安全系数低;此次极端降雨条件下矿渣堆料发生失稳、滑坡,滑坡体涌入沟道,导致行洪通道挤压,并为泥石流提供大量的松散物源,泥石流容重提升约20%,从自然状态下的稀性流转变为亚黏性流,破坏力更强。地形与物源变化共同导致泥石流强度变大,流速较自然状态下提升43%、洪峰流量增大58.84%,综合表现为泥石流行洪范围扩大,高危型性区域占主导。结论极端降雨下矿渣堆料放大了沟道 “矿渣失稳-侵蚀放大-灾害链生”灾害影响。建议针对性优化矿渣堆料的治理,强化泥石流风险防控,为祁连山东段及同类地质-气候背景区灾害防控与生态安全屏障建设提供理论依据。

       

      Abstract: ObjectiveTaking the "9·03" mining slag debris flow event in Jinyue Ravine, Xining , in 2024 as an example, the effect and cascading mechanisms of historically accumulated mining slag on channel erosion was elucidated in eastern Qilian Mountains under changing climatic conditions.Methods Through field investigations and laboratory experiments, the Iverson debris-flow initiation model, hydrodynamic analysis, and the FLO-2D model were employed to conduct a comparative analysis of disaster processes in the Jinyue Ravine under two scenarios (i.e., with and without mine waste deposits). By integrating multiple typical mining area cases in the eastern Qilian Mountains, the amplification mechanism of cascading hazards induced by mine waste accumulation in the region was revealed.Results Under the conditions of loose structure of the abandoned silica ore heap the low shear strengthand the extreme rainfall conditions, thee silica ore heap became instable and landslide occurred. The landslide body that poured into the channel led to the extrusion of the flood channel and provided a large amount of loose material source for the debris flow, leading to increased flow bulk density by about 20 %. The dilute flow changed from in the natural state to the sub-viscous flow with stronger destructive power. The change of topography and provenance led to the increase of debris flow intensity. The flow velocity was 43 % higher than that in the natural state, and the flood peak flow was increased by 58.84 %. The flood range of debris flow was expanded under extreme rainfall events and the high-risk area was dominant.Conclusions The mine residues became instable and the disasters were developed and amplified under extreme rainfall event in the eastern Qilian Mountains, providing a typical example of disaster chain processes in areas disturbed by anthropogenic mining activities. It is recommended that mitigation strategies for mine residues be optimized based on the disaster amplification process of residue-induced ravine erosion, and that debris flow risk prevention and control engineering be strengthened. These findings provide a theoretical foundation for disaster prevention and control as well as ecological security barrier construction in the eastern Qilian Mountains and other regions with similar geological and climatic backgrounds. Keywords : slag heap material;ravine erosion;disaster amplification;FLO-2D simulation;eastern section of Qilian Mountains

       

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