考虑含水率影响的露天矿排土场排弃层序结构优化

    Optimization of dumping sequence structure of open-pit dump considering moisture content effect

    • 摘要: 排土场是露天矿山用于处置开采过程中产生的剥离物的关键场所,其长期安全与稳定是矿山安全管理的核心任务。排土场边坡稳定性受排弃物料的物理特性、排弃层序结构等多种因素的综合影响。为提高排土场边坡稳定性,并最大限度地增大边坡角度以提升其有效容量,构建了排土场边坡排弃层序结构模型,综合运用有限元法、极限平衡法及相似模拟试验,系统分析了主要排弃物料在不同层序结构下对边坡滑动模式及稳定性的影响规律,重点研究了含水率变化对排弃物料力学特性的影响机制。在此基础上,进一步探究了在物料特性动态变化条件下的最优排弃层序结构对边坡稳定性的提升作用,并对层序组合进行了优化,旨在确定边坡稳定性最佳且工程条件最为合理的排土场排弃层序组合方式。研究结果表明:在岩土天然含水率状态下,细砂岩、粗砂岩和泥岩的内摩擦角与黏聚力分别为21.6°、31.27 kPa,17.3°、19.57 kPa,以及20.7°、37.09 kPa;随着含水率梯度上升,各组排弃物料的内摩擦角与黏聚力分别下降至16.2°、22.97 kPa(细砂岩),13.2°、14.73 kPa(粗砂岩),以及12.2°、21.53 kPa(泥岩)。对比发现,泥岩的力学参数对含水率变化最为敏感。通过分析排弃物料参数及层序结构变化对边坡稳定性的影响规律,最终确定了黄土−泥岩−粗砂岩−细砂岩为最优的排弃层序结构。

       

      Abstract: The waste dump is a key site for open-pit mines to dispose of overburden generated during mining operations, and its long-term safety and stability constitute the core task of mine safety management. The slope stability of the waste dump is comprehensively affected by multiple factors such as the physical properties of dumped materials and the sequence structure of dumping layers. To improve the slope stability of the waste dump and maximize the slope angle to increase its effective capacity, a model for the dumping sequence structure of waste dump slopes was established. By comprehensively applying the finite element method, limit equilibrium method and similar simulation test, this study systematically analyzed the influence laws of main dumped materials on slope sliding modes and stability under different sequence structures, and mainly investigated the influence mechanism of water content changes on the mechanical properties of dumped materials. On this basis, the study further explored the enhancement effect of the optimal dumping sequence structure on slope stability under the condition of dynamic changes in material properties, and optimized the sequence combination, aiming to determine the dumping sequence combination mode of the waste dump with the best slope stability and the most reasonable engineering conditions. The results show that under the natural water content state of rock and soil, the internal friction angles and cohesions of fine sandstone, coarse sandstone and mudstone are 21.6° & 31.27 kPa, 17.3° & 19.57 kPa, and 20.7° & 37.09 kPa, respectively. With the increase of water content gradient, the internal friction angles and cohesions of all groups of dumped materials decrease to 16.2° & 22.97 kPa (fine sandstone), 13.2° & 14.73 kPa (coarse sandstone), and 12.2° & 21.53 kPa (mudstone). Comparative analysis reveals that the mechanical parameters of mudstone are the most sensitive to water content changes. Through analyzing the influence laws of dumped material parameters and sequence structure changes on slope stability, the optimal dumping sequence structure is finally determined as loess-mudstone-coarse sandstone-fine sandstone.

       

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