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A Numerical Study on Gangue Backfilling Mining in a Thick Alluvium Soil Environment

机译:厚冲积层环境下煤ue石回填开采的数值研究

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In this paper, gangue backfilling mining in an environment of alluvium soil with different thicknesses was simulated using FLAC3D software and taking into account the actual geological conditions of a coal mine in eastern China. Furthermore, the effects of gangue backfilling mining on the surface subsidence in this environment were analyzed. The results show that with an increase in the thickness of the alluvium soil, the surface subsidence basin range significantly increases, whereas the surface subsidence, surface horizontal movement value and final compression ratio of the backfilling body decrease linearly. Moreover, the effect of the alluvium soil’s thickness on the surface subsidence coefficient, surface horizontal movement coefficient and final compression ratio of the backfilling body is larger than that of the bedrock thickness; whereas the effect of the bedrock thickness on the surface subsidence is greater that of the alluvium soil’s thickness. Additionally, with an increase in the proportion of the alluvium soil’s thickness at a certain mining depth, the surface subsidence coefficient increases exponentially and the surface horizontal movement coefficient decreases in a quadratic polynomial. Meanwhile, backfilling mining can significantly limit the failure caused by overburdening and surface deformation, and lead to the key strata supporting the overlying strata and soil mass effectively. Therefore, the soil mass in a thick alluvium soil environment only causes a small deformation, if any, and reduces the rheological behavior of the thick alluvium soil, which is better for the protection of the surface buildings. These findings have great significance with regard to understanding the surface movement rules of gangue backfilling mining in an environment of alluvium soil with different thicknesses, and could lead to better guidance in this area.
机译:本文利用FLAC3D软件模拟了不同厚度的冲积土环境中的石回填开采,并考虑了华东煤矿的实际地质情况。此外,分析了在这种环境下煤石回填开采对地面沉降的影响。结果表明,随着冲积土厚度的增加,地表沉陷盆地范围明显增大,而回填体的地表沉陷,地表水平运动值和最终压缩比线性减小。此外,冲积土厚度对回填体地表沉陷系数,地表水平运动系数和最终压缩比的影响大于基岩厚度。而基岩厚度对地表沉降的影响要大于冲积层土壤厚度的影响。另外,在一定的开采深度下,随着冲积层土壤厚度比例的增加,二次多项式的地表沉降系数呈指数增长,地表水平移动系数呈下降趋势。同时,回填开采可以显着减少因超载和地表变形引起的破坏,并导致关键地层有效地支撑上覆地层和土壤质量。因此,厚的冲积土环境中的土壤质量只会引起很小的变形(如果有的话),并且会降低厚的冲积土的流变行为,这对于保护地面建筑物更好。这些发现对于理解不同厚度的冲积土环境中脉石回填开采的地表运动规律具有重要意义,并可能在该领域提供更好的指导。

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