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基于FDEM的浅埋特厚煤层采动覆岩破断规律及地表沉陷预测

FDEM-based analysis of overlying strata fracture mechanisms and surface subsidence prediction in shallow-buried ultra-thick coal seam mining

  • 摘要: 浅埋特厚煤层广泛分布于我国西部矿区,因其埋深浅、基岩层薄和松散层厚等赋存特征,在开采过程中兼具覆岩破断开裂与地表沉陷扰动双重致灾特征。基于连续−非连续耦合的FDEM方法既可以实现变形、断裂和破碎的从连续体到非连体的过渡,又可以考虑连续开挖导致的应力扰动叠加效应,是实现浅埋特厚煤层采动地表沉陷精准预测的可行路径。通过FDEM模拟分析了回采过程中覆岩破断过程和周期来压规律,追踪随采破断引发的阶段性沉降,并基于现场监测校验最终实现沉陷的可靠预测。研究表明:浅埋特厚煤层回采中覆岩关键层初次破断导致覆岩裂隙向上发展,切落体的剪切滑移失稳伴随着冒落带与裂隙带高度不断增大,其峰值分别为采厚的5.6倍与6.1倍,覆岩断裂类型从张拉–拉剪主导向剪切破坏转型;FDEM模型精准捕捉覆岩破断诱发的矿压特征:初次破断步距与实测一致,矿压峰值及周期来压步距模拟误差<5%;浅埋特厚煤层主关键层与高位协控岩层的协同破断主导了地表沉陷的完整发育过程,FDEM模型显示回采不同距离时地表沉降变化趋势与现场实测数据相吻合;FDEM模拟结果准确复现了浅埋特厚煤层采动覆岩破断规律,精准预测了地表沉陷,模拟与监测结果的误差主要来源于时间尺度的不匹配与复杂的现场工程条件。

     

    Abstract: Shallow buried extra-thick coal seams are widely distributed in the western mining areas of China, due to their shallow burial depth, thin bedrock layers and thick loose layers, and other storage characteristics, in the process of mining both overburden rock fracture and cracking and surface subsidence perturbation of the dual disaster-causing characteristics. The FDEM method based on continuous-discontinuous coupling can not only realise the transition of deformation, fracture and breakage from continuum to discontinuity, but also take into account the superposition effect of stress perturbation caused by continuous excavation, which is a feasible path to realise the accurate prediction of surface subsidence of shallow buried extra-thick coal seam mining. The FDEM simulation analyses the overburden breakage process and the cycle pressure law during the mining process, traces the stage settlement caused by the breakage, and finally realizes the reliable prediction of subsidence based on the on-site monitoring and calibration. The study shows that: The initial breakage of the overburden key layer in the back mining of shallow buried extra-thick coal seam leads to the upward development of overburden fissures, and the shear slip instability of the cut-off body is accompanied by the increasing height of the fallout zone and the fissure zone, whose peaks are 5.6 times and 6.1 times of the mined thickness, respectively, the fracture type of overburden is transformed from tension-tension-shear dominated to shear damage; The FDEM model accurately captures the mineral pressure characteristics induced by overburden fracture: the initial fracture step is consistent with the actual measurement, and the simulation error of the peak mineral pressure and the cycle pressure step is <5%; Under the condition of shallow buried extra-thick coal seam, the fracture of the main key strata provides subsidence space for the instability of the high main control strata, and the fracture of the high main control strata further enlarges the settlement amplitude and controls the scope of the subsidence area. The FDEM model shows that the change trend of surface subsidence at different mining distances is consistent with the field measured data; The FDEM simulation results accurately reproduced the breakage law of overburden rock in shallow buried extra thick coal seam mining and accurately predicted the surface subsidence, and the error between the simulation and monitoring results mainly came from the mismatch of the time scale and the complex engineering conditions in the field.

     

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