厚松散层地表下沉盆地外边缘区沉陷特征与预计模型修正

Subsidence characteristics of mining affected boundary area and modified surface subsidence prediction model under thick unconsolidated layer

  • 摘要: 煤系地层上部覆有较厚松散层时,煤层开采后地表下沉盆地外边缘区将呈现出范围变大且收敛缓慢的特殊现象,为充分掌握厚松散层条件下地表下沉盆地外边缘区沉陷演变特征,构建出适用于厚松散层条件下的地表沉陷预计模型,以顾北煤矿13121工作面为例,基于实测资料分析了地表下沉盆地外边缘区下沉收敛和扩展的动态演变过程,研究了地表沉陷特征与地质采矿条件间的相关性,揭示了松散层厚度对地表沉陷特征的影响机理,融合Logistic函数修正了传统概率积分模型,基于鲸鱼优化算法提出了修正预计模型参数反演方法,并讨论了地质采矿条件对修正模型新增参数的影响。结果表明:外边缘区地表下沉收敛具有明显分段性,快速收敛区的下沉收敛效应随采动程度增大呈现先快速收敛而后趋缓的过程;下沉盆地外边缘区范围历经先急剧扩展—再稳定扩展—后小幅收缩的演变过程,且地表最大下沉值、快速收敛区收敛效应系数曲线斜率和盆地外边缘区扩展范围与埋深、采高、采动程度系数和松散层占比线性相关;破碎岩体充分压密、采动下沉消耗减小、松散层介质压缩与含水层失水固结4个方面衍生的附加沉降是厚松散层地表下沉盆地外边缘区产生特殊沉降现象的主要原因;修正预计模型在恢复下沉系数q实际物理意义的同时,有效解决了传统概率积分法在预计外边缘区沉陷值收敛速度过快的问题,修正模型新增参数随松散层占比和埋深的增加逐渐减小,随采动程度系数的增加波动增大,但受采高变化影响不大。将修正预计模型应用于顾北煤矿13121工作面工程实践效果较好,研究成果将为厚松散层条件下“三下”压煤开采方案设计提供科学依据,并促进两淮煤粮复合区资源开采与耕地保护的协同发展。

     

    Abstract: When the upper part of coal-bearing strata is covered by the thick unconsolidated layer, the boundary area of the subsidence basin induced by coal mining exhibits a distinctive phenomenon of range expansion and slow convergence. In order to fully understand the evolution characteristics of mining surface subsidence in the outer boundary area of subsidence basin, and build the surface subsidence prediction model under the thick unconsolidated layer. Taking the 13121up working face of Gubei Coal Mine as an example, the dynamic evolution process of surface subsidence convergence effect the outer boundary area of subsidence basin and its range expansion are analyzed using the measured data, and the correlations between surface subsidence characteristics and geological mining conditions are investigated. On this basis, the influence mechanism of unconsolidated layer thickness on surface subsidence characteristics is revealed. Then, the modified surface subsidence prediction model is proposed by integrating the Logistic function, and the parameters inversion method of the modified prediction model is proposed based on the whale optimization algorithm. Finally, the impact of geological and mining conditions on the new parameters of the modified model is discussed. The results show that the surface subsidence convergence in the outer boundary area shows a clear segmented nature, and the convergence effect in the fast convergence zone rapidly converges and then slows down as the mining degree increases, the outer boundary area expansion undergoes a process of sharp expansion, then steady expansion, and finally slight contraction. The maximum surface subsidence value, the slope of subsidence convergence effect coefficient in the fast convergence zone, and the outer boundary area expansion range are linearly correlated with the buried depth, mining height, mining degree coefficient and the proportion of unconsolidated layer in the overlying rock. The additional subsidence caused by the full compaction of broken rock, the reduction of mining subsidence consumption, the compression of unconsolidated layer medium and the consolidation of aquifer water loss is the main reason for the special subsidence phenomenon of boundary area in the thick unconsolidated layer subsidence basin. The modified surface subsidence prediction model can effectively solve the problem that the predicted results of the probability integral model converge too fast in the outer boundary area while restoring the actual physical significance of the subsidence coefficient q. The new parameters of the modified model gradually decrease with the increase of unconsolidated layer proportion and burial depth, and fluctuation increase with the increase of mining degree coefficient, but are not significantly affected by the changes of mining height. The application of the modified prediction model to the engineering practice of the 13121up working face of Gubei Coal Mine has achieved good results. These research results will provide a scientific basis for the coal mining design under buildings, water-bodies and railways in the thick unconsolidated layer condition, and promote the coordinated development of resource exploitation and farmland protection in the area where coal and grain coexist in Huainan and Huaibei.

     

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