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双断层影响下煤层开采覆岩裂隙演化分形特征研究

Study on fractal characteristics of overburden fracture evolution in coal seam mining under the influence of double faults

  • 摘要: 为研究双断层影响下覆岩裂隙时空演化规律,以贵州土城矿为工程背景,在模拟煤层开挖的基础上,通过分形几何理论定量表征覆岩裂隙发育特征,揭示覆岩裂隙网络的分形演化规律,进而对回风巷上隅角瓦斯浓度与分形维数关系进行分析。研究结果表明:断层影响区覆岩裂隙分形维数为1.056~1.544,其动态演化过程可被划分为升维、降维、二次升维和稳定4个特征阶段;当工作面推进至断层影响区域时,分形维数出现突增,据此提出了包括加密断层区域瓦斯抽采、顶端岩体及断层构造固化等在内的综合防范措施;覆岩裂隙分形维数与上隅角瓦斯浓度呈显著正相关关系。

     

    Abstract: In order to study the temporal and spatial evolution law of overburden fracture under the influence of double faults,based on the engineering background of Tucheng Coal Mine in Guizhou Province,the study employed fractal geometry theory to quantitatively characterize the development of overburden fracture on the basis of simulated coal mining activities, thereby obtaining the fractal evolution law of the overburden fracture network. Subsequently, the relationship between gas concentration in the upper corner of return airway and fractal dimension was analyzed. The results show that the fractal dimension of the overburden fracture in the fault affected area ranges from 1. 056 to 1. 544,and its dynamic evolution can be divided into four characteristic stages: dimensional enhancement stage, dimensional reduction stage, secondary dimensional enhancement stage,and stable stage. A sudden increase in the fractal dimension value is observed when the working face advances to the fault affected area,suggesting the implementation of comprehensive preventive measures including intensified gas drainage in fault zones and solidification of roof strata and fault structures. There is a significant positive correlation between the fractal dimension of overburden fractures and the gas concentration in the upper corner.

     

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