煤矿深部开采工作面覆岩运动特征分析及应力分布规律研究

Movement characteristics of overlying strata and stress distribution law in deep mining face of coal mine

  • 摘要: 【目的】针对深部工作面开采过程中覆岩多关键层组的运动特征及应力分布规律,【方法】综合应用理论分析、数值模拟方法进行研究,【结果】揭示了在深部开采条件下,某矿深部工作面上方存在多个关键层,其中6.88 m细砂岩为低位关键层,9.66 m细砂岩为高位关键层。各关键层(尤其是低位关键层)依次经历断裂、垮落等阶段并伴随应力重新分布现象。高位关键层因其厚度大、强度高的特点,成为影响覆岩稳定性的关键因素,其周期性破断直接导致了工作面周期来压。此外,研究还详细分析了采空区上方及煤壁周边的应力分布。两帮的主应力在工作面推进100 m时达到峰值21.34 MPa后开始下降,最终在采空区中部岩体压实后形成稳定的应力分布模式。【结论】该研究成果为深部矿井的安全高效开采提供了基础的理论依据,对预防开采灾害具有重要意义。

     

    Abstract: Aiming at the movement characteristics and stress distribution law of multi-key strata groups in overlying strata during the deep mining process, this paper comprehensively applies theoretical analysis and numerical simulation methods to study, revealing that there are several key strata above the deep working face in a mine under the conditions of deep mining, among which 6.88 m fine sandstone is low key strata, and 9.66 m fine sandstone is high key strata.Each key strata, especially the lower key strata, goes through the stages of fracture and caving, accompanied by the phenomenon of stress redistribution.Because of its large thickness and high strength, the upper key strata becomes the key factor affecting the stability of overlying rock, and its periodic fracture directly leads to periodic pressure of working face.In addition, the stress distribution above the goaf and around the coal wall is analyzed in detail.The principal stress of the two sides reaches a peak value of 21.34 MPa when the working face advances 100 meters and then begins to decrease, and finally a stable stress distribution pattern is formed after the rock mass is compacting in the middle of the goaf.

     

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