高承压水条件下工作面过断层理论分析

    Theoretical Analysis on Working Face Cross-fault Under High Water Pressure Condition

    • 摘要: 为研究高水压条件下工作面过断层突水机理,在考虑工作面附近矿山压力及水压分布规律的基础上,通过建立力学模型,理论分析了工作面正常推进过程中和过断层开采时底板岩层弯曲变形规律,并给出开采初期和来压过程中跨断层开采突水力学判据。研究结果表明:从开采煤壁至采空区矸石压实区之间的区域为突水脆弱区;在地质条件相似的情况下,工作面经过断层时的底板岩层弯曲量是正常推进过程中底板岩层弯曲量的48倍左右,因此工作面过断层时更易发生突水;来压过程中的作用反力使突水发生的可能性变小;为安全通过断层,应使断层破碎带至采空区矸石压实区之间的距离小于底板梁极限悬臂跨距。

       

      Abstract: In order to study the water inrush mechanism of working face cross-fault under high water pressure condition, on the basis of studying the distribution law of ground pressure and water pressure around working face, it theoretically discussed the deformation characters of the floor strata during the period of normal mining and cross-fault mining by establishing mechanical model, and finally obtained water inrush mechanics criterion of cross-fault mining during early mining period and weighting process. The research results showed the vulnerability area of water inrush was from the mining coal wall to the gangue compaction area of goaf; in the case of similar geological conditions, the volume of floor bending of mining across fault was 48 times of the volume of floor bending of normal mining, so water inrush was more likely to happen as mining across fault; because of the opposing forces, the possibility of water inrush reduced in the weighting process; in order to pass the fault safely, the distance from fault fracture zone to gangue compaction area should be less than the limit cantilever span of floor beams.

       

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