汤铸, 陈才贤, 赵忠义. 松散层在埋深中占比对地表移动变形特征的影响[J]. 煤矿安全, 2017, 48(4): 211-214.
    引用本文: 汤铸, 陈才贤, 赵忠义. 松散层在埋深中占比对地表移动变形特征的影响[J]. 煤矿安全, 2017, 48(4): 211-214.
    TANG Zhu, CHEN Caixian, ZHAO Zhongyi. Influence of Loose Bed Accounted for Depth on Surface Movement Deformation Characteristics[J]. Safety in Coal Mines, 2017, 48(4): 211-214.
    Citation: TANG Zhu, CHEN Caixian, ZHAO Zhongyi. Influence of Loose Bed Accounted for Depth on Surface Movement Deformation Characteristics[J]. Safety in Coal Mines, 2017, 48(4): 211-214.

    松散层在埋深中占比对地表移动变形特征的影响

    Influence of Loose Bed Accounted for Depth on Surface Movement Deformation Characteristics

    • 摘要: 为了研究松散层在埋深中占比对地表移动变形特征的影响,以赵固矿区地表移动观测数据为基础,研究了松散层占比对地表下沉特征、地表最大下沉速度、地表最大下沉速度滞后距以及地表不同阶段移动持续时间的影响。结果表明在厚松散层条件下,松散层在埋深中占比增大3%,地表下沉系数由0.67增大到0.96,增大近43.3%;地表最大下沉速度系数由1.26增大到1.49,增大近18.4%;地表最大下沉速度滞后距由188 m缩减到97 m,缩短近48.4%,最后通过数值模拟,得出松散层占比对地表移动的一般性规律,并拟合出适合该地质条件的主要移动参数预计公式。

       

      Abstract: In order to study the influence of loose bed accounted for depth on surface subsidence characteristics in thick unconsolidated layers, on the basis of the surface movement observation data of Zhaogu Coal Mine Area, the influence of loose bed accounted for depth on characteristics of surface subsidence, the maximum ground sinking speed, the maximum ground subsidence velocity lag distance and the influence of duration of ground surface at different stages was analyzed respectively under the condition of mining under thick unconsolidated layers. It was concluded that under the condition of thick loose bed, with the increase of loose bed accounted for depth, surface subsidence coefficient increases from 0.67 to 0.96, increasing nearly 43.3%; coefficient of maximum subsidence velocity increases from 1.26 to 1.49, increased by 18.4%; the lag distance of maximum subsidence velocity reduced from 188 m to 97 m, by almost 48.4%. At last, through the numerical simulation, the general rule of the ground surface displacement by the proportion of the loose layer was got, and the prediction formula of the main moving parameters which suit for the geological condition were fitted.

       

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