煤层开采扰动下底板岩体全时域变形破坏特征分析

Analysis of full-time-domain deformation and failure characteristics of floor rock mass under coal seam mining disturbance

  • 摘要: 现有针对工作面底板岩体变形破坏特征的研究主要聚焦于工作面采动影响阶段底板岩体的破坏特征,忽视了工作面卸荷对底板岩体的损伤破坏,所得结果具有一定的局限性。实际工况中,工作面底板岩体发生支承压力扰动—卸荷的力学状态转变,工作面卸荷亦使得底板岩体产生一定范围的张拉破坏。针对该问题,以淮南矿业(集团)有限责任公司潘二煤矿11123工作面主采煤层底板岩体为研究对象,针对其在支承压力扰动与采空区卸荷2个阶段所处不同受力状态,分别建立相应的底板岩体力学模型,并基于Mohr−Coulomb准则与岩体卸荷破坏机制,分析不同阶段底板岩体的变形破坏特征。研究结果表明:① 煤体强度、开采强度、初始受力均影响采动应力分布规律,采动应力集中系数与塑性区深度负相关。② 采高越小,超前采动支承应力越大,底板岩体压剪破坏深度越小,采高为2.5~4.0 m时,受超前采动应力扰动作用底板岩体压剪破坏深度分别为16.96,18.02,18.63,19.02 m。③ 卸荷条件下,底板岩体卸荷前后的最大主应力方向保持高度一致,超前采动支承应力增大,引起卸荷量上升,进而增大卸荷张拉破坏的深度,当采高为2.5 ~4.0 m时,底板岩体对应的卸荷破坏深度分别为21.56,19.15,18.03,17.74 m。 现场测试结果表明:初采高度为3.5 m,在光纤长度12 m(垂高8.5 m)位置处,岩层首次出现可检测的拉应变,峰值达+1 800 με;在光纤长度为15~37 m(垂高10.6~26.2 m)内,岩层呈现持续性压应变,最大值达−1 500 με;光纤长度为37~57.75 m内的岩层基本上保持稳定,没有受到明显的采动影响;垂高13.2~17.7 m内,电流值降低至10 mA,综合测试结果获得底板岩体最大破坏深度为17.7 m,该实测结果与卸荷理论所计算破坏深度大致相当。

     

    Abstract: Existing studies on the deformation and failure characteristics of the floor rock mass in working faces mainly focus on the failure characteristics during the mining disturbance stage, while neglecting the damage and failure of the floor rock mass caused by the unloading of the working face, and thus the results have certain limitations. In actual engineering conditions, the floor rock mass undergoes a mechanical state transition from abutment pressure disturbance to unloading, and the unloading of the working face also induces tensile failure within a certain range of the floor rock mass. To address this issue, the floor rock mass of the main coal seam in the working face 11123 of Pan'er Coal Mine, Huainan Mining (Group) Co., Ltd., was taken as the study object. Based on the different stress states of the floor rock mass during the abutment pressure disturbance stage and the goaf unloading stage, corresponding mechanical models of the floor rock mass were established. Combined with the Mohr-Coulomb criterion and the unloading failure mechanism of the rock mass, the deformation and failure characteristics of the floor rock mass at different stages were analyzed. The results showed that: ① Coal strength, mining intensity, and initial stress all affected the distribution pattern of mining-induced stress, and the mining-induced stress concentration coefficient was negatively correlated with the depth of the plastic zone. ② When the mining height decreased, the advanced abutment pressure increased, and the depth of compression-shear failure of the floor rock mass decreased. When the mining height was 2.5–4.0 m, the compression-shear failure depths of the floor rock mass under the disturbance of advanced abutment pressure were 16.96, 18.02, 18.63, and 19.02 m, respectively. ③ Under unloading conditions, the direction of the maximum principal stress of the floor rock mass before and after unloading remained highly consistent. Greater advanced abutment pressure led to increased unloading magnitude, thereby deepening the tensile failure induced by unloading. When the mining height was 2.5–4.0 m, the corresponding unloading failure depths of the floor rock mass were 21.56, 19.15, 18.03, and 17.74 m, respectively. Field test results showed that when the initial mining height was 3.5 m, tensile strain was first detected at an optical fiber length of 12 m (vertical height 8.5 m), with a peak value of +1 800 με. Continuous compressive strain occurred within the optical fiber length range of 15–37 m (vertical height 10.6–26.2 m), with a maximum value of −1 500 με. The rock mass within the optical fiber length range of 37–57.75 m remained basically stable and was not significantly affected by mining disturbance. Within the vertical height range of 13.2–17.7 m, the current value decreased to 10 mA. Based on comprehensive test results, the maximum failure depth of the floor rock mass was determined to be 17.7 m, which was generally consistent with the failure depth calculated by unloading theory.

     

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