许国胜, 李回贵, 关金锋. 水体下开采覆岩破断及裂隙演化规律[J]. 煤矿安全, 2018, 49(4): 42-45,49.
    引用本文: 许国胜, 李回贵, 关金锋. 水体下开采覆岩破断及裂隙演化规律[J]. 煤矿安全, 2018, 49(4): 42-45,49.
    XU Guosheng, LI Huigui, GUAN Jinfeng. Laws of Overburden Strata Rupture and Fissure Evolution During Mining Under Water Body[J]. Safety in Coal Mines, 2018, 49(4): 42-45,49.
    Citation: XU Guosheng, LI Huigui, GUAN Jinfeng. Laws of Overburden Strata Rupture and Fissure Evolution During Mining Under Water Body[J]. Safety in Coal Mines, 2018, 49(4): 42-45,49.

    水体下开采覆岩破断及裂隙演化规律

    Laws of Overburden Strata Rupture and Fissure Evolution During Mining Under Water Body

    • 摘要: 鉴于水体下开采采动裂隙发育规律对井下安全性评价的重要作用,以水库下综放开采为工程背景,采用关键层理论、组合岩梁理论,并采用相似模拟物理试验手段,研究了覆岩的破断规律,以及在覆岩组合岩层及关键层破断过程中,岩层垂直位移、导水断裂带发育高度以及覆岩裂隙网络的演化规律。研究结果表明:主关键层垮落前后,观测线采空区中部测点的下沉曲线斜率较大,岩层垂直方向上下沉剧烈;导水断裂带发育高度曲线随着覆岩岩层组合周期性垮落呈现出台阶跃升,且两台阶的间距即为覆岩的周期垮落步距;当主关键层垮落后,覆岩导水断裂带发育高度稳定,导水断裂带顶界位于亚关键层Ⅱ下部。裂隙网络的富集区主要集中在前后煤壁,且靠近开切眼侧裂隙区裂隙密度大于停采线侧裂隙密度,由于采空区中部破断岩层在上覆载荷的作用下裂隙压实闭合,造成模型裂隙密度曲线呈偏态“马鞍”状。

       

      Abstract: In view of the important role of fracture development laws in safety evaluation during coal seam mining under the water body, based on the engineering background of full-mechanized caving mining under the reservoir, by the key strata theory, the combined rock beam theory, and similar physical simulation test method, we studied the breaking laws of overburden rock and the vertical displacement of rock strata, the development height of water conducting fractured zone and the evolution laws of overlying fissure network in the process of rock forming and critical layer breaking. The research result shows that: before and after the collapse of the main key stratum, the subsidence curve slope of observation points in the middle position of gob is larger, and the overburden stratum sinks in the vertical direction shapely; water conducting fractured zone height curve steps up with the periodic rupturing of combimed rock beams, and two steps spacing is the cycle of overburden rock rupture step distance; after the main key stratum breaking down, overburden rock water conducting fractured zone finally reaches the bottom of the inferior key stratum Ⅱ. Fracture network enrichment region mainly focused on the front and rear coal walls, and the fracture density in the crack area near the open-cut hole is greater than that in the lateral fissure of the stop line. Due to the fracture compaction of the fractured rock strata in the middle of the goaf, the fracture density curve of the model is skewed to the “saddle”.

       

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