煤炭工程 ›› 2026, Vol. 58 ›› Issue (3): 121-129.doi: 10.11799/ce202603015

• 生产技术 • 上一篇    下一篇

大倾角大采高工作面矸石充填顶板应力偏转与围岩稳定性研究

王建军,王 萌,杨文化,郭 强   

  1. 1. 山西焦煤汾西矿业金辛达煤业,山西 临汾 041000

    2. 中煤科工集团北京华宇工程有限公司 西北分公司,陕西 西安 710075

    3. 西安科技大学 能源与矿业工程学院,陕西 西安 710054

  • 收稿日期:2025-09-15 修回日期:2025-11-06 出版日期:2026-03-10 发布日期:2026-04-14
  • 通讯作者: 王萌 E-mail:wangmeng0473@163.com

Study on roof stress deflection and surrounding rock stability in steeply inclined large mining height working faces with gangue backfill#br#

  • Received:2025-09-15 Revised:2025-11-06 Online:2026-03-10 Published:2026-04-14

摘要:

为探究大倾角工作面矸石支撑条件下顶板应力偏转规律与围岩稳定性特征,采用理论分析与数值计算相结合的方法,研究非均衡充填效应下矸石支撑区域及顶板岩梁的破断演化规律,分析采场煤岩非对称时空变形特征与应力偏转响应机制,揭示矸石支撑对大倾角采场围岩采动力学行为的影响机理。研究结果表明:受重力与倾角耦合作用影响,矸石支撑充填区域范围随煤层倾角及采厚动态改变,工作面矸石有效支撑区域长度为35.44m,顶板在距开切眼75m处易发生破断失稳。煤层开采卸荷致使上、下端头及矸石充填区形成应力集中区,覆岩主应力矢量呈现非对称偏转,主应力偏转角由采场中上部向两侧边界逐步递减,峰值可达70. 05°;岩层主应力差变化率与剪应力随主应力偏转角增大呈递减分布。垮落矸石可有效承担部分覆岩载荷,改变围岩应力传递路径,岩层内形成2条非对称应力偏转界线;工作面超前支承压力整体降低,其中倾向下部区域降幅最为显著,支承压力峰值向非充填区下部转移。

关键词:

大倾角煤层, 矸石充填, 非均衡约束, 应力偏转, 顶板稳定性, 支承压力, 大采高

Abstract:

In order to explore the stress deflection and stability analysis of roof under the support of gangue in large dip angle working face, the fracture evolution characteristics of gangue support area and roof rock beam under unbalanced filling effect are studied based on theoretical analysis. Combined with numerical calculation, the asymmetric space-time deformation and stress deflection response law of coal rock in stope are analyzed, and the influence mechanism of gangue on the mining dynamic behavior of surrounding rock in large dip angle stope is revealed. The research results show that : affected by the gravity inclination effect, the gangue support filling area changes with the coal seam inclination angle and coal thickness. The length of the gangue support area in the working face is 35.44 m, and the roof is prone to breakage and instability at 75 m. The unloading of coal seam mining leads to the formation of stress concentration at the upper and lower ends and the gangue filling area. The direction of the principal stress vector of the overburden rock is asymmetrically deflected. The principal stress deflection angle gradually decreases from the middle and upper regions to the two sides of the boundary. The peak value of the principal stress deflection angle is 70.05 °. The change rate of the principal stress difference and the shear stress of the rock stratum decrease with the increase of the principal stress deflection angle. The caving gangue bears part of the overburden load, and the stress transfer path changes. There are two asymmetric stress deflection boundaries in the rock layer. The advance abutment pressure of the working face decreases as a whole, and the decrease in the lower part of the tendency is the largest. The peak abutment pressure is transferred to the lower part of the non-filling area.

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