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单侧采空覆岩变形规律及导水裂隙带发育高度预测

Deformation law of overburden rock in unilateral mined-out area and prediction of development height of water conducted zone

  • 摘要: 针对厚松散层矿区单侧采空条件下导水裂隙带时空演化规律复杂、现有预测方法适应性不足等问题,探究单侧采空条件下覆岩变形演化规律,建立考虑采空区预破坏效应的导水裂隙带发育高度预测方法。以淮北矿区某煤矿866工作面为研究对象,采用理论分析与现场监测相结合的方法,构建了基于分布式光纤的“待采工作面−煤柱−邻近采空区”三位一体覆岩变形监测体系,建立了基于覆岩变形梯度分布的导水裂隙带发育高度量化判定指标,提出了单侧采空条件下的导水裂隙带发育高度预测模型。结果表明:采场覆岩空间分异特征显著,采空区沉陷呈现残余沉降与采动沉降先后主导的复合变形模式,工作面区域受强动态开采扰动控制,煤柱区表现为应力滞后传递特性;基于光纤累积绝对变形贡献率曲线拐点判据,结合不同深度区间的覆岩变形分布特征,确定导水裂隙带发育极限高度为77 m,开采稳定后导水裂隙带内岩层绝对变形量占总绝对变形量的87%;已有采空区在−280 m深度形成上压缩−下拉伸双区变形模式,导致下方岩层离层。结合关键层理论和板理论提出了考虑单侧采空区预破坏效应的导水裂隙带预测方法,根据关键层理论将覆岩划分为高位、低位岩层,结合板理论建立破坏判定模型,预测866工作面的导水裂隙带高度为71 m,与实测值的相对误差仅8.4%。

     

    Abstract: A study on the spatiotemporal evolution of the water conducted zone (WCZ) in thick loose layers under a unilateral mined-out area is conducted to overcome challenges such as the complexity of WCZ development and limitations of existing prediction methods. A prediction model for the WCZ development height is proposed, incorporating the pre-damage effect from the existing mined-out area. The research is based on the 866 working face of a coal mine in Huaibei Mining Area. A combined theoretical analysis and field monitoring approach is adopted, and a “working face-coal pillar-adjacent mining area” three-in-one monitoring system for overburden deformation is established using distributed fiber-optic technology. A quantitative determination index for the WCZ development height is formulated based on the gradient distribution of overburden deformation, and a prediction model for the development height of the WCZ under unilateral mined-out area conditions is proposed. Results show that the spatial heterogeneity of the overburden is significant. The subsidence of the mining area exhibits a composite deformation mode dominated by residual subsidence and mining-induced subsidence. The working face area is mainly controlled by dynamic mining disturbance, while the coal pillar zone exhibits stress lag characteristics. The development height of the WCZ is determined by analyzing the inflection point in the cumulative absolute deformation contribution rate curve obtained from distributed fiber optic monitoring, along with the deformation characteristics at various depths. The maximum height is identified as 77 m. After mining stabilizes, the absolute deformation of the rock layers in the WCZ accounts for 87% of the total deformation. A double-zone deformation mode, characterized by upper compression and lower tension, is formed at a depth of −280 m in the existing mining area, causing detachment of the underlying rock layers. A prediction method for the WCZ height that considers the pre-damage effect of the unilateral mined-out area is proposed based on the key stratum theory and slab theory. The overburden is divided into upper and lower rock layers using the key stratum theory, and a failure criterion model is established based on slab theory. The predicted development height of the WCZ for the 866 working face is 71 m, with a relative error of only 8.4% compared to the measured value.

     

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