近距离分岔煤层底板破坏深度及规律研究

Study on the depth and pattern of floor failure in closely spaced bifurcated coal seams

  • 摘要: 目前的底板破坏深度计算公式多针对特定底板结构。由于分岔煤层的地质特征复杂,上下煤层间的相对倾角及煤层间距的变化特性导致其底板结构与已有研究情形存在显著差异,难以直接套用现有公式进行底板破坏深度计算。针对上述问题,以霍洛湾煤矿3−1分岔煤层为工程背景,基于单一岩层塑性滑移线场理论,得到近距离分岔煤层3种破坏情况下的最大破坏深度理论解,采用数值模拟得到开采过程中底板塑性区演化规律及破坏深度,采用压水试验实测工作面底板破坏深度。理论分析结果表明:塑性滑移线旋转中心位置因底板岩性差异而变化,致使底板破坏深度先陡增后渐降,计算得到底板破坏深度为13.30~17.62 m。数值模拟结果表明:底板以剪切破坏形式为主,破坏范围由泥岩层逐渐向3−1下煤层及砂质泥岩层发育,底板煤岩结构变动导致破坏深度在12.36~16.53 m间变化,与理论分析呈现同样趋势。现场实测结果表明:工作面回采前后底板钻孔的注水漏失量出现显著变化,底板岩层裂隙发育充分,破坏深度为13.52~17.20 m。根据3−1上煤层底板破坏情况对3−1下煤层顶板进行分类并提出顶板预控对策,以保证煤层安全开采。现场实测结果验证了分岔煤层底板塑性滑移线场的实用性。

     

    Abstract: At present, most existing formulas for calculating floor failure depth are applicable to specific floor structures. Due to the complex geological characteristics of bifurcated coal seams, the variable relative dip angles and spacing between the upper and lower seams lead to a floor structure that differs significantly from those considered in previous studies, making it difficult to directly apply existing formulas to calculate the floor failure depth. To address this issue, this study took the 3-1 bifurcated coal seam in Holuowan Coal Mine as the engineering background and derived the theoretical solutions for the maximum failure depth under three failure scenarios of closely spaced bifurcated coal seams, based on the plastic slip line field theory for a single rock layer. Numerical simulations were conducted to obtain the evolution pattern of the plastic zone and the failure depth of the floor during mining. Water injection tests were employed to measure the actual failure depth of the floor in the working face. Theoretical analysis results showed that the position of the rotation center of the plastic slip line field varied with the lithology of the floor, leading to a sharp increase followed by a gradual decrease in the floor failure depth, which was calculated to be 13.30-17.62 m. Numerical simulation results indicated that shear failure was the dominant mode, and the failure zone extended from the mudstone layer to the lower 3-1 coal seam and the sandy mudstone layer. Variations in the coal-rock structure of the floor led to changes in the failure depth, ranging from 12.36 to 16.53 m, showing a similar trend to the theoretical analysis. Field measurement results showed significant changes in water loss from borehole injection before and after mining, indicating well-developed fractures in the floor strata, with a failure depth of 13.52-17.20 m. Based on the failure conditions of the floor beneath the upper 3-1 coal seam, the study classified the roof of the lower 3-1 coal seam, and pre-control strategies were proposed to ensure safe mining of the coal seam. The field measurements verified the practicality of the plastic slip line field model for bifurcated coal seam floors.

     

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