采动覆岩惯性水平移动时空演化规律及地表预计模型

Spatiotemporal evolution pattern of the inertial horizontal displacement of mining overburden and a surface prediction model considering inertial horizontal displacement

  • 摘要:
    目的 大量实测数据显示,在采动影响区中部,地表走向水平移动往往不为0,这一现象与传统认知规律相违背,导致传统水平移动预计模型在预计时总是出现系统性偏差。
    方法 以安徽淮南顾桥矿1414工作面为研究对象,利用实测数据与数值模拟分析方法,研究采动覆岩内部和地表水平移动的时空演化现象,分析采空区边界水平移动和中部惯性水平移动的来源、规律和分布特征,构建了考虑惯性水平移动的地表预计新模型,并在该矿1117工作面进行了验证。
    结果和结论 (1)走向超充分采动时,地表走向除了在采动区边界拐点的两翼存在对称的走向水平移动外,在采动区中部还会出现一种沿走向的惯性水平移动,这种移动导致最终叠加形成的地表走向水平移动与倾斜变形不成正比,与传统模型不符合。(2)惯性水平移动是地下开采过程的产物,模拟过程中递进步距越小,惯性水平移动越明显,且与采高呈明显的正比关系。(3)惯性水平移动在地表采动区中心达到最大,在采动影响区边界为0,其整体分布与地表下沉分布相似。构建的新模型在淮南顾桥矿1117工作面地表水平移动预计中取得了良好效果,准确预测了两侧边界的水平移动差异,以及采动区中部的水平移动现象,水平移动拟合中误差7.0%。研究成果对揭示地表水平移动机理,完善开采沉陷基础理论具有重要意义。

     

    Abstract:
    Objective Substantial measured data indicate that the along-strike horizontal displacement of the surface tends to be nonzero in the central part of the mining-affected zone. This phenomenon deviates from traditional understanding, leading to systematic deviations in the predicted results of the traditional prediction model for horizontal displacement.
    Methods This study investigated mining face 1414 of the Guqiao Coal Mine in the Huainan mining area, Anhui Province. Using measured data and numerical simulation methods, this study explored the spatiotemporal evolution of the horizontal displacement within the mining overburden and of the surface. Then, it analyzed the sources, patterns, and distribution characteristics of both horizontal displacement along the goaf boundary and inertial horizontal displacement in the center of the mining area. Accordingly, this study constructed a new surface prediction model considering inertial horizontal displacement. Finally, this model was verified in mining face 1117 of the Guqiao coal mine.
    Results and Conclusions  In the case of along-strike supercritical mining, the symmetrical along-strike horizontal displacement of the surface was observed on both flanks of the boundary inflection points of the mining zone. Additionally, along-strike inertial horizontal displacement also occurred in the central part of the mining zone. Consequently, the superimposed along-strike horizontal displacement of the surface was not proportional to the surface deformations in the inclination direction, failing to match traditional models. Inertial horizontal displacement arose from the underground mining process. In the simulation process, a smaller progressive step distance corresponded to more pronounced inertial horizontal displacement, which showed a distinct directly proportional relationship with the mining height. Inertial horizontal displacement peaked in the center of the surface mining zone and measured zero along the boundary of the mining-affected zone, generally resembling the distribution of surface subsidence. The new surface prediction model performed well in predicting the horizontal displacement of the surface in mining face 1117. Specifically, it yielded accurate predicted results of the difference in the horizontal displacement of the boundaries on both sides of the goaf and the horizontal displacement in the central part of the mining zone, with a fitting error of 7.0%. The results of this study hold significant implications for revealing the mechanisms underlying the horizontal displacement of the surface and improving the fundamental theory of mining subsidence.

     

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