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    煤层底板采动损伤渗流演化致灾特征及控制研究

    Study on disaster-causing characteristics and control of mining-induced damage seepage evolution of coal seam floor

    • 摘要: 煤层开采过程中,采动扰动与高承压水耦合作用易诱发底板裂隙贯通、渗流突增,严重威胁矿井安全生产。为精准揭示承压含水层条件下煤层底板采动损伤渗流致灾特征,科学有效控制底板水害,以酸刺沟煤矿工程地质条件为依托,综合考虑多场耦合机制,建立精细化底板流固耦合数值计算模型,系统探究工作面回采全过程中底板应力场分布、塑性损伤发育及渗流场动态响应演化特征。研究结果表明,工作面回采扰动后,采空区边缘与煤壁前方出现显著的应力集中效应,底板浅部岩体率先发生塑性屈服破坏与微观裂隙损伤扩展。随着工作面持续推进,底板岩体损伤裂隙逐步萌生、扩展并相互连通,岩层渗透率显著提升,承压水沿高渗损伤裂隙带向采空区内部持续运移、富集,逐步形成优势导水通道,诱发底板突水隐患。煤层底板突水是采动应力重分布、塑性损伤渐进扩展、裂隙网络导通及承压水渗流运移多因素耦合的链式失稳致灾过程。防控治理后,底板平均透水率由1.55 Lu降至0.13 Lu,整体降幅达87.35%,底板隔水防渗性能得到大幅改善。研究结果可为富水环境下煤层底板的稳定性控制及水害防控提供理论支撑和实践指导。

       

      Abstract: In the process of coal seam mining, the coupling effect of mining disturbance and high confined water is easy to induce the penetration of floor cracks and the sudden increase of seepage, which seriously threatens the safety production of the mine. In order to accurately reveal the disaster-causing characteristics of mining-induced damage and seepage of coal seam floor under the condition of confined aquifer, and scientifically and effectively control the floor water disaster, based on the engineering geological conditions of Suancigou Coal Mine, the multi-field coupling mechanism is comprehensively considered, and the numerical calculation model of fluid-solid coupling of fine floor is established. The stress field distribution, plastic damage development and dynamic response evolution characteristics of seepage field in the whole process of working face mining are systematically explored. The results show that after the mining disturbance of the working face, there is a significant stress concentration effect at the edge of the goaf and in front of the coal wall, and the plastic yield failure and micro-fracture damage expansion occur first in the shallow rock mass of the floor. With the continuous advancement of the working face, the damage fissures of the floor rock mass gradually sprout, expand and connect with each other, and the permeability of the rock layer is significantly improved. The confined water continues to migrate and enrich along the high permeability damage fissure zone to the interior of the goaf, and gradually forms the dominant water conduction channel, which induces the hidden danger of floor water inrush. Water inrush from coal seam floor is a chain instability disaster-causing process of multi-factor coupling of mining stress redistribution, plastic damage gradual expansion, fracture network conduction and confined water seepage migration. After the prevention and control, the average water permeability of the floor decreased from 1.55 Lu to 0.13 Lu, with an overall decrease of 87.35 %, and the water-proof and anti-seepage performance of the floor was greatly improved. The research results can provide theoretical support and practical guidance for the stability control of coal seam floor and water disaster prevention and control in water-rich environment.

       

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