考虑复合岩性矸石二次压缩变形的巨厚弱胶结覆岩深部局部充填开采岩层移动控制研究

    Study on strata movement control in deep partial backfill mining with massive weakly-cemented overburden considering secondary compression behavior of multi-lithology gangue

    • 摘要: 局部充填开采是一种有效控制地面沉降的主动减沉控损技术,但在西部巨厚弱胶结覆岩的复杂环境中伴随高地应力-水环境耦合影响下复合岩性矸石充填体将发生显著二次压缩变形,无法实现对冲击地压、地表沉陷等地质灾害的精准控制。因此,本文通过建立局部充填开采PFC-FLAC耦合模型,探究高地应力-水环境耦合作用下复合岩性矸石充填二次压缩变形特征,深入探讨局部真实充填率对岩层移动控制的影响规律。研究结果表明,充填率变化与上覆岩层应力、顶板下沉及地表下沉间呈线性函数关系,是减小下沉空间抑制顶板沉降和地表沉降的直接因素。在高地应力及水环境的耦合作用下复合岩性矸石充填体的二次压缩率达到5%~8%,且充填率对复合承载体的协同作用机理影响较大,当真实充填率接近81%时,复合承载体与两侧三叠拱协同作用形成马鞍-双三叠拱-半蘑菇拱应力场,使得超充分采动状态下的地表下沉系数仅为0.31。本文研究能够为复合岩性矸石充填设计提供数据参考,对于煤炭资源绿色开采和环境保护具有较高的实践价值。

       

      Abstract: Partial filling mining is an effective active subsidence control and loss reduction technology for controlling ground subsidence. However, in the complex environment of massive weakly-cemented overburden in the western region, under the coupled influence of high ground stress-water environment, the composite rock gangue filling body will undergo significant secondary compression deformation, making it impossible to precisely control geological disasters such as rock burst and surface subsidence. Therefore, by establishing the PFC-FLAC coupling model of partial filling mining, this paper explores the secondary compression deformation characteristics of multi-lithology gangue filling under the coupling action of high ground stress-water environment, and deeply discusses the influence law of partial real filling rate on rock movement control. The results show that the change of filling rate has a linear function relationship with overburden stress, roof subsidence and surface subsidence, which is a direct factor to reduce subsidence space and inhibit roof and surface settlement. Under the coupling effect of high ground stress and water environment, the secondary compression rate of the multi-lithology gangue backfill reaches 5%-8%, and the filling rate has a great influence on the synergistic mechanism of the composite carrier. When the real filling rate is close to 81%, the saddle-double triple arch-half mushroom arch stress field is formed by the synergistic interaction between the composite carrier and the triple arch on both sides, which makes the surface subsidence coefficient of the superfull mining state only 0.31. This study can provide data reference for the design of multi-lithology gangue filling, which has high practical value for the green mining of coal resources and environmental protection.

       

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