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巨厚白垩系下覆岩离层产生机理及链式灾变研究

Study on generation mechanism of overlying strata separation and chain-type catastrophe under extra-thick cretaceous strata

  • 摘要: 陕蒙深部矿井大多位于巨厚白垩系地层覆盖区,在多工作面大空间开采条件下,高位白垩系岩层与侏罗系安定组间易形成大范围离层空间。离层空间的持续发育极易导致区域应力失衡,进而引发高能矿震、高势能离层水害及地表沉陷等多元链式灾害风险。以营盘壕煤矿为工程背景,建立白垩系巨厚岩层与侏罗系软硬互层综合力学模型,分析侏罗系软硬互层岩性差异悬殊条件下伏岩层运移特征,基于概率积分法,推导得到软硬互层顶界面沉降范围与沉降曲面函数;结合厚板模型表征的白垩系巨厚岩层大面积悬板挠曲变形特征,揭示白垩系巨厚岩层与侏罗系软硬互层联动演化下离层空间产生力学机理,从而构建离层危险性预警判据及多元灾害链式演化防控技术。结果表明:侏罗系软硬互层最大下沉量为3.58 m;采动扰动引发白垩系巨厚砂岩产生挠曲变形,二者差值形成高度为2.85 m的离层空间,通过二重积分估算,离层空间体积约为1.68×106 m3;离层空间形态由初始倾向船形的盆形结构,逐渐演化为倾向倒弓形的长盘形空间结构,最终在中心区域形成凹槽形向下突起构造;以离层临界高度和离层水压作为危险性分级的关键判别指标,引入离层有效应力及开采扰动因子,构建离层危险性指数R;当离层空间发育至阈值时,岩体内部应力系统失衡,触发以高能矿震、侏罗系隔水层导水通道贯通、高势能离层突水和递进式地表沉陷等灾害链式响应;基于弱化离层危险性指数R,提出以隔离注浆技术调控离层空间结构、优化采高和推采速度等开采工艺的主动防控技术,实现白垩系地层下离层空间发育诱发多元灾害的精准预警与有效防控。

     

    Abstract: Most deep mines in Shaanxi-Inner Mongolia area are located in the coverage area of extra-thick Cretaceous strata. Under the condition of large-scale mining with multiple working faces, large-range separation spaces are prone to form between high-level Cretaceous strata and the Jurassic Anding Formation. The continuous development of separation spaces can easily give rise to regional stress imbalance, and further trigger multi-source chain disaster risks such as high-energy mine earthquakes, high-potential separation-layer water hazards and surface subsidence. Taking Yingpanhao Coal Mine as the engineering background, a comprehensive mechanical model for extra-thick Cretaceous strata and Jurassic soft-hard interbedded strata is established to analyze the migration characteristics of overlying strata under prominent lithological differences of Jurassic soft-hard interbeds. Based on the probability integral method, the subsidence range and subsidence surface function of the top interface of soft-hard interbedded strata are derived. Combined with the large-area suspended-plate flexural deformation characteristics of extra-thick Cretaceous strata characterized by the thick-plate model, the mechanical mechanism for the generation of separation spaces under the coupled evolution of extra-thick Cretaceous strata and Jurassic soft-hard interbedded strata is revealed. On this basis, the early-warning criterion for separation-layer hazard and the prevention-control technology for multi-disaster chain evolution are constructed.The results show that the maximum subsidence of Jurassic soft-hard interbedded strata is 3.58 m. Mining disturbance induces flexural deformation of extra-thick Cretaceous sandstone, and a separation space with a height of 2.85 m is formed by the subsidence difference. Estimated via double integral, the volume of the separation space is approximately 1.68×106 m3. The morphology of the separation space evolves from an initial trough-shaped basin structure along the dip direction to an inverted-arch long-plate spatial structure, and finally a downward-protruding groove-shaped structure is formed in the central zone. Taking the critical separation-layer height and separation-layer water pressure as key discrimination indices for hazard grading, the separation-layer effective stress and mining disturbance factor are introduced to establish the separation-layer hazard index R. When the separation-layer space develops to the threshold value, the internal stress system of rock mass loses balance and triggers chain disaster responses including high-energy mine earthquake, connection of water-conducting channels in Jurassic aquifuge, high-potential separation-layer water inrush and progressive surface subsidence. Targeting the reduction of separation-layer hazard index R, active prevention-control technologies including isolating grouting for regulating separation-layer spatial structure as well as mining-process optimization of mining height and advancing speed are proposed, which realize accurate early-warning and effective prevention-control of multi-hazards induced by separation-layer development beneath Cretaceous strata.

     

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