厚硬顶板超大采高工作面覆岩结构演化与强矿压产生机理

Overburden structural evolution and mechanism of strong ground pressure in ultra-large mining height longwall face with thick hard roof

  • 摘要: 厚硬岩层赋存超大采高工作面,其覆岩运移与矿压显现特征表现为覆岩结构演化复杂、支架受载强度高、动载灾害频发,对顶板稳定与安全高效开采构成严峻挑战。为揭示厚硬岩层主导下覆岩结构失稳与强矿压作用机理,以曹家滩煤矿122104我国首个10 m超大采高工作面为研究对象,综合采用相似材料模拟、数字图像相关(DIC)技术与现场实测分析等手段,从覆岩破断演化、变形场特征及支架受载响应等方面,探究厚硬岩层条件下的覆岩运移特征与矿压显现机制,建立“断裂拱—长悬臂梁—铰接岩梁”复合力学模型。结果表明:覆岩破断与运移过程可分为3个阶段,① 渐进离层损伤阶段,采动初期直接顶及低位厚硬岩层发生离层变形,垮落高度与离层高度一致;② 结构性突发失稳阶段,低位厚硬岩层形成长悬臂梁结构,在小变形条件下突发断裂,触发上覆多层岩体联动垮落,垮落高度显著大于离层高度,表现为悬臂梁破断主导的结构性失稳;③ 联动垮落阶段,高低位厚硬岩层共同参与承载,形成超长悬臂梁结构,其临界破断诱发大范围覆岩联动垮落,垮落范围显著增大。DIC监测数据揭示,悬臂梁破断前主应变小于10−2,说明覆岩在弹性小变形状态下发生突发破断。覆岩运移与支架载荷演化呈现良好对应关系,覆岩渐进垮落阶段支架阻力静态缓增,未发生明显冲击;当长悬臂梁结构达到临界跨度突发断裂时,支架工作阻力瞬时跃升,呈现强动载冲击。高低位厚硬岩层协同作用使悬臂梁跨度与承载范围显著扩大,导致静载累积水平和动载冲击烈度同步增强。基于相似材料模拟与实测结果,提出的“断裂拱—长悬臂梁—铰接岩梁”结构力学模型揭示了矿压显现由静载渐进累积向动载突变转化的力学机制,厚硬岩层主导形成的长悬臂梁是高静载的根源,其突发破断触发大范围覆岩联动失稳,是强动载产生的直接原因。现场监测表明,支架工作阻力呈现“高静载累积—多重连续动载突增—高频周期来压”特征,平均立柱下缩量693 mm,安全阀平均开启率52.6%,与模型揭示特征高度一致,验证了其工程适用性。研究成果深化了对厚硬岩层主导覆岩失稳与强矿压作用机制的认识,为10 m超大采高工作面顶板控制与动力灾害防控提供了理论依据与技术支撑,对推动高强度矿压控制理论的发展具有重要意义。

     

    Abstract: Ultra-large mining height faces with multiple thick and hard strata (MTHS) exhibit highly complex overburden structural evolution, intense support loading, and frequent dynamic events, posing serious challenges to roof stability and safe, efficient mining. To clarify the mechanisms of overburden instability and strong ground pressure under MTHS conditions, the 122104 working face of the Caojiatan coal mine, the first 10 m ultra-large mining height face in China was selected as the engineering case. A combination of physical simulation, digital image correlation (DIC) monitoring, and field measurements was employed to investigate the evolution of overburden failure, deformation characteristics, and support shield resistance behavior. Based on the findings, a composite mechanical model of “fractured arch-long cantilever beam-articulated rock beam” was established to describe the overburden structural evolution and its control over ground pressure behavior. The results indicate that overburden failure evolves through three distinct stages. ① Progressive delamination, the immediate roof and lower hard strata undergo gradual separation, and the caving height approximates the delamination height. ② Sudden structural failure, the lower hard strata form a long cantilever beam that fractures abruptly under small deformation, inducing cooperative collapse of multiple upper layers. The caving height greatly exceeds the delamination height, signifying beam-dominated instability. ③ Synergistic collapse, upper and lower hard strata jointly bear load, forming an ultra-long cantilever beam whose critical failure triggers extensive coordinated collapse. DIC observations show that the principal strain prior to beam fracture is below 10−2, indicating brittle failure under elastic deformation. Overburden movement drives variations in support shield resistance, and the two exhibit strong correspondence. During gradual caving, the resistance increases steadily without impact; when the long beam reaches its critical span and fails, the resistance rises sharply, generating intense dynamic impact. The coordinated action of multiple hard strata enlarges the beam span and bearing range, amplifying both static accumulation and dynamic response. Field monitoring revealed a pattern of “high static resistance accumulation-multi-stage dynamic surges-high-frequency periodic weighting”, with an average leg shortening of 693 mm and a 52.6% safety valve opening rate, consistent with model predictions. This study deepens the understanding of overburden instability and strong ground pressure mechanisms dominated by thick hard strata, providing theoretical and technical guidance for roof control and dynamic disaster prevention in ultra-large mining height faces.

     

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