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水力压裂弱化压力拱调控采动应力机理

Mechanism of weakening pressure arch of hydraulic fracturing to regulate mining-induced stresses

  • 摘要: 水力压裂是煤矿巷道围岩卸压的关键技术之一, 其参数优化对实现围岩有效卸压与应力转移至关重要。以某矿综采工作面为工程背景, 综合采用物理相似模型试验与UDEC离散元数值模拟, 系统研究了水力压裂作用下工作面底板及煤柱应力演化规律, 揭示了水力压裂弱化压力拱调控采动应力的卸压机理, 并分析了压裂层位高度与压裂区岩体损伤程度对卸压效果的影响。研究结果表明: (1)当水力压裂裂缝扩展区位于煤体高应力区上方时, 底板及煤体浅部高应力区域垂直应力峰值降低10.8%~12.1%, 深部低应力区垂直应力峰值增加1.1%; (2)水力压裂裂缝分布于压力拱高应力传递路径上时, 可显著削弱该区域顶板承载能力, 促使高应力向深部转移, 形成浅部小范围、大幅度卸压与深部大范围、小幅度增压分布特征, 揭示了水力压裂通过弱化压力拱结构来调控应力转移路径的卸压机理; (3)卸压效果与压裂层位高度、压裂影响区岩体劣化程度密切相关, 垂直层位升高使卸压范围向深部延伸和浅部煤体应力增大。水力压裂影响区岩体损伤程度增加则显著提升高应力区卸压幅度, 进一步抑制损伤区岩体传递压力拱高应力的能力, 促使高应力向深部岩体转移; (4)现场应用表明, 水力压裂可显著降低煤柱应力, 有效提高巷道围岩稳定性。研究结果为煤矿坚硬顶板弱化、冲击地压防治及强采动巷道卸压等水力压裂参数优化提供了理论参考和科学依据。

     

    Abstract: Hydraulic fracturing (HF) is a key technology for stress relief in surrounding rock of coal mine roadways. Optimizing its parameters is crucial for achieving effective pressure relief and stress transfer in surrounding rock. Taking a fully-mechanized mining face in a specific mine as the engineering background, the stress evolution laws of the floor and coal pillar under HF was investigated using integrated physical similarity model tests and UDEC discrete element numerical simulation. The pressure relief mechanism of HF by weakening the pressure arch to regulate mining-induced stresses was revealed. Furthermore, the influences of the HF horizon height and the rock mass damage degree in the HF-affected zone on the pressure relief effect were analyzed. The results show that when the HF fracture propagation zone is located above the high-stress zone of the coal mass, the peak vertical stress in the high-stress area of floor and shallow coal mass decreases by 10.8%-12.1%, while that in the deep low-stress zone increases by only 1.1%. When HF fractures distribute along the high-stress transfer path of the pressure arch, the load-bearing capacity of the roof in this area is significantly weakened, promoting the transfer of high stress to deeper regions. This results in a characteristic distribution featuring significant pressure relief within a shallow limited zone and slight pressure increase across a large deep zone. This elucidates the pressure relief mechanism whereby HF regulates the stress transfer path by weakening the pressure arch structure. The pressure relief effect is closely related to the HF horizon height and the rock mass damage degree in the HF-affected zone. Increasing the vertical horizon extends the pressure relief range deeper and elevates the stress in the shallow coal mass. An increase in damage degree of rock mass within the HF-affected zone significantly enhances the pressure relief magnitude in the high-stress area, further inhibiting the ability of the damaged zone to transmit the high stress of the pressure arch, thereby promoting the transfer of high stress to deeper rock mass. Field implementation demonstrates that HF significantly reduces coal pillar stress and enhances surrounding rock stability. The research findings provide theoretical bases for optimizing HF parameters to weaken hard roofs, prevent rock bursts, and de-stress in roadways subjected to intense mining-induced stresses.

     

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