应力及裂隙影响下真三轴劈裂注浆起裂特征

Fracture initiation mechanism of true triaxial fracture grouting under stress and crack influence

  • 摘要: 深部地层应力环境及裂隙赋存特征复杂,三向应力下深部地层劈裂注浆裂隙扩展特征不明,劈裂注浆参数设计经验化。为合理设计劈裂注浆参数,探明裂隙起裂扩展规律,提高劈裂注浆加固效果,通过对不同应力与预制裂隙距离影响下类岩石试件进行劈裂注浆试验,结合声发射参数特征,获得了不同主应力比σy/σz与不同预制裂隙距离L影响下注浆压力变化及裂隙扩展特征,讨论了试验起裂压力与不同劈裂理论计算起裂压力间差异性,并基于断裂力学反演修正得到不同试验环境下对应断裂韧性,将反演结果代入数值模型验证试验结果一致性,总结了相关有益结论,为劈裂注浆应用提供启示。结果表明:随着主应力比σyz不断增加,被注岩体劈裂注浆的起裂压力呈现“升—降”变化趋势,劈裂注浆裂隙扩展状态由单向扩展转向状态变为多向扩展转向状态,被注岩体劈裂注浆起裂压力与预制裂隙和注浆孔间距L成正比,随着L增加,预制裂隙对劈裂裂隙扩展路径影响越来越小,当L较大时,仅发生扩展路径偏转,劈裂裂隙不会与预制裂隙贯通;被注岩体劈裂注浆裂隙扩展过程主要以张拉破坏为主,被注岩体内部存在裂隙时,劈裂注浆裂隙扩展过程中张拉信号占比会小幅增加,L的减小,会导致劈裂裂隙扩展过程中张拉信号占比产生较大幅度的增加;三轴应力下的断裂韧性K_\mathrmIc^* 与主应力比(y轴与z轴的应力比)σy/σz成正比,σy/σz越接近1,被注岩体起裂压力越大;原生裂隙会改变地层的应力分布状态,能在一定程度上弱化被注岩体整体应力水平,降低被注岩体劈裂注浆起裂压力,但在一定距离下会提高注浆孔周围最小主应力,提高起裂压力。

     

    Abstract: The deep formation are characterized by complex stress environments and intricate fracture distributions, resulting in unclear fracture propagation behavior during split grouting under triaxial stress and an empirical approach to parameter design. To rationally design split grouting parameters, elucidate fracture initiation and propagation mechanisms, and enhance grouting reinforcement effectiveness, split grouting tests were conducted on rock-like specimens under varying stresses and distances from pre-existing fractures. By analyzing acoustic emission (AE) parameters, we obtained the variations in grouting pressure and fracture propagation characteristics under different principal stress ratios (σy/σz) and distances from pre-existing fractures. The discrepancies between the experimental fracture initiation pressures and those calculated by different splitting theories were discussed. Fracture toughness corresponding to various test conditions was derived by inverse analysis based on fracture mechanics, and the inversion results were incorporated into a numerical model to validate the experimental outcomes. Finally, the practical implications of the beneficial findings from the tests were summarized. The results indicate that as the principal stress ratio σy/σz increases, the fracture initiation pressure during split grouting exhibits a “rise-fall” trend, and the fracture propagation mode shifts from unidirectional to multidirectional expansion. The fracture initiation pressure is proportional to the distance L between the pre-existing fracture and the grouting hole. As L increases, the influence of the pre-existing fracture on the propagation path of the split fracture diminishes. At a distance of 70 mm, only deflection of the propagation path occurs, without interconnection between the split fracture and the pre-existing fracture. The fracture propagation process during split grouting is predominantly characterized by tensile failure. When fractures exist within the rock mass, the proportion of tensile cracks during propagation increases slightly. At a fracture distance of 10 mm from the grouting hole, the proportion of tensile cracks rises significantly. The fracture toughness K_\mathrmIc^* under triaxial stress is proportional to the principal stress ratio σy/σz. The closer the ratio is to 1, the higher the fracture initiation pressure. Pre-existing fractures alter the stress distribution in the stratum, weakening the overall stress level of the rock mass and reducing the fracture initiation pressure to some extent. However, at certain distances, they can increase the minimum principal stress around the grouting hole, thereby raising the fracture initiation pressure.

     

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