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An Experimental and Numerical Study on Cracking Behavior of Brittle Sandstone Containing Two Non-coplanar Fissures Under Uniaxial Compression

机译:单轴压缩下含两个非共面裂隙的脆性砂岩开裂行为的实验与数值研究

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To understand the fracture mechanism in all kinds of rock engineering, it is important to investigate the fracture evolution behavior of pre-fissured rock. In this research, we conducted uniaxial compression experiments to evaluate the influence of ligament angle on the strength, deformability, and fracture coalescence behavior of rectangular prismatic specimens (80 x 160 x 30 mm) of brittle sandstone containing two non-coplanar fissures. The experimental results show that the peak strength of sandstone containing two non-coplanar fissures depends on the ligament angle, but the elastic modulus is not closely related to the ligament angle. With the increase of ligament angle, the peak strength decreased at a ligament angle of 60A degrees, before increasing up to our maximum ligament angle of 120A degrees. Crack initiation, propagation, and coalescence were all observed and characterized from the inner and outer tips of pre-existing non-coplanar fissures using photographic monitoring. Based on the results, the sequence of crack evolution in sandstone containing two non-coplanar fissures was analyzed in detail. In order to fully understand the crack evolution mechanism of brittle sandstone, numerical simulations using PFC2D were performed for specimens containing two non-coplanar fissures under uniaxial compression. The results are in good agreement with the experimental results. By analyzing the stress field, the crack evolution mechanism in brittle sandstone containing two non-coplanar fissures under uniaxial compression is revealed. These experimental and numerical results are expected to improve the understanding of the unstable fracture mechanism of fissured rock engineering structures.
机译:为了了解各种岩石​​工程中的断裂机理,研究预裂隙岩石的断裂演化行为非常重要。在这项研究中,我们进行了单轴压缩实验,以评估韧带角度对包含两个非共面裂隙的脆性砂岩矩形棱柱试样(80 x 160 x 30 mm)的强度,可变形性和断裂聚结行为的影响。实验结果表明,含两个非共面裂隙的砂岩的峰值强度与韧带角有关,但弹性模量与韧带角并不密切相关。随着韧带角的增加,峰值强度在韧带角为60A度时减小,然后增加到最大韧带角为120A度。裂纹的萌生,扩展和聚结都可以通过照相监控从预先存在的非共面裂缝的内部和外部尖端进行观察和表征。根据结果​​,详细分析了包含两个非共面裂缝的砂岩中裂缝的演化顺序。为了充分了解脆性砂岩的裂纹演化机理,在单轴压缩下对包含两个非共面裂缝的试样进行了PFC2D数值模拟。结果与实验结果吻合良好。通过分析应力场,揭示了含两个非共面裂隙的脆性砂岩在单轴压缩下的裂纹扩展机理。这些实验和数值结果有望增进对裂隙岩石工程结构不稳定破裂机理的理解。

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