Dynamic mechanical behaviors of single-jointed rock mass under cyclic impact loadings
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摘要: 为探究节理岩体在循环动力扰动作用下的动态力学行为,采用分离式霍普金森压杆试验系统,对含单节理辉长岩试件进行了单轴循环冲击试验,从试件的抗冲击能力、应力应变性质、能量和损伤的演化对其动态力学行为进行了全面分析。结果表明,试件在循环冲击作用下的破坏模式为劈裂,节理倾角显著影响试件的抗冲击能力;试件在循环冲击过程中均出现了应变回弹现象,其力学性质并不随着冲击次数的增加而单调弱化;用耗散能表示的累积损伤系数随着冲击次数的增加近似线性增大,增幅随节理倾角的增大而减小。在低应力冲击作用下,单节理试件内的压剪应力不足以产生剪切裂纹,试件的破坏主要是由拉应力引起的张拉裂纹逐渐扩展并与节理相互贯通造成的。多节理岩体与单节理岩体的破坏机理类似,在循环冲击过程中会同时出现微缺陷的压密和节理处微裂纹的萌生,然而裂纹是否能使试件内的节理相互贯通影响了多节理试件的抗冲击能力,对于完整岩石试件,则是先出现微缺陷的压密,随后微裂纹以概率分布的形式被激活,最终导致试件破坏。Abstract: In practical engineering, rock frequently suffers from recurrent dynamic disturbances, posing serious threats to engineering safety. To investigate the dynamic mechanical behavior of jointed rock under cyclic dynamic disturbances, cyclic impact tests of single-jointed gabbro (SJG) were conducted using a split Hopkinson pressure bar (SHPB) test system. The stress equilibrium during the tests was verified using the three-wave method and the force balance coefficient method. The dynamic mechanical behavior of the specimens was comprehensively analyzed in terms of impact resistance, stress-strain relationships, energy and damage evolution, as well as dynamic failure mechanisms. The results show that single-jointed rock specimens can achieve stress equilibrium under cyclic impact conditions. The failure mode of the specimens under cyclic impacts is splitting, and the joint inclination angle significantly influences the impact resistance of the specimens. As the joint inclination angle increases, the impact resistance of the specimens also increases. During the cyclic impact process, strain rebound occurs in all specimens, and their mechanical properties do not monotonically degrade with an increasing number of impacts. The peak stress of the specimens generally exhibits a decreasing trend with the number of impacts. The cumulative damage coefficient, represented by dissipated energy, increases approximately linearly with the number of impacts, while the increase rate decreases with larger joint inclination angles. Under low-stress impact loading, the compressive-shear stress within single-jointed specimens is insufficient to generate shear cracks. The failure of specimens primarily results from the progressive propagation of tensile cracks induced by tensile stress, which eventually coalesce with the joint. The failure mechanism of multi-jointed rock masses resembles that of single-jointed rock masses. During cyclic impact loading, both compaction of micro-defects and initiation of micro-cracks at joints occur simultaneously. However, the impact resistance of multi-jointed specimens depends on whether the cracks can interconnect the joints. For intact rock specimens, the failure process initially involves compaction of micro-defects, followed by probabilistic activation of micro-cracks, ultimately leading to specimen failure.
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表 1 试验结果
Table 1. Experiment results
试件 气压/MPa 平均入射应力/MPa 最终状态 试件 气压/MPa 平均入射应力/MPa 冲击次数 最终状态 SJG-0-1 0.12 249 劈裂 SJG-60-1 0.13 275 7 劈裂 SJG-0-2 0.13 275 劈裂 SJG-60-2 0.13 275 8 劈裂 SJG-0-3 0.13 275 劈裂 SJG-60-3 0.13 275 8 劈裂 SJG-30-1 0.12 249 未破坏 SJG-90-1 0.13 275 14 劈裂 SJG-30-2 0.13 275 劈裂 SJG-90-2 0.13 275 15 劈裂 SJG-30-3 0.13 275 劈裂 SJG-90-3 0.13 275 10 劈裂 SJG-45-1 0.13 275 劈裂 完整 0.13 275 50 未破坏 SJG-45-2 0.13 275 劈裂 SJG-45-3 0.13 275 劈裂 -
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