Zhou Xiancheng, Wang Jiao
College of Architectural Engineering, Shanxi Vocational University of Engineering Science and Technology, Jinzhong, 030619, Shanxi, China.
Civil-Military Integration Geological Survey Center, China Geological Survey, Chengdu, 610036, Sichuan, China.
Sci Rep. 2025 Jul 17;15(1):25889. doi: 10.1038/s41598-025-10954-7.
Sandstone, a commonly distributed geological material, is critical to the safety of engineering structures such as mine tunnels, dams, and tunnels, particularly in terms of its mechanical properties and failure mechanisms under saturated conditions. This study investigates the influence of water on the failure characteristics of yellow sandstone using acoustic emission (AE) technology and avalanche dynamics. The results show that in the saturated state, the uniaxial compressive strength, elastic modulus, and peak strain of yellow sandstone decreased by 40.07%, 26.44%, and 22.32%, respectively. AE energy, count, and cumulative energy were reduced, and changes in the r value indicated variations in internal fractures. RA-AF-based fracture type statistics revealed that the proportion of tensile cracks increased from 18.66 to 45.57% under saturation. This suggests that moisture promotes the formation of tensile cracks, resulting in a more complex failure mode. The failure of yellow sandstone followed avalanche-like characteristics, with AE energy release displaying a power-law distribution and waiting times exhibiting a double power-law distribution, conforming to the mean-field force integration model. The mean-field indices (ε, τ', α, x, χ) increased in the saturated state. Avalanche modeling showed that water caused a more dispersed energy release during crack propagation, with AE signals revealing more low-energy events.
砂岩是一种分布广泛的地质材料,对矿山巷道、大坝和隧道等工程结构的安全至关重要,特别是在饱和条件下其力学性能和破坏机制方面。本研究采用声发射(AE)技术和雪崩动力学研究水对黄砂岩破坏特性的影响。结果表明,在饱和状态下,黄砂岩的单轴抗压强度、弹性模量和峰值应变分别降低了40.07%、26.44%和22.32%。AE能量、计数和累积能量降低,r值的变化表明内部裂缝的变化。基于RA-AF的裂缝类型统计显示,饱和状态下拉伸裂缝的比例从18.66%增加到45.57%。这表明水分促进了拉伸裂缝的形成,导致破坏模式更加复杂。黄砂岩的破坏具有类似雪崩的特征,AE能量释放呈现幂律分布,等待时间呈现双幂律分布,符合平均场力积分模型。饱和状态下平均场指数(ε、τ'、α、x、χ)增加。雪崩模型表明,水在裂纹扩展过程中导致能量释放更加分散,AE信号显示出更多低能量事件。