Xue Lei, Bu Fengchang, Chen Hongran, Xu Chao, Cui Yuan, Ding Hao
State Key Laboratory of Lithospheric and Environmental Coevolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China.
Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China.
Sci Rep. 2025 Mar 27;15(1):10541. doi: 10.1038/s41598-025-94972-5.
Rock bridges have long been recognised to provide crucial resistance against rock mass failure. Multiple rock bridges with diverse scales are widespread in natural rock masses. Despite prior positive contributions to a single rock bridge, mechanical behaviours of diverse-scale rock bridges remain elusive. In particular, whether rock bridges interact and how their failure processes evolve are still open questions. To fill in this gap, a block-based discrete element method, specifically the Universal Distinct Element Code, was employed to simulate diverse-scale rock bridges in granite subjected to direct shear to investigate their mechanical properties, stress and displacement fields, cracking processes, and acoustic emission characteristics. Results reveal a fundamental linear correlation between peak shear resistance and the proportion of rock bridges. As failure progresses, shear stress tends to concentrate at rock bridge tips, more prominently for the one farther from the shear loading end, attributed to the rotation of confining pressure plates. In addition, the irregularity of displacement distribution follows an arc-shaped configuration near rock bridges, and larger rock bridges display lower gradients in nearby displacement fields. Furthermore, wing cracks initiate from rock bridge tips in a tensile stress environment, with a greater length for rock bridges closer to the shear loading end. It is also found that rock bridges rupture in tension near the shear loading end and in shear further away. Expanding upon these findings and considering stress thresholds, we acquire new insights into the interaction patterns between diverse-scale rock bridges: when their sizes are similar, the rupture of the rock bridge closer to the shear loading end will expedite damage in the one farther away from the shear loading end towards its volume-expansion point; conversely, the rupture of a significantly larger rock bridge will overwhelmingly affect the smaller one. The identified interaction patterns provide significant proof of physical precursor patterns for reliably predicting the progressive failure of multiple rock bridges.
长期以来,人们一直认识到岩桥对岩体失稳具有至关重要的抵抗作用。多种不同尺度的岩桥广泛存在于天然岩体中。尽管此前对单个岩桥有积极贡献,但不同尺度岩桥的力学行为仍不明确。特别是,岩桥之间是否相互作用以及它们的破坏过程如何演变仍是悬而未决的问题。为填补这一空白,采用基于块体的离散单元法,即通用离散元程序,对花岗岩中不同尺度的岩桥进行直剪模拟,以研究其力学性质、应力和位移场、开裂过程及声发射特性。结果表明,峰值抗剪强度与岩桥比例之间存在基本的线性关系。随着破坏的进展,剪应力倾向于集中在岩桥尖端,离剪切加载端较远的岩桥更为明显,这归因于围压板的旋转。此外,位移分布的不规则性在岩桥附近呈弧形,较大的岩桥在附近位移场中的梯度较小。此外,翼形裂纹在拉应力环境下从岩桥尖端开始,离剪切加载端较近的岩桥裂纹长度更长。还发现,岩桥在剪切加载端附近受拉破坏,在较远位置受剪破坏。基于这些发现并考虑应力阈值,我们对不同尺度岩桥之间的相互作用模式有了新的认识:当它们的尺寸相似时,靠近剪切加载端的岩桥破裂将加速远离剪切加载端的岩桥向其体积膨胀点的破坏;相反,一个明显更大的岩桥破裂将对较小的岩桥产生压倒性影响。所确定的相互作用模式为可靠预测多个岩桥的渐进破坏提供了重要的物理前兆模式证据。