Jiang Yujing, Li Xinpeng, Liu Jiankang, Luan Hengjie, Zhang Sunhao, Wang Changsheng, Wang Dong
College of Energy and Mining Engineering, Shandong University of Science and Technology, Qingdao 266590, China.
State Key Laboratory of Mining Disaster Prevention and Control Co-Founded by Shandong Province and the Ministry of Science and Technology, Shandong University of Science and Technology, Qingdao 266590, China.
Materials (Basel). 2023 Mar 9;16(6):2210. doi: 10.3390/ma16062210.
Anisotropic discontinuity exists widely in rock masses of mines, tunnels, slopes, water conservancy and hydropower projects. The shear characteristics of bolted anisotropic rock joints are extremely important for the stability design of engineering rock mass. However, few scholars have studied the bolted anisotropic rock joint. The different rock properties on both sides of the rock joint, especially the different rock strengths, will greatly affect the deformation characteristics and failure mode of the rock mass. Based on this, a series of shear tests were carried out on the bolted anisotropic rock joint under different normal stresses, and the characteristics of shear stress-shear displacement curve, shear strength, failure characteristics of the rock joint and deformation characteristics of the bolt are discussed. λ is defined as the strength ratio of upper and lower rock on the structural surface. The results show that the effect of λ on the shear stress-shear displacement curve is not obvious at the pre-fracture stage. The shear stress-shear displacement curve at the pre-breaking stage of the bolt presents a softening stage when the normal stress is equal to 0.5 MPa, tends to be horizontal when the normal stress is equal to 1 MPa and presents a hardening stage when the normal stress is greater than 1 MPa. After the bolt is broken, the shear stress-shear displacement curve presents a stepped-down descent. With the increase in λ, the breaking shear stress of the bolt increases. Elliptic failure occurs on the surface of the bolted anisotropic rock joint, and the length of the major axis of the ellipse decreases with the increase in λ value and normal stress. The bolts with different λ values of anisotropic rock joint show "Z-shaped" tensile bending deformation characteristics after shear fracture, and the horizontal and vertical components of the bolt deformation decrease with the increase in λ value and normal stress. The fracture shear displacement of the bolt increases with the increase in normal stress and decreases with the increase in λ value. The research results are helpful to further understand the shear mechanical characteristics and differences of bolted rock joints and provide a reference for solving the engineering problems of the composite layered rock mass.
各向异性不连续性广泛存在于矿山、隧道、边坡、水利水电工程的岩体中。加锚各向异性岩石节理的剪切特性对工程岩体的稳定性设计极为重要。然而,很少有学者对加锚各向异性岩石节理进行研究。岩石节理两侧不同的岩石性质,尤其是不同的岩石强度,将极大地影响岩体的变形特性和破坏模式。基于此,对加锚各向异性岩石节理在不同法向应力下进行了一系列剪切试验,并探讨了剪应力-剪切位移曲线特征、抗剪强度、岩石节理破坏特征及锚杆变形特征。λ定义为结构面上、下岩石的强度比。结果表明,在破裂前阶段,λ对剪应力-剪切位移曲线的影响不明显。当法向应力等于0.5MPa时,锚杆在破坏前阶段的剪应力-剪切位移曲线呈现软化阶段;当法向应力等于1MPa时,趋于水平;当法向应力大于1MPa时,呈现硬化阶段。锚杆破坏后,剪应力-剪切位移曲线呈阶梯状下降。随着λ的增大,锚杆的破坏剪应力增大。加锚各向异性岩石节理表面出现椭圆形破坏,椭圆长轴长度随λ值和法向应力的增大而减小。不同λ值的各向异性岩石节理锚杆在剪切破坏后呈现“Z形”拉弯变形特征,锚杆变形的水平和垂直分量随λ值和法向应力的增大而减小。锚杆的断裂剪切位移随法向应力的增大而增大,随λ值的增大而减小。研究结果有助于进一步了解加锚岩石节理的剪切力学特性及差异,为解决复合层状岩体的工程问题提供参考。