“…In EDZ, the physical and mechanical properties of rock mass, including strength, moduli, stiffness, etc., are obviously reduced. Under the action of external force, the damaged rock mass is further deformed and destroyed, and the initial damaged area is also considered to be the starting point of the later damage evolution (Bai et al., 2020; Munoz and Taheri, 2017; Wasantha et al., 2020; Wong and Peng, 2020; Xu et al., 2004). Similarly, in contrast with intact rock, the mechanical properties of holed rock have the same variation characteristics, and the starting position of damage accumulation under external force is generally in the vicinity of the hole because of stress concentration (Fakhimiet al, 2002; Li et al., 2020; Zhao et al., 2020; Zhu et al., 2021).…”