Rock and Soil Mechanics ›› 2023, Vol. 44 ›› Issue (4): 1217-1229.doi: 10.16285/j.rsm.2022.0658

• Numerical Analysis • Previous Articles     Next Articles

Experiment and hybrid finite-discrete element modelling of crack propagation in cross-fissured rock masses

LIANG Dong-xu1, ZHANG Nong1, 2, 3, RONG Hao-yu4   

  1. 1. School of Civil Engineering, Xuzhou University of Technology, Xuzhou, Jiangsu 221116, China; 2. School of Mines, China University of Mining and Technology, Xuzhou, Jiangsu 221116, China; 3. State Key Laboratory of Coal Resources and Safe Mining, China University of Mining and Technology, Xuzhou, Jiangsu 221116, China; 4. College of Civil and Transportation Engineering, Hohai University, Nanjing, Jiangsu 210098, China
  • Received:2022-05-05 Accepted:2022-07-11 Online:2023-04-18 Published:2023-04-29
  • Supported by:
    This work was supported by the Key Program of National Natural Science Foundation of China (52034007) and the General Program of National Natural Science Foundation of China (52074263).

Abstract: Crack propagation experiments were conducted on the prefabricated cross-fissured rock specimens to study the crack initiation, propagation, and coalescence processes. The effects of the angle between the primary fissure and the axial load and the angle between the primary and minor fissures on the crack initiation stress and the coalescence stress were analyzed. The experiments were modelled and calculated with a hybrid finite-discrete element program, i.e., 3D Y-HFDEM code parallelized by a graphic processor. The transition of rock damage from continuous to the discontinuous medium was achieved. Crack categories and damage modes were identified and the phenomenon that was difficult to find in the experiments was captured. It is shown that the number of tensile cracks in the crack coalescence zone increases as the angle between the main fissure and the axial load increases. The crack initiation and coalescence stresses are proportional to the angle between the main fissure and the axial load. The damage mode of the rock changes from tensile damage to shear damage as the angle between the primary and minor fissures increases. Cross fissures increase the degree of rock fragmentation. Damage caused by mixed tensile-shear cracks initiating and propagating at the tip of the primary fissure dominates the rock damage and is the main control fissure leading to the loss of bearing capacity of the rock mass. The hybrid finite-discrete element simulation software GPGPU parallelized 3D Y-HFDEM IDE is advantageous in study of rock crack propagation to capture damage and fracture types that are difficult to detect in the laboratory, and can be a powerful tool for study of rock crack propagation.

Key words: rossed fissures, crack extension, 3D hybrid finite-discrete element modelling, coalescence category, crack initiation stress

CLC Number: 

  • TU452
[1] JIANG Hai-bo, LU Yan, LI Lin, ZHANG Jun, . Strength characteristics and damage evolution law of expansive soil in water conveyance channel under dry-wet and freeze-thaw action [J]. Rock and Soil Mechanics, 2025, 46(5): 1356-1367.
[2] WANG Gui-bin, LIU Huan-dui, TANG Ming-hao, YANG Chun-he, CHEN Shi-wan, . Excavation damage zones in granite cavern under complex stress paths [J]. Rock and Soil Mechanics, 2024, 45(9): 2539-2553.
[3] SHEN Hai-meng, LI Qi, LI Xia-ying, MA Jian-li, . Laboratory experiment and numerical simulation on brittle failure characteristics of Longmaxi formation shale in Southern Sichuan under different stress conditions [J]. Rock and Soil Mechanics, 2018, 39(S2): 254-262.
[4] LI Peng-fei , ZHAO Xing-guang , CAI Mei-feng , . Discussion on approaches to identifying cracking initiation stress of rocks under compression condition: A case study of Tianhu granodiorite in Xinjiang Autonomous Region [J]. , 2015, 36(8): 2323-2331.
[5] ZHOU Shang-zhi , DANG Fa-ning , CHEN Hou-qun , LONG Qiao-ling . Numerical method for crack extension analysis based on fatigue fracture process of rock materials [J]. , 2008, 29(3): 769-774.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!