Rock and Soil Mechanics ›› 2025, Vol. 46 ›› Issue (1): 244-256.doi: 10.16285/j.rsm.2024.0628

• Fundamental Theory and Experimental Research • Previous Articles     Next Articles

Influence of connectivity on mechanical properties of rock samples with structural planes of varying dip angles

LI Zong-en1, 2, LIU Xing-yan1, 2, ZHENG Qing-song3, HU Qi1, 2, PAN Qian-tong1, 2   

  1. 1. College of Water Conservancy & Architectural Engineering, Shihezi University, Shihezi, Xinjiang 832003, China; 2. Key Laboratory of Cold and Arid Regions Eco-Hydraulic Engineering of Xinjiang Production & Construction Corps, Shihezi University, Shihezi, Xinjiang 832003, China; 3. College of Water Resources and Hydropower, Sichuan University, Chengdu, Sichuan 610065, China
  • Received:2024-05-23 Accepted:2024-11-26 Online:2025-01-10 Published:2025-01-04
  • Supported by:
    This work is supported by the Science and Technology Innovation Talent Project of Bingtuan (2023CB008-28), the Start-up Project of Scientific Research for High-level Talents in Shihezi University (RCZK202023) and the Young Innovative Talents Program of Shihezi University (CXPY202116).

Abstract: The connectivity ratio significantly influences the mechanical properties and failure mechanisms of rock samples with structural planes of varying inclinations. Consequently, jointed rock samples with connectivity values k of 0, 0.25, 0.50, and 1.00, and dip angles β  of 15°, 30°, 45°, and 60° were manually prepared. Uniaxial and triaxial compression tests at confining pressures of 200, 400, and 600 kPa were conducted to investigate the effects of connectivity and dip angles on the mechanical properties of the rock mass. The results show that: 1) Connectivity significantly reduces the strength of the rock mass; peak strength decreases as connectivity increases. Stress-strain curves exhibit initial strain hardening followed by strain softening when k≤0.50; for k>0.50, the behavior transitions from strain softening at low angles to strain hardening at high angles. 2) Samples with structural planes initially shrink and then expand; overall expansion decreases with increasing connectivity at each dip angle; abrupt changes occur during shrinkage when k=1.00 at dip angles of 30°, 45°, and 60°. 3) Before energy inflection point α , dissipative energy Ud increases with connectivity while elastic strain energy U slightly decreases; after point α , andU both increase sharply, and different connectivity levels exhibit similar energy release rates. 4) The prediction criteria for rock samples with varying connectivity rates are classified. When k < 0.5, β=45°+φj /2 , it is suitable for judging the failure angle, where φ is the friction angle of the structural plane; when ≥0.5, the Jaeger criterion accurately reflects the failure angle of the rock mass.

Key words: triaxial test, mechanical properties, connectivity rate, energy method

CLC Number: 

  • TU443
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