Rock and Soil Mechanics ›› 2023, Vol. 44 ›› Issue (4): 975-989.doi: 10.16285/j.rsm.2022.0702

• Fundamental Theroy and Experimental Research • Previous Articles     Next Articles

Anisotropic mechanical properties and brittleness evaluation of layered phyllite

WANG Wei1, 2, ZHANG Kuan1, 2, CAO Ya-jun1, 2, CHEN Chao1, 2, ZHU Qi-zhi1, 2   

  1. 1. Key Laboratory of Ministry of Education for Geomechanics and Embankment Engineering, Hohai University, Nanjing, Jiangsu 210098, China; 2. Jiangsu Research Center for Geomechanical Engineering Technology, Hohai University, Nanjing, Jiangsu 210098, China
  • Received:2022-05-11 Accepted:2022-08-11 Online:2023-04-18 Published:2023-04-28
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (12072102, 12102129), the China Postdoctoral Science Foundation (2021M690047), the Six Talent Peaks Project in Jiangsu Province and the Program to Cultivate Middle-aged and Young Science Leaders of Colleges and Universities of Jiangsu Province, China.

Abstract: In order to study the mechanical properties and anisotropy characteristics of layered phyllite, rock mechanical tests of phyllite were conducted under different bedding inclinations and different confining pressures. The anisotropic mechanical properties in strength, deformation, brittleness and failure modes of phyllite samples were comparatively analyzed. Some findings were as follows. (1) As the bedding inclination β  increases, the strength and deformation characteristic curve of the rock sample is U-shaped; and the strength and plasticity increase, the anisotropy gradually decreases and stabilizes with the increase of confining pressure. (2) The anisotropic Saeidi criterion and the modified Ramamurthy criterion can well predict the failure strength of rock specimens under different bedding inclinations. (3) A comprehensive brittleness index of phyllite samples at different bedding inclination under different confining pressures is proposed based on the stress–strain curve characteristic and energy equilibrium. The brittleness index is lower, and the shear failure is more likely to occur when the bedding inclination β  is about 45º. The relationship between brittleness and the failure mode is revealed, and the decreasing order of brittleness is concluded as follows: tensile splitting along bedding plane > tensile splitting through bedding plane > shear along bedding plane > shear through bedding plane. (4) The failure modes of phyllite are related to the bedding inclinations and confining pressures. Under uniaxial compression conditions, complex networks of fractures are formed easily after splitting failure of rock samples; and under high confining pressure conditions, a single shear failure plane is generally formed along the bedding plane or through multiple planes after rock failure.

Key words: rock mechanics, phyllite, anisotropy, mechanical property, brittle index, failure modes

CLC Number: 

  • TU452
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