WANG Wei, ZHANG Kuan, CAO Ya-jun, et al. Anisotropic mechanical properties and brittleness evaluation of layered phyllite[J]. 2023, 44(4): 975-989.
DOI:
WANG Wei, ZHANG Kuan, CAO Ya-jun, et al. Anisotropic mechanical properties and brittleness evaluation of layered phyllite[J]. 2023, 44(4): 975-989.DOI: 10.16285/j.rsm.2022.0702.
Anisotropic mechanical properties and brittleness evaluation of layered phyllite
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 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 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.
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