Anisotropic mechanical properties and brittleness evaluation of layered phyllite

被引:0
|
作者
Wang Wei [1 ,2 ]
Zhang Kuan [1 ,2 ]
Cao Ya-jun [1 ,2 ]
Chen Chao [1 ,2 ]
Zhu Qi-zhi [1 ,2 ]
机构
[1] Hohai Univ, Key Lab, Minist Educ Geomech & Embankment Engn, Nanjing 210098, Jiangsu, Peoples R China
[2] Hohai Univ, Jiangsu Res Ctr Geomech Engn Technol, Nanjing 210098, Jiangsu, Peoples R China
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
rock mechanics; phyllite; anisotropy; mechanical property; brittle index; failure modes; FAILURE CRITERION; DEFORMATION; STRENGTH; SHALE; ROCK;
D O I
10.16285/j.rsm.2022.0702
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
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 beta 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 beta is about 45 degrees. 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.
引用
收藏
页码:975 / 989
页数:15
相关论文
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