Select
Anisotropic properties of deformation parameters and its mechanism of Wudang group schist
WANG Zhang-qiong , YAN E-chuan , LIU Yi-xue , WANG Zhong-jie,
. 2014, 35 (5 ):
1317-1322.
The common character of schist is transversely isotropic due to the existence of regular bedding planes, which means that the failure mechanism and deformation characteristics of such rocks have the obvious difference with common rocks. In view of this point, uniaxial compressive test on samples of Wudang group schist, Tongsheng tunnel, Shiyan-Fangxian expressway, that with schistosity inclination of 0°, 45° and 90° respectively is carried out. The results show that: deformation parameters and failure mode of schist show obvious anisotropic characteristics. In the order of descending values of the modulus of elasticity, schistosity inclination of the samples are 90°, 0°, 45°respectively, in the order of descending values of the Poisson ratio, schistosity inclination of the samples are 45°, 0°, 90° respectively. The main failure mode is press off perpendicular to the spatial orientation of schistosity, shear and split off when schistosity inclination is 0°, 45°and 90° respectively according to schistosity inclination. Based on above, the mechanism of deformation and failure characteristics of schist is analyzed, via electron microscope scanning and FLAC3D numerical experiment, it is considered that, the main reason is the different relationships between spatial orientation of schistosity and axial force direction, which caused obvious differences of contribution that of schistosity surface to schist deformation.
Related Articles |
Metrics