WANG Hua-bin, ZHOU Yu, YU Gang, et al. A triaxial test study on structural granite residual soil[J]. 2021, 42(4): 991-1002.
DOI:
WANG Hua-bin, ZHOU Yu, YU Gang, et al. A triaxial test study on structural granite residual soil[J]. 2021, 42(4): 991-1002.DOI: 10.16285/j.rsm.2019.2117.
A triaxial test study on structural granite residual soil
granite residual soil is widely distributed in the southeastern part of China and usually leads to engineering accidents due to its special structure. In this paper
a series of triaxle tests was conducted on the slope residual soil from Bozhi County
Zhaoqing City
Guangdong Province
to study the strain and pore pressure characteristics of structural granite residual soil under triaxial stress state as well as the structural yield characteristics of granite residual soil
which could provide useful reference for corresponding projects. Triaxial compression tests were conducted on undisturbed soil
remolded normal consolidated soil and remolded over-consolidated soil. The results showed that both undisturbed soil and remolded over-consolidated soil had certain structural characteristics
and had an obvious dilatancy during the drained shear test. The stress-strain curves of both undisturbed soil and remolded over-consolidated soil showed strain softening. The excess pore pressure of both undisturbed soil and remolded over-consolidated soil increased first and then decreased during the undrained shear test
while the excess pore pressure of undisturbed soil decreased more. The undrained shear strength of over-consolidated soil was consistent with the SHANSEP theory and the test constant was 0.67. The normalized stiffness of remolded normal consolidated soil decreased slowly with loading process going on
and it yielded completely when =15%. The normalized stiffness curves of undisturbed soil and remolded over-consolidated soil were not consistent with each other
and the structural yielding occurs at =1.5% and =1% respectively
and the overall failure occurs at =15%. In addition
the larger the confining pressure was
the more similar the structural curve of the structural soil was to the disturbed soil.