To investigate the strength characteristics of soft rocks, consolidated-drained triaxial compression tests were performed with mudstones, siltstones, tuff, weathered granite and so on. Maximum stress of applied confining pressure was about 30 MPa. Radial compression tests under confining pressure were also performed to study the mechanical properties under tensile stresses.From these series of experiments, it may be concluded that the relationships between confining pressure and strength (maximum and residual) are generally non-linear.These strength relations can be expressed as the following power function;(τ
m/τ
m0)=α(σ'
m/σ'
m0)
β where τ
m=(σ
1-σ
3)/2, σ'
m=(σ'
1+σ'
2+σ'
3)/3, τ
m0 and σ'
m0 are at the case of σ'
2=σ'
3=0. α and β are material constants for rocks and σ'
m>0. The value of α is generally about unit and in the range of 0.96-1.23 and β is in the range of 0.44-0.85.The normalization by τ
m0(=q
u/2) and σ'
m0 (=q
u/3) makes possible to represent with the same values of parameters α and β, the strength reduction due to scale effect and strength relation of sedimentary rocks which have the same geological history and of granites of various degrees of weathering which are distributed in the same petrographic province.The applicability of proposed power function to the hard rocks and rock masses were investigated. Consequently, it is clarified that the proposed equation can be applied to the hard rocks which has the unconfined compressive strength of 20-200 MPa and also applied to the closely jointed rocks which can be regarded as the model of rock masses.
View full abstract