Abstract
This paper reports the results of fracture testing of sandstone under constant minor principal stress (20 MPa) and various intermediate principal stresses. The results show that when the minor principal stress is constant, as the intermediate principal stress increases, the ratio of the octahedral shear stress (τoct) to the octahedral normal stress (σoct) decreases. The strength criterion of τoct/σoct = f(σ2) is obtained. This criterion reflects not only the hydrostatic stress and intermediate principal stress effects but also the Lode angle effect. This criterion reveals the reason why the rock strength increases and then decreases with increasing intermediate principal stress. The decreasing trend is fitted by linear, logarithmic and Boltzmann equations. The applicability of the three fitting equations for strength prediction and the π plane strength envelopes is analysed, and the results of the Boltzmann fitting equation are the best. The deformation characteristics of rock during the failure process are analysed. The changing process of the tangential deformation modulus of the rock is found to be divided into three stages during the loading process: an increasing stage, an initial decreasing stage and a rapidly decreasing stage. Based on an analysis of computed tomography (CT) images of the internal fractures of rock and photographs of the fracture surfaces, the internal fractures are found to be clear and smooth, and the shear stresses in the fracture surfaces are strengthened with increasing intermediate principal stress. The dominant shear stress in the process of failure is considered to cause these phenomena.
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Abbreviations
- σ 1 :
-
Major principal stress
- σ 2 :
-
Intermediate principal stress
- σ 3 :
-
Minor principal stress
- b :
-
Intermediate principal stress coefficient, \(b{\text{ = }}\frac{{{\sigma _2}{\text{ }} - {\text{ }}{\sigma _3}}}{{{\sigma _1}{\text{ }} - {\text{ }}{\sigma _3}}}\)
- θ :
-
Stress Lode angle
- \({\sigma _{{\text{oct}}}}\) :
-
Octahedral normal stress, \({\sigma _{{\text{oct}}}}=({\sigma _{\text{1}}}+{\sigma _2}+{\sigma _3})/3\)
- \({\tau _{{\text{oct}}}}\) :
-
Octahedral shear stress, \({\tau _{{\text{oct}}}}=\sqrt {{{({\sigma _{\text{1}}} - {\sigma _2})}^2}+{{({\sigma _{\text{1}}} - {\sigma _3})}^2}+{{({\sigma _2} - {\sigma _3})}^2}} /3\)
- B d :
-
Evaluation parameters for brittleness
- B 1d :
-
The magnitude of the relative post-peak stress drop
- B 2d :
-
Parameter for the velocity of the post-peak stress decrease
- k :
-
Absolute value of the slope of stress drop
- τ p :
-
The peak deviatoric stress
- τ r :
-
The residual deviatoric stress
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Acknowledgements
This study was financially supported by the National Natural Science Foundation of China (51434003, 51874053, 51804049), Graduate Scientific Research and Innovation Foundation of Chongqing, China (Grant nos. CYB16030, CYS17046), China Postdoctoral Science Foundation Funded Project (2017M612917) and Chongqing Postdoctoral Special Foundation Funded Project (XM2017043).
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Song, Z., Yin, G., Ranjith, P.G. et al. Influence of the Intermediate Principal Stress on Sandstone Failure. Rock Mech Rock Eng 52, 3033–3046 (2019). https://doi.org/10.1007/s00603-019-01756-1
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DOI: https://doi.org/10.1007/s00603-019-01756-1