Abstract
The fatigue fracture behaviour and a constitutive model of the freeze-thaw (F-T) sandstone are studied to investigate the failure mechanism of engineering rock in cold regions. First, the fatigue properties of the samples are analysed in terms of stress-strain, deformation characteristics, and pore structure. Second, the types of hysteresis curves are analysed using the load-unload response ratio (LURR) method. Scanning electron microscopy (SEM) and acoustic emission (AE) techniques are then used to investigate the structural damage, crack evolution, and spectral characteristics of the samples. Based on the Lemaitre strain equivalence hypothesis, the improved Harris distribution is used to propose a new constitutive model of rock that underwent F-T cycles under multilevel fatigue loading. Finally, based on the strain difference model, the nonlinear stage of the model is corrected by defining new compaction coefficients using the Weibull distribution. Research shows that the deformation modulus of the F-T rock mass under fatigue loading has degradation behaviour and F-T cycles enhance the fatigue softening of samples. The dominant frequency range of samples under coupling is 70–330 kHz, showing multiband coexistence. As fatigue loading progresses, the hysteresis curve changes from stress hysteresis to strain hysteresis, and the frequency band gradually widens and develops towards low frequencies. The occurrence of a 0 kHz dominant frequency or LURR = 1 can be used as an early warning index of rock fatigue failure. As the number of F-T cycles progresses, the porosity composition curve shifts to the right, and the distribution of AE counts and the dominant frequency shift to the early loading stage.
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Abbreviations
- A d :
-
Damage area
- A e :
-
Effective bearing area
- D :
-
Damage variable
- D FL :
-
Fatigue damage
- D FT :
-
Freeze-thaw damage
- D FTFL :
-
Coupled damage
- E :
-
Elastic modulus
- E + :
-
Loading modulus
- E − :
-
Unloading modulus
- E d :
-
Deformation modulus
- E v :
-
Initial elastic modulus
- F a :
-
Micro-scale rock unit strength
- K :
-
Compaction coefficient
- m :
-
The mth freeze-thaw cycle
- n :
-
The nth cycle
- P :
-
Porosity
- U :
-
Number of micro-scale units
- X :
-
Response rate
- ε :
-
Strain
- ε c :
-
Crack closure point strain
- ε m :
-
Maximum cyclic strain
- ε p :
-
Peak strain
- ε s :
-
Yield strain
- ε v :
-
Initial cyclic strain
- σ :
-
Stress
- σ c :
-
Crack closure point stress
- σ i :
-
Crack initiation stress
- σ m :
-
Maximum cyclic stress
- σ max :
-
Upper limit stress
- σ min :
-
Lower limit stress
- σ p :
-
Peak stress
- σ s :
-
Yield stress
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Acknowledgements
We would like to thank the journal editors and reviewers for their valuable comments.
Funding
This study was supported by the National Natural Science Foundation of China [grant number 51979293], Hunan Provincial Key Research and Development Program [grant number 2022SK2082], Science and Technology Project of Hunan Natural Resources Department [grant number 2021-52], Hunan Civil Air Defence Research Project [grant number HNRFKJ-2021-07], and Postgraduate Innovative Project of Central South University [grant number 2021XQLH154].
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Shi, Z., Li, J., Wang, M. et al. Fatigue fracture behaviour and constitutive model of freeze-thaw sandstone under multilevel fatigue loads. Bull Eng Geol Environ 82, 319 (2023). https://doi.org/10.1007/s10064-023-03338-6
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DOI: https://doi.org/10.1007/s10064-023-03338-6