Key Takeaways & Executive Findings
- •• Introduces a flexible S-shaped damage evolution model based on an improved Logistic function that captures the full damage process during rock deformation—maintenance, onset, acceleration, deceleration, and termination—in a unified expression. • Establishes a constitutive model integrating damage mechanics and effective medium theory that accurately describes complete pre-peak compaction and post-peak strain softening behavior across multiple rock types. • Validated against uniaxial and trial compression tests on Miluo granite, yellow sandstone, mudstone, and glutenite, demonstrating close agreement between theoretical curves and experimental data and significant advantages over existing models. • The damage model parameters a, r, and β have clear physical meanings and competitive interactions, jointly controlling the shape of the theoretical stress-strain curve and enabling practical calibration for engineering applications.
Abstract
This study proposed a new and more flexible S-shaped rock damage evolution model from a phenomenological perspective based on an improved Logistic function to describe the characteristics of the rock strain softening and damage process. Simultaneously, it established a constitutive model capable of describing the entire process of rock pre-peak compaction and post-peak strain softening deformation, considering the nonlinear effects of the initial compaction stage of rocks, combined with damage mechanics theory and effective medium theory. In addition, this research verified the rationality of the constructed damage constitutive model using results from uniaxial and conventional triaxial compression tests on Miluo granite, yellow sandstone, mudstone, and glutenite. The results indicate that based on the improved Logistic function, the theoretical damage model accurately describes the entire evolution of damage characteristics during rock compression deformation, from maintenance through gradual onset, accelerated development to deceleration and termination, in a simple and unified expression. At the same time, the constructed constitutive model can accurately simulate the stress-strain process of different rock types under uniaxial and conventional triaxial compression, and the theoretical model curve closely aligns with experimental data. Compared to existing constitutive models, the proposed model has significant advantages. The damage model parameters a, r and β have clear physical meanings and interact competitively, where the three parameters collectively determine the shape of the theoretical stress-strain curve.
1. Introduction
Due to the large-scale development of infrastructure and the trend of energy extraction shifting from shallow to deep, numerous deep rock engineering projects, such as deeply buried tunnels and underground chambers, have emerged. These deep rock masses are influenced by complex geological environments characterized by high ground stress, high ground temperature, high karst water pressure, and mining disturbances. They exhibit pronounced nonlinear characteristics in their deformation and damage processes, making them susceptible to engineering disasters such as rockbursts [1]. Therefore, examining the evolution of rock damage and establishing suitable constitutive relationships is crucial for the stability analysis of the surrounding engineering rocks.
Since the application of damage theory in rock mechanics, utilizing this theory to develop rock constitutive relationships has proven highly effective. These damage mechanics models are typically categorized into macroscopic, mesoscopic, and microscopic phenomenology [2]. The macroscopic phenomenological model, for instance, treats the rock material as a continuous medium and often relies on macroscopic mechanical experiments. It utilizes variations in easily obtainable parameters to depict the rock damage evolution process, such as the elastic modulus [3, 4], crack body strain [5, 6], acoustic emission (AE) characteristic parameters [7, 8], and energy dissipation [9, 10]. In addition, statistical damage models generally assume that the physical properties of rock microelements follow a specific distribution function, including Weibull distribution.
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GUO Yun-peng, LIU Dong-qiao, YANG Sheng-kai, LI Jie-yu (2025). A new damage constitutive model for rock strain softening based on an improved Logistic function. Journal of Central South University. https://doi.org/10.1007/s11771-025-6027-y
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Frequently Asked Questions
What is the improved Logistic function-based damage constitutive model?
The proposed model is a phenomenological S-shaped damage evolution model that uses an improved Logistic function to describe the complete rock strain softening and damage process. It is combined with damage mechanics and effective medium theory to capture both pre-peak compaction and post-peak strain softening deformation.
How was the damage constitutive model validated?
The model was verified against uniaxial and conventional triaxial compression tests on four rock types: Miluo granite, yellow sandstone, mudstone, and glutenite. Theoretical stress-strain curves closely matched experimental data, demonstrating broad applicability and significant advantages over existing constitutive models.
What do the model parameters a, r, and β represent?
Parameters a, r, and β have clear physical meanings and interact competitively. Together they determine the shape of the theoretical stress-strain curve, providing flexibility to characterize different rock damage evolution behaviors.
Why is the improved Logistic function suitable for describing rock damage?
It can express the entire damage evolution in a simple and unified expression—spanning maintenance, gradual onset, accelerated development, deceleration, and termination—making it more flexible and accurate than conventional S-shaped functions.
What are the engineering applications of this research?
By accurately simulating the nonlinear deformation and damage of deep rock masses, the constitutive model supports stability analysis of deeply buried tunnels, underground chambers, and other engineering structures subjected to high stress, helping to mitigate hazards such as rockbursts.
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