ArticleMaterials (Basel, Switzerland)2023
Fracture Closure Empirical Model and Theoretical Damage Model of Rock under Compression.
Article in Materials (Basel, Switzerland), 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.
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5 citing papers in PubMed.
- Mechanical properties and piecewise constitutive model of fine sandstone in mining area of western China.Scientific reports · 2025Article
- Failure Mechanism and Control Mechanism of Intermittent Jointed Rock Bridge Based on Acoustic Emission (AE) and Digital Image Correlation (DIC).Materials (Basel, Switzerland) · 2024Article
- Numerical Study on the Impact of Locked-In Stress on Rock Failure Processes and Energy Evolutions.Materials (Basel, Switzerland) · 2023Article
- Constitutive Model for Grouted Rock Mass by Macro-Meso Damage.Materials (Basel, Switzerland) · 2023Article
- Nonlinear Strength Reduction Method of Rock Mass in Slope Stability Evaluation.Materials (Basel, Switzerland) · 2023Article
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9 authors.
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Abstract
The rock or rock mass in engineering often contains joints, fractures, voids, and other defects, which are the root cause of local or overall failure. In response to most of the current constitutive models that fail to simulate the nonlinear fracture compaction deformation in the whole process of rock failure, especially brittle rocks, a piecewise constitutive model was proposed to represent the global constitutive relation of rocks in this study, which was composed of the fracture compaction empirical model and the damage statistical constitutive model. The fracture empirical compaction model was determined by fitting the expressions of fracture closure curves of various rocks, while the rock damage evolution equation was derived underpinned by the fracture growth. According to the effective stress concept and strain equivalence hypothesis, the rock damage constitutive model was deduced. The model parameters of the fracture compaction empirical model and damage statistical constitutive model were all calculated by the geometrical characteristics of the global axial stress-strain curve to guarantee that the models are continuous and smooth at the curve intersection, which is also simple and ready to program. Finally, the uniaxial compression test data and the triaxial compression test data of different rocks in previous studies were employed to validate the models, and the determination coefficient was used to measure the accuracy. The results showed great consistency between the model curves and test data, especially in the pre-peak stage.
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