Evolutionary Analysis of Heterogeneous Granite Microcracks Based on Digital Image Processing in Grain-Block Model
Guanlin Liu1, Youliang Chen1, Xi Du1
1Department of Civil Engineering, School of Environment and Architecture, University of Shanghai for Science and Technology, Shanghai 200093, China.
Materials (Basel, Switzerland)
|March 10, 2022
Summary
Microstructure heterogeneity in rocks causes stress concentrations, leading to microcracks and failure. Numerical models reveal crack initiation at grain boundaries and varying crack patterns in quartz, feldspar, and biotite under compression.
Area of Science:
- Rock mechanics
- Computational geosciences
- Materials science
Background:
- Rock microstructure heterogeneity significantly influences microcrack evolution during compression.
- Understanding grain-scale damage mechanisms is crucial for predicting rock failure.
Purpose of the Study:
- To investigate the damage mechanism and microcrack characteristics of heterogeneous Biotite granite under compression.
- To develop and validate a numerical model for simulating rock fracture at the grain scale.
Main Methods:
- Digital image processing techniques to construct a digital image-based heterogeneous grain model.
- Discrete element method (DEM) to simulate compression and fracture.
- Model calibration against laboratory macroscopic properties of biotite granite.
Main Results:
- Microcracking initiates at weak grain boundaries; intragranular shear cracks indicate peak strength.
- Microstructure heterogeneity causes stress concentration, essential for crack initiation and rupture.
- Crack patterns vary across mineral types (quartz, feldspar, biotite), influenced by confining pressure.
Conclusions:
- Numerical simulations accurately replicate experimental observations of microcrack propagation and damage modes.
- Microstructure heterogeneity is a primary driver of rock fracture complexity.
- Confining pressure alters failure modes from tensile splitting to shear failure.
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