Quantifying crack and fractal features in multi-hole limestone combined with x-ray CT and machine learning
摘要
Dissolution channels significantly affect the mechanical behavior of karst slopes. Triaxial compression tests, 3D X-ray CT scanning, and machine learning are employed to investigate the failure characteristics and crack evolution in multi-hole limestone. A random forest model was developed to predict the crack fractal dimension, enabling a quantitative assessment of post-failure crack complexity. Results indicate that holed limestone develops through-going shear cracks and intersecting tensile cracks, with crack propagation increasing in quantity, length, and uniformity as hole number rises. The proportion of short cracks decreased from 69.50% to 50.70%, while ultra-long cracks increased from 35 to 93, and maximum crack area expanded by 68.37%. Peak and residual strength declined quadratically with increasing CT volume fracture (Vct); when Vct rose from 5.5% to 10.8%, peak and residual strength dropped by 22.32% and 46.07%, respectively. A strong positive correlation observed between Vct and 3D fractal dimension (Ds). The proposed random forest model achieved MSE, RMSE, and MAE values below 0.02, with R² >0.9, demonstrating high predictive accuracy. These findings provide a robust foundation for rock stability assessment in karst regions, offering insights into failure mechanisms and disaster prevention strategies.