Characterization of the Fine-Scale Evolution of Damage in Shale under the Influence of Two-Way Stress Differences Based on CT Images and Fractal Theory—The Example of the Anba Dyke in the Wufeng–Longmaxi Formation

• Published in: Fractal and fractional Vol. 8; no. 3; p. 142
• Main Authors: Lan, Baofeng, Yang, Ruidong, Wu, Zhonghu, Jiang, Haishen, Li, Xinzheng
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01-02-2024
• Subjects: Algorithms; Complexity; Computed tomography; CT imaging; CT reconfiguration; Damage; Deformation; differential horizontal stress; Digital imaging; Fractal analysis; fractal dimension; Fractal geometry; Fractals; Fractures; Hydraulic fracturing; Investigations; Medical imaging; Morphology; Network formation; Numerical models; Plate tectonics; Residual strength; Simulation; Stress analysis; Stress concentration; Stress ratio; triaxial compression; Triaxial compression tests; China; Guizhou China
• ISSN: 2504-3110; 2504-3110
• DOI: 10.3390/fractalfract8030142

To better understand the influence of different levels of two-way stress differences on the development of damage in Anchang diametral laminar shale in the northern Qianbei area, a numerical model of laminar shale with a representative fine-scale structure was established by using RFPA3D-CT. A triaxial compression test was conducted; a three-dimensional mesoscale fracture box dimension algorithm based on digital images was generated by using MATLAB R2020b; and the fractal characteristics were quantitatively analyzed. The results showed that under the influence of the horizontal stress ratio and two-way stress, the greater the two-way stress is, the more notable the plastic characteristics of specimen damage are, and the higher the residual strength is. The specimens with lower two-way stress exhibited obvious brittle damage characteristics. The difficulty degree of complex fracture network formation increased with the increase in the horizontal tension ratio, and the degree of increase in the fracture network complexity gradually decreased. At a horizontal stress ratio of 1.25, the fractal dimension was the highest, which indicates that the cracks were the most pronounced. Fracture formation after specimen damage was the most common phenomenon. Under the condition of a lower horizontal stress ratio, a large number of fracture structures could be generated in shale specimens after damage, promoting the expansion of natural fractures.