Fracture System Characteristics and Their Control on Permeability Anisotropy in Bright and Dull Coal

Coal permeability, a key parameter influencing coalbed methane production and geological storage, is strongly governed by the dual-porosity nature of coal and the stress-dependent evolution of its fracture network. This study investigates the development characteristics of filled and unfilled fractures, and the resulting permeability anisotropy, in typical bright and dull coals from the deep 8# coal seam of the Ordos Basin. Utilizing CT scanning and permeability anisotropy testing, we analyze how fracture development impacts coal permeability and its evolution under stress. Bright coal exhibits a grid-like distribution of mineral-filled fractures with good vertical connectivity, and a complex network of unfilled fractures. In contrast, dull coal displays a scattered distribution of mineral-filled fractures with poor vertical connectivity and a limited number of unfilled fractures. Results indicate an exponential decay trend in permeability with increasing confining pressure, strongly correlated with fracture system development. Permeability also demonstrates significant heterogeneity (face cleat > butt cleat > vertical). Bright coal exhibits a greater permeability decay rate than dull coal, indicating heightened stress sensitivity, while its permeability anisotropy is weaker, aligning with the observed fracture development patterns.