Numerical Simulation on Non-Darcy Flow in a Single Rock Fracture Domain Inverted by Digital Images

• Published in: Geofluids Vol. 2020; no. 2020; pp. 1 - 13
• Main Authors: Wang, Zaiyong, Sun, Wenbin, Zhang, Qi, Shao, Jianli, Zhu, Xianxiang
• Format: Journal Article
• Language: English
• Published: Cairo, Egypt Hindawi Publishing Corporation 2020; Hindawi; Hindawi Limited; Wiley
• Subjects: Algorithms; Analysis; Apertures; Coal; Coalbed methane; Coefficients; Computational fluid dynamics; Computer simulation; Digital imaging; Domains; Flow (Dynamics); Fluid flow; Fractures; Geotechnical engineering; Inertia; Inversion; Mathematical models; Numerical analysis; Numerical simulations; Permeability; Polymethyl methacrylate; Porous materials; Pressure gradients; Reynolds number; Rocks; Roughness; Roughness coefficient; Seepage; Simulation
• ISSN: 1468-8115; 1468-8123
• DOI: 10.1155/2020/8814327

The influence of rock seepage must be considered in geotechnical engineering, and understanding the fluid flow in rock fractures is of great concern in the seepage effect investigation. This study is aimed at developing a model for inversion of rock fracture domains based on digital images and further study of non-Darcy flow. The visualization model of single rock fracture domain is realized by digital images, which is further used in flow numerical simulation. We further discuss the influence of fracture domain geometry on non-Darcy flow. The results show that it is feasible to study non-Darcy flow in rock fracture domains by inversion based on digital images. In addition, as the joint roughness coefficient (JRC) increases or the fracture aperture decreases, distortion of the fluid flow path increases, and the pressure gradient loss caused by the inertial force increases. Both coefficients of the Forchheimer equation decrease with increasing fracture aperture and increase with increasing JRC. Meanwhile, the critical Reynolds number tends to decrease when JRC increases or the fracture aperture decreases, indicating that the fluid tends to non-Darcy flow. This work provides a reference for the study of non-Darcy flow through rock fractures.