Local Cubic Law Simulation of Stress-dependent Aperture-based Permeability
Abstract:
The experiment shows that permeability change is greater than expected from mean aperture change at different stress levels. LCL simulation demonstrates that this is mainly due to the change of fluid flow pattern with stress, which is caused by aperture distribution change. LCL simulation also exhibits that channeling behavior plays an important role in fluid flow in fractures, and sometimes a small number of channels dominate the flow. In the experiment, we apply different flow rates to assess the LCL simulation at different Reynolds number. The simulation results show that fluid flow rate (1.24 < Re < 15.28) does not have a large impact on LCL predictability in the highly tortuous and rough rock fractures, which agrees with the results of Konzuk and Kueper (2004).
References:
Brown, S. R., 1987, Fluid flow through rock joints: The effect of surface roughness, J. Geophys. Res., 92(B2), 1337-1347
Konzuk, J. and Kueper, B.H., 2004. Evaluation of cubic law based models describing single-phase flow through a rough-walled fractured. Water Resources Research, Vol. 40, No. 2
Witherspoon, P.A., JSY. Wang, K. Iwai, and J.E. Gale (1980), “Validity of cubic law for fluid-flow in a deformable rock fracture”, Water Resour. Res., 16:1016-1024
