English

Flow through three-dimensional self-affine fractures

Fluid Dynamics 2020-10-14 v1 Geophysics

Abstract

We investigate through numerical simulations of the Navier-Stokes equations the influence of the surface roughness on the fluid flow through fracture joints. Using the Hurst exponent HH to characterize the roughness of the self-affine surfaces that constitute the fracture, our analysis reveal the important interplay between geometry and inertia on the flow. Precisely, for low values of Reynolds numbers Re, we use Darcy's law to quantify the hydraulic resistance GG of the fracture and show that its dependence on HH can be explained in terms of a simple geometrical model for the tortuosity τ\tau of the channel. At sufficiently high values of Re, when inertial effects become relevant, our results reveal that nonlinear corrections up to third-order to Darcy's law are aproximately proportional to HH. These results imply that the resistance GG to the flow follows a universal behavior by simply rescaling it in terms of the fracture resistivity and using an effective Reynolds number, namely, Re/HH. Our results also reveal the presence of quasi-one-dimensional channeling, even considering the absence of shear displacement between upper and lower surfaces of the self-affine fracture.

Keywords

Cite

@article{arxiv.2006.04846,
  title  = {Flow through three-dimensional self-affine fractures},
  author = {H. J. Seybold and H. A. Carmona and F. A. Leandro Filho and A. D. Araújo and F. Nepomuceno Filho and J. S. Andrade},
  journal= {arXiv preprint arXiv:2006.04846},
  year   = {2020}
}

Comments

10 pages, 8 figures

R2 v1 2026-06-23T16:09:31.939Z