Cluster evolution in steady-state two-phase flow in porous media
arXiv:cond-mat/0511599 · doi:10.1103/PhysRevE.73.026306
Abstract
We report numerical studies of the cluster development of two-phase flow in a steady-state environment of porous media. This is done by including biperiodic boundary conditions in a two-dimensional flow simulator. Initial transients of wetting and non-wetting phases that evolve before steady-state has occurred, undergo a cross-over where every initial patterns are broken up. For flow dominated by capillary effects with capillary numbers in order of , we find that around a critical saturation of non-wetting fluid the non-wetting clusters of size have a power-law distribution with the exponent for large clusters. This is a lower value than the result for ordinary percolation. We also present scaling relation and time evolution of the structure and global pressure.
12 pages, 11 figures. Minor corrections. Accepted for publication in Phys. Rev. E
References in corpus (4)
- A study of fragmentation processes using a discrete element method
- Burst dynamics during drainage displacements in porous media: Simulations and experiments
- Competition between Diffusion and Fragmentation: An Important Evolutionary Process of Nature
- Viscous stabilization of 2D drainage displacements with trapping
Cited by in corpus (5)
- History-independence of steady-state in simultaneous two-phase flow through porous media
- On the scaling of probability density functions with apparent power-law exponents less than unity
- Local Wettability Reversal during Steady-State Two-Phase Flow in Porous Media
- Capillary-Driven Instability of Immiscible Fluid Interfaces Flowing in Parallel in Porous Media
- Local Statistics of Immiscible and Incompressible Two-Phase Flow in Porous Media