https://doi.org/10.1140/epjb/e2006-00168-y
Numerical studies of gravity destabilized percolation in 2D porous media
1
Key Laboratory of Mineral Resource, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, P.R. China
2
Laboratoire de tectonophysique (UMR5568), ISTEEM, CNRS & Université Montpellier II, 34095 Montpellier, France
3
SISYPHE, UMR, Boîte 123, Université Paris 6, 75252 Paris Cedex 05, France
Corresponding author: a loggia@univ-montp2.fr
Received:
22
April
2005
Revised:
3
January
2006
Published online:
17
May
2006
Two dimensional simulations of percolation are realized on square networks of pore throats with a random capillary pressure distribution. We analyse the influence of a destabilizing gravity field (g) and of the standard deviation of the distribution of the capillary pressure thresholds (Wt). The fragmentation process is not taken into account in this study. For an increase of g or/and when Wt decreases, two transitions are analyzed with three different regimes displacement patterns: Invasion percolation, invasion percolation in a gradient, and invasion in a pure gradient. The transitions are controlled both by the ratio g/Wt and by the sample size (L). A scaling law between the saturation at the percolation threshold and g/Wt allows delineating the three regimes in agreement with theoretical argument of the percolation in a gradient.
PACS: 47.55.Mh – Flows through porous media / 61.43.Hv – Fractals; macroscopic aggregates (including diffusion-limited aggregates) / 47.55.Kf – Particle-laden flows
© EDP Sciences, Società Italiana di Fisica, Springer-Verlag, 2006