International audienceWe study viscous fingering during drainage experiments in linear Hele-Shaw cells filled with a random porous medium. The central zone of the cell is found to be statistically more occupied than the average, and to have a lateral width of 40% of the system width, irrespectively of the capillary number Ca. A crossover length wf ∝ Ca−1 separates lower scales where the invader's fractal dimension D sime 1.83 is identical to capillary fingering, and larger scales where the dimension is found to be D sime 1.53. The lateral width and the large-scale dimension are lower than the results for Diffusion Limited Aggregation, but can be explained in terms of Dielectric Breakdown Model. Indeed, we show that when averaging over the q...
International audienceWe study the formation of viscous fingering and fracturing patterns that occur...
Numerical simulation is used to study the effect of different factors on unstable miscible displacem...
Finger-like protrusions that form along fluid−fluid displacement fronts in porous media are often ex...
International audienceWe study viscous fingering during drainage experiments in linear Hele-Shaw cel...
4 pages, 4 figures, Europhysics LettersWe study viscous fingering during drainage experiments in lin...
We study viscous fingering during drainage experiments in linear Hele-Shaw cells filled with a rando...
PACS. 47.20.Gv – Viscous instability. PACS. 47.54.+r – Pattern selection; pattern formation. PACS. 4...
We study viscous fingering during drainage experiments in linear Hele-Shaw cells filled with a rando...
We present a study of viscous fingering using the Volume Of Fluid method and a central injection geo...
11 pages 11 figuresWe present in this paper an experimental study of the invasion activity during un...
We describe a crossover from the viscous fingering instability to a compact invasion regime during v...
The invasion process during unstable drainage in porous Hele-Shaw cell was analyzed under displaced ...
Viscous fingering occurs when a less viscous fluid is driven into a more viscous fluid in a porous ...
Viscous fingering occurs when a less viscous fluid is driven into a more viscous fluid in a porous ...
The applications of carbon dioxide sequestration in brine-saturated reservoirs, as well as recovery...
International audienceWe study the formation of viscous fingering and fracturing patterns that occur...
Numerical simulation is used to study the effect of different factors on unstable miscible displacem...
Finger-like protrusions that form along fluid−fluid displacement fronts in porous media are often ex...
International audienceWe study viscous fingering during drainage experiments in linear Hele-Shaw cel...
4 pages, 4 figures, Europhysics LettersWe study viscous fingering during drainage experiments in lin...
We study viscous fingering during drainage experiments in linear Hele-Shaw cells filled with a rando...
PACS. 47.20.Gv – Viscous instability. PACS. 47.54.+r – Pattern selection; pattern formation. PACS. 4...
We study viscous fingering during drainage experiments in linear Hele-Shaw cells filled with a rando...
We present a study of viscous fingering using the Volume Of Fluid method and a central injection geo...
11 pages 11 figuresWe present in this paper an experimental study of the invasion activity during un...
We describe a crossover from the viscous fingering instability to a compact invasion regime during v...
The invasion process during unstable drainage in porous Hele-Shaw cell was analyzed under displaced ...
Viscous fingering occurs when a less viscous fluid is driven into a more viscous fluid in a porous ...
Viscous fingering occurs when a less viscous fluid is driven into a more viscous fluid in a porous ...
The applications of carbon dioxide sequestration in brine-saturated reservoirs, as well as recovery...
International audienceWe study the formation of viscous fingering and fracturing patterns that occur...
Numerical simulation is used to study the effect of different factors on unstable miscible displacem...
Finger-like protrusions that form along fluid−fluid displacement fronts in porous media are often ex...