Characterization of the crossover from capillary invasion to viscous fingering to fracturing during drainage in a vertical 2D porous medium

•Experimental and analytical study related to CO2 injection in saline aquifers.•Two-dimensional drainage under gravity.•Vertical injection of air in a water-saturated Hele-Shaw cell filled with glass beads.•Image processing and fractal analysis of the drainage invasion patterns.•Transitions from cap...

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Bibliographic Details
Published inInternational journal of multiphase flow Vol. 58; pp. 279 - 291
Main Authors Islam, Amina, Chevalier, Sylvie, Ben Salem, Imen, Bernabe, Yves, Juanes, Ruben, Sassi, Mohamed
Format Journal Article
LanguageEnglish
Published Kidlington Elsevier Ltd 01.01.2014
Elsevier
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Summary:•Experimental and analytical study related to CO2 injection in saline aquifers.•Two-dimensional drainage under gravity.•Vertical injection of air in a water-saturated Hele-Shaw cell filled with glass beads.•Image processing and fractal analysis of the drainage invasion patterns.•Transitions from capillary invasion to viscous fingering and to fracturing. We experimentally studied the displacement of a viscous wetting fluid (water) by an inviscid non-wetting fluid (air) injected at the bottom of a vertical Hele-Shaw cell filled with glass microbeads. In order to cover a wide parameter space, the permeability of the porous medium was varied by using different bead size ranges and diverse air flow rates were generated by means of a syringe pump. A LED light table was used to back illuminate the experimental cell, allowing a high speed camera to capture images of the drainage process at equal time intervals. The invasion occurred in intermittent bursts. Image processing of the bursts and fractal analysis showed successive transitions from capillary invasion to viscous fingering to fracturing during the same experiment, dependent on the medium permeability, the air injection flow rate, and the vertical position in the cell. The interplay between the capillary, viscous and gravity forces determines the nature of the invasion pattern and the transitions, from capillary invasion to viscous fingering with decreasing fluid pressure on one hand and from viscous fingering to fracturing with decreasing effective overburden pressure on the other hand.
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ISSN:0301-9322
1879-3533
DOI:10.1016/j.ijmultiphaseflow.2013.10.002