Wettability control on multiphase flow in patterned microfluidics

Multiphase flow in porous media is important in many natural and industrial processes, including geologic CO₂ sequestration, enhanced oil recovery, and water infiltration into soil. Although it is well known that the wetting properties of porous media can vary drastically depending on the type of me...

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Bibliographic Details
Main Authors: Zhao, Benzhong (Contributor), MacMinn, Christopher W. (Author), Juanes, Ruben (Contributor)
Other Authors: Massachusetts Institute of Technology. Department of Civil and Environmental Engineering (Contributor)
Format: Article
Language:English
Published: National Academy of Sciences (U.S.), 2017-05-11T18:17:55Z.
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Online Access:Get fulltext
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100 1 0 |a Zhao, Benzhong  |e author 
100 1 0 |a Massachusetts Institute of Technology. Department of Civil and Environmental Engineering  |e contributor 
100 1 0 |a Zhao, Benzhong  |e contributor 
100 1 0 |a Juanes, Ruben  |e contributor 
700 1 0 |a MacMinn, Christopher W.  |e author 
700 1 0 |a Juanes, Ruben  |e author 
245 0 0 |a Wettability control on multiphase flow in patterned microfluidics 
260 |b National Academy of Sciences (U.S.),   |c 2017-05-11T18:17:55Z. 
856 |z Get fulltext  |u http://hdl.handle.net/1721.1/108824 
520 |a Multiphase flow in porous media is important in many natural and industrial processes, including geologic CO₂ sequestration, enhanced oil recovery, and water infiltration into soil. Although it is well known that the wetting properties of porous media can vary drastically depending on the type of media and pore fluids, the effect of wettability on multiphase flow continues to challenge our microscopic and macroscopic descriptions. Here, we study the impact of wettability on viscously unfavorable fluid-fluid displacement in disordered media by means of high-resolution imaging in microfluidic flow cells patterned with vertical posts. By systematically varying the wettability of the flow cell over a wide range of contact angles, we find that increasing the substrate's affinity to the invading fluid results in more efficient displacement of the defending fluid up to a critical wetting transition, beyond which the trend is reversed. We identify the pore-scale mechanisms-cooperative pore filling (increasing displacement efficiency) and corner flow (decreasing displacement efficiency)-responsible for this macroscale behavior, and show that they rely on the inherent 3D nature of interfacial flows, even in quasi-2D media. Our results demonstrate the powerful control of wettability on multiphase flow in porous media, and show that the markedly different invasion protocols that emerge-from pore filling to postbridging-are determined by physical mechanisms that are missing from current pore-scale and continuum-scale descriptions. 
520 |a United States. Department of Energy (DE-SC0003907) 
520 |a United States. Department of Energy (DE-FE0009738) 
546 |a en_US 
655 7 |a Article 
773 |t Proceedings of the National Academy of Sciences