Influence of Wetting on Viscous Fingering Via 2D Lattice Boltzmann Simulations

Abstract We present simulations of two-phase flow using the Rothman and Keller colour gradient Lattice Boltzmann method to study viscous fingering when a "red fluid" invades a porous model initially filled with a "blue" fluid with different viscosity. We conducted eleven suites o...

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Bibliographic Details
Main Authors: Mora, Peter (Author), Morra, Gabriele (Author), Yuen, Dave A. (Author), Juanes, Ruben (Author)
Other Authors: Massachusetts Institute of Technology. Department of Civil and Environmental Engineering (Contributor)
Format: Article
Language:English
Published: Springer Netherlands, 2022-07-06T18:55:11Z.
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042 |a dc 
100 1 0 |a Mora, Peter  |e author 
100 1 0 |a Massachusetts Institute of Technology. Department of Civil and Environmental Engineering  |e contributor 
700 1 0 |a Morra, Gabriele  |e author 
700 1 0 |a Yuen, Dave A.  |e author 
700 1 0 |a Juanes, Ruben  |e author 
245 0 0 |a Influence of Wetting on Viscous Fingering Via 2D Lattice Boltzmann Simulations 
260 |b Springer Netherlands,   |c 2022-07-06T18:55:11Z. 
856 |z Get fulltext  |u https://hdl.handle.net/1721.1/136899.2 
520 |a Abstract We present simulations of two-phase flow using the Rothman and Keller colour gradient Lattice Boltzmann method to study viscous fingering when a "red fluid" invades a porous model initially filled with a "blue" fluid with different viscosity. We conducted eleven suites of 81 numerical experiments totalling 891 simulations, where each suite had a different random realization of the porous model and spanned viscosity ratios in the range $$M\in [0.01,100]$$ M ∈ [ 0.01 , 100 ] and wetting angles in the range $$\theta _w\in [180^\circ ,0^\circ ]$$ θ w ∈ [ 180 ∘ , 0 ∘ ] to allow us to study the effect of these parameters on the fluid-displacement morphology and saturation at breakthrough (sweep). Although sweep often increased with wettability, this was not always so and the sweep phase space landscape, defined as the difference in saturation at a given wetting angle relative to saturation for the non-wetting case, had hills, ridges and valleys. At low viscosity ratios, flow at breakthrough is localized through narrow fingers that span the model. After breakthrough, the flow field continues to evolve and the saturation continues to increase albeit at a reduced rate, and eventually exceeds 90% for both non-wetting and wetting cases. The existence of a complicated sweep phase space at breakthrough, and continued post-breakthrough evolution suggests the hydrodynamics and sweep is a complicated function of wetting angle, viscosity ratio and time, which has major potential implications to Enhanced Oil Recovery by water flooding, and hence, on estimates of global oil reserves. Validation of these results via experiments is required to ensure they translate to field studies. 
546 |a en 
655 7 |a Article