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dc.contributor.authorMora, Peter
dc.contributor.authorMorra, Gabriele
dc.contributor.authorYuen, Dave A.
dc.contributor.authorJuanes, Ruben
dc.date.accessioned2022-01-24T14:54:17Z
dc.date.available2021-10-29T16:22:35Z
dc.date.available2022-01-24T14:54:17Z
dc.date.issued2021-06
dc.date.submitted2020-12
dc.identifier.issn1573-1634
dc.identifier.issn0169-3913
dc.identifier.urihttps://hdl.handle.net/1721.1/136735.2
dc.description.abstractAbstract 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.en_US
dc.publisherSpringer Netherlandsen_US
dc.relation.isversionofhttps://doi.org/10.1007/s11242-021-01629-8en_US
dc.rightsCreative Commons Attributionen_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_US
dc.sourceSpringer Netherlandsen_US
dc.titleInfluence of Wetting on Viscous Fingering Via 2D Lattice Boltzmann Simulationsen_US
dc.typeArticleen_US
dc.identifier.citationMora, Peter, Morra, Gabriele, Yuen, Dave A. and Juanes, Ruben. 2021. "Influence of Wetting on Viscous Fingering Via 2D Lattice Boltzmann Simulations."en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Civil and Environmental Engineering
dc.relation.journalTransport in Porous Mediaen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dc.date.updated2021-06-06T03:11:20Z
dc.language.rfc3066en
dc.rights.holderThe Author(s)
dspace.embargo.termsN
dspace.date.submission2021-06-06T03:11:20Z
mit.journal.volume138en_US
mit.licensePUBLISHER_CC
mit.metadata.statusAuthority Work Neededen_US


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