The Role of Local Instabilities in Fluid Invasion into Permeable Media

Abstract Wettability is an important factor which controls the displacement of immiscible fluids in permeable media, with far reaching implications for storage of CO2 in deep saline aquifers, fuel cells, oil recovery, and for the remediation of oil contaminated soils. Considering the paradigmatic ca...

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Main Authors: Kamaljit Singh, Hagen Scholl, Martin Brinkmann, Marco Di Michiel, Mario Scheel, Stephan Herminghaus, Ralf Seemann
Format: Article
Language:English
Published: Nature Publishing Group 2017-03-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-017-00191-y
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spelling doaj-c9a90de3441742c9aadb4d5e9215e3d62020-12-08T02:22:18ZengNature Publishing GroupScientific Reports2045-23222017-03-017111110.1038/s41598-017-00191-yThe Role of Local Instabilities in Fluid Invasion into Permeable MediaKamaljit Singh0Hagen Scholl1Martin Brinkmann2Marco Di Michiel3Mario Scheel4Stephan Herminghaus5Ralf Seemann6Saarland University, Experimental PhysicsSaarland University, Experimental PhysicsSaarland University, Experimental PhysicsESRF, The European SynchrotronESRF, The European SynchrotronMax Planck Institute for Dynamics and Self-OrganizationSaarland University, Experimental PhysicsAbstract Wettability is an important factor which controls the displacement of immiscible fluids in permeable media, with far reaching implications for storage of CO2 in deep saline aquifers, fuel cells, oil recovery, and for the remediation of oil contaminated soils. Considering the paradigmatic case of random piles of spherical beads, fluid front morphologies emerging during slow immiscible displacement are investigated in real time by X-ray micro–tomography and quantitatively compared with model predictions. Controlled by the wettability of the bead matrix two distinct displacement patterns are found. A compact front morphology emerges if the invading fluid wets the beads while a fingered morphology is found for non–wetting invading fluids, causing the residual amount of defending fluid to differ by one order of magnitude. The corresponding crossover between these two regimes in terms of the advancing contact angle is governed by an interplay of wettability and pore geometry and can be predicted on the basis of a purely quasi–static consideration of local instabilities that control the progression of the invading interface.https://doi.org/10.1038/s41598-017-00191-y
collection DOAJ
language English
format Article
sources DOAJ
author Kamaljit Singh
Hagen Scholl
Martin Brinkmann
Marco Di Michiel
Mario Scheel
Stephan Herminghaus
Ralf Seemann
spellingShingle Kamaljit Singh
Hagen Scholl
Martin Brinkmann
Marco Di Michiel
Mario Scheel
Stephan Herminghaus
Ralf Seemann
The Role of Local Instabilities in Fluid Invasion into Permeable Media
Scientific Reports
author_facet Kamaljit Singh
Hagen Scholl
Martin Brinkmann
Marco Di Michiel
Mario Scheel
Stephan Herminghaus
Ralf Seemann
author_sort Kamaljit Singh
title The Role of Local Instabilities in Fluid Invasion into Permeable Media
title_short The Role of Local Instabilities in Fluid Invasion into Permeable Media
title_full The Role of Local Instabilities in Fluid Invasion into Permeable Media
title_fullStr The Role of Local Instabilities in Fluid Invasion into Permeable Media
title_full_unstemmed The Role of Local Instabilities in Fluid Invasion into Permeable Media
title_sort role of local instabilities in fluid invasion into permeable media
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2017-03-01
description Abstract Wettability is an important factor which controls the displacement of immiscible fluids in permeable media, with far reaching implications for storage of CO2 in deep saline aquifers, fuel cells, oil recovery, and for the remediation of oil contaminated soils. Considering the paradigmatic case of random piles of spherical beads, fluid front morphologies emerging during slow immiscible displacement are investigated in real time by X-ray micro–tomography and quantitatively compared with model predictions. Controlled by the wettability of the bead matrix two distinct displacement patterns are found. A compact front morphology emerges if the invading fluid wets the beads while a fingered morphology is found for non–wetting invading fluids, causing the residual amount of defending fluid to differ by one order of magnitude. The corresponding crossover between these two regimes in terms of the advancing contact angle is governed by an interplay of wettability and pore geometry and can be predicted on the basis of a purely quasi–static consideration of local instabilities that control the progression of the invading interface.
url https://doi.org/10.1038/s41598-017-00191-y
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