Nonwetting phase residual saturation in sand packs

We measure residual nonwetting phase saturation in six unconsolidated sands of different average grain sizes. Wealso analyze the pore structure using three-dimensional images from which topologically equivalent pore networks are extracted. The residual saturations range from 10.8% to 13.1%, which is...

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Main Authors: Gittins, P., Iglauer, Stefan, Pentland, C., Al-Mansoori, S., Al-Sayari, S., Bijeljic, B., Blunt, M.
Format: Journal Article
Published: Begell House 2010
Online Access:http://hdl.handle.net/20.500.11937/18962
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author Gittins, P.
Iglauer, Stefan
Pentland, C.
Al-Mansoori, S.
Al-Sayari, S.
Bijeljic, B.
Blunt, M.
author_facet Gittins, P.
Iglauer, Stefan
Pentland, C.
Al-Mansoori, S.
Al-Sayari, S.
Bijeljic, B.
Blunt, M.
author_sort Gittins, P.
building Curtin Institutional Repository
collection Online Access
description We measure residual nonwetting phase saturation in six unconsolidated sands of different average grain sizes. Wealso analyze the pore structure using three-dimensional images from which topologically equivalent pore networks are extracted. The residual saturations range from 10.8% to 13.1%, which is lower than for most consolidated media. Higher porosity is associated with lower residual saturations, while there is little correlation between grain and pore shape and the degree of trapping. We also study layered packs: the residual saturations are reduced compared to comparable homogeneous systems. We discuss the results in the context of capillary trapping during carbon storage in aquifers.
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institution Curtin University Malaysia
institution_category Local University
last_indexed 2025-11-14T07:28:14Z
publishDate 2010
publisher Begell House
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spelling curtin-20.500.11937-189622017-09-13T13:44:35Z Nonwetting phase residual saturation in sand packs Gittins, P. Iglauer, Stefan Pentland, C. Al-Mansoori, S. Al-Sayari, S. Bijeljic, B. Blunt, M. We measure residual nonwetting phase saturation in six unconsolidated sands of different average grain sizes. Wealso analyze the pore structure using three-dimensional images from which topologically equivalent pore networks are extracted. The residual saturations range from 10.8% to 13.1%, which is lower than for most consolidated media. Higher porosity is associated with lower residual saturations, while there is little correlation between grain and pore shape and the degree of trapping. We also study layered packs: the residual saturations are reduced compared to comparable homogeneous systems. We discuss the results in the context of capillary trapping during carbon storage in aquifers. 2010 Journal Article http://hdl.handle.net/20.500.11937/18962 10.1615/JPorMedia.v13.i7.10 Begell House restricted
spellingShingle Gittins, P.
Iglauer, Stefan
Pentland, C.
Al-Mansoori, S.
Al-Sayari, S.
Bijeljic, B.
Blunt, M.
Nonwetting phase residual saturation in sand packs
title Nonwetting phase residual saturation in sand packs
title_full Nonwetting phase residual saturation in sand packs
title_fullStr Nonwetting phase residual saturation in sand packs
title_full_unstemmed Nonwetting phase residual saturation in sand packs
title_short Nonwetting phase residual saturation in sand packs
title_sort nonwetting phase residual saturation in sand packs
url http://hdl.handle.net/20.500.11937/18962