X-ray tomography measurements of power-law cluster size distributions for the nonwetting phase in sandstones.

Three-dimensional images of sandstones containing residual nonwetting phase were obtained using synchrotron x-ray tomography with a resolution of approximately 9 µm. We determined the size distribution of disconnected nonwetting phase clusters (ganglia); the number of ganglia of size s is N(s)~s(-t)...

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Main Authors: Iglauer, Stefan, Favretto, S., Spinelli, G., Schena, G., Blunt, M.
Format: Journal Article
Published: The American Physical Society 2010
Online Access:http://hdl.handle.net/20.500.11937/35477
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author Iglauer, Stefan
Favretto, S.
Spinelli, G.
Schena, G.
Blunt, M.
author_facet Iglauer, Stefan
Favretto, S.
Spinelli, G.
Schena, G.
Blunt, M.
author_sort Iglauer, Stefan
building Curtin Institutional Repository
collection Online Access
description Three-dimensional images of sandstones containing residual nonwetting phase were obtained using synchrotron x-ray tomography with a resolution of approximately 9 µm. We determined the size distribution of disconnected nonwetting phase clusters (ganglia); the number of ganglia of size s is N(s)~s(-t) with t=2.05 . The vast majority of the residual phase was contained in large clusters, spanning many pores. This result implies that we have clusters of all sizes providing a huge surface area for geochemical reactions and dissolution while allowing mobilization of the residual phase during improved oil recovery in hydrocarbon reservoirs and carbon dioxide storage in aquifers.
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publishDate 2010
publisher The American Physical Society
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spelling curtin-20.500.11937-354772017-09-13T15:26:49Z X-ray tomography measurements of power-law cluster size distributions for the nonwetting phase in sandstones. Iglauer, Stefan Favretto, S. Spinelli, G. Schena, G. Blunt, M. Three-dimensional images of sandstones containing residual nonwetting phase were obtained using synchrotron x-ray tomography with a resolution of approximately 9 µm. We determined the size distribution of disconnected nonwetting phase clusters (ganglia); the number of ganglia of size s is N(s)~s(-t) with t=2.05 . The vast majority of the residual phase was contained in large clusters, spanning many pores. This result implies that we have clusters of all sizes providing a huge surface area for geochemical reactions and dissolution while allowing mobilization of the residual phase during improved oil recovery in hydrocarbon reservoirs and carbon dioxide storage in aquifers. 2010 Journal Article http://hdl.handle.net/20.500.11937/35477 10.1103/PhysRevE.82.056315 The American Physical Society restricted
spellingShingle Iglauer, Stefan
Favretto, S.
Spinelli, G.
Schena, G.
Blunt, M.
X-ray tomography measurements of power-law cluster size distributions for the nonwetting phase in sandstones.
title X-ray tomography measurements of power-law cluster size distributions for the nonwetting phase in sandstones.
title_full X-ray tomography measurements of power-law cluster size distributions for the nonwetting phase in sandstones.
title_fullStr X-ray tomography measurements of power-law cluster size distributions for the nonwetting phase in sandstones.
title_full_unstemmed X-ray tomography measurements of power-law cluster size distributions for the nonwetting phase in sandstones.
title_short X-ray tomography measurements of power-law cluster size distributions for the nonwetting phase in sandstones.
title_sort x-ray tomography measurements of power-law cluster size distributions for the nonwetting phase in sandstones.
url http://hdl.handle.net/20.500.11937/35477