Influence of CO2-wettability on CO2 migration and trapping capacity in deep saline aquifers

CO2 migration and trapping capacity in deep saline aquifers are highly influenced by various rock and fluid parameters. One of the key parameters, which has received little attention, is CO2-wettability. We thus simulated the behavior of a CO2 plume in a deep saline aquifer as a function of rock wet...

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Main Authors: Al-Khdheeawi, E., Vialle, S., Barifcani, Ahmed, Sarmadivaleh, M., Iglauer, Stefan
Format: Journal Article
Published: Wiley 2017
Online Access:http://hdl.handle.net/20.500.11937/10629
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author Al-Khdheeawi, E.
Vialle, S.
Barifcani, Ahmed
Sarmadivaleh, M.
Iglauer, Stefan
author_facet Al-Khdheeawi, E.
Vialle, S.
Barifcani, Ahmed
Sarmadivaleh, M.
Iglauer, Stefan
author_sort Al-Khdheeawi, E.
building Curtin Institutional Repository
collection Online Access
description CO2 migration and trapping capacity in deep saline aquifers are highly influenced by various rock and fluid parameters. One of the key parameters, which has received little attention, is CO2-wettability. We thus simulated the behavior of a CO2 plume in a deep saline aquifer as a function of rock wettability and predicted various associated CO2 migration patterns and trapping capacities. We clearly show that CO2-wet reservoirs are most permeable for CO2; CO2 migrates furthest upwards and the plume has a candle-like shape, while in a water-wet reservoir the plume is more compact and rain-drop shaped. Furthermore, higher residual trapping capacities are achieved in water-wet rock, while solubility trapping is more efficient in CO2-wet rock. We thus conclude that rock wettability has a highly significant impact on both CO2 migration and trapping capacities and that water-wet reservoirs are preferable CO2 sinks due to their higher storage capacities and higher containment security.
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spelling curtin-20.500.11937-106292019-02-19T05:34:46Z Influence of CO2-wettability on CO2 migration and trapping capacity in deep saline aquifers Al-Khdheeawi, E. Vialle, S. Barifcani, Ahmed Sarmadivaleh, M. Iglauer, Stefan CO2 migration and trapping capacity in deep saline aquifers are highly influenced by various rock and fluid parameters. One of the key parameters, which has received little attention, is CO2-wettability. We thus simulated the behavior of a CO2 plume in a deep saline aquifer as a function of rock wettability and predicted various associated CO2 migration patterns and trapping capacities. We clearly show that CO2-wet reservoirs are most permeable for CO2; CO2 migrates furthest upwards and the plume has a candle-like shape, while in a water-wet reservoir the plume is more compact and rain-drop shaped. Furthermore, higher residual trapping capacities are achieved in water-wet rock, while solubility trapping is more efficient in CO2-wet rock. We thus conclude that rock wettability has a highly significant impact on both CO2 migration and trapping capacities and that water-wet reservoirs are preferable CO2 sinks due to their higher storage capacities and higher containment security. 2017 Journal Article http://hdl.handle.net/20.500.11937/10629 10.1002/ghg.1648 Wiley fulltext
spellingShingle Al-Khdheeawi, E.
Vialle, S.
Barifcani, Ahmed
Sarmadivaleh, M.
Iglauer, Stefan
Influence of CO2-wettability on CO2 migration and trapping capacity in deep saline aquifers
title Influence of CO2-wettability on CO2 migration and trapping capacity in deep saline aquifers
title_full Influence of CO2-wettability on CO2 migration and trapping capacity in deep saline aquifers
title_fullStr Influence of CO2-wettability on CO2 migration and trapping capacity in deep saline aquifers
title_full_unstemmed Influence of CO2-wettability on CO2 migration and trapping capacity in deep saline aquifers
title_short Influence of CO2-wettability on CO2 migration and trapping capacity in deep saline aquifers
title_sort influence of co2-wettability on co2 migration and trapping capacity in deep saline aquifers
url http://hdl.handle.net/20.500.11937/10629