Supercritical CO2 intrusion into caprocks: experimental observations and numerical simulations
Geologic storage of carbon dioxide (CO2), mainly in deep saline aquifers, has emerged as a key solution to reach the Paris Agreement goal of limiting the global temperature increase below 2ºC and effectively mitigate climate change. The injected CO2 is less dense at the storage condictions than the resident brine and tends to flow upward by buoyancy. Therefore, to achieve the primary objective of permanently storing CO2 underground during geological time scales, the host reservoir should be overlain by a low-permeability and high-entry pressure caprock that prevents CO2 escaping from the storage formation. Meanwhile, the caprock sealing capacity is of particular significance and yet to be assessed in more detail. In this presentation, we aim at shedding light on the flow processes governing potential CO2 leakage through shaly caprocks by combining experimental observations and numerical simulations. We present breakthrough experiments on Opalinus Clay, which is a representative caprock for CO2 storage. These experiments reproduce supercritical CO2 intrusion and flow through the caprock sample under representative reservoir conditions. Next, we address numerical simulation of the breakthrough experiments using a twophase flow model in deformable porous media to provide a mechanistic interpretation of experimental observations. Overall, we conclude that CO2 leakage through the caprock is dominated by molecular diffusion rather than by rapid bulk volumetric advection.
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Language: | English |
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2021-01-21
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Subjects: | Geologic carbon storage, Caprock, CO2, |
Online Access: | http://hdl.handle.net/10261/246835 |
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dig-idaea-es-10261-2468352021-07-30T06:26:59Z Supercritical CO2 intrusion into caprocks: experimental observations and numerical simulations Rahimzadeh Kivi, I. Vilarrasa, Víctor Makhnenko, R. Vilarrasa, Víctor [0000-0003-1169-4469] Geologic carbon storage Caprock CO2 Geologic storage of carbon dioxide (CO2), mainly in deep saline aquifers, has emerged as a key solution to reach the Paris Agreement goal of limiting the global temperature increase below 2ºC and effectively mitigate climate change. The injected CO2 is less dense at the storage condictions than the resident brine and tends to flow upward by buoyancy. Therefore, to achieve the primary objective of permanently storing CO2 underground during geological time scales, the host reservoir should be overlain by a low-permeability and high-entry pressure caprock that prevents CO2 escaping from the storage formation. Meanwhile, the caprock sealing capacity is of particular significance and yet to be assessed in more detail. In this presentation, we aim at shedding light on the flow processes governing potential CO2 leakage through shaly caprocks by combining experimental observations and numerical simulations. We present breakthrough experiments on Opalinus Clay, which is a representative caprock for CO2 storage. These experiments reproduce supercritical CO2 intrusion and flow through the caprock sample under representative reservoir conditions. Next, we address numerical simulation of the breakthrough experiments using a twophase flow model in deformable porous media to provide a mechanistic interpretation of experimental observations. Overall, we conclude that CO2 leakage through the caprock is dominated by molecular diffusion rather than by rapid bulk volumetric advection. Peer reviewed 2021-07-29T10:57:50Z 2021-07-29T10:57:50Z 2021-01-21 material didáctico UPC-CSIC Hydrogeology Group Seminar, Technical University of Catalonia (UPC), Barcelona, Spain http://hdl.handle.net/10261/246835 en Sí open |
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Geologic carbon storage Caprock CO2 Geologic carbon storage Caprock CO2 |
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Geologic carbon storage Caprock CO2 Geologic carbon storage Caprock CO2 Rahimzadeh Kivi, I. Vilarrasa, Víctor Makhnenko, R. Supercritical CO2 intrusion into caprocks: experimental observations and numerical simulations |
description |
Geologic storage of carbon dioxide (CO2), mainly in deep saline aquifers, has emerged as a key
solution to reach the Paris Agreement goal of limiting the global temperature increase below 2ºC
and effectively mitigate climate change. The injected CO2 is less dense at the storage condictions
than the resident brine and tends to flow upward by buoyancy. Therefore, to achieve the primary
objective of permanently storing CO2 underground during geological time scales, the host reservoir
should be overlain by a low-permeability and high-entry pressure caprock that prevents CO2
escaping from the storage formation. Meanwhile, the caprock sealing capacity is of particular
significance and yet to be assessed in more detail. In this presentation, we aim at shedding light on
the flow processes governing potential CO2 leakage through shaly caprocks by combining
experimental observations and numerical simulations. We present breakthrough experiments on
Opalinus Clay, which is a representative caprock for CO2 storage. These experiments reproduce
supercritical CO2 intrusion and flow through the caprock sample under representative reservoir
conditions. Next, we address numerical simulation of the breakthrough experiments using a twophase
flow model in deformable porous media to provide a mechanistic interpretation of
experimental observations. Overall, we conclude that CO2 leakage through the caprock is
dominated by molecular diffusion rather than by rapid bulk volumetric advection. |
author2 |
Vilarrasa, Víctor [0000-0003-1169-4469] |
author_facet |
Vilarrasa, Víctor [0000-0003-1169-4469] Rahimzadeh Kivi, I. Vilarrasa, Víctor Makhnenko, R. |
format |
material didáctico |
topic_facet |
Geologic carbon storage Caprock CO2 |
author |
Rahimzadeh Kivi, I. Vilarrasa, Víctor Makhnenko, R. |
author_sort |
Rahimzadeh Kivi, I. |
title |
Supercritical CO2 intrusion into caprocks: experimental observations and numerical simulations |
title_short |
Supercritical CO2 intrusion into caprocks: experimental observations and numerical simulations |
title_full |
Supercritical CO2 intrusion into caprocks: experimental observations and numerical simulations |
title_fullStr |
Supercritical CO2 intrusion into caprocks: experimental observations and numerical simulations |
title_full_unstemmed |
Supercritical CO2 intrusion into caprocks: experimental observations and numerical simulations |
title_sort |
supercritical co2 intrusion into caprocks: experimental observations and numerical simulations |
publishDate |
2021-01-21 |
url |
http://hdl.handle.net/10261/246835 |
work_keys_str_mv |
AT rahimzadehkivii supercriticalco2intrusionintocaprocksexperimentalobservationsandnumericalsimulations AT vilarrasavictor supercriticalco2intrusionintocaprocksexperimentalobservationsandnumericalsimulations AT makhnenkor supercriticalco2intrusionintocaprocksexperimentalobservationsandnumericalsimulations |
_version_ |
1777669539006251008 |