Frictional Properties and Seismogenic Potential of Caprock Shales

Fractures and faults are critical elements affecting the geomechanical integrity of CO2 storage sites. In particular, the slip of fractures and faults may affect reservoir integrity and increase potential for breach, may be monitored via the resulting seismicity. This paper presents an experimental...

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Published in:Energies
Main Authors: Bohloli, Bahman, Soldal, Magnus, Smith, Halvard, Skurtveit, Elin, Choi, Jung Chan, Sauvin, Guillaume
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:https://hdl.handle.net/11250/2721200
https://doi.org/10.3390/en13236275
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spelling ftngi:oai:ngi.brage.unit.no:11250/2721200 2023-05-15T18:29:51+02:00 Frictional Properties and Seismogenic Potential of Caprock Shales Bohloli, Bahman Soldal, Magnus Smith, Halvard Skurtveit, Elin Choi, Jung Chan Sauvin, Guillaume 2020 application/pdf https://hdl.handle.net/11250/2721200 https://doi.org/10.3390/en13236275 eng eng Norges forskningsråd: 223122 urn:issn:1996-1073 https://hdl.handle.net/11250/2721200 https://doi.org/10.3390/en13236275 cristin:1859261 13 Energies 23 Peer reviewed Journal article 2020 ftngi https://doi.org/10.3390/en13236275 2022-10-13T05:49:56Z Fractures and faults are critical elements affecting the geomechanical integrity of CO2 storage sites. In particular, the slip of fractures and faults may affect reservoir integrity and increase potential for breach, may be monitored via the resulting seismicity. This paper presents an experimental study on shale samples from Draupne and Rurikfjellet formations from the North Sea and Svalbard, Norway, using a laboratory test procedure simulating the slip of fractures and faults under realistic stress conditions for North Sea CO2 storage sites. The motivation of the study is to investigate whether the slip along the fractures within these shales may cause detectable seismic events, based on a slip stability criterion. Using a direct shear apparatus, frictional properties of the fractures were measured during shearing, as a function of the shear velocity and applied stress normal to the fracture. We calculated the friction coefficient of the fractures during the different stages of the shear tests and analysed its dependency on shear velocity. Information on velocity-dependent friction coefficient and its evolution with increasing slip were then used to assess whether slip was stable (velocity-strengthening) or unstable (velocity-weakening). Results showed that friction coefficient for both Draupne and Rurikfjellet shales increased when the shear velocity was increased from 10 to 50 µm/s, indicating a velocity-strengthening behaviour. Such a behaviour implies that slip on fractures and faults within these formations may be less prone to producing detectable seismicity during a slip event. These results will have implications for the type of techniques to be used for monitoring reservoir and caprock integrity, for instance, for CO2 storage sites publishedVersion Article in Journal/Newspaper Svalbard Norwegian Geotechnical Institute (NGI) Digital Archive Norway Rurikfjellet ENVELOPE(18.217,18.217,77.983,77.983) Svalbard Energies 13 23 6275
institution Open Polar
collection Norwegian Geotechnical Institute (NGI) Digital Archive
op_collection_id ftngi
language English
description Fractures and faults are critical elements affecting the geomechanical integrity of CO2 storage sites. In particular, the slip of fractures and faults may affect reservoir integrity and increase potential for breach, may be monitored via the resulting seismicity. This paper presents an experimental study on shale samples from Draupne and Rurikfjellet formations from the North Sea and Svalbard, Norway, using a laboratory test procedure simulating the slip of fractures and faults under realistic stress conditions for North Sea CO2 storage sites. The motivation of the study is to investigate whether the slip along the fractures within these shales may cause detectable seismic events, based on a slip stability criterion. Using a direct shear apparatus, frictional properties of the fractures were measured during shearing, as a function of the shear velocity and applied stress normal to the fracture. We calculated the friction coefficient of the fractures during the different stages of the shear tests and analysed its dependency on shear velocity. Information on velocity-dependent friction coefficient and its evolution with increasing slip were then used to assess whether slip was stable (velocity-strengthening) or unstable (velocity-weakening). Results showed that friction coefficient for both Draupne and Rurikfjellet shales increased when the shear velocity was increased from 10 to 50 µm/s, indicating a velocity-strengthening behaviour. Such a behaviour implies that slip on fractures and faults within these formations may be less prone to producing detectable seismicity during a slip event. These results will have implications for the type of techniques to be used for monitoring reservoir and caprock integrity, for instance, for CO2 storage sites publishedVersion
format Article in Journal/Newspaper
author Bohloli, Bahman
Soldal, Magnus
Smith, Halvard
Skurtveit, Elin
Choi, Jung Chan
Sauvin, Guillaume
spellingShingle Bohloli, Bahman
Soldal, Magnus
Smith, Halvard
Skurtveit, Elin
Choi, Jung Chan
Sauvin, Guillaume
Frictional Properties and Seismogenic Potential of Caprock Shales
author_facet Bohloli, Bahman
Soldal, Magnus
Smith, Halvard
Skurtveit, Elin
Choi, Jung Chan
Sauvin, Guillaume
author_sort Bohloli, Bahman
title Frictional Properties and Seismogenic Potential of Caprock Shales
title_short Frictional Properties and Seismogenic Potential of Caprock Shales
title_full Frictional Properties and Seismogenic Potential of Caprock Shales
title_fullStr Frictional Properties and Seismogenic Potential of Caprock Shales
title_full_unstemmed Frictional Properties and Seismogenic Potential of Caprock Shales
title_sort frictional properties and seismogenic potential of caprock shales
publishDate 2020
url https://hdl.handle.net/11250/2721200
https://doi.org/10.3390/en13236275
long_lat ENVELOPE(18.217,18.217,77.983,77.983)
geographic Norway
Rurikfjellet
Svalbard
geographic_facet Norway
Rurikfjellet
Svalbard
genre Svalbard
genre_facet Svalbard
op_source 13
Energies
23
op_relation Norges forskningsråd: 223122
urn:issn:1996-1073
https://hdl.handle.net/11250/2721200
https://doi.org/10.3390/en13236275
cristin:1859261
op_doi https://doi.org/10.3390/en13236275
container_title Energies
container_volume 13
container_issue 23
container_start_page 6275
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