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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Online Access: | https://hdl.handle.net/11250/2721200 https://doi.org/10.3390/en13236275 |
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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 |
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Open Polar |
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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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1766213257940434944 |