Impact of Gas Saturation and Gas Column Height at the Base of the Gas Hydrate Stability Zone on Fracturing and Seepage at Vestnesa Ridge, West-Svalbard Margin

The Vestnesa Ridge, located off the west Svalbard margin, is a >60 km long ridge consisting of fine-grained sediments that host a deep-marine gas hydrate and associated seepage system. Geological and geophysical observations indicate the predominance of vertical fluid expulsion through fractures...

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Published in:Energies
Main Authors: Ramachandran, Hariharan, Plaza-Faverola, Andreia, Daigle, Hugh
Format: Article in Journal/Newspaper
Language:English
Published: MDPI 2022
Subjects:
Online Access:https://hdl.handle.net/10037/24938
https://doi.org/10.3390/en15093156
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spelling ftunivtroemsoe:oai:munin.uit.no:10037/24938 2023-05-15T18:29:45+02:00 Impact of Gas Saturation and Gas Column Height at the Base of the Gas Hydrate Stability Zone on Fracturing and Seepage at Vestnesa Ridge, West-Svalbard Margin Ramachandran, Hariharan Plaza-Faverola, Andreia Daigle, Hugh 2022-04-26 https://hdl.handle.net/10037/24938 https://doi.org/10.3390/en15093156 eng eng MDPI Energies Ramachandran H, Plaza-Faverola A, Daigle H. Impact of Gas Saturation and Gas Column Height at the Base of the Gas Hydrate Stability Zone on Fracturing and Seepage at Vestnesa Ridge, West-Svalbard Margin. Energies. 2022;15(9):3156 FRIDAID 2019677 doi:10.3390/en15093156 1996-1073 https://hdl.handle.net/10037/24938 openAccess Copyright 2022 The Author(s) Journal article Tidsskriftartikkel Peer reviewed publishedVersion 2022 ftunivtroemsoe https://doi.org/10.3390/en15093156 2022-05-04T22:58:43Z The Vestnesa Ridge, located off the west Svalbard margin, is a >60 km long ridge consisting of fine-grained sediments that host a deep-marine gas hydrate and associated seepage system. Geological and geophysical observations indicate the predominance of vertical fluid expulsion through fractures with pockmarks expressed on the seafloor along the entire ridge. However, despite the apparent evidence for an extended free gas zone (FGZ) below the base of the gas hydrate stability zone (BGHSZ), present-day seafloor seepage has been confirmed only on the eastern half of the sedimentary ridge. In this study, we combine the relationships between aqueous phase pressure, capillary pressure, sediment clay fraction, porosity, and total stress to simulate how much gas is required to open preexisting fractures from the BGHSZ towards the seafloor. Data from four specific sites with different lithology and pressure regime along the ridge are used to constrain the simulations. Results demonstrate that fracturing is favored from the FGZ (with gas saturations < 0.1 and gas column heights < 15 m) towards the seafloor. Neglecting the capillary pressure overpredicts the size of the gas column by up to 10 times, leading to erroneous maximum gas vent volume predictions and associated ocean biosphere consequences. Further parametric analyses indicate that variations in the regional stress regime have the potential to modify the fracture criterion, thus driving the differences in venting across the ridge. Our results are in line with independent geophysical observations and petroleum system modeling in the study area, adding confidence to the proposed approach and highlighting the importance of the capillary pressure influence on gas pressure Article in Journal/Newspaper Svalbard Svalbard margin University of Tromsø: Munin Open Research Archive Long Ridge ENVELOPE(73.583,73.583,-53.100,-53.100) Svalbard Energies 15 9 3156
institution Open Polar
collection University of Tromsø: Munin Open Research Archive
op_collection_id ftunivtroemsoe
language English
description The Vestnesa Ridge, located off the west Svalbard margin, is a >60 km long ridge consisting of fine-grained sediments that host a deep-marine gas hydrate and associated seepage system. Geological and geophysical observations indicate the predominance of vertical fluid expulsion through fractures with pockmarks expressed on the seafloor along the entire ridge. However, despite the apparent evidence for an extended free gas zone (FGZ) below the base of the gas hydrate stability zone (BGHSZ), present-day seafloor seepage has been confirmed only on the eastern half of the sedimentary ridge. In this study, we combine the relationships between aqueous phase pressure, capillary pressure, sediment clay fraction, porosity, and total stress to simulate how much gas is required to open preexisting fractures from the BGHSZ towards the seafloor. Data from four specific sites with different lithology and pressure regime along the ridge are used to constrain the simulations. Results demonstrate that fracturing is favored from the FGZ (with gas saturations < 0.1 and gas column heights < 15 m) towards the seafloor. Neglecting the capillary pressure overpredicts the size of the gas column by up to 10 times, leading to erroneous maximum gas vent volume predictions and associated ocean biosphere consequences. Further parametric analyses indicate that variations in the regional stress regime have the potential to modify the fracture criterion, thus driving the differences in venting across the ridge. Our results are in line with independent geophysical observations and petroleum system modeling in the study area, adding confidence to the proposed approach and highlighting the importance of the capillary pressure influence on gas pressure
format Article in Journal/Newspaper
author Ramachandran, Hariharan
Plaza-Faverola, Andreia
Daigle, Hugh
spellingShingle Ramachandran, Hariharan
Plaza-Faverola, Andreia
Daigle, Hugh
Impact of Gas Saturation and Gas Column Height at the Base of the Gas Hydrate Stability Zone on Fracturing and Seepage at Vestnesa Ridge, West-Svalbard Margin
author_facet Ramachandran, Hariharan
Plaza-Faverola, Andreia
Daigle, Hugh
author_sort Ramachandran, Hariharan
title Impact of Gas Saturation and Gas Column Height at the Base of the Gas Hydrate Stability Zone on Fracturing and Seepage at Vestnesa Ridge, West-Svalbard Margin
title_short Impact of Gas Saturation and Gas Column Height at the Base of the Gas Hydrate Stability Zone on Fracturing and Seepage at Vestnesa Ridge, West-Svalbard Margin
title_full Impact of Gas Saturation and Gas Column Height at the Base of the Gas Hydrate Stability Zone on Fracturing and Seepage at Vestnesa Ridge, West-Svalbard Margin
title_fullStr Impact of Gas Saturation and Gas Column Height at the Base of the Gas Hydrate Stability Zone on Fracturing and Seepage at Vestnesa Ridge, West-Svalbard Margin
title_full_unstemmed Impact of Gas Saturation and Gas Column Height at the Base of the Gas Hydrate Stability Zone on Fracturing and Seepage at Vestnesa Ridge, West-Svalbard Margin
title_sort impact of gas saturation and gas column height at the base of the gas hydrate stability zone on fracturing and seepage at vestnesa ridge, west-svalbard margin
publisher MDPI
publishDate 2022
url https://hdl.handle.net/10037/24938
https://doi.org/10.3390/en15093156
long_lat ENVELOPE(73.583,73.583,-53.100,-53.100)
geographic Long Ridge
Svalbard
geographic_facet Long Ridge
Svalbard
genre Svalbard
Svalbard margin
genre_facet Svalbard
Svalbard margin
op_relation Energies
Ramachandran H, Plaza-Faverola A, Daigle H. Impact of Gas Saturation and Gas Column Height at the Base of the Gas Hydrate Stability Zone on Fracturing and Seepage at Vestnesa Ridge, West-Svalbard Margin. Energies. 2022;15(9):3156
FRIDAID 2019677
doi:10.3390/en15093156
1996-1073
https://hdl.handle.net/10037/24938
op_rights openAccess
Copyright 2022 The Author(s)
op_doi https://doi.org/10.3390/en15093156
container_title Energies
container_volume 15
container_issue 9
container_start_page 3156
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