Modeling Changes in Hydrate Stability Associated with Arctic Warming and its Impact on Slope ...

If global warming continues at its current rate, widespread methane hydrate dissociation may occur leading to submarine slope instabilities. In this study, numerical models were developed to investigate the impact of different parameters, such as geothermal gradient, slope angle, rate of seafloor te...

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Main Author: Debnath, Khokan
Format: Article in Journal/Newspaper
Language:English
Published: Schulich School of Engineering 2018
Subjects:
Online Access:https://dx.doi.org/10.11575/prism/34984
https://prism.ucalgary.ca/handle/1880/109364
id ftdatacite:10.11575/prism/34984
record_format openpolar
spelling ftdatacite:10.11575/prism/34984 2023-08-27T04:07:51+02:00 Modeling Changes in Hydrate Stability Associated with Arctic Warming and its Impact on Slope ... Debnath, Khokan 2018 https://dx.doi.org/10.11575/prism/34984 https://prism.ucalgary.ca/handle/1880/109364 en eng Schulich School of Engineering University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Gas Hydrate Hydrate stability zone hydrate dissociated zone Hydrate bearing slope analysis permafrost Frozen ground Engineering--Civil CreativeWork article 2018 ftdatacite https://doi.org/10.11575/prism/34984 2023-08-07T14:24:23Z If global warming continues at its current rate, widespread methane hydrate dissociation may occur leading to submarine slope instabilities. In this study, numerical models were developed to investigate the impact of different parameters, such as geothermal gradient, slope angle, rate of seafloor temperature rise, and hydrate saturation on the dissociated volume and potential for slope instabilities. It was found that the geothermal gradient impacts the shape of the hydrate stability zone and the pattern of hydrate dissociation. Slope stability analyses showed that steeper slopes fail earlier and produce lower dissociated hydrate volumes. Higher rate of seafloor temperature produces larger dissociated volume and leads to earlier slope failure. On the other hand, higher hydrate saturation leads to lower hydrate dissociated volume and causes to fail slope comparatively later than a slope with lower hydrate saturation. ... Article in Journal/Newspaper Arctic Global warming Methane hydrate permafrost DataCite Metadata Store (German National Library of Science and Technology) Arctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Gas Hydrate
Hydrate stability zone
hydrate dissociated zone
Hydrate bearing slope analysis
permafrost
Frozen ground
Engineering--Civil
spellingShingle Gas Hydrate
Hydrate stability zone
hydrate dissociated zone
Hydrate bearing slope analysis
permafrost
Frozen ground
Engineering--Civil
Debnath, Khokan
Modeling Changes in Hydrate Stability Associated with Arctic Warming and its Impact on Slope ...
topic_facet Gas Hydrate
Hydrate stability zone
hydrate dissociated zone
Hydrate bearing slope analysis
permafrost
Frozen ground
Engineering--Civil
description If global warming continues at its current rate, widespread methane hydrate dissociation may occur leading to submarine slope instabilities. In this study, numerical models were developed to investigate the impact of different parameters, such as geothermal gradient, slope angle, rate of seafloor temperature rise, and hydrate saturation on the dissociated volume and potential for slope instabilities. It was found that the geothermal gradient impacts the shape of the hydrate stability zone and the pattern of hydrate dissociation. Slope stability analyses showed that steeper slopes fail earlier and produce lower dissociated hydrate volumes. Higher rate of seafloor temperature produces larger dissociated volume and leads to earlier slope failure. On the other hand, higher hydrate saturation leads to lower hydrate dissociated volume and causes to fail slope comparatively later than a slope with lower hydrate saturation. ...
format Article in Journal/Newspaper
author Debnath, Khokan
author_facet Debnath, Khokan
author_sort Debnath, Khokan
title Modeling Changes in Hydrate Stability Associated with Arctic Warming and its Impact on Slope ...
title_short Modeling Changes in Hydrate Stability Associated with Arctic Warming and its Impact on Slope ...
title_full Modeling Changes in Hydrate Stability Associated with Arctic Warming and its Impact on Slope ...
title_fullStr Modeling Changes in Hydrate Stability Associated with Arctic Warming and its Impact on Slope ...
title_full_unstemmed Modeling Changes in Hydrate Stability Associated with Arctic Warming and its Impact on Slope ...
title_sort modeling changes in hydrate stability associated with arctic warming and its impact on slope ...
publisher Schulich School of Engineering
publishDate 2018
url https://dx.doi.org/10.11575/prism/34984
https://prism.ucalgary.ca/handle/1880/109364
geographic Arctic
geographic_facet Arctic
genre Arctic
Global warming
Methane hydrate
permafrost
genre_facet Arctic
Global warming
Methane hydrate
permafrost
op_rights University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission.
op_doi https://doi.org/10.11575/prism/34984
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