Submarine Slope Failure Primed and Triggered by Bottom Water Warming in Oceanic Hydrate-Bearing Deposits

Many submarine slope failures in hydrate-bearing sedimentary deposits might be directly triggered, or at least primed, by gas hydrate dissociation. It has been reported that during the past 55 years (1955–2010) the 0–2000 m layer of oceans worldwide has been warmed by 0.09 °C because of global warmi...

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Main Authors: Tae-Hyuk Kwon, Gye-Chun Cho
Format: Article in Journal/Newspaper
Language:unknown
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Online Access:https://www.mdpi.com/1996-1073/5/8/2849/pdf
https://www.mdpi.com/1996-1073/5/8/2849/
id ftrepec:oai:RePEc:gam:jeners:v:5:y:2012:i:8:p:2849-2873:d:19277
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spelling ftrepec:oai:RePEc:gam:jeners:v:5:y:2012:i:8:p:2849-2873:d:19277 2024-04-14T08:14:53+00:00 Submarine Slope Failure Primed and Triggered by Bottom Water Warming in Oceanic Hydrate-Bearing Deposits Tae-Hyuk Kwon Gye-Chun Cho https://www.mdpi.com/1996-1073/5/8/2849/pdf https://www.mdpi.com/1996-1073/5/8/2849/ unknown https://www.mdpi.com/1996-1073/5/8/2849/pdf https://www.mdpi.com/1996-1073/5/8/2849/ article ftrepec 2024-03-19T10:31:24Z Many submarine slope failures in hydrate-bearing sedimentary deposits might be directly triggered, or at least primed, by gas hydrate dissociation. It has been reported that during the past 55 years (1955–2010) the 0–2000 m layer of oceans worldwide has been warmed by 0.09 °C because of global warming. This raises the following scientific concern: if warming of the bottom water of deep oceans continues, it would dissociate natural gas hydrates and could eventually trigger massive slope failures. The present study explored the submarine slope instability of oceanic gas hydrate-bearing deposits subjected to bottom water warming. One-dimensional coupled thermal-hydraulic-mechanical (T-H-M) finite difference analyses were performed to capture the underlying physical processes initiated by bottom water warming, which includes thermal conduction through sediments, thermal dissociation of gas hydrates, excess pore pressure generation, pressure diffusion, and hydrate dissociation against depressurization. The temperature rise at the seafloor due to bottom water warming is found to create an excess pore pressure that is sufficiently large to reduce the stability of a slope in some cases. Parametric study results suggest that a slope becomes more susceptible to failure with increases in thermal diffusivity and hydrate saturation and decreases in pressure diffusivity, gas saturation, and water depth. Bottom water warming can be further explored to gain a better understanding of the past methane hydrate destabilization events on Earth, assuming that more reliable geological data is available. submarine slope failure; underwater landslide; bottom water warming; global warming; gas hydrate; dissociation Article in Journal/Newspaper Methane hydrate RePEc (Research Papers in Economics)
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description Many submarine slope failures in hydrate-bearing sedimentary deposits might be directly triggered, or at least primed, by gas hydrate dissociation. It has been reported that during the past 55 years (1955–2010) the 0–2000 m layer of oceans worldwide has been warmed by 0.09 °C because of global warming. This raises the following scientific concern: if warming of the bottom water of deep oceans continues, it would dissociate natural gas hydrates and could eventually trigger massive slope failures. The present study explored the submarine slope instability of oceanic gas hydrate-bearing deposits subjected to bottom water warming. One-dimensional coupled thermal-hydraulic-mechanical (T-H-M) finite difference analyses were performed to capture the underlying physical processes initiated by bottom water warming, which includes thermal conduction through sediments, thermal dissociation of gas hydrates, excess pore pressure generation, pressure diffusion, and hydrate dissociation against depressurization. The temperature rise at the seafloor due to bottom water warming is found to create an excess pore pressure that is sufficiently large to reduce the stability of a slope in some cases. Parametric study results suggest that a slope becomes more susceptible to failure with increases in thermal diffusivity and hydrate saturation and decreases in pressure diffusivity, gas saturation, and water depth. Bottom water warming can be further explored to gain a better understanding of the past methane hydrate destabilization events on Earth, assuming that more reliable geological data is available. submarine slope failure; underwater landslide; bottom water warming; global warming; gas hydrate; dissociation
format Article in Journal/Newspaper
author Tae-Hyuk Kwon
Gye-Chun Cho
spellingShingle Tae-Hyuk Kwon
Gye-Chun Cho
Submarine Slope Failure Primed and Triggered by Bottom Water Warming in Oceanic Hydrate-Bearing Deposits
author_facet Tae-Hyuk Kwon
Gye-Chun Cho
author_sort Tae-Hyuk Kwon
title Submarine Slope Failure Primed and Triggered by Bottom Water Warming in Oceanic Hydrate-Bearing Deposits
title_short Submarine Slope Failure Primed and Triggered by Bottom Water Warming in Oceanic Hydrate-Bearing Deposits
title_full Submarine Slope Failure Primed and Triggered by Bottom Water Warming in Oceanic Hydrate-Bearing Deposits
title_fullStr Submarine Slope Failure Primed and Triggered by Bottom Water Warming in Oceanic Hydrate-Bearing Deposits
title_full_unstemmed Submarine Slope Failure Primed and Triggered by Bottom Water Warming in Oceanic Hydrate-Bearing Deposits
title_sort submarine slope failure primed and triggered by bottom water warming in oceanic hydrate-bearing deposits
url https://www.mdpi.com/1996-1073/5/8/2849/pdf
https://www.mdpi.com/1996-1073/5/8/2849/
genre Methane hydrate
genre_facet Methane hydrate
op_relation https://www.mdpi.com/1996-1073/5/8/2849/pdf
https://www.mdpi.com/1996-1073/5/8/2849/
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