Comment on "Excess pore pressure resulting from methane hydrate dissociation in marine sediments: A theoretical approach" by Wenyue Xu and Leonid N. Germanovich - art. no. B02103
While it is well accepted that gas hydrate dissociation at the base of the Gas Hydrate Stability Zone (GHSZ) can generate high excess pore pressure and leads to sediment deformation, the consequence in terms of pore pressure of the dissolution of the gas hydrate at the top of the Gas Hydrate Occurre...
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ftarchimer:oai:archimer.ifremer.fr:2318 2023-05-15T17:11:56+02:00 Comment on "Excess pore pressure resulting from methane hydrate dissociation in marine sediments: A theoretical approach" by Wenyue Xu and Leonid N. Germanovich - art. no. B02103 Sultan, Nabil 2007-02 application/pdf https://archimer.ifremer.fr/doc/2007/publication-2318.pdf https://doi.org/10.1029/2006JB004527 https://archimer.ifremer.fr/doc/00000/2318/ eng eng American Geophysical Union https://archimer.ifremer.fr/doc/2007/publication-2318.pdf doi:10.1029/2006JB004527 https://archimer.ifremer.fr/doc/00000/2318/ 2006 AGU info:eu-repo/semantics/openAccess restricted use Journal of Geophysical Research (0148-0227) (American Geophysical Union), 2007-02 , Vol. 112 , N. B2 , P. NIL_78-NIL_84 pore pressure hydrate dissolution Dissociation text Publication info:eu-repo/semantics/article 2007 ftarchimer https://doi.org/10.1029/2006JB004527 2021-09-23T20:14:37Z While it is well accepted that gas hydrate dissociation at the base of the Gas Hydrate Stability Zone (GHSZ) can generate high excess pore pressure and leads to sediment deformation, the consequence in terms of pore pressure of the dissolution of the gas hydrate at the top of the Gas Hydrate Occurrence Zone (GHOZ) remains neglected. The purpose of this comment on Xu and Germanovich [2006] article is to demonstrate that gas hydrate dissolution in the GHSZ may generate excess pore pressure and to point out the risk related to hydrate dissolution at the top of the GHOZ. Article in Journal/Newspaper Methane hydrate Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Journal of Geophysical Research 112 B2 |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
topic |
pore pressure hydrate dissolution Dissociation |
spellingShingle |
pore pressure hydrate dissolution Dissociation Sultan, Nabil Comment on "Excess pore pressure resulting from methane hydrate dissociation in marine sediments: A theoretical approach" by Wenyue Xu and Leonid N. Germanovich - art. no. B02103 |
topic_facet |
pore pressure hydrate dissolution Dissociation |
description |
While it is well accepted that gas hydrate dissociation at the base of the Gas Hydrate Stability Zone (GHSZ) can generate high excess pore pressure and leads to sediment deformation, the consequence in terms of pore pressure of the dissolution of the gas hydrate at the top of the Gas Hydrate Occurrence Zone (GHOZ) remains neglected. The purpose of this comment on Xu and Germanovich [2006] article is to demonstrate that gas hydrate dissolution in the GHSZ may generate excess pore pressure and to point out the risk related to hydrate dissolution at the top of the GHOZ. |
format |
Article in Journal/Newspaper |
author |
Sultan, Nabil |
author_facet |
Sultan, Nabil |
author_sort |
Sultan, Nabil |
title |
Comment on "Excess pore pressure resulting from methane hydrate dissociation in marine sediments: A theoretical approach" by Wenyue Xu and Leonid N. Germanovich - art. no. B02103 |
title_short |
Comment on "Excess pore pressure resulting from methane hydrate dissociation in marine sediments: A theoretical approach" by Wenyue Xu and Leonid N. Germanovich - art. no. B02103 |
title_full |
Comment on "Excess pore pressure resulting from methane hydrate dissociation in marine sediments: A theoretical approach" by Wenyue Xu and Leonid N. Germanovich - art. no. B02103 |
title_fullStr |
Comment on "Excess pore pressure resulting from methane hydrate dissociation in marine sediments: A theoretical approach" by Wenyue Xu and Leonid N. Germanovich - art. no. B02103 |
title_full_unstemmed |
Comment on "Excess pore pressure resulting from methane hydrate dissociation in marine sediments: A theoretical approach" by Wenyue Xu and Leonid N. Germanovich - art. no. B02103 |
title_sort |
comment on "excess pore pressure resulting from methane hydrate dissociation in marine sediments: a theoretical approach" by wenyue xu and leonid n. germanovich - art. no. b02103 |
publisher |
American Geophysical Union |
publishDate |
2007 |
url |
https://archimer.ifremer.fr/doc/2007/publication-2318.pdf https://doi.org/10.1029/2006JB004527 https://archimer.ifremer.fr/doc/00000/2318/ |
genre |
Methane hydrate |
genre_facet |
Methane hydrate |
op_source |
Journal of Geophysical Research (0148-0227) (American Geophysical Union), 2007-02 , Vol. 112 , N. B2 , P. NIL_78-NIL_84 |
op_relation |
https://archimer.ifremer.fr/doc/2007/publication-2318.pdf doi:10.1029/2006JB004527 https://archimer.ifremer.fr/doc/00000/2318/ |
op_rights |
2006 AGU info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1029/2006JB004527 |
container_title |
Journal of Geophysical Research |
container_volume |
112 |
container_issue |
B2 |
_version_ |
1766068682311598080 |