Search: onr:"swepub:oai:DiVA.org:lnu-81673" >
Can anaerobic oxida...
Can anaerobic oxidation of methane prevent seafloor gas escape in a warming climate?
-
- Stranne, Christian (author)
- Stockholms universitet,Institutionen för geologiska vetenskaper,Stockholm University, Sweden
-
- O’Regan, Matt (author)
- Stockholm University, Sweden
-
- Jakobsson, Martin (author)
- Stockholms universitet,Institutionen för geologiska vetenskaper,Stockholm University, Sweden
-
show more...
-
- Brüchert, Volker (author)
- Stockholms universitet,Institutionen för geologiska vetenskaper,Stockholm University, Sweden
-
- Ketzer, João Marcelo (author)
- Linnéuniversitetet,Institutionen för biologi och miljö (BOM)
-
- O'Regan, Matthew (author)
- Stockholms universitet,Institutionen för geologiska vetenskaper
-
show less...
-
(creator_code:org_t)
- 2019-09-16
- 2019
- English.
-
In: Solid Earth. - : Copernicus GmbH. - 1869-9510 .- 1869-9529. ; 10:5, s. 1541-1554
- Related links:
-
https://doi.org/10.5...
-
show more...
-
https://se.copernicu...
-
https://urn.kb.se/re...
-
https://doi.org/10.5...
-
https://urn.kb.se/re...
-
show less...
Abstract
Subject headings
Close
- Assessments of future climate-warming-induced seafloor methane (CH4) release rarely include anaerobic ox- idation of methane (AOM) within the sediments. Consider- ing that more than 90 % of the CH4 produced in ocean sed- iments today is consumed by AOM, this may result in sub- stantial overestimations of future seafloor CH4 release. Here, we integrate a fully coupled AOM module with a numerical hydrate model to investigate under what conditions rapid re- lease of CH4 can bypass AOM and result in significant fluxes to the ocean and atmosphere. We run a number of different model simulations for different permeabilities and maximum AOM rates. In all simulations, a future climate warming sce- nario is simulated by imposing a linear seafloor temperature increase of 3 ◦C over the first 100 years. The results presented in this study should be seen as a first step towards under- standing AOM dynamics in relation to climate change and hydrate dissociation. Although the model is somewhat poorly constrained, our results indicate that vertical CH4 migration through hydraulic fractures can result in low AOM efficien- cies. Fracture flow is the predicted mode of methane trans- port under warming-induced dissociation of hydrates on up- per continental slopes. Therefore, in a future climate warm- ing scenario, AOM might not significantly reduce methane release from marine sediments.
Subject headings
- NATURVETENSKAP -- Geovetenskap och miljövetenskap (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences (hsv//eng)
Keyword
- Natural Science
- Naturvetenskap
Publication and Content Type
- ref (subject category)
- art (subject category)
Find in a library
To the university's database