Characterization of atmospheric methane release in the outer Mackenzie River Delta from biogenic and thermogenic sources
The Mackenzie River delta is the second largest Arctic river delta in the world. Thin and destabilizing permafrost coupled with vast natural gas reserves at depth, high organic-content soils, and a high proportion of wetlands create a unique ecosystem conducive to high rates of methane (CH 4 ) emiss...
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ftcopernicus:oai:publications.copernicus.org:egusphere104809 2024-01-14T10:04:53+01:00 Characterization of atmospheric methane release in the outer Mackenzie River Delta from biogenic and thermogenic sources Wesley, Daniel Dallimore, Scott MacLeod, Roger Sachs, Torsten Risk, David 2023-12-13 application/pdf https://doi.org/10.5194/egusphere-2022-549 https://egusphere.copernicus.org/preprints/2022/egusphere-2022-549/ eng eng doi:10.5194/egusphere-2022-549 https://egusphere.copernicus.org/preprints/2022/egusphere-2022-549/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2022-549 2023-12-18T17:24:22Z The Mackenzie River delta is the second largest Arctic river delta in the world. Thin and destabilizing permafrost coupled with vast natural gas reserves at depth, high organic-content soils, and a high proportion of wetlands create a unique ecosystem conducive to high rates of methane (CH 4 ) emission from biogenic and thermogenic sources. Hotspots are known to have a significant contribution to summertime CH 4 emissions in the region. Still, little research has been done to determine how often geologic or biogenic CH 4 contributes to hotspots in the Mackenzie River delta. In the present study, stable carbon isotope analysis was used to identify the source of CH 4 at several aquatic and terrestrial sites thought to be hotspots of CH 4 flux to the atmosphere. Walking transects and point samples of atmospheric CH 4 and CO 2 concentrations were measured. Source stable carbon isotope ( δ 13 C-CH 4 ) signatures were derived from keeling plots of point samples and ranged from −42 ‰ to −88 ‰ δ 13 C-CH 4 , identifying both biogenic and thermogenic sources. A CH 4 source was determined for eight hotspots, two of which were thermogenic in origin ( −42.5 ‰ , −44.7 ‰ ), four of which were biogenic in origin ( −71.9 ‰ to −88.3 ‰ ), and two of which may have been produced by the oxidation of biogenic CH 4 ( −53.0 ‰ , −63.6 ‰ ), as evidenced by δ 13 C-CH 4 signatures. This indicates that the largest hotspots of CH 4 production in the Mackenzie River delta are caused by a variety of sources. Text Arctic Mackenzie river permafrost Copernicus Publications: E-Journals Arctic Mackenzie River |
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Copernicus Publications: E-Journals |
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English |
description |
The Mackenzie River delta is the second largest Arctic river delta in the world. Thin and destabilizing permafrost coupled with vast natural gas reserves at depth, high organic-content soils, and a high proportion of wetlands create a unique ecosystem conducive to high rates of methane (CH 4 ) emission from biogenic and thermogenic sources. Hotspots are known to have a significant contribution to summertime CH 4 emissions in the region. Still, little research has been done to determine how often geologic or biogenic CH 4 contributes to hotspots in the Mackenzie River delta. In the present study, stable carbon isotope analysis was used to identify the source of CH 4 at several aquatic and terrestrial sites thought to be hotspots of CH 4 flux to the atmosphere. Walking transects and point samples of atmospheric CH 4 and CO 2 concentrations were measured. Source stable carbon isotope ( δ 13 C-CH 4 ) signatures were derived from keeling plots of point samples and ranged from −42 ‰ to −88 ‰ δ 13 C-CH 4 , identifying both biogenic and thermogenic sources. A CH 4 source was determined for eight hotspots, two of which were thermogenic in origin ( −42.5 ‰ , −44.7 ‰ ), four of which were biogenic in origin ( −71.9 ‰ to −88.3 ‰ ), and two of which may have been produced by the oxidation of biogenic CH 4 ( −53.0 ‰ , −63.6 ‰ ), as evidenced by δ 13 C-CH 4 signatures. This indicates that the largest hotspots of CH 4 production in the Mackenzie River delta are caused by a variety of sources. |
format |
Text |
author |
Wesley, Daniel Dallimore, Scott MacLeod, Roger Sachs, Torsten Risk, David |
spellingShingle |
Wesley, Daniel Dallimore, Scott MacLeod, Roger Sachs, Torsten Risk, David Characterization of atmospheric methane release in the outer Mackenzie River Delta from biogenic and thermogenic sources |
author_facet |
Wesley, Daniel Dallimore, Scott MacLeod, Roger Sachs, Torsten Risk, David |
author_sort |
Wesley, Daniel |
title |
Characterization of atmospheric methane release in the outer Mackenzie River Delta from biogenic and thermogenic sources |
title_short |
Characterization of atmospheric methane release in the outer Mackenzie River Delta from biogenic and thermogenic sources |
title_full |
Characterization of atmospheric methane release in the outer Mackenzie River Delta from biogenic and thermogenic sources |
title_fullStr |
Characterization of atmospheric methane release in the outer Mackenzie River Delta from biogenic and thermogenic sources |
title_full_unstemmed |
Characterization of atmospheric methane release in the outer Mackenzie River Delta from biogenic and thermogenic sources |
title_sort |
characterization of atmospheric methane release in the outer mackenzie river delta from biogenic and thermogenic sources |
publishDate |
2023 |
url |
https://doi.org/10.5194/egusphere-2022-549 https://egusphere.copernicus.org/preprints/2022/egusphere-2022-549/ |
geographic |
Arctic Mackenzie River |
geographic_facet |
Arctic Mackenzie River |
genre |
Arctic Mackenzie river permafrost |
genre_facet |
Arctic Mackenzie river permafrost |
op_source |
eISSN: |
op_relation |
doi:10.5194/egusphere-2022-549 https://egusphere.copernicus.org/preprints/2022/egusphere-2022-549/ |
op_doi |
https://doi.org/10.5194/egusphere-2022-549 |
_version_ |
1788059319160274944 |