Sources of methane to an Arctic lake in Alaska: An isotopic investigation
Sources of dissolved methane (CH 4 ) at Toolik Lake, Alaska, include both diffusion from lake sediments and groundwater entering the lake from its perimeter. Here we use hydrogen and oxygen isotopes in water (H 2 O), carbon and hydrogen isotopes in CH 4 , and carbon isotopes in dissolved inorganic c...
Published in: | Journal of Geophysical Research: Biogeosciences |
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Online Access: | http://www.osti.gov/servlets/purl/1542702 https://www.osti.gov/biblio/1542702 https://doi.org/10.1002/2016JG003491 |
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ftosti:oai:osti.gov:1542702 2023-07-30T04:01:49+02:00 Sources of methane to an Arctic lake in Alaska: An isotopic investigation Lecher, Alanna L. Chuang, Pei -Chuan Singleton, Michael Paytan, Adina 2021-08-02 application/pdf http://www.osti.gov/servlets/purl/1542702 https://www.osti.gov/biblio/1542702 https://doi.org/10.1002/2016JG003491 unknown http://www.osti.gov/servlets/purl/1542702 https://www.osti.gov/biblio/1542702 https://doi.org/10.1002/2016JG003491 doi:10.1002/2016JG003491 58 GEOSCIENCES 54 ENVIRONMENTAL SCIENCES 2021 ftosti https://doi.org/10.1002/2016JG003491 2023-07-11T09:35:03Z Sources of dissolved methane (CH 4 ) at Toolik Lake, Alaska, include both diffusion from lake sediments and groundwater entering the lake from its perimeter. Here we use hydrogen and oxygen isotopes in water (H 2 O), carbon and hydrogen isotopes in CH 4 , and carbon isotopes in dissolved inorganic carbon (DIC) to calculate the relative importance of lake sediment and groundwater discharge as sources of dissolved CH 4 to Toolik Lake. We also resolve the relative importance of the source contribution spatially within the lake and determine the processes controlling CH 4 concentrations in groundwater surrounding the lake. Our findings, from a mixing model based on isotopes in CH 4 , suggest that groundwater is a more important source of CH 4 at the perimeter of the lake where the water-to-air flux is high. In addition, we find on the local scale that high groundwater methane concentrations may be better linked to areas around the lake where rain is the dominant source of water to the active layer, indicating that changes in precipitation and active layer thaw depth will impact methane concentrations in the active layer and, ultimately, the groundwater associated flux to Toolik Lake. Other/Unknown Material Arctic Alaska SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Arctic Arctic Lake ENVELOPE(-130.826,-130.826,57.231,57.231) Journal of Geophysical Research: Biogeosciences 122 4 753 766 |
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Open Polar |
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SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) |
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ftosti |
language |
unknown |
topic |
58 GEOSCIENCES 54 ENVIRONMENTAL SCIENCES |
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58 GEOSCIENCES 54 ENVIRONMENTAL SCIENCES Lecher, Alanna L. Chuang, Pei -Chuan Singleton, Michael Paytan, Adina Sources of methane to an Arctic lake in Alaska: An isotopic investigation |
topic_facet |
58 GEOSCIENCES 54 ENVIRONMENTAL SCIENCES |
description |
Sources of dissolved methane (CH 4 ) at Toolik Lake, Alaska, include both diffusion from lake sediments and groundwater entering the lake from its perimeter. Here we use hydrogen and oxygen isotopes in water (H 2 O), carbon and hydrogen isotopes in CH 4 , and carbon isotopes in dissolved inorganic carbon (DIC) to calculate the relative importance of lake sediment and groundwater discharge as sources of dissolved CH 4 to Toolik Lake. We also resolve the relative importance of the source contribution spatially within the lake and determine the processes controlling CH 4 concentrations in groundwater surrounding the lake. Our findings, from a mixing model based on isotopes in CH 4 , suggest that groundwater is a more important source of CH 4 at the perimeter of the lake where the water-to-air flux is high. In addition, we find on the local scale that high groundwater methane concentrations may be better linked to areas around the lake where rain is the dominant source of water to the active layer, indicating that changes in precipitation and active layer thaw depth will impact methane concentrations in the active layer and, ultimately, the groundwater associated flux to Toolik Lake. |
author |
Lecher, Alanna L. Chuang, Pei -Chuan Singleton, Michael Paytan, Adina |
author_facet |
Lecher, Alanna L. Chuang, Pei -Chuan Singleton, Michael Paytan, Adina |
author_sort |
Lecher, Alanna L. |
title |
Sources of methane to an Arctic lake in Alaska: An isotopic investigation |
title_short |
Sources of methane to an Arctic lake in Alaska: An isotopic investigation |
title_full |
Sources of methane to an Arctic lake in Alaska: An isotopic investigation |
title_fullStr |
Sources of methane to an Arctic lake in Alaska: An isotopic investigation |
title_full_unstemmed |
Sources of methane to an Arctic lake in Alaska: An isotopic investigation |
title_sort |
sources of methane to an arctic lake in alaska: an isotopic investigation |
publishDate |
2021 |
url |
http://www.osti.gov/servlets/purl/1542702 https://www.osti.gov/biblio/1542702 https://doi.org/10.1002/2016JG003491 |
long_lat |
ENVELOPE(-130.826,-130.826,57.231,57.231) |
geographic |
Arctic Arctic Lake |
geographic_facet |
Arctic Arctic Lake |
genre |
Arctic Alaska |
genre_facet |
Arctic Alaska |
op_relation |
http://www.osti.gov/servlets/purl/1542702 https://www.osti.gov/biblio/1542702 https://doi.org/10.1002/2016JG003491 doi:10.1002/2016JG003491 |
op_doi |
https://doi.org/10.1002/2016JG003491 |
container_title |
Journal of Geophysical Research: Biogeosciences |
container_volume |
122 |
container_issue |
4 |
container_start_page |
753 |
op_container_end_page |
766 |
_version_ |
1772812565121859584 |