Mobile open dynamic chamber measurement of methane macroseeps in lakes
Methane (CH 4 ) seepage; i.e., steady or episodic flow of gaseous hydrocarbons from subsurface reservoirs, has been identified as a significant source of atmospheric CH 4 . However, radiocarbon data from polar ice cores recently brought into question the magnitude of fossil CH 4 seepage naturally oc...
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ftcopernicus:oai:publications.copernicus.org:hessd88642 2023-05-15T15:11:38+02:00 Mobile open dynamic chamber measurement of methane macroseeps in lakes Thalasso, Frederic Walter Anthony, Katey Irzak, Olya Chaleff, Ethan Barker, Laughlin Anthony, Peter Hanke, Philip Gonzalez-Valencia, Rodrigo 2020-09-09 application/pdf https://doi.org/10.5194/hess-2020-420 https://hess.copernicus.org/preprints/hess-2020-420/ eng eng doi:10.5194/hess-2020-420 https://hess.copernicus.org/preprints/hess-2020-420/ eISSN: 1607-7938 Text 2020 ftcopernicus https://doi.org/10.5194/hess-2020-420 2020-09-14T16:22:13Z Methane (CH 4 ) seepage; i.e., steady or episodic flow of gaseous hydrocarbons from subsurface reservoirs, has been identified as a significant source of atmospheric CH 4 . However, radiocarbon data from polar ice cores recently brought into question the magnitude of fossil CH 4 seepage naturally occurring. In northern high latitudes, seepage of subsurface CH 4 is impeded by permafrost and glaciers, which are under an increasing risk of thawing and melting in a globally warming world, implying the potential release of large stores of CH 4 in the future. Resolution of these important questions requires a better constraint and monitoring of actual emissions from seepage areas. The measurement of these seeps is challenging, particularly in aquatic environments, because they involve large and irregular gas flowrates, unevenly distributed both spatially and temporally. Large macroseeps are particularly difficult to measure due to a lack of lightweight, inexpensive methods that can deployed in remote Arctic environments. Here, we report the use of a mobile chamber for measuring emissions at the surface of ice-free lakes subject to intense CH 4 macroseepage. Tested in a remote Alaskan lake, the method was validated for the measurement of fossil CH 4 emissions of up to 1.08 × 104 g CH 4 m -2 d -1 (13.0 L m -2 min -1 of 83.4 % CH 4 bubbles), which is within the range of global fossil methane seepage and several orders of magnitude above standard ecological emissions from lakes. In addition, this method allows for low diffusive flux measurements. Thus, the mobile chamber approach presented here covers the entire magnitude range of CH 4 emissions currently identified, from those standardly observed in lakes to intense macroseeps, with a single apparatus of moderate cost. Text Arctic Ice permafrost Copernicus Publications: E-Journals Arctic |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
Methane (CH 4 ) seepage; i.e., steady or episodic flow of gaseous hydrocarbons from subsurface reservoirs, has been identified as a significant source of atmospheric CH 4 . However, radiocarbon data from polar ice cores recently brought into question the magnitude of fossil CH 4 seepage naturally occurring. In northern high latitudes, seepage of subsurface CH 4 is impeded by permafrost and glaciers, which are under an increasing risk of thawing and melting in a globally warming world, implying the potential release of large stores of CH 4 in the future. Resolution of these important questions requires a better constraint and monitoring of actual emissions from seepage areas. The measurement of these seeps is challenging, particularly in aquatic environments, because they involve large and irregular gas flowrates, unevenly distributed both spatially and temporally. Large macroseeps are particularly difficult to measure due to a lack of lightweight, inexpensive methods that can deployed in remote Arctic environments. Here, we report the use of a mobile chamber for measuring emissions at the surface of ice-free lakes subject to intense CH 4 macroseepage. Tested in a remote Alaskan lake, the method was validated for the measurement of fossil CH 4 emissions of up to 1.08 × 104 g CH 4 m -2 d -1 (13.0 L m -2 min -1 of 83.4 % CH 4 bubbles), which is within the range of global fossil methane seepage and several orders of magnitude above standard ecological emissions from lakes. In addition, this method allows for low diffusive flux measurements. Thus, the mobile chamber approach presented here covers the entire magnitude range of CH 4 emissions currently identified, from those standardly observed in lakes to intense macroseeps, with a single apparatus of moderate cost. |
format |
Text |
author |
Thalasso, Frederic Walter Anthony, Katey Irzak, Olya Chaleff, Ethan Barker, Laughlin Anthony, Peter Hanke, Philip Gonzalez-Valencia, Rodrigo |
spellingShingle |
Thalasso, Frederic Walter Anthony, Katey Irzak, Olya Chaleff, Ethan Barker, Laughlin Anthony, Peter Hanke, Philip Gonzalez-Valencia, Rodrigo Mobile open dynamic chamber measurement of methane macroseeps in lakes |
author_facet |
Thalasso, Frederic Walter Anthony, Katey Irzak, Olya Chaleff, Ethan Barker, Laughlin Anthony, Peter Hanke, Philip Gonzalez-Valencia, Rodrigo |
author_sort |
Thalasso, Frederic |
title |
Mobile open dynamic chamber measurement of methane macroseeps in lakes |
title_short |
Mobile open dynamic chamber measurement of methane macroseeps in lakes |
title_full |
Mobile open dynamic chamber measurement of methane macroseeps in lakes |
title_fullStr |
Mobile open dynamic chamber measurement of methane macroseeps in lakes |
title_full_unstemmed |
Mobile open dynamic chamber measurement of methane macroseeps in lakes |
title_sort |
mobile open dynamic chamber measurement of methane macroseeps in lakes |
publishDate |
2020 |
url |
https://doi.org/10.5194/hess-2020-420 https://hess.copernicus.org/preprints/hess-2020-420/ |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Ice permafrost |
genre_facet |
Arctic Ice permafrost |
op_source |
eISSN: 1607-7938 |
op_relation |
doi:10.5194/hess-2020-420 https://hess.copernicus.org/preprints/hess-2020-420/ |
op_doi |
https://doi.org/10.5194/hess-2020-420 |
_version_ |
1766342471000784896 |