Technical note: Mobile open dynamic chamber measurement of methane macroseeps in lakes

<p>Methane (CH<span class="inline-formula"><sub>4</sub></span>) seepage (i.e., steady or episodic flow of gaseous hydrocarbons from subsurface reservoirs) has been identified as a significant source of atmospheric CH<span class="inline-formula">...

Full description

Bibliographic Details
Main Authors: F. Thalasso, K. Walter Anthony, O. Irzak, E. Chaleff, L. Barker, P. Anthony, P. Hanke, R. Gonzalez-Valencia
Format: Article
Language:English
Published: Copernicus Publications 2020-12-01
Series:Hydrology and Earth System Sciences
Online Access:https://hess.copernicus.org/articles/24/6047/2020/hess-24-6047-2020.pdf
_version_ 1818644420633821184
author F. Thalasso
K. Walter Anthony
K. Walter Anthony
O. Irzak
E. Chaleff
L. Barker
P. Anthony
P. Hanke
R. Gonzalez-Valencia
author_facet F. Thalasso
K. Walter Anthony
K. Walter Anthony
O. Irzak
E. Chaleff
L. Barker
P. Anthony
P. Hanke
R. Gonzalez-Valencia
author_sort F. Thalasso
collection DOAJ
description <p>Methane (CH<span class="inline-formula"><sub>4</sub></span>) seepage (i.e., steady or episodic flow of gaseous hydrocarbons from subsurface reservoirs) has been identified as a significant source of atmospheric CH<span class="inline-formula"><sub>4</sub></span>. However, radiocarbon data from polar ice cores have recently brought into question the magnitude of fossil CH<span class="inline-formula"><sub>4</sub></span> seepage naturally occurring. In northern high latitudes, seepage of subsurface CH<span class="inline-formula"><sub>4</sub></span> 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<span class="inline-formula"><sub>4</sub></span> 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 flow rates, unevenly distributed both spatially and temporally. Large macroseeps are particularly difficult to measure due to a lack of lightweight, inexpensive methods that can be 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<span class="inline-formula"><sub>4</sub></span> macroseepage. Tested in a remote Alaskan lake, the method was validated for the measurement of fossil CH<span class="inline-formula"><sub>4</sub></span> emissions of up to 1.08 <span class="inline-formula">×</span> 10<span class="inline-formula"><sup>4</sup></span> g CH<span class="inline-formula"><sub>4</sub></span> m<span class="inline-formula"><sup>−2</sup></span> d<span class="inline-formula"><sup>−1</sup></span> (13.0 L m<span class="inline-formula"><sup>−2</sup></span> min<span class="inline-formula"><sup>−1</sup></span> of 83.4 % CH<span class="inline-formula"><sub>4</sub></span> 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<span class="inline-formula"><sub>4</sub></span> emissions currently identified, from those standardly observed in lakes to intense macroseeps, with a single apparatus of moderate cost.</p>
first_indexed 2024-12-17T00:14:34Z
format Article
id doaj.art-787cb023fea84c35a6f050850642fe8e
institution Directory Open Access Journal
issn 1027-5606
1607-7938
language English
last_indexed 2024-12-17T00:14:34Z
publishDate 2020-12-01
publisher Copernicus Publications
record_format Article
series Hydrology and Earth System Sciences
spelling doaj.art-787cb023fea84c35a6f050850642fe8e2022-12-21T22:10:44ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382020-12-01246047605810.5194/hess-24-6047-2020Technical note: Mobile open dynamic chamber measurement of methane macroseeps in lakesF. Thalasso0K. Walter Anthony1K. Walter Anthony2O. Irzak3E. Chaleff4L. Barker5P. Anthony6P. Hanke7R. Gonzalez-Valencia8Biotechnology and Bioengineering Department, Cinvestav, Avenida IPN 2508, Mexico City, 07360, MexicoWater and Environmental Research Center, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USAInternational Arctic Research Center, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USAFrost Methane, Oakland, California 94612, USAFrost Methane, Oakland, California 94612, USAFrost Methane, Oakland, California 94612, USAWater and Environmental Research Center, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USAWater and Environmental Research Center, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USABiotechnology and Bioengineering Department, Cinvestav, Avenida IPN 2508, Mexico City, 07360, Mexico<p>Methane (CH<span class="inline-formula"><sub>4</sub></span>) seepage (i.e., steady or episodic flow of gaseous hydrocarbons from subsurface reservoirs) has been identified as a significant source of atmospheric CH<span class="inline-formula"><sub>4</sub></span>. However, radiocarbon data from polar ice cores have recently brought into question the magnitude of fossil CH<span class="inline-formula"><sub>4</sub></span> seepage naturally occurring. In northern high latitudes, seepage of subsurface CH<span class="inline-formula"><sub>4</sub></span> 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<span class="inline-formula"><sub>4</sub></span> 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 flow rates, unevenly distributed both spatially and temporally. Large macroseeps are particularly difficult to measure due to a lack of lightweight, inexpensive methods that can be 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<span class="inline-formula"><sub>4</sub></span> macroseepage. Tested in a remote Alaskan lake, the method was validated for the measurement of fossil CH<span class="inline-formula"><sub>4</sub></span> emissions of up to 1.08 <span class="inline-formula">×</span> 10<span class="inline-formula"><sup>4</sup></span> g CH<span class="inline-formula"><sub>4</sub></span> m<span class="inline-formula"><sup>−2</sup></span> d<span class="inline-formula"><sup>−1</sup></span> (13.0 L m<span class="inline-formula"><sup>−2</sup></span> min<span class="inline-formula"><sup>−1</sup></span> of 83.4 % CH<span class="inline-formula"><sub>4</sub></span> 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<span class="inline-formula"><sub>4</sub></span> emissions currently identified, from those standardly observed in lakes to intense macroseeps, with a single apparatus of moderate cost.</p>https://hess.copernicus.org/articles/24/6047/2020/hess-24-6047-2020.pdf
spellingShingle F. Thalasso
K. Walter Anthony
K. Walter Anthony
O. Irzak
E. Chaleff
L. Barker
P. Anthony
P. Hanke
R. Gonzalez-Valencia
Technical note: Mobile open dynamic chamber measurement of methane macroseeps in lakes
Hydrology and Earth System Sciences
title Technical note: Mobile open dynamic chamber measurement of methane macroseeps in lakes
title_full Technical note: Mobile open dynamic chamber measurement of methane macroseeps in lakes
title_fullStr Technical note: Mobile open dynamic chamber measurement of methane macroseeps in lakes
title_full_unstemmed Technical note: Mobile open dynamic chamber measurement of methane macroseeps in lakes
title_short Technical note: Mobile open dynamic chamber measurement of methane macroseeps in lakes
title_sort technical note mobile open dynamic chamber measurement of methane macroseeps in lakes
url https://hess.copernicus.org/articles/24/6047/2020/hess-24-6047-2020.pdf
work_keys_str_mv AT fthalasso technicalnotemobileopendynamicchambermeasurementofmethanemacroseepsinlakes
AT kwalteranthony technicalnotemobileopendynamicchambermeasurementofmethanemacroseepsinlakes
AT kwalteranthony technicalnotemobileopendynamicchambermeasurementofmethanemacroseepsinlakes
AT oirzak technicalnotemobileopendynamicchambermeasurementofmethanemacroseepsinlakes
AT echaleff technicalnotemobileopendynamicchambermeasurementofmethanemacroseepsinlakes
AT lbarker technicalnotemobileopendynamicchambermeasurementofmethanemacroseepsinlakes
AT panthony technicalnotemobileopendynamicchambermeasurementofmethanemacroseepsinlakes
AT phanke technicalnotemobileopendynamicchambermeasurementofmethanemacroseepsinlakes
AT rgonzalezvalencia technicalnotemobileopendynamicchambermeasurementofmethanemacroseepsinlakes