Volatile organic compound fluxes in a subarctic peatland and lake

Ecosystems exchange climate-relevant trace gases with the atmosphere, including volatile organic compounds (VOCs) that are a small but highly reactive part of the carbon cycle. VOCs have important ecological functions and implications for atmospheric chemistry and climate.We measured the ecosystem-level surface-atmosphere VOC fluxes using the eddy covariance technique at a shallow subarctic lake and an adjacent graminoid-dominated fen in northern Sweden during two contrasting periods: the peak growing season (mid-July) and the senescent period post-growing season (September-October). In July, the fen was a net source of methanol, acetaldehyde, acetone, dimethyl sulfide, isoprene, and monoterpenes. All of these VOCs showed a diel cycle of emission with maxima around noon and isoprene dominated the fluxes (93±22 μmolm-2 d-1, mean±SE). Isoprene emission was strongly stimulated by temperature and presented a steeper response to temperature (Q10 = 14:5) than that typically assumed in biogenic emission models, supporting the high temperature sensitivity of arctic vegetation. In September, net emissions of methanol and isoprene were drastically reduced, while acetaldehyde and acetone were deposited to the fen, with rates of up to-6:7±2:8 μmolm-2 d-1 for acetaldehyde. Remarkably, the lake was a sink for acetaldehyde and acetone during both periods, with average fluxes up to -19±1:3 μmolm-2 d-1 of acetone in July and up to-8:5± 2:3 μmolm-2 d-1 of acetaldehyde in September. The deposition of both carbonyl compounds correlated with their atmospheric mixing ratios, with deposition velocities of-0:23± 0:01 and-0:68±0:03 cm s-1 for acetone and acetaldehyde, respectively. Even though these VOC fluxes represented less than 0.5%and less than 5%of the CO2 and CH4 net carbon ecosystem exchange, respectively, VOCs alter the oxidation capacity of the atmosphere. Thus, understanding the response of their emissions to climate change is important for accurate prediction of the future climatic conditions in this rapidly warming area of the planet.

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Main Authors: Seco, Roger, Holst, Thomas, Sillesen Matzen, Mikkel, Westergaard-Nielsen, Andreas, Li, Tao, Simin, Tihomir, Jansen, Joachim, Crill, Patrick, Friborg, Thomas, Rinne, Janne, Rinnan, Riikka
Other Authors: European Commission
Format: artículo biblioteca
Language:English
Published: European Geosciences Union 2020-11-11
Subjects:Volatile organic compounds (VOCs), Atmospheric chemistry, Gases, Climate, Take urgent action to combat climate change and its impacts,
Online Access:http://hdl.handle.net/10261/344967
http://dx.doi.org/10.13039/501100000780
https://api.elsevier.com/content/abstract/scopus_id/85096466976
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spelling dig-idaea-es-10261-3449672024-05-14T21:02:53Z Volatile organic compound fluxes in a subarctic peatland and lake Seco, Roger Holst, Thomas Sillesen Matzen, Mikkel Westergaard-Nielsen, Andreas Li, Tao Simin, Tihomir Jansen, Joachim Crill, Patrick Friborg, Thomas Rinne, Janne Rinnan, Riikka European Commission Volatile organic compounds (VOCs) Atmospheric chemistry Gases Climate Take urgent action to combat climate change and its impacts Ecosystems exchange climate-relevant trace gases with the atmosphere, including volatile organic compounds (VOCs) that are a small but highly reactive part of the carbon cycle. VOCs have important ecological functions and implications for atmospheric chemistry and climate.We measured the ecosystem-level surface-atmosphere VOC fluxes using the eddy covariance technique at a shallow subarctic lake and an adjacent graminoid-dominated fen in northern Sweden during two contrasting periods: the peak growing season (mid-July) and the senescent period post-growing season (September-October). In July, the fen was a net source of methanol, acetaldehyde, acetone, dimethyl sulfide, isoprene, and monoterpenes. All of these VOCs showed a diel cycle of emission with maxima around noon and isoprene dominated the fluxes (93±22 μmolm-2 d-1, mean±SE). Isoprene emission was strongly stimulated by temperature and presented a steeper response to temperature (Q10 = 14:5) than that typically assumed in biogenic emission models, supporting the high temperature sensitivity of arctic vegetation. In September, net emissions of methanol and isoprene were drastically reduced, while acetaldehyde and acetone were deposited to the fen, with rates of up to-6:7±2:8 μmolm-2 d-1 for acetaldehyde. Remarkably, the lake was a sink for acetaldehyde and acetone during both periods, with average fluxes up to -19±1:3 μmolm-2 d-1 of acetone in July and up to-8:5± 2:3 μmolm-2 d-1 of acetaldehyde in September. The deposition of both carbonyl compounds correlated with their atmospheric mixing ratios, with deposition velocities of-0:23± 0:01 and-0:68±0:03 cm s-1 for acetone and acetaldehyde, respectively. Even though these VOC fluxes represented less than 0.5%and less than 5%of the CO2 and CH4 net carbon ecosystem exchange, respectively, VOCs alter the oxidation capacity of the atmosphere. Thus, understanding the response of their emissions to climate change is important for accurate prediction of the future climatic conditions in this rapidly warming area of the planet. This research has been supported by the European Research Council (TUVOLU – Tundra biogenic volatile emissions in the 21st century, grant no. 771012) and the Marie Skłodowska-Curie actions (HIVOL, grant no. 751684) under the European Union's Horizon 2020 research and innovation programme, the Independent Research Fund Denmark | Natural Sciences, the Swedish Research Council (grant no. 2013-5562), the European Commission under the Seventh Framework Programme (PAGE21, grant no. 282700), and by the Danish National Research Foundation (CENPERM DNRF100). Peer reviewed 2024-02-02T07:46:33Z 2024-02-02T07:46:33Z 2020-11-11 artículo http://purl.org/coar/resource_type/c_6501 Atmospheric Chemistry and Physics 20: 13399–13416 (2020) 16807316 http://hdl.handle.net/10261/344967 10.5194/acp-20-13399-2020 http://dx.doi.org/10.13039/501100000780 2-s2.0-85096466976 https://api.elsevier.com/content/abstract/scopus_id/85096466976 en #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/EC/FP7/282700 Atmospheric Chemistry and Physics Publisher's version https://doi.org/10.5194/acp-20-13399-2020 Sí open European Geosciences Union
institution IDAEA ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-idaea-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del IDAEA España
language English
topic Volatile organic compounds (VOCs)
Atmospheric chemistry
Gases
Climate
Take urgent action to combat climate change and its impacts
Volatile organic compounds (VOCs)
Atmospheric chemistry
Gases
Climate
Take urgent action to combat climate change and its impacts
spellingShingle Volatile organic compounds (VOCs)
Atmospheric chemistry
Gases
Climate
Take urgent action to combat climate change and its impacts
Volatile organic compounds (VOCs)
Atmospheric chemistry
Gases
Climate
Take urgent action to combat climate change and its impacts
Seco, Roger
Holst, Thomas
Sillesen Matzen, Mikkel
Westergaard-Nielsen, Andreas
Li, Tao
Simin, Tihomir
Jansen, Joachim
Crill, Patrick
Friborg, Thomas
Rinne, Janne
Rinnan, Riikka
Volatile organic compound fluxes in a subarctic peatland and lake
description Ecosystems exchange climate-relevant trace gases with the atmosphere, including volatile organic compounds (VOCs) that are a small but highly reactive part of the carbon cycle. VOCs have important ecological functions and implications for atmospheric chemistry and climate.We measured the ecosystem-level surface-atmosphere VOC fluxes using the eddy covariance technique at a shallow subarctic lake and an adjacent graminoid-dominated fen in northern Sweden during two contrasting periods: the peak growing season (mid-July) and the senescent period post-growing season (September-October). In July, the fen was a net source of methanol, acetaldehyde, acetone, dimethyl sulfide, isoprene, and monoterpenes. All of these VOCs showed a diel cycle of emission with maxima around noon and isoprene dominated the fluxes (93±22 μmolm-2 d-1, mean±SE). Isoprene emission was strongly stimulated by temperature and presented a steeper response to temperature (Q10 = 14:5) than that typically assumed in biogenic emission models, supporting the high temperature sensitivity of arctic vegetation. In September, net emissions of methanol and isoprene were drastically reduced, while acetaldehyde and acetone were deposited to the fen, with rates of up to-6:7±2:8 μmolm-2 d-1 for acetaldehyde. Remarkably, the lake was a sink for acetaldehyde and acetone during both periods, with average fluxes up to -19±1:3 μmolm-2 d-1 of acetone in July and up to-8:5± 2:3 μmolm-2 d-1 of acetaldehyde in September. The deposition of both carbonyl compounds correlated with their atmospheric mixing ratios, with deposition velocities of-0:23± 0:01 and-0:68±0:03 cm s-1 for acetone and acetaldehyde, respectively. Even though these VOC fluxes represented less than 0.5%and less than 5%of the CO2 and CH4 net carbon ecosystem exchange, respectively, VOCs alter the oxidation capacity of the atmosphere. Thus, understanding the response of their emissions to climate change is important for accurate prediction of the future climatic conditions in this rapidly warming area of the planet.
author2 European Commission
author_facet European Commission
Seco, Roger
Holst, Thomas
Sillesen Matzen, Mikkel
Westergaard-Nielsen, Andreas
Li, Tao
Simin, Tihomir
Jansen, Joachim
Crill, Patrick
Friborg, Thomas
Rinne, Janne
Rinnan, Riikka
format artículo
topic_facet Volatile organic compounds (VOCs)
Atmospheric chemistry
Gases
Climate
Take urgent action to combat climate change and its impacts
author Seco, Roger
Holst, Thomas
Sillesen Matzen, Mikkel
Westergaard-Nielsen, Andreas
Li, Tao
Simin, Tihomir
Jansen, Joachim
Crill, Patrick
Friborg, Thomas
Rinne, Janne
Rinnan, Riikka
author_sort Seco, Roger
title Volatile organic compound fluxes in a subarctic peatland and lake
title_short Volatile organic compound fluxes in a subarctic peatland and lake
title_full Volatile organic compound fluxes in a subarctic peatland and lake
title_fullStr Volatile organic compound fluxes in a subarctic peatland and lake
title_full_unstemmed Volatile organic compound fluxes in a subarctic peatland and lake
title_sort volatile organic compound fluxes in a subarctic peatland and lake
publisher European Geosciences Union
publishDate 2020-11-11
url http://hdl.handle.net/10261/344967
http://dx.doi.org/10.13039/501100000780
https://api.elsevier.com/content/abstract/scopus_id/85096466976
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