Total hydrocarbon flux dynamics at a subarctic mire in northern Sweden
(2008) In Journal of Geophysical Research 113(G3).- Abstract
- This is a study of the spatial and temporal variability of total hydrocarbon (THC) emissions from vegetation and soil at a subarctic mire, northern Sweden. THCs include methane (CH4) and nonmethane volatile organic compounds (NMVOCs), both of which are atmospherically important trace gases and constitute a significant proportion of the carbon exchange between biosphere and atmosphere. Reliable characterization of the magnitude and the dynamics of the THC fluxes from high latitude peatlands are important when considering to what extent trace gas emissions from such ecosystems may change and feed back on climate regulation as a result of warmer climate and melting permafrost. High frequency measurements of THC and carbon dioxide (CO2) were... (More)
- This is a study of the spatial and temporal variability of total hydrocarbon (THC) emissions from vegetation and soil at a subarctic mire, northern Sweden. THCs include methane (CH4) and nonmethane volatile organic compounds (NMVOCs), both of which are atmospherically important trace gases and constitute a significant proportion of the carbon exchange between biosphere and atmosphere. Reliable characterization of the magnitude and the dynamics of the THC fluxes from high latitude peatlands are important when considering to what extent trace gas emissions from such ecosystems may change and feed back on climate regulation as a result of warmer climate and melting permafrost. High frequency measurements of THC and carbon dioxide (CO2) were conducted during four sequential growing seasons in three localities representing the trophic range of plant communities at the mire. The magnitude of the THC flux followed the moisture gradient with increasing emissions from a dry Palsa site (2.2 +/- 0.1 mgC m(-2) d(-1)), to a wet intermediate melt feature with Sphagnum spp. (28 +/- 0.3 mgC m(-2) d(-1)) and highest emissions from a wet Eriophorum spp. site (122 +/- 1.4 mgC m(-2) d(-1)) (overall mean +/- 1 SE, n = 2254, 2231 and 2137). At the Palsa site, daytime THC flux was most strongly related to air temperature while daytime THC emissions at the Sphagnum site had a stronger relation to ground temperature. THC emissions at both the wet sites were correlated to net ecosystem exchange of CO2. An overall spatial correlation indicated that areas with highly productive vegetation communities also had high THC emission potential. (Less)
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/1247753
- author
- Baeckstrand, Kristina ; Crill, Patrick M. ; Mastepanov, Mikhail LU ; Christensen, Torben LU and Bastviken, David
- organization
- publishing date
- 2008
- type
- Contribution to journal
- publication status
- published
- subject
- in
- Journal of Geophysical Research
- volume
- 113
- issue
- G3
- publisher
- Wiley-Blackwell
- external identifiers
-
- wos:000258822700001
- scopus:67649856153
- ISSN
- 2156-2202
- DOI
- 10.1029/2008JG000703
- language
- English
- LU publication?
- yes
- id
- 05bcfda8-6a44-4138-92b2-9e8f6a407431 (old id 1247753)
- date added to LUP
- 2016-04-01 11:56:43
- date last changed
- 2022-02-25 23:35:25
@article{05bcfda8-6a44-4138-92b2-9e8f6a407431,
abstract = {{This is a study of the spatial and temporal variability of total hydrocarbon (THC) emissions from vegetation and soil at a subarctic mire, northern Sweden. THCs include methane (CH4) and nonmethane volatile organic compounds (NMVOCs), both of which are atmospherically important trace gases and constitute a significant proportion of the carbon exchange between biosphere and atmosphere. Reliable characterization of the magnitude and the dynamics of the THC fluxes from high latitude peatlands are important when considering to what extent trace gas emissions from such ecosystems may change and feed back on climate regulation as a result of warmer climate and melting permafrost. High frequency measurements of THC and carbon dioxide (CO2) were conducted during four sequential growing seasons in three localities representing the trophic range of plant communities at the mire. The magnitude of the THC flux followed the moisture gradient with increasing emissions from a dry Palsa site (2.2 +/- 0.1 mgC m(-2) d(-1)), to a wet intermediate melt feature with Sphagnum spp. (28 +/- 0.3 mgC m(-2) d(-1)) and highest emissions from a wet Eriophorum spp. site (122 +/- 1.4 mgC m(-2) d(-1)) (overall mean +/- 1 SE, n = 2254, 2231 and 2137). At the Palsa site, daytime THC flux was most strongly related to air temperature while daytime THC emissions at the Sphagnum site had a stronger relation to ground temperature. THC emissions at both the wet sites were correlated to net ecosystem exchange of CO2. An overall spatial correlation indicated that areas with highly productive vegetation communities also had high THC emission potential.}},
author = {{Baeckstrand, Kristina and Crill, Patrick M. and Mastepanov, Mikhail and Christensen, Torben and Bastviken, David}},
issn = {{2156-2202}},
language = {{eng}},
number = {{G3}},
publisher = {{Wiley-Blackwell}},
series = {{Journal of Geophysical Research}},
title = {{Total hydrocarbon flux dynamics at a subarctic mire in northern Sweden}},
url = {{http://dx.doi.org/10.1029/2008JG000703}},
doi = {{10.1029/2008JG000703}},
volume = {{113}},
year = {{2008}},
}