A Novel Approach for High-Frequency in-situ Quantification of Methane Oxidation in Peatlands

Methane (CH4) oxidation is an important process for regulating CH4 emissions from peatlands as it oxidizes CH4 to carbon dioxide (CO2). Our current knowledge about its temporal dynamics and contribution to ecosystem CO2 fluxes is, however, limited due to methodological constraints. Here, we present...

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Published in:Soil Systems
Main Authors: Cecilie Skov Nielsen, Niles J. Hasselquist, Mats B. Nilsson, Mats Öquist, Järvi Järveoja, Matthias Peichl
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2018
Subjects:
Online Access:https://doi.org/10.3390/soilsystems3010004
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spelling ftmdpi:oai:mdpi.com:/2571-8789/3/1/4/ 2023-08-20T04:08:47+02:00 A Novel Approach for High-Frequency in-situ Quantification of Methane Oxidation in Peatlands Cecilie Skov Nielsen Niles J. Hasselquist Mats B. Nilsson Mats Öquist Järvi Järveoja Matthias Peichl agris 2018-12-31 application/pdf https://doi.org/10.3390/soilsystems3010004 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/soilsystems3010004 https://creativecommons.org/licenses/by/4.0/ Soil Systems; Volume 3; Issue 1; Pages: 4 Methane oxidation peatland heterotrophic respiration carbon CO 2 mire Text 2018 ftmdpi https://doi.org/10.3390/soilsystems3010004 2023-07-31T21:56:25Z Methane (CH4) oxidation is an important process for regulating CH4 emissions from peatlands as it oxidizes CH4 to carbon dioxide (CO2). Our current knowledge about its temporal dynamics and contribution to ecosystem CO2 fluxes is, however, limited due to methodological constraints. Here, we present the first results from a novel method for quantifying in-situ CH4 oxidation at high temporal resolution. Using an automated chamber system, we measured the isotopic signature of heterotrophic respiration (CO2 emissions from vegetation-free plots) at a boreal mire in northern Sweden. Based on these data we calculated CH4 oxidation rates using a two-source isotope mixing model. During the measurement campaign, 74% of potential CH4 fluxes from vegetation-free plots were oxidized to CO2, and CH4 oxidation contributed 20 ± 2.5% to heterotrophic respiration corresponding to 10 ± 0.5% of ecosystem respiration. Furthermore, the contribution of CH4 oxidation to heterotrophic respiration showed a distinct diurnal cycle being negligible during nighttime while contributing up to 35 ± 3.0% during the daytime. Our results show that CH4 oxidation may represent an important component of the peatland ecosystem respiration and highlight the value of our method for measuring in-situ CH4 oxidation to better understand carbon dynamics in peatlands. Text Northern Sweden MDPI Open Access Publishing Soil Systems 3 1 4
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Methane oxidation
peatland
heterotrophic respiration
carbon
CO 2
mire
spellingShingle Methane oxidation
peatland
heterotrophic respiration
carbon
CO 2
mire
Cecilie Skov Nielsen
Niles J. Hasselquist
Mats B. Nilsson
Mats Öquist
Järvi Järveoja
Matthias Peichl
A Novel Approach for High-Frequency in-situ Quantification of Methane Oxidation in Peatlands
topic_facet Methane oxidation
peatland
heterotrophic respiration
carbon
CO 2
mire
description Methane (CH4) oxidation is an important process for regulating CH4 emissions from peatlands as it oxidizes CH4 to carbon dioxide (CO2). Our current knowledge about its temporal dynamics and contribution to ecosystem CO2 fluxes is, however, limited due to methodological constraints. Here, we present the first results from a novel method for quantifying in-situ CH4 oxidation at high temporal resolution. Using an automated chamber system, we measured the isotopic signature of heterotrophic respiration (CO2 emissions from vegetation-free plots) at a boreal mire in northern Sweden. Based on these data we calculated CH4 oxidation rates using a two-source isotope mixing model. During the measurement campaign, 74% of potential CH4 fluxes from vegetation-free plots were oxidized to CO2, and CH4 oxidation contributed 20 ± 2.5% to heterotrophic respiration corresponding to 10 ± 0.5% of ecosystem respiration. Furthermore, the contribution of CH4 oxidation to heterotrophic respiration showed a distinct diurnal cycle being negligible during nighttime while contributing up to 35 ± 3.0% during the daytime. Our results show that CH4 oxidation may represent an important component of the peatland ecosystem respiration and highlight the value of our method for measuring in-situ CH4 oxidation to better understand carbon dynamics in peatlands.
format Text
author Cecilie Skov Nielsen
Niles J. Hasselquist
Mats B. Nilsson
Mats Öquist
Järvi Järveoja
Matthias Peichl
author_facet Cecilie Skov Nielsen
Niles J. Hasselquist
Mats B. Nilsson
Mats Öquist
Järvi Järveoja
Matthias Peichl
author_sort Cecilie Skov Nielsen
title A Novel Approach for High-Frequency in-situ Quantification of Methane Oxidation in Peatlands
title_short A Novel Approach for High-Frequency in-situ Quantification of Methane Oxidation in Peatlands
title_full A Novel Approach for High-Frequency in-situ Quantification of Methane Oxidation in Peatlands
title_fullStr A Novel Approach for High-Frequency in-situ Quantification of Methane Oxidation in Peatlands
title_full_unstemmed A Novel Approach for High-Frequency in-situ Quantification of Methane Oxidation in Peatlands
title_sort novel approach for high-frequency in-situ quantification of methane oxidation in peatlands
publisher Multidisciplinary Digital Publishing Institute
publishDate 2018
url https://doi.org/10.3390/soilsystems3010004
op_coverage agris
genre Northern Sweden
genre_facet Northern Sweden
op_source Soil Systems; Volume 3; Issue 1; Pages: 4
op_relation https://dx.doi.org/10.3390/soilsystems3010004
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/soilsystems3010004
container_title Soil Systems
container_volume 3
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