Wintertime Greenhouse Gas Fluxes in Hemiboreal Drained Peatlands

The aim of this study is to estimate wintertime emissions of greenhouse gases CO<sub>2</sub>, N<sub>2</sub>O and CH<sub>4</sub> in two abandoned peat extraction areas (APEA), Ess-soo and Laiuse, and in two Oxalis site-type drained peatland forests (DPF) on nitroge...

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Main Authors: Birgit Viru, Gert Veber, Jaak Jaagus, Ain Kull, Martin Maddison, Mart Muhel, Mikk Espenberg, Alar Teemusk, Ülo Mander
Format: Article
Language:English
Published: MDPI AG 2020-07-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/11/7/731
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author Birgit Viru
Gert Veber
Jaak Jaagus
Ain Kull
Martin Maddison
Mart Muhel
Mikk Espenberg
Alar Teemusk
Ülo Mander
author_facet Birgit Viru
Gert Veber
Jaak Jaagus
Ain Kull
Martin Maddison
Mart Muhel
Mikk Espenberg
Alar Teemusk
Ülo Mander
author_sort Birgit Viru
collection DOAJ
description The aim of this study is to estimate wintertime emissions of greenhouse gases CO<sub>2</sub>, N<sub>2</sub>O and CH<sub>4</sub> in two abandoned peat extraction areas (APEA), Ess-soo and Laiuse, and in two Oxalis site-type drained peatland forests (DPF) on nitrogen-rich sapric histosol, a Norway spruce and a Downy birch forest, located in eastern Estonia. According to the long-term study using a closed chamber method, the APEAs emitted less CO<sub>2</sub> and N<sub>2</sub>O, and more CH<sub>4</sub> than the DPFs. Across the study sites, CO<sub>2</sub> flux correlated positively with soil, ground and air temperatures. Continuous snow depth > 5 cm did not influence CO<sub>2</sub>, but at no snow or a thin snow layer the fluxes varied on a large scale (from −1.1 to 106 mg C m<sup>−2</sup> h<sup>−1</sup>). In all sites, the highest N<sub>2</sub>O fluxes were observed at a water table depth of −30 to −40 cm. CH<sub>4</sub> was consumed in the DPFs and was always emitted from the APEAs, whereas the highest flux appeared at a water table >20 cm above the surface. Considering the global warming potential (GWP) of the greenhouse gas emissions from the DPFs in the wintertime, the flux of N<sub>2</sub>O was the main component of warming, showing 3–6 times higher radiative forcing values than that of CO<sub>2</sub> flux, while the role of CH<sub>4</sub> was unimportant. In the APEAs, CO<sub>2</sub> and CH<sub>4</sub> made up almost equal parts, whereas the impact of N<sub>2</sub>O on GWP was minor.
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spelling doaj.art-c183c6984f6845b2afac683f72192a3c2023-11-20T06:22:44ZengMDPI AGAtmosphere2073-44332020-07-0111773110.3390/atmos11070731Wintertime Greenhouse Gas Fluxes in Hemiboreal Drained PeatlandsBirgit Viru0Gert Veber1Jaak Jaagus2Ain Kull3Martin Maddison4Mart Muhel5Mikk Espenberg6Alar Teemusk7Ülo Mander8Department of Geography, Institute of Ecology and Earth Sciences, University of Tartu, Vanemuine St. 46, 51014 Tartu, EstoniaDepartment of Geography, Institute of Ecology and Earth Sciences, University of Tartu, Vanemuine St. 46, 51014 Tartu, EstoniaDepartment of Geography, Institute of Ecology and Earth Sciences, University of Tartu, Vanemuine St. 46, 51014 Tartu, EstoniaDepartment of Geography, Institute of Ecology and Earth Sciences, University of Tartu, Vanemuine St. 46, 51014 Tartu, EstoniaDepartment of Geography, Institute of Ecology and Earth Sciences, University of Tartu, Vanemuine St. 46, 51014 Tartu, EstoniaDepartment of Geography, Institute of Ecology and Earth Sciences, University of Tartu, Vanemuine St. 46, 51014 Tartu, EstoniaDepartment of Geography, Institute of Ecology and Earth Sciences, University of Tartu, Vanemuine St. 46, 51014 Tartu, EstoniaDepartment of Geography, Institute of Ecology and Earth Sciences, University of Tartu, Vanemuine St. 46, 51014 Tartu, EstoniaDepartment of Geography, Institute of Ecology and Earth Sciences, University of Tartu, Vanemuine St. 46, 51014 Tartu, EstoniaThe aim of this study is to estimate wintertime emissions of greenhouse gases CO<sub>2</sub>, N<sub>2</sub>O and CH<sub>4</sub> in two abandoned peat extraction areas (APEA), Ess-soo and Laiuse, and in two Oxalis site-type drained peatland forests (DPF) on nitrogen-rich sapric histosol, a Norway spruce and a Downy birch forest, located in eastern Estonia. According to the long-term study using a closed chamber method, the APEAs emitted less CO<sub>2</sub> and N<sub>2</sub>O, and more CH<sub>4</sub> than the DPFs. Across the study sites, CO<sub>2</sub> flux correlated positively with soil, ground and air temperatures. Continuous snow depth > 5 cm did not influence CO<sub>2</sub>, but at no snow or a thin snow layer the fluxes varied on a large scale (from −1.1 to 106 mg C m<sup>−2</sup> h<sup>−1</sup>). In all sites, the highest N<sub>2</sub>O fluxes were observed at a water table depth of −30 to −40 cm. CH<sub>4</sub> was consumed in the DPFs and was always emitted from the APEAs, whereas the highest flux appeared at a water table >20 cm above the surface. Considering the global warming potential (GWP) of the greenhouse gas emissions from the DPFs in the wintertime, the flux of N<sub>2</sub>O was the main component of warming, showing 3–6 times higher radiative forcing values than that of CO<sub>2</sub> flux, while the role of CH<sub>4</sub> was unimportant. In the APEAs, CO<sub>2</sub> and CH<sub>4</sub> made up almost equal parts, whereas the impact of N<sub>2</sub>O on GWP was minor.https://www.mdpi.com/2073-4433/11/7/731carbon dioxidedrained forestsmethanenitrous oxidepeat extraction areaspeatlands
spellingShingle Birgit Viru
Gert Veber
Jaak Jaagus
Ain Kull
Martin Maddison
Mart Muhel
Mikk Espenberg
Alar Teemusk
Ülo Mander
Wintertime Greenhouse Gas Fluxes in Hemiboreal Drained Peatlands
Atmosphere
carbon dioxide
drained forests
methane
nitrous oxide
peat extraction areas
peatlands
title Wintertime Greenhouse Gas Fluxes in Hemiboreal Drained Peatlands
title_full Wintertime Greenhouse Gas Fluxes in Hemiboreal Drained Peatlands
title_fullStr Wintertime Greenhouse Gas Fluxes in Hemiboreal Drained Peatlands
title_full_unstemmed Wintertime Greenhouse Gas Fluxes in Hemiboreal Drained Peatlands
title_short Wintertime Greenhouse Gas Fluxes in Hemiboreal Drained Peatlands
title_sort wintertime greenhouse gas fluxes in hemiboreal drained peatlands
topic carbon dioxide
drained forests
methane
nitrous oxide
peat extraction areas
peatlands
url https://www.mdpi.com/2073-4433/11/7/731
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