Response of Methane and Nitrous Oxide Emissions from Peatlands to Permafrost Thawing in Xiaoxing’an Mountains, Northeast China

Permafrost thawing may lead to the release of carbon and nitrogen in high-latitude regions of the Northern Hemisphere, mainly in the form of greenhouse gases. Our research aims to reveal the effects of permafrost thawing on CH<sub>4</sub> and N<sub>2</sub>O emissions from pea...

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Main Authors: Xiaoxin Sun, Hongjun Wang, Changchun Song, Xin Jin, Curtis J. Richardson, Tijiu Cai
Format: Article
Language:English
Published: MDPI AG 2021-02-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/12/2/222
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author Xiaoxin Sun
Hongjun Wang
Changchun Song
Xin Jin
Curtis J. Richardson
Tijiu Cai
author_facet Xiaoxin Sun
Hongjun Wang
Changchun Song
Xin Jin
Curtis J. Richardson
Tijiu Cai
author_sort Xiaoxin Sun
collection DOAJ
description Permafrost thawing may lead to the release of carbon and nitrogen in high-latitude regions of the Northern Hemisphere, mainly in the form of greenhouse gases. Our research aims to reveal the effects of permafrost thawing on CH<sub>4</sub> and N<sub>2</sub>O emissions from peatlands in Xiaoxing’an Mountains, Northeast China. During four growing seasons (2011–2014), in situ CH<sub>4</sub> and N<sub>2</sub>O emissions were monitored from peatland under permafrost no-thawing, mild-thawing, and severe-thawing conditions in the middle of the Xiaoxing’an Mountains by a static-chamber method. Average CH<sub>4</sub> emissions in the severe-thawing site were 55-fold higher than those in the no-thawing site. The seasonal variation of CH<sub>4</sub> emission became more aggravated with the intensification of permafrost thawing, in which the emission peaks became larger and the absorption decreased to zero. The increased CH<sub>4</sub> emissions were caused by the expansion of the thawing layer and the subsequent increases in soil temperature, water table, and shifts of plant communities. However, N<sub>2</sub>O emissions did not change with thawing. Permafrost thawing increased CH<sub>4</sub> emissions but did not impact N<sub>2</sub>O emissions in peatlands in the Xiaoxing’an Mountains. Increased CH<sub>4</sub> emissions from peatlands in this region may amplify global warming.
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spelling doaj.art-1be5501a913d4f0d809e786de2927bf82023-12-03T12:38:17ZengMDPI AGAtmosphere2073-44332021-02-0112222210.3390/atmos12020222Response of Methane and Nitrous Oxide Emissions from Peatlands to Permafrost Thawing in Xiaoxing’an Mountains, Northeast ChinaXiaoxin Sun0Hongjun Wang1Changchun Song2Xin Jin3Curtis J. Richardson4Tijiu Cai5Key Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, School of Forestry, Northeast Forestry University, Harbin 150040, ChinaDuke University Wetland Center, Nicholas School of the Environment, Duke University, Durham, NC 27708, USANortheast Institute of Geography and Agroecology, Chinese Academy of Science, Changchun 130102, ChinaKey Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, School of Forestry, Northeast Forestry University, Harbin 150040, ChinaDuke University Wetland Center, Nicholas School of the Environment, Duke University, Durham, NC 27708, USAKey Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, School of Forestry, Northeast Forestry University, Harbin 150040, ChinaPermafrost thawing may lead to the release of carbon and nitrogen in high-latitude regions of the Northern Hemisphere, mainly in the form of greenhouse gases. Our research aims to reveal the effects of permafrost thawing on CH<sub>4</sub> and N<sub>2</sub>O emissions from peatlands in Xiaoxing’an Mountains, Northeast China. During four growing seasons (2011–2014), in situ CH<sub>4</sub> and N<sub>2</sub>O emissions were monitored from peatland under permafrost no-thawing, mild-thawing, and severe-thawing conditions in the middle of the Xiaoxing’an Mountains by a static-chamber method. Average CH<sub>4</sub> emissions in the severe-thawing site were 55-fold higher than those in the no-thawing site. The seasonal variation of CH<sub>4</sub> emission became more aggravated with the intensification of permafrost thawing, in which the emission peaks became larger and the absorption decreased to zero. The increased CH<sub>4</sub> emissions were caused by the expansion of the thawing layer and the subsequent increases in soil temperature, water table, and shifts of plant communities. However, N<sub>2</sub>O emissions did not change with thawing. Permafrost thawing increased CH<sub>4</sub> emissions but did not impact N<sub>2</sub>O emissions in peatlands in the Xiaoxing’an Mountains. Increased CH<sub>4</sub> emissions from peatlands in this region may amplify global warming.https://www.mdpi.com/2073-4433/12/2/222CH<sub>4</sub> emissionN<sub>2</sub>O emissionpeatlandpermafrost thawing
spellingShingle Xiaoxin Sun
Hongjun Wang
Changchun Song
Xin Jin
Curtis J. Richardson
Tijiu Cai
Response of Methane and Nitrous Oxide Emissions from Peatlands to Permafrost Thawing in Xiaoxing’an Mountains, Northeast China
Atmosphere
CH<sub>4</sub> emission
N<sub>2</sub>O emission
peatland
permafrost thawing
title Response of Methane and Nitrous Oxide Emissions from Peatlands to Permafrost Thawing in Xiaoxing’an Mountains, Northeast China
title_full Response of Methane and Nitrous Oxide Emissions from Peatlands to Permafrost Thawing in Xiaoxing’an Mountains, Northeast China
title_fullStr Response of Methane and Nitrous Oxide Emissions from Peatlands to Permafrost Thawing in Xiaoxing’an Mountains, Northeast China
title_full_unstemmed Response of Methane and Nitrous Oxide Emissions from Peatlands to Permafrost Thawing in Xiaoxing’an Mountains, Northeast China
title_short Response of Methane and Nitrous Oxide Emissions from Peatlands to Permafrost Thawing in Xiaoxing’an Mountains, Northeast China
title_sort response of methane and nitrous oxide emissions from peatlands to permafrost thawing in xiaoxing an mountains northeast china
topic CH<sub>4</sub> emission
N<sub>2</sub>O emission
peatland
permafrost thawing
url https://www.mdpi.com/2073-4433/12/2/222
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