Influence of vegetation cover and soil features on CO2, CH4 and N2O fluxes in northern Finnish Lapland

Understanding the drivers affecting SOM decomposition, GHG emissions and feedback to climate change in subarctic fragile and highly patterned landforms is crucial nowadays. A field campaign was conducted at catchment scale in Finnish Lapland, aiming at detecting differences in GHG fluxes in a mosaic...

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Published in:Polar Science
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16023
http://id.nii.ac.jp/1291/00015911/
id ftnipr:oai:nipr.repo.nii.ac.jp:00016023
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00016023 2023-05-15T17:54:26+02:00 Influence of vegetation cover and soil features on CO2, CH4 and N2O fluxes in northern Finnish Lapland 2020-06 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16023 http://id.nii.ac.jp/1291/00015911/ en eng https://doi.org/10.1016/j.polar.2020.100531 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16023 http://id.nii.ac.jp/1291/00015911/ Polar Science, 24, 100531(2020-06) 18739652 Greenhouse gas fluxes Subarctic soil Boreal forest Wetland Tundra Journal Article 2020 ftnipr https://doi.org/10.1016/j.polar.2020.100531 2022-12-03T19:43:16Z Understanding the drivers affecting SOM decomposition, GHG emissions and feedback to climate change in subarctic fragile and highly patterned landforms is crucial nowadays. A field campaign was conducted at catchment scale in Finnish Lapland, aiming at detecting differences in GHG fluxes in a mosaic of subarctic landforms: pine, mixed, birch and open birch forest, alpine tundra, alpine palsa, non-mire wetland, palsa mires and wetland mires. Soil profiles were described and analyzed for chemical and physical properties. CO2, CH4 and N2O fluxes from vegetated soil surface were measured by static chamber method.The largest amount of CO2 was emitted by birch forests>palsa mires>tundra and pine forest>wetlands and was driven by organic layer thickness in palsas and by priming effect mechanisms when environmental conditions favored the mineralization of organic matter stored in birch forest. Depth and organic matter content of humified organic layer, vegetation development and permanent flooding conditions triggered CH4 emissions, with 6-fold higher emissions from wetland than palsa mires and net uptake in the other landform types. N2O emissions in tundra and birch forests derived mainly from nitrification, sustained by oxygen and N availability. Differently, the higher C/N ratio and lower pH in pine and mixed forests caused N2O uptake in the soil.Possible feedbacks to climate change in the next few years or decades were identified: i) huge CH4 emissions in case of seasonally frozen soil or permafrost disappearance and ii) an increase of CO2 and N2O emissions in response to birch forest expansion. Article in Journal/Newspaper palsa palsas permafrost Polar Science Polar Science Subarctic Tundra Lapland National Institute of Polar Research Repository, Japan Polar Science 24 100531
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
topic Greenhouse gas fluxes
Subarctic soil
Boreal forest
Wetland
Tundra
spellingShingle Greenhouse gas fluxes
Subarctic soil
Boreal forest
Wetland
Tundra
Influence of vegetation cover and soil features on CO2, CH4 and N2O fluxes in northern Finnish Lapland
topic_facet Greenhouse gas fluxes
Subarctic soil
Boreal forest
Wetland
Tundra
description Understanding the drivers affecting SOM decomposition, GHG emissions and feedback to climate change in subarctic fragile and highly patterned landforms is crucial nowadays. A field campaign was conducted at catchment scale in Finnish Lapland, aiming at detecting differences in GHG fluxes in a mosaic of subarctic landforms: pine, mixed, birch and open birch forest, alpine tundra, alpine palsa, non-mire wetland, palsa mires and wetland mires. Soil profiles were described and analyzed for chemical and physical properties. CO2, CH4 and N2O fluxes from vegetated soil surface were measured by static chamber method.The largest amount of CO2 was emitted by birch forests>palsa mires>tundra and pine forest>wetlands and was driven by organic layer thickness in palsas and by priming effect mechanisms when environmental conditions favored the mineralization of organic matter stored in birch forest. Depth and organic matter content of humified organic layer, vegetation development and permanent flooding conditions triggered CH4 emissions, with 6-fold higher emissions from wetland than palsa mires and net uptake in the other landform types. N2O emissions in tundra and birch forests derived mainly from nitrification, sustained by oxygen and N availability. Differently, the higher C/N ratio and lower pH in pine and mixed forests caused N2O uptake in the soil.Possible feedbacks to climate change in the next few years or decades were identified: i) huge CH4 emissions in case of seasonally frozen soil or permafrost disappearance and ii) an increase of CO2 and N2O emissions in response to birch forest expansion.
format Article in Journal/Newspaper
title Influence of vegetation cover and soil features on CO2, CH4 and N2O fluxes in northern Finnish Lapland
title_short Influence of vegetation cover and soil features on CO2, CH4 and N2O fluxes in northern Finnish Lapland
title_full Influence of vegetation cover and soil features on CO2, CH4 and N2O fluxes in northern Finnish Lapland
title_fullStr Influence of vegetation cover and soil features on CO2, CH4 and N2O fluxes in northern Finnish Lapland
title_full_unstemmed Influence of vegetation cover and soil features on CO2, CH4 and N2O fluxes in northern Finnish Lapland
title_sort influence of vegetation cover and soil features on co2, ch4 and n2o fluxes in northern finnish lapland
publishDate 2020
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16023
http://id.nii.ac.jp/1291/00015911/
genre palsa
palsas
permafrost
Polar Science
Polar Science
Subarctic
Tundra
Lapland
genre_facet palsa
palsas
permafrost
Polar Science
Polar Science
Subarctic
Tundra
Lapland
op_relation https://doi.org/10.1016/j.polar.2020.100531
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16023
http://id.nii.ac.jp/1291/00015911/
Polar Science, 24, 100531(2020-06)
18739652
op_doi https://doi.org/10.1016/j.polar.2020.100531
container_title Polar Science
container_volume 24
container_start_page 100531
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