Carbon and nitrogen cycling in tundra soils - Churchill
The landscapes were divided into five landform units: (1) upper slope, (2) back slope, (3) lower slope, (4) hummock, and (5) interhummock, which represented a great diversity of Static and Turbic Cryosolic soils including Brunisolic, Gleysolic, and Organic subgroups. Soil gross N mineralization was...
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Canadian Cryospheric Information Network
2009
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Online Access: | https://dx.doi.org/10.5443/10960 https://www.polardata.ca/pdcsearch/?doi_id=10960 |
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ftdatacite:10.5443/10960 2023-05-15T14:50:53+02:00 Carbon and nitrogen cycling in tundra soils - Churchill Bedard-Haughn, Angela Paré, Maxime 2009 https://dx.doi.org/10.5443/10960 https://www.polardata.ca/pdcsearch/?doi_id=10960 en eng Canadian Cryospheric Information Network Public Cape Churchill Carbon Carbon dioxide Greenhouse gas Landscape Nitrogen Nutrients Soils International Polar Year-Climate change impacts on Canadian Arctic tundra ecosystems Interdisciplinary and multi-scale assessments dataset Dataset 2009 ftdatacite https://doi.org/10.5443/10960 2021-11-05T12:55:41Z The landscapes were divided into five landform units: (1) upper slope, (2) back slope, (3) lower slope, (4) hummock, and (5) interhummock, which represented a great diversity of Static and Turbic Cryosolic soils including Brunisolic, Gleysolic, and Organic subgroups. Soil gross N mineralization was measured using the 15N dilution technique, whereas soil GHG emissions (N2O, CH4, and CO2) were measured using a multicomponent Fourier transform infrared gas analyzer. Soil organic matter characteristics were determined by (1) water-extractable organic matter, (2) density fractionation of SOM, and (3) solid-state CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy. : Purpose: Knowledge of the ability of the soil to mineralize nitrogen (N) and release greenhouse gases (GHG) at the landscape scale is critical to predict and model future effects of climate change on Arctic soil organic matter (SOM). The objective was to examine how SOM characteristics influences soil gross nitrogen mineralization and soil carbon dynamics in several Arctic ecosystems. : Summary: Not Applicable Dataset Arctic Climate change International Polar Year Tundra DataCite Metadata Store (German National Library of Science and Technology) Arctic Cape Churchill ENVELOPE(-93.218,-93.218,58.763,58.763) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Cape Churchill Carbon Carbon dioxide Greenhouse gas Landscape Nitrogen Nutrients Soils International Polar Year-Climate change impacts on Canadian Arctic tundra ecosystems Interdisciplinary and multi-scale assessments |
spellingShingle |
Cape Churchill Carbon Carbon dioxide Greenhouse gas Landscape Nitrogen Nutrients Soils International Polar Year-Climate change impacts on Canadian Arctic tundra ecosystems Interdisciplinary and multi-scale assessments Bedard-Haughn, Angela Paré, Maxime Carbon and nitrogen cycling in tundra soils - Churchill |
topic_facet |
Cape Churchill Carbon Carbon dioxide Greenhouse gas Landscape Nitrogen Nutrients Soils International Polar Year-Climate change impacts on Canadian Arctic tundra ecosystems Interdisciplinary and multi-scale assessments |
description |
The landscapes were divided into five landform units: (1) upper slope, (2) back slope, (3) lower slope, (4) hummock, and (5) interhummock, which represented a great diversity of Static and Turbic Cryosolic soils including Brunisolic, Gleysolic, and Organic subgroups. Soil gross N mineralization was measured using the 15N dilution technique, whereas soil GHG emissions (N2O, CH4, and CO2) were measured using a multicomponent Fourier transform infrared gas analyzer. Soil organic matter characteristics were determined by (1) water-extractable organic matter, (2) density fractionation of SOM, and (3) solid-state CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy. : Purpose: Knowledge of the ability of the soil to mineralize nitrogen (N) and release greenhouse gases (GHG) at the landscape scale is critical to predict and model future effects of climate change on Arctic soil organic matter (SOM). The objective was to examine how SOM characteristics influences soil gross nitrogen mineralization and soil carbon dynamics in several Arctic ecosystems. : Summary: Not Applicable |
format |
Dataset |
author |
Bedard-Haughn, Angela Paré, Maxime |
author_facet |
Bedard-Haughn, Angela Paré, Maxime |
author_sort |
Bedard-Haughn, Angela |
title |
Carbon and nitrogen cycling in tundra soils - Churchill |
title_short |
Carbon and nitrogen cycling in tundra soils - Churchill |
title_full |
Carbon and nitrogen cycling in tundra soils - Churchill |
title_fullStr |
Carbon and nitrogen cycling in tundra soils - Churchill |
title_full_unstemmed |
Carbon and nitrogen cycling in tundra soils - Churchill |
title_sort |
carbon and nitrogen cycling in tundra soils - churchill |
publisher |
Canadian Cryospheric Information Network |
publishDate |
2009 |
url |
https://dx.doi.org/10.5443/10960 https://www.polardata.ca/pdcsearch/?doi_id=10960 |
long_lat |
ENVELOPE(-93.218,-93.218,58.763,58.763) |
geographic |
Arctic Cape Churchill |
geographic_facet |
Arctic Cape Churchill |
genre |
Arctic Climate change International Polar Year Tundra |
genre_facet |
Arctic Climate change International Polar Year Tundra |
op_rights |
Public |
op_doi |
https://doi.org/10.5443/10960 |
_version_ |
1766321940283260928 |