Dissolved organic matter characterization in soils and streams in a small coastal low-Arctic catchment
Ongoing climate warming in the western Canadian Arctic is leading to thawing of permafrost soils and subsequent mobilization of its organic matter pool. Part of this mobilized terrestrial organic matter enters the aquatic system as dissolved organic matter (DOM) and is laterally transported from lan...
Published in: | Biogeosciences |
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2022
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Online Access: | https://research.vu.nl/en/publications/a25519d0-e46e-4013-88ef-d445608f77cd https://doi.org/10.5194/bg-19-3073-2022 https://hdl.handle.net/1871.1/a25519d0-e46e-4013-88ef-d445608f77cd http://www.scopus.com/inward/record.url?scp=85133666676&partnerID=8YFLogxK http://www.scopus.com/inward/citedby.url?scp=85133666676&partnerID=8YFLogxK |
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ftvuamstcris:oai:research.vu.nl:publications/a25519d0-e46e-4013-88ef-d445608f77cd 2024-10-20T14:05:32+00:00 Dissolved organic matter characterization in soils and streams in a small coastal low-Arctic catchment Speetjens, Niek Jesse Tanski, George Martin, Victoria Wagner, Julia Richter, Andreas Hugelius, Gustaf Boucher, Chris Lodi, Rachele Knoblauch, Christian Koch, Boris P. Wünsch, Urban Lantuit, Hugues Vonk, Jorien E. 2022-07-01 https://research.vu.nl/en/publications/a25519d0-e46e-4013-88ef-d445608f77cd https://doi.org/10.5194/bg-19-3073-2022 https://hdl.handle.net/1871.1/a25519d0-e46e-4013-88ef-d445608f77cd http://www.scopus.com/inward/record.url?scp=85133666676&partnerID=8YFLogxK http://www.scopus.com/inward/citedby.url?scp=85133666676&partnerID=8YFLogxK eng eng info:eu-repo/semantics/openAccess Speetjens , N J , Tanski , G , Martin , V , Wagner , J , Richter , A , Hugelius , G , Boucher , C , Lodi , R , Knoblauch , C , Koch , B P , Wünsch , U , Lantuit , H & Vonk , J E 2022 , ' Dissolved organic matter characterization in soils and streams in a small coastal low-Arctic catchment ' , Biogeosciences , vol. 19 , no. 12 , pp. 3073-3097 . https://doi.org/10.5194/bg-19-3073-2022 article 2022 ftvuamstcris https://doi.org/10.5194/bg-19-3073-2022 2024-10-10T00:22:43Z Ongoing climate warming in the western Canadian Arctic is leading to thawing of permafrost soils and subsequent mobilization of its organic matter pool. Part of this mobilized terrestrial organic matter enters the aquatic system as dissolved organic matter (DOM) and is laterally transported from land to sea. Mobilized organic matter is an important source of nutrients for ecosystems, as it is available for microbial breakdown, and thus a source of greenhouse gases. We are beginning to understand spatial controls on the release of DOM as well as the quantities and fate of this material in large Arctic rivers. Yet, these processes remain systematically understudied in small, high-Arctic watersheds, despite the fact that these watersheds experience the strongest warming rates in comparison. Here, we sampled soil (active layer and permafrost) and water (porewater and stream water) from a small ice wedge polygon (IWP) catchment along the Yukon coast, Canada, during the summer of 2018. We assessed the organic carbon (OC) quantity (using dissolved (DOC) and particulate OC (POC) concentrations and soil OC content), quality (δ13C DOC, optical properties and source apportionment) and bioavailability (incubations; optical indices such as slope ratio, Sr; and humification index, HIX) along with stream water properties (temperature, T; pH; electrical conductivity, EC; and water isotopes). We classify and compare different landscape units and their soil horizons that differ in microtopography and hydrological connectivity, giving rise to differences in drainage capacity. Our results show that porewater DOC concentrations and yield reflect drainage patterns and waterlogged conditions in the watershed. DOC yield (in mgDOCg-1soilOC) generally increases with depth but shows a large variability near the transition zone (around the permafrost table). Active-layer porewater DOC generally is more labile than permafrost DOC, due to various reasons (heterogeneity, presence of a paleo-active-layer and sampling strategies). Despite these ... Article in Journal/Newspaper Arctic Arctic Ice permafrost wedge* Yukon Vrije Universiteit Amsterdam (VU): Research Portal Arctic Canada Yukon Biogeosciences 19 12 3073 3097 |
institution |
Open Polar |
collection |
Vrije Universiteit Amsterdam (VU): Research Portal |
op_collection_id |
ftvuamstcris |
language |
English |
description |
Ongoing climate warming in the western Canadian Arctic is leading to thawing of permafrost soils and subsequent mobilization of its organic matter pool. Part of this mobilized terrestrial organic matter enters the aquatic system as dissolved organic matter (DOM) and is laterally transported from land to sea. Mobilized organic matter is an important source of nutrients for ecosystems, as it is available for microbial breakdown, and thus a source of greenhouse gases. We are beginning to understand spatial controls on the release of DOM as well as the quantities and fate of this material in large Arctic rivers. Yet, these processes remain systematically understudied in small, high-Arctic watersheds, despite the fact that these watersheds experience the strongest warming rates in comparison. Here, we sampled soil (active layer and permafrost) and water (porewater and stream water) from a small ice wedge polygon (IWP) catchment along the Yukon coast, Canada, during the summer of 2018. We assessed the organic carbon (OC) quantity (using dissolved (DOC) and particulate OC (POC) concentrations and soil OC content), quality (δ13C DOC, optical properties and source apportionment) and bioavailability (incubations; optical indices such as slope ratio, Sr; and humification index, HIX) along with stream water properties (temperature, T; pH; electrical conductivity, EC; and water isotopes). We classify and compare different landscape units and their soil horizons that differ in microtopography and hydrological connectivity, giving rise to differences in drainage capacity. Our results show that porewater DOC concentrations and yield reflect drainage patterns and waterlogged conditions in the watershed. DOC yield (in mgDOCg-1soilOC) generally increases with depth but shows a large variability near the transition zone (around the permafrost table). Active-layer porewater DOC generally is more labile than permafrost DOC, due to various reasons (heterogeneity, presence of a paleo-active-layer and sampling strategies). Despite these ... |
format |
Article in Journal/Newspaper |
author |
Speetjens, Niek Jesse Tanski, George Martin, Victoria Wagner, Julia Richter, Andreas Hugelius, Gustaf Boucher, Chris Lodi, Rachele Knoblauch, Christian Koch, Boris P. Wünsch, Urban Lantuit, Hugues Vonk, Jorien E. |
spellingShingle |
Speetjens, Niek Jesse Tanski, George Martin, Victoria Wagner, Julia Richter, Andreas Hugelius, Gustaf Boucher, Chris Lodi, Rachele Knoblauch, Christian Koch, Boris P. Wünsch, Urban Lantuit, Hugues Vonk, Jorien E. Dissolved organic matter characterization in soils and streams in a small coastal low-Arctic catchment |
author_facet |
Speetjens, Niek Jesse Tanski, George Martin, Victoria Wagner, Julia Richter, Andreas Hugelius, Gustaf Boucher, Chris Lodi, Rachele Knoblauch, Christian Koch, Boris P. Wünsch, Urban Lantuit, Hugues Vonk, Jorien E. |
author_sort |
Speetjens, Niek Jesse |
title |
Dissolved organic matter characterization in soils and streams in a small coastal low-Arctic catchment |
title_short |
Dissolved organic matter characterization in soils and streams in a small coastal low-Arctic catchment |
title_full |
Dissolved organic matter characterization in soils and streams in a small coastal low-Arctic catchment |
title_fullStr |
Dissolved organic matter characterization in soils and streams in a small coastal low-Arctic catchment |
title_full_unstemmed |
Dissolved organic matter characterization in soils and streams in a small coastal low-Arctic catchment |
title_sort |
dissolved organic matter characterization in soils and streams in a small coastal low-arctic catchment |
publishDate |
2022 |
url |
https://research.vu.nl/en/publications/a25519d0-e46e-4013-88ef-d445608f77cd https://doi.org/10.5194/bg-19-3073-2022 https://hdl.handle.net/1871.1/a25519d0-e46e-4013-88ef-d445608f77cd http://www.scopus.com/inward/record.url?scp=85133666676&partnerID=8YFLogxK http://www.scopus.com/inward/citedby.url?scp=85133666676&partnerID=8YFLogxK |
geographic |
Arctic Canada Yukon |
geographic_facet |
Arctic Canada Yukon |
genre |
Arctic Arctic Ice permafrost wedge* Yukon |
genre_facet |
Arctic Arctic Ice permafrost wedge* Yukon |
op_source |
Speetjens , N J , Tanski , G , Martin , V , Wagner , J , Richter , A , Hugelius , G , Boucher , C , Lodi , R , Knoblauch , C , Koch , B P , Wünsch , U , Lantuit , H & Vonk , J E 2022 , ' Dissolved organic matter characterization in soils and streams in a small coastal low-Arctic catchment ' , Biogeosciences , vol. 19 , no. 12 , pp. 3073-3097 . https://doi.org/10.5194/bg-19-3073-2022 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/bg-19-3073-2022 |
container_title |
Biogeosciences |
container_volume |
19 |
container_issue |
12 |
container_start_page |
3073 |
op_container_end_page |
3097 |
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1813443304114618368 |