Combining geochemical and geophysical parameters to characterize permafrost degradation at Abisko, Sweden: implications for iron-organic carbon interactions

Between 30 and 80% of soil organic carbon (OC) in permafrost environments can be stabilized by interactions with mineral surfaces or metals such as iron. Iron-OC interactions may be modified by changing hydrological conditions upon permafrost thaw resulting in local subsidence. The challenge is to i...

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Bibliographic Details
Main Authors: du Bois d'Aische, Eléonore, Thomas, Maxime, Jonard, François, Villani, Maëlle, Hirst, Catherine, Giesler, Reiner, Mörth, Carl-Magnus, Opfergelt, Sophie, Arctic Science Summit Week
Other Authors: UCL - SST/ELI/ELIE - Environmental Sciences
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:http://hdl.handle.net/2078.1/268744