Flow-path changes in permafrost soils affect Fe-organic carbon interactions: evidence from silicon isotopes

Silicon isotope fractionation upon amorphous silica precipitation is sensitive to freeze-thaw cycles in arctic soils that are composed of carbon-rich permafrost (i.e. soil layer that remains frozen for at least two consecutive years) covered by an active layer (i.e. soil layer that thaws in summer i...

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Bibliographic Details
Main Authors: Villani, Maëlle, Hirst, Catherine, Thomas, Maxime, du Bois d'Aische, Eléonore, Vanderelst, Sarah, Lundin, Erik, Giesler, Reiner, Mörth, Magnus, Opfergelt, Sophie, 2024 Belgian Polar Community Day
Other Authors: UCL - SST/ELI/ELIE - Environmental Sciences
Format: Conference Object
Language:English
Published: 2024
Subjects:
Online Access:http://hdl.handle.net/2078.1/287448