Strontium isotopes trace the dissolution and precipitation of mineral organic carbon interactions in thawing permafrost

Interactions between minerals and organic carbon (OC) in soils are key to stabilize OC and mitigate greenhouse gas emissions upon permafrost thaw. However, changes in soil water pathways upon permafrost thaw are likely to affect the stability of mineral OC interactions by inducing their dissolution...

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Bibliographic Details
Published in:Geoderma
Main Authors: Monhonval, Arthur, Hirst, Catherine, Jens Strauss, Edward Schuur, Opfergelt, Sophie
Other Authors: UCL - SST/ELI/ELIE - Environmental Sciences
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier BV 2023
Subjects:
Yar
Online Access:http://hdl.handle.net/2078.1/273934
https://doi.org/10.1016/j.geoderma.2023.116456