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, Strauß, Jens, Schuur, Edward AG, Opfergelt, Sophie
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier 2023
Subjects:
Yar
Online Access:https://epic.awi.de/id/eprint/58578/
https://epic.awi.de/id/eprint/58578/1/Monhonval_1-s2.0-S0016706123001337-main.pdf
https://hdl.handle.net/10013/epic.096180d9-f65d-42b2-bd5d-0cc825232ce8