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...
Published in: | Geoderma |
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Main Authors: | , , , , |
Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier BV
2023
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Subjects: | |
Online Access: | http://hdl.handle.net/2078.1/273934 https://doi.org/10.1016/j.geoderma.2023.116456 |