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...
Main Authors: | , , , , , , , , |
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Other Authors: | |
Format: | Conference Object |
Language: | English |
Published: |
2023
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Subjects: | |
Online Access: | http://hdl.handle.net/2078.1/268744 |