Coupling of geochemical and geophysical measurements to characterize iron and organic carbon co-mobility upon permafrost thaw in an Arctic peatland in Abisko, Sweden.
Permafrost region covers 24% of the Earth’s total area and holds 1460-1600 Pg of carbon. A significant portion of this carbon (1035 ± 150 Pg) can be found in top three meters of the soil. With the degradation of permafrost due to the increase in air temperature in high latitudes (0.6 °C over the...
Main Authors: | , , , , , , , , , |
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Other Authors: | |
Format: | Conference Object |
Language: | English |
Published: |
2022
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Subjects: | |
Online Access: | http://hdl.handle.net/2078.1/268740 |