Iron Dynamics during Thermokarst Processes in the Yedoma Domain and Implications for Interactions between Iron and Organic Carbon
Iron (Fe) plays a key role in mediating organic carbon (OC) decomposition rates in permafrost soils. Fe-bearing minerals stabilize OC through complexation, co-precipitation or aggregation processes and thus hinder degradation of OC. In addition, Fe(III) reduction can inhibit methanogenesis and decre...
Main Authors: | , , , , , , , , , , |
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Other Authors: | |
Format: | Conference Object |
Language: | English |
Published: |
2020
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Subjects: | |
Online Access: | http://hdl.handle.net/2078.1/239965 |