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...

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Bibliographic Details
Main Authors: Monhonval, Arthur, Opfergelt, Sophie, Mauclet, Elisabeth, Hirst, Catherine, Pereira, Benoît, Vandeuren, Aubry, Bemelmans, Nathan, Grosse Guido, Schirrmeister Lutz, Fuchs Matthias, AGU FALL MEETING
Other Authors: UCL - SST/ELI/ELIE - Environmental Sciences
Format: Conference Object
Language:English
Published: 2020
Subjects:
Ice
Online Access:http://hdl.handle.net/2078.1/239965