Influence of pO on Iron Redox Cycling and Anaerobic Organic Carbon Mineralization in a Humid Tropical Forest Soil.

Ferrous iron (Fe) oxidation is an important pathway for generating reactive Fe phases in soils, which can affect organic carbon (OC) persistence/decomposition. We explored how pO concentration influences Fe oxidation rates and Fe mineral composition, and how this impacts the subsequent Fe reduction and anaerobic OC mineralization following a transition from oxic to anoxic conditions. We conducted batch soil slurry experiments within a humid tropical forest soil amended with isotopically labeled Fe. The slurries were oxidized with either 21% or 1% pO for 9 days and then incubated for 20 days under anoxic conditions. Exposure to 21% pO led to faster Fe oxidation rates and greater partitioning of the amended Fe into low-crystallinity Fe-(oxyhydr)oxides (based on Mössbauer analysis) than exposure to 1% pO. During the subsequent anoxic period, low-crystallinity Fe-(oxyhydr)oxides were preferentially reduced relative to more crystalline forms with higher net rates of anoxic Fe and CO production-which were well correlated-following exposure to 21% pO than to 1% pO. This study illustrates that in redox-dynamic systems, the magnitude of O fluctuations can influence the coupled iron and organic carbon cycling in soils and more broadly, that reaction rates during periods of anoxia depend on the characteristics of prior oxidation events.