Iron is the most abundant redox‐active metal in the Earth's crust. The one electron transfer
between the two most common redox states, Fe (II) and Fe (III), plays a role in a huge range …

Reduction–oxidation (redox) reactions underlie essentially all biogeochemical cycles. Like
most soil properties and processes, redox is spatiotemporally heterogeneous. However …

Despite substantial experimental evidence of electron transfer, atom exchange, and
mineralogical transformation during the reaction of Fe (II) aq with synthetic Fe (III) minerals …

Iron (Fe) phases are tightly linked to the preservation rather than the loss of organic carbon
(OC) in soil; however, during redox fluctuations, OC may be lost due to Fe phase-mediated …

Understanding the processes controlling organic matter (OM) stocks in upland soils, and the
ability to management them, is crucial for maintaining soil fertility and carbon (C) storage as …

Enhancing soil carbon (C) storage has the potential to offset human‐caused increases in
atmospheric CO2. Rising CO2 has occurred concurrently with increasing supply rates of …

Deep carbon cycle is crucial for mantle dynamics and maintaining Earth's habitability.
Recycled carbonates are a strong oxidant in mantle carbon-iron redox reactions, leading to …

Global warming poses an unprecedented threat to agroecosystems. Although temperature
increases are more pronounced during winter than in other seasons, the impact of winter …

Iron oxides are important structural and biogeochemical components of soils that can be
strongly altered by redox-driven processes. This study examined the influence of temporal …

Aggregate hierarchy, a fundamental soil feature controlling various physical and
biogeochemical processes, is well-studied for soils dominated by crystalline minerals but not …