Understanding the relationships among phosphorus (P), soil organic carbon (SOC) and
aggregate stability is vital for improving soil fertility and P and C cycling in different land-use …

It is known that the association of soil organic matter (SOM) with iron minerals limits carbon
mobilization and degradation in aerobic soils and sediments. However, the efficacy of iron …

Hydrological changes significantly affect organic matter export in flood plains, which is a vital
aspect of aquatic food webs and biogeochemical cycles. The frequency and duration of …

Mineral-associated soil organic matter (SOM) is critical for stabilizing organic carbon and
mitigating climate change. However, mineral-SOM interactions at the molecular scale …

How sea level rise (SLR) alters carbon (C) dynamics in tidal salt marsh soils is unresolved.
Changes in hydrodynamics could influence organo-mineral associations, influencing …

The cycling of iron (Fe) and carbon in the rhizosphere of submerged plants and the
associated impact on organic carbon (OC) sequestration are poorly understood. We …

Tidal channels are biogeochemical hotspots that horizontally exchange carbon (C) with
marsh platforms, but the physiochemical drivers controlling these dynamics are poorly …

Fe-bearing clay minerals are frequently present in oil reservoirs as potential electron
acceptor. Compounds in crude oil may mediate microbial reduction of structural Fe (III) in …

Natural and anthropogenic disturbances lead to degradation of (soil organic carbon) SOC
content black soil in northeast china. Goethite (α-FeO (OH)) as widely distributed mineral …

Fertilization is crucial for increasing crop productivity and it alters soil microbial biomass and
activities. These alterations exert implications for soil carbon (C) stocks, primarily through the …