Predicting and mitigating changes in soil carbon (C) stocks under global change requires a
coherent understanding of the factors regulating soil organic matter (SOM) formation and …

Iron (Fe) oxides are widely recognized to prevent the degradation of organic matter (OM) in
environments, thereby promoting the persistence of organic carbon (OC) in soils. Thus …

Investigating the influence mechanism of drying-wetting cycles on the availability and
mobility of heavy metals in sediment from the perspective of the molecular composition of …

Natural ferrihydrites (Fh) can activate H 2 O 2 to produce reactive oxygen species in Fenton-
like system, while the inefficient Fe 2+ regeneration limited its application. A novel …

Long residence times of soil organic matter have been attributed to reactive mineral surface
sites that sorb organic species and cause inaccessibility due to physical isolation and …

Mineral binding is a major mechanism for soil carbon (C) stabilization, and mineral
availability for C binding critically affects C storage. Yet, the mechanisms regulating mineral …

Iron (Fe)-bearing mineral phases contribute disproportionately to adsorption of soil organic
matter (SOM) due to their elevated chemical reactivity and specific surface area (SSA) …

Understanding the fate and transport of engineered and naturally-occurring nanoparticles is
vital to predicting their ecological and toxicological impacts. Much of the current literature …

While the importance of organic matter adsorption onto reactive iron-bearing mineral
surfaces to carbon stabilization in soils and sediments has been well-established …

Coprecipitation of Fe/Cr hydroxides with natural organic matter (NOM) is an important
pathway for Cr immobilization. However, the role of NOM in coprecipitation is still …