Soils and sediments are major reservoirs of organic matter (OM), whose dynamic turnover
has a major impact on carbon cycling and global climate. OM in soils and sediments is …

Soil, the largest terrestrial carbon reservoir, is central to climate change and relevant
feedback to environmental health. Minerals are the essential components that contribute to …

Iron (oxyhydr) oxides and organic matter (OM) are intimately associated in natural
environments, and their fate might be linked to sulfur during sulfidation–reoxidation cycling …

Current understanding of soil carbon dynamics suggests that plant litter quality and soil
mineralogy control the formation of mineral-associated soil organic carbon (SOC). Due to …

The association of poorly crystalline iron (hydr) oxides with organic matter (OM), such as
extracellular polymeric substances (EPS), exerts a profound effect on Fe and C cycles in …

Iron (oxyhydr) oxides, especially ferrihydrite (Fh), abundant in the natural environment, are
frequently applied in controlling the migration of heavy metals like antimony (Sb) and …

Reactive iron (Fe R) plays an important role in the preservation of organic carbon (OC) in
coastal sediments, yet changes in the OC bound to Fe R (OC-Fe R), during transport and …

Phosphate and dissolved organic matter (DOM) mediate the crystalline transformation of
ferrihydrite catalyzed by Fe (II) in subsurface environments such as soils and groundwater …

Adsorption fractionation of dissolved organic matter (DOM) induced by soil minerals is a
common geochemical process, which has been widely documented on natural DOM …

The mobility of chromium (Cr) is controlled by minerals, especially iron (oxyhydr) oxides. The
influence of organic carbon (OC) on the mobility and fate of Cr (VI) during Fe (II)-induced …