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 …

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 …

Reactive oxygen species (ROS) play key roles in driving biogeochemical processes. Recent
studies have revealed nonphotochemical electron transfer from redox-active substances …

We report an unrecognized, tidal source of reactive oxygen species (ROS). Using a newly
developed ROS-trapping gel film, we observed hot spots for ROS generation within∼ 2.5 …

Iron (hydr) oxides as a kind of natural mineral actively participate in the transformation of
organic pollutants, but there is a large knowledge gap in their impacts on photochemical …

Soil organic carbon (SOC) is a crucial component that significantly affects the soil fertility,
soil remediation, and carbon sequestration. Here, we review the redox-induced …

Microbially mediated iron redox processes are of great significance in the biogeochemical
cycles of elements, which are often coupled with soil organic matter (SOM) in the …

Peroxydisulfate (PDS) is widely used in groundwater remediation systems. Previous studies
investigated its activation by natural sediments under oxic conditions. However, the role of …

The redox activity of Fe-bearing minerals is coupled with the transformation of organic matter
(OM) in redox dynamic environments, but the underlying mechanism remains unclear. In this …

Dark formation of hydroxyl radicals (• OH) from soil/sediment oxygenation has been
increasingly reported, and solid Fe (II) is considered as the main electron donor for O2 …