Fe (hydr) oxides and organic matter (OM) are two of the main active substances ubiquitously
occurring in natural environments. Fe (hydr) oxides rarely exist as a discrete component in …

Dissolved organic matter (DOM), the most reactive fraction of forest soil organic matter, is
increasingly impacted by wildfires worldwide. However, few studies have quantified the …

Sustainable engineering and management of hydromorphic arable soils need deep
knowledge about the redox-mediated interactions between nutrients and soil colloids …

Colloidal organo–mineral associations contribute to soil organic matter (OM) preservation
and mainly occur in two forms:(i) as water-dispersible colloids that are potentially mobile …

Colloid generation, stability, and transport are important processes that can significantly
influence the fate and transport of nutrients and contaminants in environmental systems …

Black carbon such as biochar has been shown to possess electron storage capacity (ESC),
which enables black carbon to store and reversibly exchange electrons with its …

Mineral-associated organic matter (MAOM) is the largest soil organic carbon (OC) pool with
the longest turnover. MAOM is expected to have relatively little sensitivity to climate change …

Sediment interfaces in alluvial aquifers have a disproportionately large influence on
biogeochemical activity and, therefore, on groundwater quality. Previous work showed that …

In this study, the combined forms of Pb in Cladophora rupestris (L.)(C. rupestris) were
investigated via X-ray photoelectron spectroscopy (XPS) and nuclear magnetic resonance …

The onset of oxic-anoxic events in soil induces biogeochemical processes that may have
profound influences on the fate and transport of soil organic carbon (OC). An 18-wk long …