Natural aquatic systems undergo fluctuating redox conditions due to microbial activities,
varying water saturation levels, and nutrient dynamics. With fluctuating redox conditions …

Redox state fluctuations are a primary mechanism controlling the mobilization of trace
metals in soils. However, underlying lithology may modulate the effect that redox fluctuations …

Aerobic and anaerobic incubation experiments on a wetland soil samples were used to
assess the respective roles of organic matter (OM) release, Fe-oxyhydroxides reduction and …

Increased variability in lake and river water levels associated with changing climate could
impact the fate and effects of metals in redox‐sensitive sediments through the alteration of …

Understanding the effect of soil redox conditions on contaminant dynamics is of significant
importance for evaluating their lability, mobility and potential transfer to other environmental …

Wetlands play an important role in determining the water quality of streams and are
generally considered to act as a sink for many reactive species. However, retention of …

Studies about the mobilization of potentially toxic elements (PTEs) in deltaic soils can be
challenging, provide critical information on assessing the potential risk and fate of these …

The subterranean estuary (STE) has been historically defined in terms of the mixing of saline
and fresh water, in an analogy to surface estuaries. However, redox gradients are also a …

Soil zinc contamination is a major threat to water quality and sensitive ecosystems. While Zn
itself is not redox-active in soils, transitions in soil redox conditions may promote …

Acid sulfate soils (ASS) contain substantial quantities of iron sulfide minerals or the oxidation
reaction products of these sulfidic minerals. Transformation of iron (Fe) and sulfur (S) …