Reduction–oxidation (redox) reactions underlie essentially all biogeochemical cycles. Like
most soil properties and processes, redox is spatiotemporally heterogeneous. However …

Groundwater uranium (U) concentrations have been measured above the US EPA
maximum contaminant level (30 μg/L) in many US aquifers, including in areas not …

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

Although the mobility of arsenic (As) and cadmium (Cd) in soils during the flooding-drainage
process has been intensively studied, predicting their dissolution among various soils still …

The impact of dam on the distribution and transformation of elements in riparian zones has
received increasing attention. However, previous studies mainly focused on the site scale …

Aquifer groundwater quality is largely controlled by sediment composition and physical
heterogeneity, which commonly sustains a unique redox gradient pattern. Attenuation of …

Sedimentary interfaces between contrasting hydrogeological facies in alluvial aquifers drive
the development of biogeochemical interfaces that influence subsurface and surface water …

Redox conditions play a decisive role in regulating contaminant and nutrient transformation
in groundwater. Here we quantitatively described and interpreted the temporal and spatial …

Increased periods of bottom water anoxia in deep temperate lakes due to decreasing
frequency and depth of water column mixing in a warming climate may result in the reductive …

Anoxic microsites, zones of oxygen depletion in otherwise well-aerated soils, serve as
prominent controls on several biogeochemical cycles (eg, carbon, nitrogen, iron). However …