The high demand and extensive exploitation of uranium resources resulted in the ubiquity
and high detection levels of uranium mineral-related substances in various environment …

Despite decades of research, we lack an accurate framework to predict and manage
hydrologic exchange in the river corridor and the associated ecosystem services and …

Environmental transitions often result in resource mixtures that overcome limitations to
microbial metabolism, resulting in biogeochemical hotspots and moments. Riverine systems …

The hyporheic corridor (HC) encompasses the river–groundwater continuum, where the
mixing of groundwater (GW) with river water (RW) in the HC can stimulate biogeochemical …

Dam operations commonly cause large, frequent fluctuations in river stage, which persist for
long distances downstream. The stage fluctuations force river water into and out of the …

Hyporheic exchanges in riparian zones induced by stream stage fluctuations, referred to as
bank storage, can influence contaminant transport and transformation when mixing of …

We examine subsurface uranium (U) plumes at two US Department of Energy sites that are
located near large river systems and are influenced by groundwater–river hydrologic …

The hyporheic zone is the interface beneath and adjacent to streams and rivers where
surface water and groundwater interact. The hyporheic zone presents unique conditions for …

Hyporheic zones (HZ) are active biogeochemical regions where groundwater and surface
water mix. N transformations in HZ sediments were investigated in columns with a focus on …

Identifying groundwater (GW)–surface water (SW) interactions in riparian zones is important
for assessing the transport pathways of pollutants and all potential biochemical processes …