Fifty years of hyporheic zone research have shown the important role played by the
hyporheic zone as an interface between groundwater and surface waters. However, it is only …

An understanding of the transport and survival of microbial pathogens (pathogens hereafter)
in agricultural settings is needed to assess the risk of pathogen contamination to water and …

The hyporheic zone, defined by shallow subsurface pathways through river beds and banks
beginning and ending at the river, is an integral and unique component of fluvial systems. It …

Abstract Low-gradient fluvial landscapes (1–50 cm km− 1) occupy diverse settings (inland,
tidal, and deltaic wetlands, large-river floodplains, lowland streams) but share many …

Hyporheic flow in streams has typically been studied separately from geomorphic
processes. We investigated interactions between bed mobility and dynamic hyporheic …

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 …

Hyporheic hydrodynamics are a control on stream ecosystems, yet we lack a thorough
understanding of catchment controls on these flow paths, including valley constraint and …

The accumulation of discharge along a stream valley is frequently assumed to be the
primary control on solute transport processes. Relationships of both increasing and …

Although most field and modeling studies of river corridor exchange have been conducted at
scales ranging from tens to hundreds of meters, results of these studies are used to predict …

The hyporheic zone (HZ), where surface water and groundwater interact in sediments
beneath streams, presents unique conditions for nutrient dynamics, such as carbon and …