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 …

Stream denitrification is thought to be enhanced by hyporheic transport but there is little
direct evidence from the field. To investigate at a field site, we injected 15NO3−, Br …

In the last decade, as computing power has increased, there has been an explosion in the
use of eddy-resolving numerical methods in the engineering, earth and environmental …

The fate of biologically available nitrogen (N) and carbon (C) in stream ecosystems is
controlled by the coupling of physical transport and biogeochemical reaction kinetics …

In this chapter, the authors provide a comprehensive analysis and synthesis of the
interactions between important drivers and controls of hyporheic exchange and …

Work over the last decade has documented methods for estimating fluxes between streams
and streambeds from time series of temperature at two depths in the streambed. We present …

Exchange of water and solutes across the stream‐sediment interface is an important control
for biogeochemical transformations in the hyporheic zone (HZ). In this paper, we investigate …

Hyporheic flows, which stem from the interaction between stream flow and bedform,
transport solute‐laden surface waters into the streambed sediments, where reactive solutes …

Discharge varies in space and time, driving hyporheic exchange processes in river corridors
that affect biogeochemical cycling and ultimately control the dynamics of biogeochemical hot …

Stream channel morphology from grain‐scale roughness to large meanders drives
hyporheic exchange flow. In practice, it is difficult to model hyporheic flow over the wide …