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 …

We report the first laboratory simulations of hyporheic exchange in gravel pool‐riffle
channels, which are characterized by coarse sediment, steep slopes, and three …

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 …

Hyporheic exchange is the mixing of surface and shallow subsurface water through porous
sediment surrounding a river and is driven by spatial and temporal variations in channel …

Metals pollution in surface waters from point and non-point sources (NPS) is a widespread
problem in the United States and worldwide (Lofts et al., 2007; USEPA, 2007). In the western …

Stream‐tracer injections were used to examine the effect of channel morphology and
changing stream discharge on hyporheic exchange flows. Direct observations were made …

The disciplines of geomorphology, hydrology, and hydrogeology have had a marked
influence on the evolution of systems thinking in stream ecology. The River Continuum …

Shallow benthic biolayers at the top of the streambed are believed to be places of enhanced
biogeochemical turnover within the hyporheic zone. They can be investigated by reactive …

The interaction between surface and subsurface water has a crucial influence on the
biochemistry of stream environments. Even though the river discharge and the flow …

The transport of solutes in rivers is influenced by the exchange of water between the river
and the underlying hyporheic zone. The residence times of solutes in the hyporheic zone …