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 …

Fine sediment represents an important part of the solid flux of rivers. Due to the size of these
particles, they are often transported as suspended load. They gradually fill the pores of the …

Rivers are important ecosystems under continuous anthropogenic stresses. The hyporheic
zone is a ubiquitous, reactive interface between the main channel and its surrounding …

Increasing nitrogen concentrations in the world's major rivers have led to over-fertilization of
sensitive downstream waters,,,. Flow through channel bed and bank sediments acts to …

The interface between groundwater and surface water within riverine/riparian ecosystems—
the hyporheic zone (HZ)—is experiencing a rapid growth of research interest from a range of …

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

Hyporheic exchange has been hypothesized to have basin‐scale consequences; however,
predictions throughout river networks are limited by available geomorphic and …

It is necessary to improve our understanding of the exchange of dissolved constituents
between surface and subsurface waters in river systems in order to better evaluate the fate …

Downstream flow in rivers is repeatedly delayed by hydrologic exchange with off‐channel
storage zones where biogeochemical processing occurs. We present a dimensionless …

The exchange of water between the surface and subsurface environments plays a crucial
role in hydrological, biogeochemical, and ecological processes. The exchange of water is …