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 …

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 …

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

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 …

Characterizing the collective behavior of particle transport on the Earth surface is a key
ingredient in describing landscape evolution. We seek equations that capture essential …

Hyporheic flow can be extremely variable in space and time, and our understanding of
complicated flow systems, such as exchange around small dams, has generally been limited …

Low river flows are commonly controlled by river‐aquifer exchange, the magnitude of which
is governed by hydraulic properties of both aquifer and aquitard materials beneath the river …

Rivers are the great shapers of terrestrial landscapes. Very few points on Earth above sea
level do not lie within a drainage basin. Even points distant from the nearest channel are …

We propose that the mechanisms driving hyporheic exchange vary systematically with
different channel morphologies and associated fluvial processes that occur in mountain …

Recent observations reveal a paradox of anaerobic respiration occurring in seemingly oxic‐
saturated sediments. Here we demonstrate a residence time‐based explanation for this …