Previously regarded as the passive drains of watersheds, over the past 50 years, rivers have
progressively been recognized as being actively connected with off‐channel environments …

Floodplains perform diverse functions, including attenuation of fluxes of water, solutes, and
particulate material. Critical details of floodplain storage including magnitude, duration, and …

Nitrate contamination in ground-and surface water is a persistent problem in countries with
intense agriculture. The transition zone between rivers and their riparian aquifers, where …

Hydrologic connectivity is the linkage of separate regions of a catchment via water flow.
Knowledge of hillslope–stream connectivity (both at the surface and in the subsurface) is …

Watersheds are three‐dimensional hydrologic systems where the longitudinal
expansion/contraction of stream networks, vertical connection/disconnection between …

To obtain a better understanding of water's journey from the hillslope to the stream, water
level time series from 26 groundwater wells in a hillslope–riparian study area in the Panola …

Understanding near‐stream groundwater dynamics and flow directions is important for
predicting hillslope‐stream connectivity, streamflow generation, and hydrologic controls of …

Coupled hydrological-hydrogeological models, emphasising the importance of the stream–
aquifer interface, are more and more used in hydrological sciences for pluri-disciplinary …

As water grows scarcer in semiarid and arid regions around the world, new tools are needed
to quantify fluxes of water and chemicals between aquifers and rivers. In this study, we …

The biogeochemical functioning of stream ecosystems is heavily dependent on water and
water‐borne nutrient fluxes between the stream itself and the streambed and banks (ie, the …