In spite of trying to understand processes in the same spatial domain, the catchment
hydrology and water quality scientific communities are relatively disconnected and so are …

River corridors integrate the active channels, geomorphic floodplain and riparian areas, and
hyporheic zone while receiving inputs from the uplands and groundwater and exchanging …

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 …

Here we review the fundamental interactions between hydrology and the cycling of carbon
(C) and nitrogen (N) in terrestrial and stream ecosystems. We organize this review around …

Water tracks are zones of high soil moisture that route water downslope over the ice table in
polar environments. We present physical, hydrological, and geochemical evidence collected …

There is a growing recognition of the importance of connections between streams and
adjacent alluvial aquifers. The exchange of water, mass, and energy between these …

The stream tracer technique has been widely used as a method of characterizing hyporheic
exchange in stream-catchment studies, commonly incorporating the use of the numerical …

Studies of hyporheic exchange flows have identified physical features of channels that
control exchange flow at the channel unit scale, namely slope breaks in the longitudinal …

We tested the hypothesis that reservoirs with low water residence time and autochthonous
production influence river biogeochemistry in eutrophied river systems draining cultivated …

Hyporheic zones are of broad interest, given their location at the interface between surface
and groundwaters, numerous ecological functions, and location as a zone of interdependent …