Most rivers exchange water with surrounding aquifers,. Where groundwater levels lie below
nearby streams, streamwater can infiltrate through the streambed, reducing streamflow and …

The streambed constitutes the physical interface between the surface and the subsurface of
a stream. Across all spatial scales, the physical properties of the streambed control surface …

The estimation and modeling of streambed hydraulic conductivity (K) is an emerging interest
due to its connection to water quality, aquatic habitat, and groundwater recharge. Existing …

Streambed hydraulic conductivity is one of the main factors controlling variability in surface
water‐groundwater interactions, but only few studies aim at quantifying its spatial and …

Streambed substrates have pervasive effects on stream biodiversity and biogeochemistry.
The excessive input of fine sediments in streams and the subsequent alteration of the …

Fine particle deposition and streambed clogging affect many ecological and biogeochemical
processes, but little is known about the effects of groundwater flow into and out of rivers on …

In gaining streams, groundwater seeps out into the streams. In losing streams, stream water
moves into groundwater systems. The flow moving through the streambed sediments under …

Colloids moving from the stream into the hyporheic zone may have a negative impact on
aquatic ecosystems as they are potential contaminants or carriers of contaminants …

As a transitional zone between terrestrial and aquatic ecosystems, riparian ecosystems are
critical in maintaining the health of river-ways and watersheds, and particularly sensitive to …

The change of vertical hydraulic conductivity (K^ sub v^) before and after a flood season is
crucial in understanding the long-term temporal variation of streambed permeability …