Driven by the need for integrated management of groundwater (GW) and surface water
(SW), quantification of GW–SW interactions and associated contaminant transport has …

The ecological activities within the hyporheic zone (HZ) heavily rely on water flow dynamics.
The arrangement of the hyporheic community is influenced significantly by the hydrological …

Common approaches for characterizing streambed architecture, and its influence on
groundwater-surface water (GW-SW) exchanges, are generally limited by their invasiveness …

Hyporheic zone (HZ) systems have a natural purification capacity, and they are commonly
used to provide high quality drinking water. However, the presence of organic contaminants …

Rivers have a significant role in global carbon and nitrogen cycles, serving as a nexus for
nutrient transport between terrestrial and marine ecosystems. Although rivers have a small …

The fate of nutrients and contaminants in fluvial ecosystems is strongly affected by the
mixing dynamics between surface water and groundwater within the hyporheic zone …

Dissolved oxygen (DO) is critical for aquatic ecosystems, however, few studies have focused
on the long‐term DO dynamics in hyporheic zones, which are a function of both transport …

Attenuation of groundwater ammonium (NH 4+) is expected to occur through redox reaction
and adsorption of the riverbank. Previous studies determined that NH 4+ mostly degraded …

The effects of regional (hydrogeology and geomorphology) and local (sediment and
hydrology) characteristics on hyporheic assemblages were studied along a 40-km reach of a …

Ammonium has detrimental effects on the survival and physiology of freshwater
invertebrates, however, the effects of ammonium on the functionality of hyporheic …