Hyporheic exchange has been hypothesized to have basin‐scale consequences; however,
predictions throughout river networks are limited by available geomorphic and …

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 …

River water circulates vertically through the river bed and laterally through bank sediments,,,.
This hyporheic exchange brings river water into contact with microbes in the adjacent …

In this chapter, the authors provide a comprehensive analysis and synthesis of the
interactions between important drivers and controls of hyporheic exchange and …

Hyporheic hydrodynamics are a control on stream ecosystems, yet we lack a thorough
understanding of catchment controls on these flow paths, including valley constraint and …

Many hyporheic papers state that the hyporheic zone is a critical component of stream
ecosystems, and many of these papers focus on the biogeochemical effects of the hyporheic …

Heterogeneity in hydraulic conductivity (K) and channel morphology both control surface
water‐groundwater exchange (hyporheic exchange), which influences stream ecosystem …

Although surface water and groundwater are increasingly referred to as one resource, there
remain environmental and ecosystem needs to study the 10 m to 1 km reach scale as one …

The relative roles of dynamic hydrologic forcing and geomorphology as controls on the
timescales and magnitudes of stream‐aquifer exchange and hyporheic flow paths are …

Stream channel morphology from grain‐scale roughness to large meanders drives
hyporheic exchange flow. In practice, it is difficult to model hyporheic flow over the wide …