Results 71 to 80 of about 5,645 (215)
Physical and biological controls on fine sediment transport and storage in rivers [PDF]
Excess fine sediment, comprising particles
Casas-Mulet, R. +10 more
core +3 more sources
ABSTRACT Assessing spatial and temporal variability of clogging in gravel‐bed rivers is challenging because field methods typically rely on labor‐intensive measurements of fine‐sediment content, porosity, or hydraulic conductivity. Clogging is also highly dynamic, driven by hydro‐sedimentary conditions; yet few studies have examined it at large scales ...
D. Hernandez, B. Camenen, A. Bonnefoy
wiley +1 more source
It is well known that land surface topography governs surface–groundwater interactions under some circumstances and can be separated in a Fourier-series spectrum that provides an exact analytical solution of both the surface and the underlying three ...
Bowen He, Qun Guan
doaj +1 more source
Temporal responses of groundwater-surface water exchange to successive storm events [PDF]
Groundwater-surface water exchange within the hyporheic zone is widely recognized as a key mechanism controlling the fate of nutrients within catchments.
Andrew Binley +47 more
core +1 more source
Abstract Trace organic compounds (TrOCs) in lotic systems pose risks for ecosystem and human health. TrOCs can enter groundwater along losing river sections, yet little is known about the spatial extent of infiltration zones and the biogeochemical factors controlling the spatial variability of TrOC reactivity and removal, particularly along river‐to ...
Jonas L. Schaper +6 more
wiley +1 more source
Hyporheic zones are commonly regarded as resilient and enduring interfaces between groundwater and surface water in river corridors. In particular, bedform‐induced advective pumping hyporheic exchange (bedform‐induced exchange) is often perceived as a ...
L. Wu +3 more
doaj +1 more source
This study tested the applicability of a novel drive‐point multilevel system (DP‐MLS) for measuring head profiles and characterizing contaminant concentrations in the hyporheic zone of a well‐studied temperate region effluent dominated stream (EDS).
Jessica R. Meyer +4 more
wiley +1 more source
Hydrodynamics of Four Moments in the Life of a Floodplain Forest in Compound Channels
Abstract Natural rivers often function as compound channels, comprising main channel and floodplain. Flow dynamics in these systems, particularly during floods, are influenced by factors such as vegetation, and flood intensity. Floodplain vegetation significantly modifies flow structures, affecting hydraulic conveyance and ecological functions.
Luiz E. D. de Oliveira +6 more
wiley +1 more source
Quantifying the impact of the stream-aquifer interaction on the surface-subsurface exchange [PDF]
The exchange of oxygen and nutrients between the well-aerated stream water and the subsurface water is crucial for the biochemical conditions of the hyporheic zone, i.e., the interface region between the stream and the deep aquifer. The hyporheic zone is
Boano, Fulvio +2 more
core
Controls on spatial and temporal variations in sand delivery to salmonid spawning riffles [PDF]
Fine sediment infiltration into gravel interstices is known to be detrimental to incubating salmonid embryos. Infiltration into spawning riffles can show large spatial variations at the scale of a morphological unit and over time, with significant ...
Milan, David
core +1 more source

