Blueprint for a coupled model of sedimentology, hydrology, and hydrogeology in streambeds
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 …
a stream. Across all spatial scales, the physical properties of the streambed control surface …
Modeling riverbed elevation and bedload tracer transport resting times using fractional Laplace motion
Riverbed elevations play a crucial role in sediment transport and flow resistance, making it
essential to understand and quantify their effects. This knowledge is vital for various fields …
essential to understand and quantify their effects. This knowledge is vital for various fields …
Autogenic formation of bimodal grain size distributions in rivers and its contribution to gravel‐sand transitions
Riverbeds often fine downstream, with a gravel‐bedded reach, a relatively abrupt gravel‐
sand transition (GST), and a sand‐bedded reach. Underlying this behavior, bed grain size …
sand transition (GST), and a sand‐bedded reach. Underlying this behavior, bed grain size …
Geomorphic and ecological consequences of riprap placement in river systems
Riprap, consisting of large boulders or concrete blocks, is extensively used to stabilize
streambanks and to inhibit lateral erosion of rivers, yet its effect on river morphology and its …
streambanks and to inhibit lateral erosion of rivers, yet its effect on river morphology and its …
Controls on fluvial sediment evacuation following an earthquake-triggered landslide: Observations from LiDAR time series
Catastrophic sediment overloading of mountain streams in response to coseismic
landsliding causes river systems to fundamentally reorganize their morphology and …
landsliding causes river systems to fundamentally reorganize their morphology and …
A model to predict the evolution of a gravel bed river under an imposed cyclic hydrograph and its application to the Trinity River
E Viparelli, D Gaeuman, P Wilcock… - Water Resources …, 2011 - Wiley Online Library
Major changes in the morphology of the Trinity River in California, such as narrowing of the
cross section and sedimentation of fine sediment in pools, occurred after the closure of a …
cross section and sedimentation of fine sediment in pools, occurred after the closure of a …
Well-balanced numerical modelling of non-uniform sediment transport in alluvial rivers
H Qian, Z Cao, G Pender, H Liu, P Hu - International Journal of Sediment …, 2015 - Elsevier
The last two decades have witnessed the development and application of well-balanced
numerical models for shallow flows in natural rivers. However, until now there have been no …
numerical models for shallow flows in natural rivers. However, until now there have been no …
Gravel‐bed river evolution in earthquake‐prone regions subject to cycled hydrographs and repeated sediment pulses
Sediment often enters rivers in the form of sediment pulses associated with landslides and
debris flows. This is particularly so in gravel‐bed rivers in earthquake‐prone mountain …
debris flows. This is particularly so in gravel‐bed rivers in earthquake‐prone mountain …
Mathematical analysis of the S aint‐V enant‐H irano model for mixed‐sediment morphodynamics
Sediment of different size are transported in rivers under the action of flow. The first and still
most popular sediment continuity model able to deal with mixed sediment is the so‐called …
most popular sediment continuity model able to deal with mixed sediment is the so‐called …
Morphodynamic model of the lower Yellow River: Flux or entrainment form for sediment mass conservation?
Sediment mass conservation is a key factor that constrains river morphodynamic processes.
In most models of river morphodynamics, sediment mass conservation is described by the …
In most models of river morphodynamics, sediment mass conservation is described by the …