In this paper we analyze the Hirano active layer model used in mixed sediment river morphodynamics concerning its ill-posedness. Ill-posedness causes the solution to be unstable to short-wave perturbations. This implies that the solution presents spurious oscillations, the amplitude of which depends on the domain discretization. Ill-posedness not only produces physically unrealistic results but may also cause failure of numerical simulations. By considering a two-fraction sediment mixture we obtain analytical expressions for the mathematical characterization of the model. Using these we show that the ill-posed domain is larger than what was found in previous analyses, not only comprising cases of bed degradation into a substrate finer than ...
The stability of a uniform flow above an erodible bed composed of a bimodal mixture of sediments is ...
Sediment nourishments have become an increasingly attractive alternative to deal with continuous bed...
In Chapter I a derivation of the equations and an extension of the mathematical model will be carrie...
<p>In this paper we analyze the Hirano active layer model used in mixed sediment river morphodynamic...
A two-dimensional model describing river morphodynamic processes under mixed-size sediment condition...
A two-dimensional model describing river morphodynamic processes under mixed-size sediment condition...
The active layer model (Hirano, 1971) is frequently used for modeling mixed-size sediment river morp...
The mixed-size character of sediment is a necessary property to ex- plain physical phenomena such as...
The set of equations used in modelling river morphodynamics needs to be (at least) wellposed to be...
A notable drawback in mixed-size sediment morphodynamic modeling is the fact that the most commonly ...
Abstract Sediment of different size are transported in rivers under the action of flow. The first an...
We present an accurate numerical approximation to the Saint-Venant-Hirano model for mixed-sediment m...
River bed degradation is sometimes counteracted with nourishment of sediment material. Numerical mod...
Modelling the morphodynamic evolution of rivers due to flow-driven sediment transport requires the a...
This paper presents an assessment of the strengths and weaknesses of four sediment continuity models...
The stability of a uniform flow above an erodible bed composed of a bimodal mixture of sediments is ...
Sediment nourishments have become an increasingly attractive alternative to deal with continuous bed...
In Chapter I a derivation of the equations and an extension of the mathematical model will be carrie...
<p>In this paper we analyze the Hirano active layer model used in mixed sediment river morphodynamic...
A two-dimensional model describing river morphodynamic processes under mixed-size sediment condition...
A two-dimensional model describing river morphodynamic processes under mixed-size sediment condition...
The active layer model (Hirano, 1971) is frequently used for modeling mixed-size sediment river morp...
The mixed-size character of sediment is a necessary property to ex- plain physical phenomena such as...
The set of equations used in modelling river morphodynamics needs to be (at least) wellposed to be...
A notable drawback in mixed-size sediment morphodynamic modeling is the fact that the most commonly ...
Abstract Sediment of different size are transported in rivers under the action of flow. The first an...
We present an accurate numerical approximation to the Saint-Venant-Hirano model for mixed-sediment m...
River bed degradation is sometimes counteracted with nourishment of sediment material. Numerical mod...
Modelling the morphodynamic evolution of rivers due to flow-driven sediment transport requires the a...
This paper presents an assessment of the strengths and weaknesses of four sediment continuity models...
The stability of a uniform flow above an erodible bed composed of a bimodal mixture of sediments is ...
Sediment nourishments have become an increasingly attractive alternative to deal with continuous bed...
In Chapter I a derivation of the equations and an extension of the mathematical model will be carrie...