A rheological approach of muddy debris flows is presented for environmental engineering and risk assessment purposes. The debris flow is viewed as a hyperconcentrated suspension of non brownian solid particles. Experimental and theoretical studies are presented versus the concentration. The experimental work generally consists in generating the flow of well characterized suspensions by a dam break. Then, the time evolution of the front as well as that of the stage at given position are accurately determined. On the theoretical framework, the viscous equations of motion of the suspension are written with the shallow water approximation, and the asymptotic solution in a non dimensional form is derived. Finally, the experimental and the theore...
The goal of this article is to study in detail the problems related to the rheometry of debris flow...
The main characteristics of geological flows such as debris flows, avalanches and lahars is due to t...
Abstract:- Debris flows such as avalanches and lahars differ from the classical dam-break problem of...
To predict debris flow dynamics a numerical model, based on 1D De Saint Venant (SV) equations, was de...
Debris and hyper-concentrated flows are among the most destructive of all water – related disasters....
Mud flows and debris flows are natural phenomena representing serious hazard for population and stru...
Debris and hyper-concentrated flows are among the most destructive of all water-related disasters. T...
The paper describes the development and the assessment of a numerical model for the simulation of de...
The paper describes the development and the assessment of a numerical model for the simulation of de...
AbstractThe paper describes the development and the assessment of a numerical model for the simulati...
We develop a physical model of the dam-break flow of fine non-cohesive particles initially fluidized...
To predict flood and debris flow dynamics a numerical model,based on 1D De Saint Venant (SV) equatio...
To predict floods and debris flow dynamics a numerical model, based on 1D De Saint Venant (SV) equat...
To predict floods and debris flow dynamics a numerical model,based on 1D De saint Venant (SV) equati...
Mud flows represent one of the major causes of natural hazards in mountain regions. Similarly to deb...
The goal of this article is to study in detail the problems related to the rheometry of debris flow...
The main characteristics of geological flows such as debris flows, avalanches and lahars is due to t...
Abstract:- Debris flows such as avalanches and lahars differ from the classical dam-break problem of...
To predict debris flow dynamics a numerical model, based on 1D De Saint Venant (SV) equations, was de...
Debris and hyper-concentrated flows are among the most destructive of all water – related disasters....
Mud flows and debris flows are natural phenomena representing serious hazard for population and stru...
Debris and hyper-concentrated flows are among the most destructive of all water-related disasters. T...
The paper describes the development and the assessment of a numerical model for the simulation of de...
The paper describes the development and the assessment of a numerical model for the simulation of de...
AbstractThe paper describes the development and the assessment of a numerical model for the simulati...
We develop a physical model of the dam-break flow of fine non-cohesive particles initially fluidized...
To predict flood and debris flow dynamics a numerical model,based on 1D De Saint Venant (SV) equatio...
To predict floods and debris flow dynamics a numerical model, based on 1D De Saint Venant (SV) equat...
To predict floods and debris flow dynamics a numerical model,based on 1D De saint Venant (SV) equati...
Mud flows represent one of the major causes of natural hazards in mountain regions. Similarly to deb...
The goal of this article is to study in detail the problems related to the rheometry of debris flow...
The main characteristics of geological flows such as debris flows, avalanches and lahars is due to t...
Abstract:- Debris flows such as avalanches and lahars differ from the classical dam-break problem of...