The authors discuss interaction between the river flow and the formation of the river bed as a single dynamic self-regulating system. Changes in the physical-mechanical properties of river bed sediments occurring under the influence of natural and anthropogenic factors, and the impact of these changes produced on the processes of sedimentation and erosion of river channels are considered in the article. Free and constrained precipitation of particles of different density, shape and size are analyzed. A universal formula of the hydraulic resistance coefficient, applicable to particles in the course of their sedimentation into the liquid, which takes account of both the front resistance and the surface friction, is proposed. The authors also ...
[1] Incipient motion of particles on a river bed can, in principle, be understood and predicted from...
A physically based, analytical model of river response is developed. RIVERMOD was designed to aid in...
Vegetations are often used in rivers and streams to help as a control with bank stability and also a...
Alluvial rivers, insofar as they transport the material of which their channels are composed, posses...
The article describes the active equilibrium motion of bed forms, which occurs in rivers during high...
The morphology of alluvial river channels is a consequence of complex interaction among a number of ...
Rivers consist of a collection of several tributaries, and these tributaries are formed mainly in mo...
Natural rivers tend to adjust their plane shape and longitudinal profile in order to assume a config...
The paper presents recommendations for using the results obtained in sediment transport simulation a...
The article presents the main results of substantiating the materials used when conducting experimen...
Experiments were made to determine the relative effects on the friction factor of a flow of the susp...
In a river channel the prevailing bedload transport rate is not solely independent upon hydraulic pa...
International audienceThis presentation concerns the modelling of the transport mode and the suspens...
The problem of sedimentation in rivers has become a familiar phenomenon in the maintenance of a rive...
An experimental investigation was made of the friction characteristics of streams with sediment load...
[1] Incipient motion of particles on a river bed can, in principle, be understood and predicted from...
A physically based, analytical model of river response is developed. RIVERMOD was designed to aid in...
Vegetations are often used in rivers and streams to help as a control with bank stability and also a...
Alluvial rivers, insofar as they transport the material of which their channels are composed, posses...
The article describes the active equilibrium motion of bed forms, which occurs in rivers during high...
The morphology of alluvial river channels is a consequence of complex interaction among a number of ...
Rivers consist of a collection of several tributaries, and these tributaries are formed mainly in mo...
Natural rivers tend to adjust their plane shape and longitudinal profile in order to assume a config...
The paper presents recommendations for using the results obtained in sediment transport simulation a...
The article presents the main results of substantiating the materials used when conducting experimen...
Experiments were made to determine the relative effects on the friction factor of a flow of the susp...
In a river channel the prevailing bedload transport rate is not solely independent upon hydraulic pa...
International audienceThis presentation concerns the modelling of the transport mode and the suspens...
The problem of sedimentation in rivers has become a familiar phenomenon in the maintenance of a rive...
An experimental investigation was made of the friction characteristics of streams with sediment load...
[1] Incipient motion of particles on a river bed can, in principle, be understood and predicted from...
A physically based, analytical model of river response is developed. RIVERMOD was designed to aid in...
Vegetations are often used in rivers and streams to help as a control with bank stability and also a...