Particle travel length is one of the main dimensions of bedload and strongly influences river morpho-dynamics, particularly when exploring the interactions between sediment transport and channel morphology. This process has been traditionally studied by using tagged stones that allow tracking the movement experienced by individual grains during transport episodes. In this paper, we relate measured particle travel lengths to flow metrics and river channel parameters. First, we link the event-based bedload volumes to the active-layer dimensions, and the product between the average bedload rates and the duration of competent flows. We then hypothesize that travel length depends on channel width, surface grain-size, particle size, bed structure...
Bedload transport has been studied in Ardenne rivers using different methods. Experiments with marke...
In order to predict the response of mountain streams to perturbations caused by climate and land use...
Evolution of bed material mobility and bedload grain size distributions under a range of discharges ...
Particle travel length is one of the main dimensions of bedload and strongly influences river morpho...
Particle travel length is one of the main dimensions of bedload and strongly influences river morpho...
Data from tracer experiments were compiled and analysed in order to explore the role of geomorpholog...
The path length (downstream displacement over a given time period) of individual bed particles in gr...
[Departement_IRSTEA]EauxInternational audienceData from tracer experiments were compiled and analyse...
Understanding the mechanics of bed load at the flood scale is necessary to link hydrology to landsca...
Streambed mobility in gravel-bed rivers is largely controlled by the rate at which particles with di...
[1] Previous work highlights the need for data collection to identify appropriate models for tempora...
Transport of coarse sediment in gravel-bed streams alternates between mobile and immobile phases. M...
International audienceThis work analysed the factors controling the spatiotemporal variability in be...
Understanding the mechanics of bed load at the flood scale is necessary to link hydrology to lands...
Bedload transport has been studied in Ardenne rivers using different methods. Experiments with marke...
In order to predict the response of mountain streams to perturbations caused by climate and land use...
Evolution of bed material mobility and bedload grain size distributions under a range of discharges ...
Particle travel length is one of the main dimensions of bedload and strongly influences river morpho...
Particle travel length is one of the main dimensions of bedload and strongly influences river morpho...
Data from tracer experiments were compiled and analysed in order to explore the role of geomorpholog...
The path length (downstream displacement over a given time period) of individual bed particles in gr...
[Departement_IRSTEA]EauxInternational audienceData from tracer experiments were compiled and analyse...
Understanding the mechanics of bed load at the flood scale is necessary to link hydrology to landsca...
Streambed mobility in gravel-bed rivers is largely controlled by the rate at which particles with di...
[1] Previous work highlights the need for data collection to identify appropriate models for tempora...
Transport of coarse sediment in gravel-bed streams alternates between mobile and immobile phases. M...
International audienceThis work analysed the factors controling the spatiotemporal variability in be...
Understanding the mechanics of bed load at the flood scale is necessary to link hydrology to lands...
Bedload transport has been studied in Ardenne rivers using different methods. Experiments with marke...
In order to predict the response of mountain streams to perturbations caused by climate and land use...
Evolution of bed material mobility and bedload grain size distributions under a range of discharges ...