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Article Dans Une Revue Advances in Geosciences Année : 2013

Tracer dispersion in bedload transport

Résumé

Bedload particles entrained by rivers tends to disperse as they move downstream. In this paper, we use the erosion-deposition model of Charru et al. (2004) to describe the velocity and the spreading of a plume of tracer particles. We restrict our analysis to steady-state transport above a flat bed of uniform sediment. The transport of tracer particles is then controlled by downstream advection and particle exchange with the immobile bed. After a transitional regime dominated by initial conditions, the evolution of a plume of markers tends asymptotically towards classical advection-diffusion: its average position grows linearly with time, whereas it spreads like the square root of time.
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Dates et versions

hal-01500386 , version 1 (05-04-2017)

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E Lajeunesse, O Devauchelle, M Houssais, G Seizille. Tracer dispersion in bedload transport. Advances in Geosciences, 2013, 37, pp.1--6. ⟨10.5194/adgeo-37-1-2013⟩. ⟨hal-01500386⟩
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