Tracer dispersion in bedload transport

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 o...

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Main Authors: E. Lajeunesse, O. Devauchelle, M. Houssais, G. Seizilles
Format: Article
Language:English
Published: Copernicus Publications 2013-12-01
Series:Advances in Geosciences
Online Access:http://www.adv-geosci.net/37/1/2013/adgeo-37-1-2013.pdf
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author E. Lajeunesse
O. Devauchelle
M. Houssais
G. Seizilles
author_facet E. Lajeunesse
O. Devauchelle
M. Houssais
G. Seizilles
author_sort E. Lajeunesse
collection DOAJ
description 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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spelling doaj.art-70050374c8774753ac309ea96763cd682022-12-22T01:29:54ZengCopernicus PublicationsAdvances in Geosciences1680-73401680-73592013-12-01371610.5194/adgeo-37-1-2013Tracer dispersion in bedload transportE. Lajeunesse0O. Devauchelle1M. Houssais2G. Seizilles3Institut de Physique du Globe – Sorbonne Paris Cité, Équipe de Dynamique des fluides géologiques, 1 rue Jussieu, 75238 Paris cedex 05, FranceInstitut de Physique du Globe – Sorbonne Paris Cité, Équipe de Dynamique des fluides géologiques, 1 rue Jussieu, 75238 Paris cedex 05, FranceInstitut de Physique du Globe – Sorbonne Paris Cité, Équipe de Dynamique des fluides géologiques, 1 rue Jussieu, 75238 Paris cedex 05, FranceInstitut de Physique du Globe – Sorbonne Paris Cité, Équipe de Dynamique des fluides géologiques, 1 rue Jussieu, 75238 Paris cedex 05, FranceBedload 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.http://www.adv-geosci.net/37/1/2013/adgeo-37-1-2013.pdf
spellingShingle E. Lajeunesse
O. Devauchelle
M. Houssais
G. Seizilles
Tracer dispersion in bedload transport
Advances in Geosciences
title Tracer dispersion in bedload transport
title_full Tracer dispersion in bedload transport
title_fullStr Tracer dispersion in bedload transport
title_full_unstemmed Tracer dispersion in bedload transport
title_short Tracer dispersion in bedload transport
title_sort tracer dispersion in bedload transport
url http://www.adv-geosci.net/37/1/2013/adgeo-37-1-2013.pdf
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