Tracer dispersion in bedload transport
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Abstract. 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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2015 ◽
Vol 817
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pp. 531-537
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2021 ◽
Keyword(s):
1975 ◽
Vol 22
(5)
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pp. 391-396
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Keyword(s):
1992 ◽
Vol 29
(02)
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pp. 418-429
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Keyword(s):
2009 ◽
Vol 46
(02)
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pp. 363-371
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