2013
DOI: 10.1680/wama.11.00066
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A mixing length model for estimating channel conveyance

Abstract: This paper describes a simple, physically based mixing length model that explains the functional form of Manning's equation for mean velocity in open channels. Manning's equation has been used to describe mean velocity for over 100 years and is essentially an empirical result rather than being based on an understanding of physical processes.The model described in this paper uses Prandtl's mixing length hypothesis, with mixing length modelled at each point within the cross-section being proportional to the dist… Show more

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Cited by 2 publications
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“…and 'why is the power two-thirds?' The first paper, by Horritt and Wright (2013), describes the use of a mixing length model for estimating channel conveyance and shows that this simple, physically based model explains the functional form of Manning's equation and the Colebrook-White formula. The model applies Prandtl's mixing length hypothesis, with the mixing length at each point in a river cross-section being proportional to the distance to the nearest solid boundary.…”
mentioning
confidence: 99%
“…and 'why is the power two-thirds?' The first paper, by Horritt and Wright (2013), describes the use of a mixing length model for estimating channel conveyance and shows that this simple, physically based model explains the functional form of Manning's equation and the Colebrook-White formula. The model applies Prandtl's mixing length hypothesis, with the mixing length at each point in a river cross-section being proportional to the distance to the nearest solid boundary.…”
mentioning
confidence: 99%