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An Entropic Model for the Assessment of Streamwise Velocity Dip in Wide Open Channels

The three-dimensional structure of river flow and the presence of secondary currents, mainly near walls, often cause the maximum cross-sectional velocity to occur below the free surface, which is known as the “dip” phenomenon. The present study proposes a theoretical model derived from the entropy t...

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Autori principali: Domenica Mirauda, Marilena Pannone, Annamaria De Vincenzo
Natura: Artigo
Lingua:Inglês
Pubblicazione: MDPI AG 2018-01-01
Serie:Entropy
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Accesso online:http://www.mdpi.com/1099-4300/20/1/69
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