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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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Detalles Bibliográficos
Autores principales: Mirauda, Domenica, Pannone, Marilena, De Vincenzo, Annamaria
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2018
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7512268/
https://www.ncbi.nlm.nih.gov/pubmed/33265154
http://dx.doi.org/10.3390/e20010069