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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...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
MDPI
2018
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| 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 |