Onset of sediment transport is a continuous transition driven by fluid shear and granular creep

Fluid-sheared granular transport sculpts landscapes and undermines infrastructure, yet predicting the onset of sediment transport remains notoriously unreliable. For almost a century, this onset has been treated as a discontinuous transition at which hydrodynamic forces overcome gravity-loaded grain...

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Detalles Bibliográficos
Autores principales: Houssais, Morgane, Ortiz, Carlos P., Durian, Douglas J., Jerolmack, Douglas J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Pub. Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4366508/
https://www.ncbi.nlm.nih.gov/pubmed/25751296
http://dx.doi.org/10.1038/ncomms7527

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4366508/
https://www.ncbi.nlm.nih.gov/pubmed/25751296
http://dx.doi.org/10.1038/ncomms7527

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