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A theoretical analysis of free-surface flows of saturated granular-liquid mixtures

Author
BERZI, D1 ; JENKINS, J. T2
[1] Department of Environmental, Hydraulic, Infrastructures and Surveying Engineering, Politecnico di Milano, Milan 20133, Italy
[2] Department of Theoretical and Applied Mechanics, Cornell University, Ithaca, NY 14853, United States
Source

Journal of Fluid Mechanics. 2008, Vol 608, pp 393-410, 18 p ; ref : 1 p

CODEN
JFLSA7
ISSN
0022-1120
Scientific domain
Mechanics acoustics
Publisher
Cambridge University Press, Cambridge
Publication country
United Kingdom
Document type
Article
Language
English
Keyword (fr)
Angle inclinaison Condition aux limites Eau Ecoulement diphasique Ecoulement surface libre Erosion Etude théorique Fluidisation Matériau granulaire Plan incliné Sédimentation 4755K 8380F
Keyword (en)
Inclination Boundary conditions Water Two-phase flow Free surface flow Erosion Theoretical study Fluidization Granular materials Inclined plan Sedimentation
Keyword (es)
Flujo superficie libre Plano inclinado
Classification
Pascal
001 Exact sciences and technology / 001B Physics / 001B40 Fundamental areas of phenomenology (including applications) / 001B40G Fluid dynamics / 001B40G55 Nonhomogeneous flows / 001B40G55K Multiphase and particle-laden flows

Pascal
001 Exact sciences and technology / 001B Physics / 001B80 Cross-disciplinary physics: materials science; rheology / 001B80C Rheology / 001B80C70 Material form / 001B80C70F Granular solids

Discipline
Physics : fluid mechanics Physics of condensed state : structure, mechanical and thermal properties
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
20502207

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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