A two-phase two-layer model for fluidized granular flows with dilatancy effects
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Publication:4976769
DOI10.1017/jfm.2016.417zbMath1445.76087OpenAlexW2505524366WikidataQ57964517 ScholiaQ57964517MaRDI QIDQ4976769
Enrique D. Fernández-Nieto, Anne Mangeney-Castelnau, Gladys Narbona-Reina, François Bouchut
Publication date: 2 August 2017
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://idus.us.es/xmlui/handle/11441/50741
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Cites Work
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- Bi-velocity hydrodynamics: multicomponent fluids
- A new Savage-Hutter type model for submarine avalanches and generated tsunami
- A new model of Saint Venant and Savage--Hutter type for gravity driven shallow water flows.
- Unified derivation of thin-layer reduced models for shallow free-surface gravity flows of viscous fluids
- A Saint-Venant model for gravity driven shallow water flows with variable density and compressibility effects
- Gravity driven shallow water models for arbitrary topography
- A depth-averaged -rheology for shallow granular free-surface flows
- A Roe-type scheme for two-phase shallow granular flows over variable topography
- A two-phase flow description of the initiation of underwater granular avalanches
- Submarine granular flows down inclined planes
- Steady and Intermittent Slipping in a Model of Landslide Motion Regulated by Pore-Pressure Feedback
- Dynamic stability analysis of undrained simple shear on water-saturated granular soils
- The motion of a finite mass of granular material down a rough incline
- A two-phase shallow debris flow model with energy balance
- Coupling strategies for compressible-low Mach number flows
- A two-fluid model for avalanche and debris flows
- Initiation of underwater granular avalanches: Influence of the initial volume fraction
- Migration of rigid particles in non-Brownian viscous suspensions
- A depth-averaged debris-flow model that includes the effects of evolving dilatancy. I. Physical basis
- A depth-averaged debris-flow model that includes the effects of evolving dilatancy. II. Numerical predictions and experimental tests
- Shallow two-component gravity-driven flows with vertical variation
- Flows of Dense Granular Media
