Deprecated: $wgMWOAuthSharedUserIDs=false is deprecated, set $wgMWOAuthSharedUserIDs=true, $wgMWOAuthSharedUserSource='local' instead [Called from MediaWiki\HookContainer\HookContainer::run in /var/www/html/w/includes/HookContainer/HookContainer.php at line 135] in /var/www/html/w/includes/Debug/MWDebug.php on line 372
A two-phase flow description of the initiation of underwater granular avalanches - MaRDI portal

A two-phase flow description of the initiation of underwater granular avalanches

From MaRDI portal
Publication:3550306

DOI10.1017/S0022112009007460zbMath1183.76906OpenAlexW2097301590MaRDI QIDQ3550306

Mickaël Pailha, Olivier Pouliquen

Publication date: 31 March 2010

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1017/s0022112009007460




Related Items (30)

Dilatancy in dry granular flows with a compressible \(\mu(I)\) rheologyInvestigation of influence of an obstacle on granular flows by virtue of a depth-integrated theoryMultilayer models for shallow two-phase debris flows with dilatancy effectsThe granular column collapse as a continuum: validity of a two-dimensional Navier–Stokes model with a μ(I)-rheologyA viscoplastic approach to the behaviour of fluidized geomaterials with application to fast landslidesDepth averaged models for fast landslide propagation: mathematical, rheological and numerical aspectsFormation of dry granular fronts and watery tails in debris flowsRheology of dense granular suspensionsNon-isochoric stable granular models taking into account fluidisation by pore gas pressureCoupled Fluid-Particle Modeling of Submerged Granular CollapseA mixture theory formulation for hydraulic or pneumatic transport of solid particlesTwo-phase modelling of submarine granular flows with shear-induced volume change and pore-pressure feedbackTensorial rheological model for concentrated non-colloidal suspensions: normal stress differencesImmersed granular collapse: from viscous to free-fall unsteady granular flowsA coupled finite volume and material point method for two-phase simulation of liquid-sediment and gas-sediment flowsA two-fluid model for immersed granular avalanches with dilatancy effectsModeling dynamic flows of grain-fluid mixtures by coupling the mixture theory with a dilatancy lawMixed finite element - discontinuous finite volume element discretization of a general class of multicontinuum modelsThe compressible granular collapse in a fluid as a continuum: validity of a Navier–Stokes model with , -rheologyAsymmetric breaking size-segregation waves in dense granular free-surface flowsA two-phase two-layer model for fluidized granular flows with dilatancy effectsA two-phase shallow debris flow model with energy balanceDebris flows with pore pressure and intergranular friction on rugged topographyCompressibility regularizes the 𝜇(I)-rheology for dense granular flowsA general fluid–sediment mixture model and constitutive theory validated in many flow regimesEntrainment and adaptation processes in the evolution of collisional bedload layersA theoretical formulation of dilatation/contraction for continuum modelling of granular flowsDrift-diffusive liquid migration in partly saturated sheared granular mediaTransient flows and migration in granular suspensions: key role of Reynolds-like dilatancyDynamics of landslide-generated tsunamis and their dependence on the particle concentration of initial release mass



Cites Work


This page was built for publication: A two-phase flow description of the initiation of underwater granular avalanches