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
Selection of the ripple length on a granular bed sheared by a liquid flow - MaRDI portal

Selection of the ripple length on a granular bed sheared by a liquid flow

From MaRDI portal
Publication:3531758

DOI10.1063/1.2397005zbMath1146.76347OpenAlexW1968493970MaRDI QIDQ3531758

François Charru

Publication date: 3 November 2008

Published in: Physics of Fluids (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1063/1.2397005




Related Items (22)

Subaqueous barchan dunes in turbulent shear flow. Part 1. Dune motionBedforms in a turbulent stream: ripples, chevrons and antidunesOn the influence of the thickness of the sediment moving layer in the definition of the bedload transport formula in Exner systemsSediment dynamics. Part 2. Dune formation in pipe flowAeolian and subaqueous bedforms in shear flowsOn the scaling of the instability of a flat sediment bed with respect to ripple-like patternsFormation of sediment patterns in channel flow: minimal unstable systems and their temporal evolutionLinear and nonlinear instabilities of a granular bed: determination of the scales of ripples and dunes in riversReport of the Symposium on Interactions for Dispersed Systems in Newtonian and Viscoelastic Fluids, Guanajuato, Mexico, 2006Streamwise streaks induced by bedload diffusionStability of bedforms in laminar flows with free surface: from bars to ripplesA 1D numerical model for the simulation of unsteady and highly erosive flows in riversThe role of bed-penetrating Kelvin–Helmholtz vortices on local and instantaneous bedload sediment transportBedforms in a turbulent stream: formation of ripples by primary linear instability and of dunes by nonlinear pattern coarseningLagrangian drift near a wavy boundary in a viscous oscillating flowFormation of sand ripples under a turbulent liquid flowParticle diffusion in non-equilibrium bedload transport simulationsModelling of bedload sediment transport for weak and strong regimesThe phase lead of shear stress in shallow-water flow over a perturbed bottomTransport relaxation time and length scales in turbulent suspensionsA semi-implicit approach for sediment transport models with gravitational effectsOpen-channel flow over evolving subaqueous ripples




Cites Work




This page was built for publication: Selection of the ripple length on a granular bed sheared by a liquid flow