Aeolian and subaqueous bedforms in shear flows
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Publication:2955580
DOI10.1098/rsta.2012.0364zbMath1353.86007OpenAlexW2043890685WikidataQ38160000 ScholiaQ38160000MaRDI QIDQ2955580
Philippe Claudin, Bruno Andreotti
Publication date: 13 January 2017
Published in: Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1098/rsta.2012.0364
Hydrology, hydrography, oceanography (86A05) Fluid-solid interactions (including aero- and hydro-elasticity, porosity, etc.) (74F10) Meteorology and atmospheric physics (86A10)
Related Items (3)
On the scaling of the instability of a flat sediment bed with respect to ripple-like patterns ⋮ Formation of sediment patterns in channel flow: minimal unstable systems and their temporal evolution ⋮ Open-channel flow over evolving subaqueous ripples
Cites Work
- Bedforms in a turbulent stream: ripples, chevrons and antidunes
- Fluvial Sedimentary Patterns
- Transport relaxation time and length scales in turbulent suspensions
- Saltating particles in a turbulent boundary layer: experiment and theory
- Selection of the ripple length on a granular bed sheared by a liquid flow
- An experimental investigation of turbulent flows over a hilly surface
- Bedforms in a turbulent stream: formation of ripples by primary linear instability and of dunes by nonlinear pattern coarsening
- The formation of ripples and dunes on an erodible bed
- TURBULENT FLOW OVER HILLS AND WAVES
- Revisiting the linear theory of sand dune formation
- Sand Ripples and Dunes
- Formation of waves on a horizontal erodible bed of particles
- Sediment dynamics. Part 1. Bed-load transport by laminar shearing flows
- Saltation of uniform grains in air
- The mechanics of dunes and antidunes in erodible-bed channels
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