Sediment dynamics. Part 2. Dune formation in pipe flow
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Publication:5306109
DOI10.1017/S0022112009007927zbMath1183.76909OpenAlexW2147031503MaRDI QIDQ5306109
Malika Ouriemi, Élisabeth Guazzelli, Pascale Aussillous
Publication date: 29 March 2010
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/s0022112009007927
Hydrology, hydrography, oceanography (86A05) Experimental work for problems pertaining to fluid mechanics (76-05) Multiphase and multicomponent flows (76T99) Parallel shear flows in hydrodynamic stability (76E05)
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Cites Work
- On the formation of ripples on an erodible bed
- Selection of the ripple length on a granular bed sheared by a liquid flow
- Onset of erosion and avalanche for an inclined granular bed sheared by a continuous laminar flow
- The formation of ripples and dunes on an erodible bed
- On the development of dunes in erodible channels
- ‘Phase diagram’ of interfacial instabilities in a two-layer Couette flow and mechanism of the long-wave instability
- Instability of a bed of particles sheared by a viscous flow
- Erosion and deposition of particles on a bed sheared by a viscous flow
- Revisiting the linear theory of sand dune formation
- Determination of the critical Shields number for particle erosion in laminar flow
- Ripple formation on a particle bed sheared by a viscous liquid. Part 1. Steady flow
- The mechanics of dunes and antidunes in erodible-bed channels
