Erosion and deposition of particles on a bed sheared by a viscous flow

By By F. Charru, H. Mouilleron, O. Eiff. Journal of Fluid Mechanics, 2004

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The Physics of Sediment Transport Initiation, Cessation, and Entrainment Across Aeolian and Fluvial Environments (2020, background): “For nearly monodisperse beds of spherical particles, most studies reported Θmaxt ≈ 0.12 [Charru et al., 2004; Loiseleux et al., 2005; Ouriemi et al., 2007; Seizilles et al., 2014; Houssais et al., 2015], but larger values of up to about 0.37 have also been reported [Lobkovsky et al., 2008; Hong et…”
Bed load transport in turbulent flow at the grain scale: Experiments and modeling (2010, methodology): “A second group of investigators studied the trajectories of bed load particles over an erodible bed [Fernandez‐ Luque and Van Beek, 1976; Van Rijn, 1984; Nino and Garcia, 1994; Charru et al., 2004].”
A three-dimensional numerical model for incompressible two-phase flow of a granular bed submitted to a laminar shearing flow (2010, methodology): “If the Shields number based on the fluid bed shear stress is lower than a critical value hc the particle flux is zero otherwise it evolves as a function of h and hc [13,4,32,11,28].”