Saltating particles in a turbulent boundary layer: experiment and theory

By M. Creyssels, Pascal Dupont, Ahmed Ould Mohamed Moctar, A. Valance, I. Cantat, J. Jenkins, Jose Miguel Pasini, K. Rasmussen. Journal of Fluid Mechanics, 2009

239 citations recorded by the source corpus.

Subfields: Earth-Surface Processes, Ocean Engineering, Soil Science

View Paper: https://www.semanticscholar.org/paper/1508094f97bf45145d2f36af4e7b7e6fa90cf06f

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Earth-Surface Processes

1. Orencio Durán
2. J. Kok
3. Bruno Andreotti
4. P. Claudin
5. Thomas Pahtz
6. Abram H. Clark
7. Manousos Valyrakis
8. Olivier Pouliquen

In Ocean Engineering

1. Orencio Durán
2. Bruno Andreotti
3. J. Kok
4. Eric J. R. Parteli
5. T. Michaels
6. D. Karam
7. P. Claudin
8. Thomas Pahtz

In Soil Science

1. Orencio Durán
2. J. Kok
3. P. Claudin
4. Thomas Pahtz
5. Abram H. Clark
6. Manousos Valyrakis
7. Bruno Andreotti
8. Olivier Pouliquen

Citations in the corpus

• The physics of wind-blown loess: Implications for grain size proxy interpretations in Quaternary paleoclimate studies (2016, background): “…moving higher up in the saltation layer increases with higher friction velocities, while the mean particle impact speed (vip) at the surface is independent of u⁎ (Rasmussen and Sorensen, 2008; Creyssels et al., 2009, Kok and Renno, 2009; Ho et al., 2011; Durán et al., 2011; Kok et al., 2012).”
• The Physics of Sediment Transport Initiation, Cessation, and Entrainment Across Aeolian and Fluvial Environments (2020, background): “…to model fluvial bedload [Berzi et al., 2016; Pähtz et al., 2020] and aeolian saltation transport [Andreotti, 2004; Claudin and Andreotti, 2006; Creyssels et al., 2009; Kok and Renno, 2009; Kok, 2010a; Jenkins et al., 2010; Lämmel et al., 2012; Pähtz et al., 2012; Huang et al., 2014; Jenkins…”
• Measurements of the aeolian sand transport saturation length (2008, background): “The density of transported grains decreases exponentially with height over a length-scale on the order of few cm (Liu and Dong, 2004; Creyssels et al., 2009); so, most of the sand traps do not have sufficient spatial resolution to measure the overall flux accurately.”
• The physics of wind-blown sand and dust (2012, result): “A range of recent wind tunnel measurements (Rasmussen and Sorensen 2008, Creyssels et al 2009, Ho et al 2011), field measurements (Namikas 2003) and numerical saltation models (Kok and Renno 2009a, Durán et al 2011a) confirm both these results (figures 14 and 15).”
• On aeolian transport: Grain-scale interactions, dynamical mechanisms and scaling laws (2011, background): “The same behavior is also found in wind tunnel experiments by Creyssels et al. (2009), exploring shear velocities up to three times the threshold value ud.”