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

By F. Charru. 2006

147 citations recorded by the source corpus.

Subfields: Earth-Surface Processes, Ecology, Soil Science

View Paper: https://www.semanticscholar.org/paper/e4667e43b4cfc46b77251266e8d1bec8c194da2b

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. Bruno Andreotti
2. P. Claudin
3. Olivier Pouliquen
4. L. Malverti
5. E. Lajeunesse
6. F. Charru
7. Orencio Durán
8. J. Kok

In Ecology

1. L. Malverti
2. E. Lajeunesse
3. Bruno Andreotti
4. P. Claudin
5. Olivier Pouliquen
6. F. Charru

In Soil Science

1. P. Claudin
2. Bruno Andreotti
3. Olivier Pouliquen
4. L. Malverti
5. E. Lajeunesse
6. Orencio Durán
7. J. Kok
8. Thomas Pahtz

Citations in the corpus

• Measurements of the aeolian sand transport saturation length (2008, background): “…order equation: Lsat dq dx = qsat − q. (1) DIfferent physical mechanisms can be responsible for this saturation length e.g., the grain hop length [Charru 2006 ], the length needed to accelerate new grains (called the drag length) [Andreotti et al. 2002, Hersen et al. 2002, Andreotti and…”
• Bed load transport in turbulent flow at the grain scale: Experiments and modeling (2010, methodology): “the model of Charru [2006] accounts for a relaxation effect which strongly influences the development of bed forms.”