Measurements of the aeolian sand transport saturation length

By Bruno Andreotti, P. Claudin, Olivier Pouliquen. 2008

147 citations recorded by the source corpus.

The wavelength at which a dune pattern emerges from a flat sand bed is controlled by the sediment transport saturation length, which is the length needed for the sand flux to adapt to a change in wind strength. The influence of the wind shear velocity on this saturation length and on the subsequent dune initial wavelength has remained controversial. In this paper, we present direct measurements of the saturation length performed in a wind tunnel experiment. Complementary to this, initial dune wavelengths are measured under different wind conditions — in particular after storms. Using the linear stability analysis of dune formation, it is then possible to deduce the saturation length from field data. Both direct and indirect measurements agree that the saturation length is almost independent of the wind strength. This result supports the idea that grain inertia is the dominant dynamical mechanism limiting sediment transport saturation on dunes.

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

View Paper: https://www.semanticscholar.org/paper/e253ce6af8d24d37316902667a25df827b2078bc

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. Eric J. R. Parteli
  6. T. Michaels
  7. D. Karam
  8. Thomas Pahtz

In Mechanical Engineering

  1. Orencio Durán
  2. P. Claudin
  3. Bruno Andreotti
  4. Eric J. R. Parteli

In Soil Science

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

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