Passer à la navigation principale Passer à la recherche Passer au contenu principal

A simple model accounting for the uptake, transport, and deposition of wind-eroded mineral particles in the hyperarid coastal Atacama Desert of northern Chile

  • Stephane C. Alfaro
  • , Valentina Flores-Aqueveque
  • , Gilles Foret
  • , Sandrine Caquineau
  • , Gabriel Vargas
  • , Jose A. Rutllant

Résultats de recherche: Contribution à un journalArticleRevue par des pairs

Résumé

As previously observed in marine sediments collected downwind of African or South American continental sources, recent studies of sediment cores collected at the bottom of Mejillones Bay in north Chile (23°S) show a laminated structure in which the amount of particles of aeolian origin and their size create significant differences between the layers. This suggests inter-annual to inter-decadal variations in the strength of the local southerly winds responsible for (1) the erosion of the adjacent hyperarid surface of the Mejillones Pampa, and (2) the subsequent transport of the eroded particles towards the bay. A simple model accounting for the vertical uptake, transport, and deposition of the particles initially set into motion by wind at the surface of the pampa is proposed. This model, which could be adapted to other locations, assumes that the initial rate of (vertical) uptake is proportional to the (horizontal) saltation flux quantified by means of White's equation, that particles are lifted to a height (H), increasing with the magnitude of turbulence, and that sedimentation progressively removes the coarsest particles from the air column as it moves towards the bay. In this model, the proportionality constant (A) linking the vertical flux of particles with the horizontal flux, and the injection height (H) control the magnitude and size distribution of the deposition flux in the bay. Their values are determined using the wind speed measured over the pampa and the size distribution of particles collected in sediment traps deployed in the bay as constraints. After calibration, the model is used to assess the sensitivity of the deposition flux to the wind intensity variations. The possibility of performing such quantitative studies is necessary for interpreting precisely the variability of the aeolian material in the sediment cores collected at the bottom of Mejillones Bay.

langue originaleAnglais
Pages (de - à)923-932
Nombre de pages10
journalEarth Surface Processes and Landforms
Volume36
Numéro de publication7
Les DOIs
étatPublié - 15 juin 2011
Modification externeOui

SDG des Nations Unies

Ce résultat contribue à ou aux Objectifs de développement durable suivants

  1. SDG 14 - Vie sous l’eau
    SDG 14 Vie sous l’eau

Empreinte digitale

Examiner les sujets de recherche de « A simple model accounting for the uptake, transport, and deposition of wind-eroded mineral particles in the hyperarid coastal Atacama Desert of northern Chile ». Ensemble, ils forment une empreinte digitale unique.

Contient cette citation