Mots-clés
Charge solide ; Contrainte de cisaillement ; Cours d'eau ; Expérimentation ; Granulométrie ; Géomorphodynamique ; Montagne ; Pente de versant ; Transport sédimentaire ; Tri cinétiqueEarth surface processes ; Experimentation ; Grain size distribution ; Kinetic sorting ; Mountain ; Sediment load ; Sediment transport ; Shear stress ; Slope gradient ; StreamCarga solida ; Corriente de agua ; Experimentación ; Geomorfodinámica ; Granulometría ; Inclinación de la vertiente ; Montaña ; Tensión de cizallamiento ; Transporte sedimentarioThe effects of kinetic sorting on sediment mobility on steep slopes
Auteur(s) et Affiliation(s)
BACCHI, V.
IRSTEA, ER ETGR, Centre de Grenoble, St-Martin d'Hères, France
Univ. Grenoble Alpes, Grenoble, France
RECKING, A.
IRSTEA, ER ETGR, Centre de Grenoble, St-Martin d'Hères, France
Univ. Grenoble Alpes, Grenoble, France
ECKERT, N.
IRSTEA, ER ETGR, Centre de Grenoble, St-Martin d'Hères, France
Univ. Grenoble Alpes, Grenoble, France
FREY, P.
IRSTEA, ER ETGR, Centre de Grenoble, St-Martin d'Hères, France
Univ. Grenoble Alpes, Grenoble, France
PITON, G.
IRSTEA, ER ETGR, Centre de Grenoble, St-Martin d'Hères, France
Univ. Grenoble Alpes, Grenoble, France
NAAIM, M.
IRSTEA, ER ETGR, Centre de Grenoble, St-Martin d'Hères, France
Univ. Grenoble Alpes, Grenoble, France
Description :
The AA. hypothesized that kinetic sorting can be an important contributor to the morphodynamics of mountain streams and attempted to demonstrate this with new flume experiments. Two long runs were produced with natural poorly sorted sediments, and with different transport stages of the coarse fraction. Both runs produced an efficient transfer downstream of the injected material, but with a major difference : the first run (no kinetic sorting) produced permanent armour figuring clusters; the second run (with kinetic sorting) also produced bed armouring, but this armour was periodically totally destroyed, leading to substantial bed erosion. The consequence is that fine materials are hidden to the flow during aggradation, allowing the slope to attain values much steeper than would have been expected at equilibrium for the mixture. However, whereas the surface armouring tends to stabilize the bed, construction of a layer of fine sediments at the subsurface also contributes to making it very unstable. These 2 contradictory effects explain the complex bed behaviours and the existence of very large bedload and slope fluctuations.
Type de document :
Article de périodique
Source :
Earth surface processes and landforms, issn : 0197-9337, 2014, vol. 39, n°. 8, p. 1075-1086, nombre de pages : 12, Références bibliographiques : 2 p.
Date :
2014
Editeur :
Pays édition : Royaume-Uni, Chichester, Wiley
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)