Diffusivelike buffering and saturation of large rivers - Université Paris Cité Access content directly
Journal Articles Physical Review E Year : 1999

Diffusivelike buffering and saturation of large rivers

F Métivier


We use mass balance data from Asian rivers together with a first-order diffusive simplification of the St. Venant-Exner equations to characterize river floodplain processes and discuss the reaction of a large model river to a hillslope supply of eroded masses. The simple analytical solution derived for the long-term profile of the river bed shows that (i) the system converges towards a state in which it reacts to perturbations in erosion of the landscape by small-amplitude oscillations around an average “stationary” state, (ii) to have an effective influence on the river plain profile, the perturbations need to have frequencies smaller than the characteristic frequencies of the river system, and (iii) this river buffering might be linked with a possible long-term saturation of the system carrying capacity.
Fichier principal
Vignette du fichier
physreve.60.5827.pdf (415.22 Ko) Télécharger le fichier
Origin : Publisher files allowed on an open archive

Dates and versions

hal-01499568 , version 1 (21-08-2023)



F Métivier. Diffusivelike buffering and saturation of large rivers. Physical Review E , 1999, 60 (5), pp.5827. ⟨10.1103/PhysRevE.60.5827⟩. ⟨hal-01499568⟩
111 View
4 Download



Gmail Facebook X LinkedIn More