Perturbation of fluvial sediment fluxes following the 2008 Wenchuan earthquake - Archive ouverte HAL Accéder directement au contenu
Article Dans Une Revue Earth Surface Processes and Landforms Année : 2017

Perturbation of fluvial sediment fluxes following the 2008 Wenchuan earthquake

Wei Wang
  • Fonction : Auteur
Jing Liu-Zeng
  • Fonction : Auteur
Dirk Scherler
  • Fonction : Auteur
Chong Xu
  • Fonction : Auteur
  • PersonId : 1330868
Jinyu Zhang
  • Fonction : Auteur
Kejia Xie
  • Fonction : Auteur
Claire Ansberque
  • Fonction : Auteur
Julia De Sigoyer
  • Fonction : Auteur

Résumé

Quantifying the removal of co-seismic landslide material after a large-magnitude earthquake is central to our understanding of geomorphic recovery from seismic events and the topographic evolution of tectonically active mountain ranges. In order to gain more insight into the fluvial erosion response to co-seismic landslides, we focus on the sediment fluxes of rivers flowing through the rupture zone of the 2008 M-w 7.9 Wenchuan earthquake in the Longmen Shan of the eastern Tibetan Plateau. Over the post-seismic period of 2008-2013, we annually collected river sediment samples (0.25-1mm) at 19 locations and measured the concentration of cosmogenic Be-10 in quartz. When compared with published pre-earthquake data, the Be-10 concentrations declined dramatically after the earthquake at all sampling sites, but with significant spatial differences in the amplitude of this decrease, and were starting to increase toward pre-earthquake level in several basins over the 5-year survey. Our analysis shows that the amplitude of Be-10 decrease is controlled by the amount of landslides directly connected to the river network. Calculations based on Be-10 mixing budgets indicate that the sediment flux of the 0.25-1mm size fraction increased up to sixfold following the Wenchuan earthquake. Our results also suggest that fluvial erosion became supply limited shortly after the earthquake, and predict that it could take a few years to several decades for fluvial sediment fluxes to go back to pre-earthquake characteristics, depending on catchment properties. We also estimate that it will take at least decades and possibly up to thousands of years to remove the co-seismic landslide materials from the catchments in the Longmen Shan. Copyright (c) 2017 John Wiley & Sons, Ltd.
Fichier non déposé

Dates et versions

hal-01765613 , version 1 (13-04-2018)

Identifiants

Citer

Wei Wang, Vincent Godard, Jing Liu-Zeng, Dirk Scherler, Chong Xu, et al.. Perturbation of fluvial sediment fluxes following the 2008 Wenchuan earthquake. Earth Surface Processes and Landforms, 2017, 42 (15), pp.2611-2622. ⟨10.1002/esp.4210⟩. ⟨hal-01765613⟩
145 Consultations
0 Téléchargements

Altmetric

Partager

Gmail Facebook X LinkedIn More