Perturbation of fluvial sediment fluxes following the 2008 Wenchuan earthquake |
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| Authors: | Wei Wang Vincent Godard Jing Liu‐Zeng Dirk Scherler Chong Xu Jinyu Zhang Kejia Xie Olivier Bellier Claire Ansberque Julia de Sigoyer ASTER Team |
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| Institution: | 1. Institute of Geology, China Earthquake Administration, Beijing, China;2. Aix‐Marseille Université, CNRS, IRD, Collège de France, CEREGE, Aix en Provence, France;3. GFZ German Research Centre for Geoscience, Potsdam, Germany;4. Freie Universit?t Berlin, Berlin, Germany;5. First Team of Henan Provincial Non‐ferrous Metals Geological and Mineral Resources Bureau, Henan, China;6. Université Grenoble Alpes, CNRS, UMR 5275, ISTerre, Grenoble, France |
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| Abstract: | 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 Mw 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 (0.25–1 mm) at 19 locations and measured the concentration of cosmogenic 10Be in quartz. When compared with published pre‐earthquake data, the 10Be 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 10Be decrease is controlled by the amount of landslides directly connected to the river network. Calculations based on 10Be mixing budgets indicate that the sediment flux of the 0.25–1 mm 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 © 2017 John Wiley & Sons, Ltd. |
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| Keywords: | co‐seismic landslides Wenchuan earthquake Longmen Shan cosmogenic nuclides fluvial processes |
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