Fundamental changes of granular flow dynamics, deposition, and erosion processes at high slope angles: Insights from laboratory experiments

Author:

Farin Maxime1,Mangeney Anne12,Roche Olivier3

Affiliation:

1. Institut de Physique du Globe de Paris, Equipe Sismologie, CNRS-UMR 7154; Université Paris-Diderot, PRES Sorbonne Paris Cité; Paris France

2. ANGE team; INRIA, CETMEF, Lab. J. Louis Lions; Paris France

3. Laboratoire Magmas et Volcans; Université Blaise Pascal-CNRS-IRD; Clermont-Ferrand France

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Reference49 articles.

1. Direct measurement of channel erosion by debris flows, Illgraben, Switzerland;Berger;J. Geophys. Res.,2011

2. Granular collapse in two dimensions;Balmforth;J. Fluid Mech.,2005

3. Bernard , K. B. Van Wyk de Vries 2011 Characterization of breccia structure at the base of large landslides: A necessary step for modeling

4. A new model of Saint-Venant and Savage-Hutter type for gravity driven shallow water flows;Bouchut;C. R. Acad. Sci. Paris Ser. I,2003

5. Gravity driven shallow water models for arbitrary topography;Bouchut;Comm. Math. Sci.,2004

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