Granular Matter

, 10:353

Granular flows down inclined channels with a strain-rate dependent friction coefficient. Part I: Non-cohesive materials

Authors

    • École des Mines d’Albi, UMR CNRS 2392
  • Renaud Ansart
    • École des Mines d’Albi, UMR CNRS 2392
  • John A. Dodds
    • École des Mines d’Albi, UMR CNRS 2392
Article

DOI: 10.1007/s10035-008-0105-3

Cite this article as:
de Ryck, A., Ansart, R. & Dodds, J.A. Granular Matter (2008) 10: 353. doi:10.1007/s10035-008-0105-3

Abstract

The flow of a granular material down an incline of finite width with a strain-rate dependent coefficient of friction and a conical yield criterion is semi-analytically obtained using a characteristic method for flows on a deep layer of grains. This analysis leads to a flow field with three distinct zones: a Bagnold-flow zone below the free surface, a dead-zone and a matching zone between the two, linked to slippage at the wall. A good agreement between the computed flow field and experimental data is obtained.

Keywords

Granular materialsSurface flows

Copyright information

© Springer-Verlag 2008