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On dense granular flows.

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TLDR
A quantitative comparison between data coming from different experiments in the same geometry identifies the robust features in each case and a transverse analysis of the data across the different configurations allows to identify the relevant dimensionless parameters, the different flow regimes and to propose simple interpretations.
Abstract
The behaviour of dense assemblies of dry grains submitted to continuous shear deformation has been the subject of many experiments and discrete particle simulations. This paper is a collective work carried out among the French research group Groupement de Recherche Milieux Divises (GDR MiDi). It proceeds from the collection of results on steady uniform granular flows obtained by different groups in six different geometries both in experiments and numerical works. The goal is to achieve a coherent presentation of the relevant quantities to be measured i.e. flowing thresholds, kinematic profiles, effective friction, etc. First, a quantitative comparison between data coming from different experiments in the same geometry identifies the robust features in each case. Second, a transverse analysis of the data across the different configurations, allows us to identify the relevant dimensionless parameters, the different flow regimes and to propose simple interpretations. The present work, more than a simple juxtaposition of results, demonstrates the richness of granular flows and underlines the open problem of defining a single rheology.

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Citations
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Journal ArticleDOI

Criticality and Scaling Relations in a Sheared Granular Material

TL;DR: In this article, the authors investigate a rheological property of a dense granular material under shear and find a critical volume fraction at which the stress and the pressure behave as power-law functions of the shear strain rate.
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Rheology and Mixing of Granular Materials

TL;DR: A review of recent advances in the field which are of relevance to polymer processing can be found in this paper, where a new model for description of the rheology of dense granular flows is reviewed.
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Applying GSH to a wide range of experiments in granular media

TL;DR: Granular solid hydrodynamics may be taken as a unifying framework, providing the appropriate macroscopic vocabulary and mindset that help one coming to terms with the breadth of granular physics.
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Size Polydispersity Tunes Slip Avalanches of Granular Gouge

TL;DR: In this article, the authors examined granular systems with varying size polydispersity from monosized spheres to highly polydisperse packings and found the signature of tunable avalanche statistics.
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Frictional hysteresis and particle deposition in granular free-surface flows

TL;DR: In this paper, the hysteretic behavior of shallow granular avalanches on slopes close to repose was studied. But the authors did not consider the effect of the altitude on the stability of the avalanches.
References
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Journal ArticleDOI

Dynamics of viscoplastic deformation in amorphous solids

TL;DR: In this article, a dynamical theory of low-temperature shear deformation in amorphous solids is proposed based on molecular-dynamics simulations of a two-dimensional, two-component non-crystalline system.
Journal ArticleDOI

Rapid granular flows

TL;DR: In this article, the authors present a review of the fluid-like behavior of granular solids and, in particular, those flows for which the material is rapidly sheared, and discuss various modeling techniques used to describe the motion of the bulk material.
Book

Statics and Kinematics of Granular Materials

TL;DR: In this article, Coulomb's method of wedges and differential slices were used to determine the stress and strain rate of Coulomb material, and the conical yield function was used to predict mass flow rate.
Journal ArticleDOI

Granular flow down an inclined plane: Bagnold scaling and rheology

TL;DR: A systematic, large-scale simulation study of granular media in two and three dimensions, investigating the rheology of cohesionless granular particles in inclined plane geometries, finds that a steady-state flow regime exists in which the energy input from gravity balances that dissipated from friction and inelastic collisions is found.
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