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μ(I) rheology

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This is an old revision of this page, as edited by Kateshortforbob (talk | contribs) at 14:40, 24 July 2015 (+Category:Rheology; +Category:Granularity of materials using HotCat). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.


In granular mechanics, the μ(I) rheology is one model of the flow properties of a granular material. The flow of a granular material is assumed to be governed by the strain rate, the pressure and shear stress, and the model attempts to connect these fields. The effective friction μ is treated as a function of the inertial number I; the name alludes to this dependence.

The μ(I) rheology was developed by Jop et al. in 2006.[1]

References

  1. ^ Holyoake, Alex (December 2011). Rapid Granular Flows in an Inclined Chute (PDF). Retrieved 21 July 2015.
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