Abstract
We suggest a mechanism by which vorticity structuring and velocity rolls can form in complex fluids, triggered by the linear instability of one-dimensional gradient shear banded flow. We support this with a numerical study of the diffusive Johnson-Segalman model. In the steady vorticity structured state, the thickness of the interface between the bands remains finite in the limit of zero stress diffusivity, presenting a possible challenge to the accepted theory of shear banding.
- Received 26 June 2006
- Publisher error corrected 26 July 2007
DOI:https://doi.org/10.1103/PhysRevE.76.016311
©2007 American Physical Society
Corrections
26 July 2007