arXiv · 0903.5394
Superposition rheology of shear-banding wormlike micelles
Abstract
Wormlike micelle solutions are submitted to small-amplitude oscillatory shear superimposed to steady shear in the shear banding regime. By imposing a shear oscillation, the interface between high- and low-shear regions oscillates in time. A two-fluid semi-phenomenological model is proposed for superposition rheology in the shear banding regime, which allows us to extract a characteristic velocity for the interface dynamics from experiments involving only a standard rheometer. Estimates of the stress diffusion coefficient ${\cal D}$ can also be inferred from such superposition experiments. The validity of our model is confirmed by directly recording the interface displacement using ultrasonic velocimetry.
Explore related subjects
Keep this discovery
P. Ballesta, M. P. Lettinga, S. Manneville. 2009-03-31. Superposition rheology of shear-banding wormlike micelles. https://doi.org/10.1122/1.2750665
Cite the original work for its findings. Save a collection to share your selection of sources.