Superposition rheology of shear-banding wormlike micelles
arXiv:0903.5394 · doi:10.1122/1.2750665
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 can also be inferred from such superposition experiments. The validity of our model is confirmed by directly recording the interface displacement using ultrasonic velocimetry.
24 pages, 13 figures
References in corpus (5)
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- Early stages of the shear banding instability in wormlike micelles