The time evolution of flow-induced structures in low-concentration worm-like micellar solutions is studied using direct visualization and rheological methods. The visualization measurements show growth of a new viscous shear-induced phase (SIP) starting on the inner wall of a Couette shear cell at a time t 1 after the commencement of shear flow. The SIP continues to grow across the shear cell until it fills the entire gap at a time t 2 . Rheological measurements show that the time t 1 corresponds to the induction time for the increase in stress and that t 2 corresponds to the plateau time for the saturation of stress. These measurements provide convincing evidence that the increase of stress with time results from the inhomogeneous growth of a new shear-induced phase in the flow cell. The growth of the new phase across the cell is approximately linear in time.
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Boltenhagen et al. (1997) studied this question.
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