Shear thickening in low-concentration solutions of wormlike micelles. II. Slip, fracture, and stability of the shear-induced phase
Author(s) -
Yuntao Hu,
Philippe Boltenhagen,
E.F. Matthys,
David J. Pine
Publication year - 1998
Publication title -
journal of rheology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.098
H-Index - 107
eISSN - 1520-8516
pISSN - 0148-6055
DOI - 10.1122/1.550917
Subject(s) - dilatant , shear rate , materials science , shear (geology) , shear stress , rheology , critical resolved shear stress , slip (aerodynamics) , viscosity , apparent viscosity , composite material , thermodynamics , physics
The rheology of the shear-thickened state is investigated in low-concentration solutions of wormlike micellar solutions using mechanical, optical, and velocity profile measurements. The zero-shear-rate viscosity of the solutions increases by more than a factor of 1000 as the concentration of surfactant is increased from 1 to 10 mM. By contrast, the apparent viscosity of the shear-thickened state of these same solutions is observed to be remarkably independent of concentration over a wide range of shear rates. This is shown to be a consequence of the development of slip layers between the very viscous gellike shear-induced structures (SISs) which form in the bulk of the surfactant solution and on the walls of the Couette devices in which the measurements are made. As the applied shear stress is increased even further, there is evidence that the SIS fractures give rise to a shear-rate-independent stress and an apparent viscosity, which decreases with increasing shear rate. After the SIS fractures, large flu...
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