Progress and Trends in Rheology V 1998
DOI: 10.1007/978-3-642-51062-5_299
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Multi-Structural Thixotropic Model

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“…This fitting is done by considering that the lineal variation of shear rate is a succession of step-changes, where each shear rate is kept constant for a small increment of time, t, and the initial viscosity of each increment does not change with shear rate. The latter consideration is not valid for dispersions that show shear-thinning behavior, when the viscosity changes with step changes of shear rate [33,34]. When the shear rate increases, the internal unions between Laponite particles can be stretched, giving a viscosity lower than the previous one, and further broken down.…”
Section: Rheological Behavior Under Flow Of the 2 Wt% Laponite Dispermentioning
confidence: 99%
“…This fitting is done by considering that the lineal variation of shear rate is a succession of step-changes, where each shear rate is kept constant for a small increment of time, t, and the initial viscosity of each increment does not change with shear rate. The latter consideration is not valid for dispersions that show shear-thinning behavior, when the viscosity changes with step changes of shear rate [33,34]. When the shear rate increases, the internal unions between Laponite particles can be stretched, giving a viscosity lower than the previous one, and further broken down.…”
Section: Rheological Behavior Under Flow Of the 2 Wt% Laponite Dispermentioning
confidence: 99%