Particle migration in a Couette apparatus: Experiment and modeling

Suspensions comprised of neutrally buoyant spheres in Newtonian fluids undergoing creeping flow in the annular region between two rotating, coaxial cylinders (a wide-gap Couette) display a bulk migration of particles towards regions of lower shear rate. A series of experiments are performed to chara...

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Bibliographic Details
Published inJournal of rheology (New York : 1978) Vol. 42; no. 2; pp. 307 - 327
Main Authors Tetlow, Nicholas, Graham, Alan L., Ingber, Marc S., Subia, Samuel R., Mondy, Lisa A., Altobelli, Steve A.
Format Journal Article
LanguageEnglish
Published 01.03.1998
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Summary:Suspensions comprised of neutrally buoyant spheres in Newtonian fluids undergoing creeping flow in the annular region between two rotating, coaxial cylinders (a wide-gap Couette) display a bulk migration of particles towards regions of lower shear rate. A series of experiments are performed to characterize this particle migration, including the influence of particle size, surface roughness, and volume fraction. Little, if any, effect of particle surface roughness is observed. An existing continuum diffusive-flux model [Phillips et al. (1992)] for predicting particle concentration profiles in monomodal suspensions is evaluated using the current series of experimental data. This model predicts a dependence of the migration rate on the square of the suspended particles’ radius, a 2 ; whereas the present experiments indicate that systems with average particle volume fractions of 50% display a rate that scales with a 3 . Previous use of the diffusive-flux model has assumed constant values for diffusion coefficients which serve as tuning parameters in the phenomenological equation. Here the experimental data are used to investigate variations of the model in which the diffusion coefficients depend upon either the local or global particle volume fraction. For initially uniform suspensions, the coefficients are found to be best modeled as functions of the local particle volume fraction.
ISSN:0148-6055
1520-8516
DOI:10.1122/1.550954