1986
DOI: 10.1122/1.549845
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Rheological effects of nonuniform particle distributions in dilute suspensions

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Cited by 44 publications
(9 citation statements)
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“…Subsequent work has shown that this phenomenon is quite general, being observed both experimentally and computationally in Poiseuille 3,4 and Couette [5][6][7] flows, and also as a function of particle density, 8,9 asphericity, and/or deformability. 10,11 The cause of migration in these flows has largely been attributed to buoyancy effects 12,13 and/or non-linear fluid effects, [14][15][16] which arise at moderate Reynolds numbers; however, particle migration has also been observed in dense multiparticle flows even in the case of vanishing Reynolds number (that is, an ideal Stokes' flow). This is credited to hydrodynamic interactions between the particles 17 and termed "shearinduced migration."…”
Section: Introductionmentioning
confidence: 97%
“…Subsequent work has shown that this phenomenon is quite general, being observed both experimentally and computationally in Poiseuille 3,4 and Couette [5][6][7] flows, and also as a function of particle density, 8,9 asphericity, and/or deformability. 10,11 The cause of migration in these flows has largely been attributed to buoyancy effects 12,13 and/or non-linear fluid effects, [14][15][16] which arise at moderate Reynolds numbers; however, particle migration has also been observed in dense multiparticle flows even in the case of vanishing Reynolds number (that is, an ideal Stokes' flow). This is credited to hydrodynamic interactions between the particles 17 and termed "shearinduced migration."…”
Section: Introductionmentioning
confidence: 97%
“…The rougher the fracture wall, the greater the velocity of particles in comparison with the mean flow velocity. Such an effect was noted first, probably, by Small et al (1976), and an attempt at its interpretation was made by McTigue et al (1986). Champ and Schroeter (1988) and Harvey et al (1989) stated that, in their field experiments, the rate of migration of colloidal particles in the geologic medium was much higher than the mean velocity of subsurface water flow.…”
Section: Mobility Of Colloidal Particlesmentioning
confidence: 92%
“…However, it is also possible to obtain the particle velocity directly as described by Meyer [150]. Recently, McTigue et al [151] developed a continuum mixture theory for the slow flow of a dilute suspension of solid particle in a viscous fluid.…”
Section: Role Of Hydrodynamics In Deposition Processesmentioning
confidence: 99%