2013
DOI: 10.1122/1.4809732
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Rheology of sedimenting particle pastes

Abstract: We study the local and global rheology of non-Brownian suspensions in a solvent that is not density-matched, leading to either creaming or sedimentation of the particles. Both local and global measurements show that the incomplete density matching leads to the appearance of a critical shear rate above which the suspension is homogenized by the flow, and below which sedimentation or creaming happens. We show that the value of the critical shear rate and its dependence on the experimental parameters are governed… Show more

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Cited by 12 publications
(17 citation statements)
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“…4b and 4c, respectively. The corresponding values of µ 0 ~ 0.5 and η eff ~ 10 4 are consistent with those found in literature 8,9,27 . Similarly to previous studies [18][19][20][21][22][23][24][25][26][27][28] , we consider the effect of horizontal vibration as a controlled perturbation, or effective temperature, that modifies the mechanical properties of granular media such as yield stress and effective viscosity.…”
Section: Discussionsupporting
confidence: 91%
“…4b and 4c, respectively. The corresponding values of µ 0 ~ 0.5 and η eff ~ 10 4 are consistent with those found in literature 8,9,27 . Similarly to previous studies [18][19][20][21][22][23][24][25][26][27][28] , we consider the effect of horizontal vibration as a controlled perturbation, or effective temperature, that modifies the mechanical properties of granular media such as yield stress and effective viscosity.…”
Section: Discussionsupporting
confidence: 91%
“…Dispersions of non-Brownian particles in Newtonian fluids (i.e., granular suspensions) display a wide array of rheological behaviors: yield stress [17][18][19][20], shear banding [17,19,21], shear thickening [22,23], and normal stress dilation [24][25][26], to name a few. Most important to the work presented here is the phenomenon known as resuspenion; the process in which an initially settled layer of negatively buoyant particles are remobilized and convected into the surrounding bulk fluid.…”
Section: Introductionmentioning
confidence: 99%
“…The instantaneous settling velocity v or acceleration a is obtained by numerically differentiating z or v over a time interval. These experimental results are then analyzed with the granular rheology law µ(I) revealed in dry packings [3], being extended to dense granular suspensions [4][5][6][7]. We find that external shaking primarily affects the yield stress [8][9][10] and consequently controls the depth of sinking.…”
Section: Introductionmentioning
confidence: 93%
“…The Reynolds number Re = F i /F v ~ 10 -4 is very small and also the Stokes number St = U p d 2 K f (dJ/dt) i 1 with the density of glass grains U p = 2500 kg/m 3 and the strain rate dJ/dt ~ (dz/dt)/R, indicating that viscous forces dominate at the particle scale and the internal time is given by a viscous scaling. In this case, the constitutive equation for the frictional rheology can be written as [4,6,7]:…”
Section: Frictional Rheologymentioning
confidence: 99%
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