Abstract

When a mixture of viscous oil and non-colloidal particles displaces air between two parallel plates, the shear-induced migration of particles leads to the gradual accumulation of particles on the advancing oil–air interface. This particle accumulation results in the fingering of an otherwise stable fluid–fluid interface. While previous works have focused on the resultant instability, one unexplored yet striking feature of the experiments is the self-similarity in the concentration profile of the accumulating particles. In this paper, we rationalise this self-similar behaviour by deriving a depth-averaged particle transport equation based on the suspension balance model, following the theoretical framework of Ramachandran (J. Fluid Mech., vol. 734, 2013, pp. 219–252). The solutions to the particle transport equation are shown to be self-similar with slight deviations, and in excellent agreement with experimental observations. Our results demonstrate that the combination of the shear-induced migration, the advancing fluid–fluid interface and Taylor dispersion yield the self-similar and gradual accumulation of particles.

Highlights

  • Particle-laden flows have been studied extensively both theoretically and experimentally, owing to their relevance in avalanches and mudflows (Savage & Lun 1988; Gray & Ancey 2009; Gray & Kokelaar 2010), three-dimensional printing of complex fluids (Lewis 2006; Roh et al 2017) and cell migration in biological systems (Vejlens 1938; Zhou & Chang 2005)

  • Zhou & Chang (2005) demonstrated that the accumulation of red blood cells at the meniscus causes the penetration failure of blood suspensions into a capillary with a diameter smaller than 100 micrometres, which is a major obstacle in miniaturising blood diagnostic tools

  • Summary and conclusions In summary, our work has focused on understanding the self-similar behaviour of particle accumulation observed in suspension flow, through experiments and theoretical modelling

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Summary

Introduction

Particle-laden flows have been studied extensively both theoretically and experimentally, owing to their relevance in avalanches and mudflows (Savage & Lun 1988; Gray & Ancey 2009; Gray & Kokelaar 2010), three-dimensional printing of complex fluids (Lewis 2006; Roh et al 2017) and cell migration in biological systems (Vejlens 1938; Zhou & Chang 2005). Connecting shear-induced migration to particle accretion, particles migrate towards the channel centreline in pressure-driven flow and assume a higher particle average velocity than that of the fluid upstream of the interface This velocity differential results in a net flux of particles towards the meniscus and causes particle accumulation (Xu, Kim & Lee 2016; Luo, Chen & Lee 2018). Xu et al (2016) experimentally characterised fingering patterns for varying particle volume fractions They successfully validated the effects of shear-induced migration that leads to the accumulation of particles on the advancing oil–air interface, which was followed by the exploration of the role of channel confinement (Kim, Xu & Lee 2017) and linear stability analysis to predict the critical wavenumber (Hooshanginejad, Druecke & Lee 2019).

Materials and methods
Theory
Model assumptions and multiple-time-scale expansion
Leading order solutions
Particle transport equation and self-similarity
Simulation results: comparison with experiments
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