ISSN 0015-4628, Fluid Dynamics, 2018, Vol. 53, No. 2, pp. 255–269. c Pleiades Publishing, Ltd., 2018. Original Russian Text c A.A. Gavrilov, A.V. Shebelev, 2018, published in Izvestiya Rossiiskoi Akademii Nauk, Mekhanika Zhidkosti i Gaza, 2018, No. 2, pp. 84–98. Single-Fluid Model of a Mixture for Laminar Flows of Highly Concentrated Suspensions A. A. Gavrilov 1* and A. V. Shebelev 2** 1 Kutateladze Institute of Thermophysics SB RAS, Novosibirsk, Russia 2 Siberian Federal University, Krasnoyarsk, Russia Received January 27, 2017 AbstractA model of laminar ow of a highly concentrated suspension is proposed. The model includes the equation of motion for the mixture as a whole and the transport equation for the particle concentration, taking into account a phase slip velocity. The suspension is treated as a Newtonian uid with an eective viscosity depending on the local particle concentration. The pressure of the solid phase induced by particle-particle interactions and the hydrodynamic drag force with account of the hindering eect are described using empirical formulas. The partial-slip boundary condition for the mixture velocity on the wall models the formation of a slip layer near the wall. The model is validated against experimental data for rotational Couette ow, a plane-channel ow with neutrally buoyant particles, and a fully developed ow with heavy particles in a horizontal pipe. Based on the comparison with the experimental data, it is shown that the model predicts well the dependence of the pressure dierence on the mixture velocity and satisfactorily describes the dependence of the delivered particle concentration on the ow velocity. DOI: 10.1134/S0015462818020064 Channel ows of a liquid-solid particlemixture are commonly encountered in engineering practice in many branches of industry. At low ow velocities in horizontal channels, the particles are deposited on the bottom wall, forming a dense layer of particles. Laminar ows of mixtures, which occur at low velocities and often with the formation of a layer of settled particles, have not been well understood. In laminar pipe ows of suspensions, an eective resuspension of particles is observed, caused by a transverse migration of particles (see, for instance, the review [1]). In a shear ow at small but nite particle Reynolds numbers, a slow migration of single particles from the wall is attributable to the onset of the Saman lift force exerted on a spherical particle by the shear ow [2, 3]. In dense suspensions, the eect of particle migration in the direction of reduced shear rate and particle concentration is detected in [4]. The particle migration eect explains the particle resuspension phenomenon observed when a shear stress is applied to a particle layer, with the subsequent removal of the particles in the carrier ow and erosion of the layer. The migration of particles caused by the particle-particle interactions was rst described for non- colloidal suspensions in paper [5], devoted to experimental studies of long-term transient processes in a Couette viscometer. Then, the eect of particle migration induced by shear was conrmed experimentally in a plane-channel [6] and a circular-pipe ow [7, 8]. The rst closed mathematical model of suspension ow with account of the particle migration eect, called the diusion model, was proposed in [9]. The model describes the appearance of a particle drift in a shear ow in the direction of decrease in the eective viscosity of the mixture and decrease in the shear rate. In a recent paper [10], a regularization of the diusion model was proposed to resolve the singularities in the region with a vanishingly small shear rate, and a parametric study of suspension ow in an inclined plane channel was performed, but no comparison with experiment was provided. The second class of empirical models uses the hypothesis of the onset of particle migration under the action of nonuniform normal stresses in the solid phase, with the isotropic part of these stresses, called the particle pressure, being associated with the energy of particle chaotic velocities. The Suspension * E-mail: gavand@yandex.ru. ** E-mail: aleksandr-shebelev@mail.ru. 255