Prediction of Viscosity of Slurry Suspended Fine Particles Using Coupled DEM-DNS Simulation

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A publication of 2089 CHEMICAL ENGINEERING TRANSACTIONS VOL. 32, 2013 Chief Editors: Sauro Pierucci, Jiří J. Klemeš Copyright 2013, AIDIC Servizi S.r.l., ISBN 978-88-95608-23-5; ISSN 1974-9791 The Italian Association of Chemical Engineering Online at: www.aidic.it/cet Prediction of Viscosity of Slurry Suspended Fine Particles Using Coupled DEM-DNS Simulation Yuichi Yoshida, Taichi Katsumoto, Shun Taniguchi, Atsuko Shimosaka, Yoshiyuki Shirakawa, Jusuke Hidaka a Department of Chemical Engineering and Materials Science, Doshisha University,1-3, Tatara-Miyakodani, Kyotanabe, Kyoto 610-0321, Japan jhidaka@mail.doshisha.ac.jp Prediction of the apparent viscosity of a slurry suspended fine particles is important for developing slurrytreating processes. After Einstein s formulation for the apparent viscosity of a dilute, completely dispersed slurry, several viscosity equations were proposed. However, viscosity depends not only on the volume fraction of solid particles but also on many factors such as particle shape, particle interaction, the aggregation structure of suspended particles and the structure of fluid flow. A hybrid simulation employing the distinct element method (DEM) and the direct numerical simulation method (DNS) was developed to obtain the relation between these factors and the apparent viscosity of slurry suspended fine particles. The apparent viscosity of a completely dispersed slurry obtained by the simulation is in good agreement with the experimental and calculated values obtained by the empirical equations. Shear-thinning behavior due to the collapse of agglomerates with increase in mean shear rate was observed for the case of a slurry with agglomerated particles. This behavior was caused by the existence of so-called immobile water in the agglomerates. The influences of the shape of aggregation and particle interaction on the apparent viscosity are investigated by the simulation. 1. Introduction Prediction of the rheological properties of slurry is important for slurry treatment technology. In particular, these properties depend on the microscopic structures of suspended fine particles in the slurry, and the dispersion or aggregation state of the fine particles strongly affects the properties of the final products of industrial processes. Therefore, the detection and control of the dispersion state of fine particles in the slurry are required to derive the functional characteristics of the final products. Currently, the apparent viscosity of the slurry is used to detect the dispersion or the aggregation state of the particles. However, the relation between the apparent viscosity and the dispersion or aggregation state of the suspended particles in the slurry is not understood sufficiently well for it to be used in the control of the dispersion state of fine particles in the slurry. Since the prediction theory of the viscosity for a well-dispersed dilute suspension proposed by Einstein, many modifications of Einstein s equation for application to a higher concentration range have been proposed considering the interaction between particles; for example, Simha s modification (Simha,1952), Mooney s equation (Mooney,1951), and Thomas s equation (Thomas,1965). In real-world slurry treatment processes, however, most slurries show an agglomerative nature, and suspended particles form agglomerated particles. Usui et al. proposed an estimation method for the apparent viscosity of slurry containing agglomerated particles (Usui et al, 2001). However, the shape and size distribution of agglomerated particles in the slurry are not taken into consideration in the model. In this study, a hybrid simulation employing the distinct element method (DEM) and the direct numerical simulation method (DNS) was developed to predict the apparent viscosity of slurry suspended fine particles. The influences of particle concentration and degree of zeta potential on the apparent viscosity

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2094 4.3 Influence of particle diameter Figure 8 shows the influence of particle diameter of suspended particles on the relative viscosity. For well dispersed slurry, the relative velocity is not dependent on the particle size, though the agglomeration of suspended particles is observed in low shear velocity. Figure 8(c) shows the comparison of calculated relative viscosity with the measured ones for agglomerative slurry which the zeta potential is -10 mv and the particle concentration is 25.2 Vol.%. In the region of low shear velocity, the dependence of particle diameter for the relative viscosity is remarkable since the finer particles are easy to form the aggregates. 4.4 Influence of the structure of agglomerated particles on the apparent viscosity The apparent viscosity of the agglomerative slurry is greater than that of the dispersed slurry, and that of slurry suspended agglomerated particles with a block structure is larger than that of slurry suspended agglomerated particles with a chain structure. To estimate the effect of immobile water on the apparent viscosity of the agglomerative slurry, we tried to calculate the apparent solid concentration quantitatively. The apparent solid concentration could be calculated by using the threshold value of the velocity gradient. Using the apparent solid concentration, the apparent viscosity of the agglomerative slurry can be estimated by an empirical equation. 5. Conclusions The DNS-DEM hybrid simulation was developed to predict the apparent viscosity of slurries. The proposed method can be very reliable since the estimated relative viscosity of a completely dispersed slurry obtained by the proposed simulation is in good agreement with the measured and calculated values from the empirical formula. The shear-thinning behaviour resulting from the collapse of agglomerates due to an increase in the mean shear rate is observed in the case of agglomerative slurry. This phenomenon is due to the existence of the so-called immobile water contained in the agglomerates. The apparent solid concentration, which is obtained by regarding the volume of the immobile water as that of solid, is defined. With the apparent solid concentration, the apparent velocity of the agglomerative slurry can be estimated by an empirical equation. The apparent viscosity of the slurry depends on the shape of the aggregates in the slurry. The proposed simulation clarifies the relation between the apparent viscosity of slurry and the characteristics of the suspended particles in the slurry. References Cundall P. A., Strack O. D. L., 1979, A discrete numerical model for granular assemblies, Geotechnique, 29, 47 65. Kajishima T., Ohta T., Okazaki K., Miyake Y.. 1998, High-order finite-difference method for incompressible flows using collocated grid system, JSME,( B), Fluids and thermal engineering, 41, 830 839. Kajishima T., Takiguchi S., Hamasaki H., Miyake Y., 2001, Turbulence structure of particleladen flow in a vertical plane channel due to vortex shedding, JSME (B), 44, 526 535. Mooney M., 1951, The viscosity of a concentrated suspension of spherical particles, J. Colloid Sci., 6, 162 170. Mori Y., Ototake N., 1956, On the viscosity of suspensions, Chemical Engineering, 20,488-493 (in Japanese). Simha R., 1952, A treatment of the viscosity of concentrated suspensions. J. Appl. Phys., 23, 1020-1024. Thomas D. G., 1965, Transport characteristics of suspension: Viii. a note on the viscosity of Newtonian suspensions of uniform spherical particles, J. Colloid Sci., 20, 267 277. Usui H., Kishimoto K., Suzuki H., 2001, Non-newtonian viscosity of dense slurries prepared by spherical particles, Chem. Eng. Sci., 56, 2979 2989. Russel W. B., 1980, Review of the role of colloidal forces in the rheology of suspensions, J. Rheology, 24, 287-317.