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An investigation of the behavior of a classifying hydrocyclone with pseudoplastic fluids

Abstract

The procedure usually employed for specifying a set of hydrocyclones used in Newtonian fluid-solid separation processes can be extended to the case of non-Newtonian fluids. The apparent viscosity, µapp, is the link between the two cases, and can be evaluated from the knowledge of the shear stress function, S, and the characteristic rate of shear, λ*. In order to verify the validity of this, experiments using suspensions of different solids in an aqueous solution of carboxymethylcellulose (CMC), with pseudoplastic behavior, in an AKW commercial hydrocyclone have been performed. The results obtained in this work indicated that the separation process and the pressure drop in the hydrocyclone cannot be characterized by a single apparent viscosity associated parameter.

Solid-fluid separation; Hydrocyclone; Non-Newtonian fluid


FLUID DYNAMICS; HEAT AND MASS TRANSFER; AND OTHER

An investigation of the behavior of a classifying hydrocyclone with pseudoplastic fluids

C. M. Scheid* * To whom correspondence should be addressed ; L. A. Calçada, R. S. A. Gonçalves; G. Massarani

DEQ/IT/Federal Rural University of Rio de Janeiro, BR 465, km 7, CEP: 23890-000, Seropédica, RJ - Brazil. E-mail: scheid@ufrrj.br

ABSTRACT

The procedure usually employed for specifying a set of hydrocyclones used in Newtonian fluid-solid separation processes can be extended to the case of non-Newtonian fluids. The apparent viscosity, µapp, is the link between the two cases, and can be evaluated from the knowledge of the shear stress function, S, and the characteristic rate of shear, λ*. In order to verify the validity of this, experiments using suspensions of different solids in an aqueous solution of carboxymethylcellulose (CMC), with pseudoplastic behavior, in an AKW commercial hydrocyclone have been performed. The results obtained in this work indicated that the separation process and the pressure drop in the hydrocyclone cannot be characterized by a single apparent viscosity associated parameter.

Keywords: Solid-fluid separation; Hydrocyclone; Non-Newtonian fluid.

INTRODUCTION

Several studies have been carried out in order to improve the analysis and design of the performance of hydrocyclones. Most of these have focused on the study of the equipment operation using Newtonian fluids. The classical formulation developed along several years establishes that the equipment performance depends upon its dimensions, the relative proportions among them (hydrocyclone configuration), the physical properties of the particle system (e.g., solid and fluid densities, fluid viscosity, and particle size distribution), and the operational conditions (e.g., fluid flow rate and feed solids concentration). Following the classical approach, the evaluation and characterization of hydrocyclones is generally performed by the separation cut diameter, the total and grade efficiencies, and the relation between flow rate and pressure drop (Bradley, 1965, and Svarovsky, 1981 and 1984).

The cut diameter represents the diameter of the particle that has a 50% probability of ending up in either the coarse or the fine product, and may be evaluated by the following equation, as proposed by Svarovsky (1981):

where K is a constant which takes into account the equipment geometry, Dc is the diameter of the cylindrical part of the cyclone, Cv is the volumetric concentration of solids in the feed, and Rf is the underflow-to-throughput ratio (by volume), defined as the ratio of the underflow to the feed flow volumetric rates.

The function f(Rf) is related to the correction of the stream splitting effect, in such a way that the value of D* obtained for the centrifugal separation is greater than the value of D* obtained considering the whole separation. This may be explained by the fact that the hydrocyclone efficiency is related to two phenomena: one being the centrifugal separation efficiency and other being the effect of dividing the main flow of the suspension in two (overflow and underflow), creating an inherent efficiency of the equipment, which has nothing to do with the field caused by centrifugal flow. Regarding the effect of the solids concentration in the feed, the correction is performed by the function g(Cv). This is explained by the fact that, in hydrocyclones as well as in other separation devices, the increase in the solids concentration results in a increase of the cut diameter and, therefore, a decrease in the total efficiency (Svarovsky, 1990).

The grade efficiency represents the efficiency with which each size of particle is separated, and it is evaluated based on the feed and underflow particle size distribution and the global efficiency. It is given by:

where η is the total efficiency, D is the particle diameter, and X and Xu represent the weight fraction of particles smaller then a given diameter for the feed and underflow, respectively. In order to analyze the efficiency of the centrifugal field alone, the reduced grade efficiency may be evaluated from:

which takes into account the separation due to the centrifugal field alone.

In the study of hydrocyclone performance it is customary to work with reduced grade efficiency as a function of D / D *. This is because the efficiency curve obtained in this case is constant for geometrically similar cyclones. The efficiency curve is not a function of system operating conditions (Svarovsky, 1981) nor of the size distribution of solid particles in the hydrocyclone feed (Lynch and Rao, 1975). The literature also offers several empirical equations for G' as a function of D / D * (Bradley, 1965; Plitt, 1971; Lynch and Rao, 1968; Lynch et al., 1974; Rao et al., 1976).

The total efficiency is related to G' (D) and Rf through the following equation:

Finally, according to Svarovsky (1984), in order to complete the characterization of the hydrocyclone it is necessary to establish the relation between the flow rate and pressure drop, which is given by:

where uc is the fluid velocity in the cylindrical section of the hydrocyclone.

Equations (1) to (5) establish the formulation developed for hydrocyclones when operating with Newtonian fluid-solid suspensions. The published literature on the operation of hydrocyclones using non-Newtonian fluids can be divided into two groups. The first group focuses on the experimental observation of the separation phenomena that take place inside the equipment, presenting empirical equations for evaluation of its performance (Lynch and Rao, 1975; Plitt, 1971; Linch and Rao, 1968; Lynch et al., 1974; Rao et al., 1976; Lilge, 1961, 1962; Napier-Munn, 1980; Upadrashta and Venkateswarlu, 1983; Walker et al., 1992; Horsley et al., 1992; Yoshida et al., 2004). The second group focuses on the mathematical modeling of the fluid flow in the body of the hydrocyclone and also in the fluid boundary layer adjacent to the equipment internal walls. As a result of this approach, fluid velocity profiles are obtained by solving the momentum and continuity equations. These velocity profiles are used in the determination of the particle trajectory and, consequently, the collection efficiency of the equipment (Upadrashta et al., 1987; Barrientos and Concha, 1992; Dyakowski et al., 1994; Yablonskii, 2000; Tavares et al., 2002; Yablonskii, 2004; Yablonskii, 2005; Yablonskii and Ryabchuk, 2005; Brenan et.al., 2007; Davailles et. al., 2012).

The present contribution aims at validating the classical formulation for operation of hydrocyclones using Newtonian fluids and to extend its applicability to the operation using non-Newtonian fluids. The strategy consists of replacing the fluid viscosity by an apparent viscosity, which can be calculated from the shear stress function S (which is a material property of the fluid), and the characteristic rate of shear λ* (which is a kinematic property of the flow). The apparent viscosity is given by:

Attempts to establish the expression of the flow characteristic rate of shear for this system, as well as for others, use mostly dimensional analysis combined with results from experiments with non-Newtonian fluids. We mention, for instance, the work developed by Massarani and Silva Telles (1978) and Laruccia (1990), on the study of non-Newtonian fluid flow in the surroundings of solid particles, which resulted in the following expression for λ*:

where θ(φ,β) is a function of the particle sphericity and the ratio of the particle to the tube diameter, u is the fluid velocity and v is the solid particle velocity, u - v is the relative fluid-particle flow velocity, and dp is the diameter of a sphere with the same volume as the particle.

For the case of separation in hydrocyclones, the establishment of the general form of the characteristic shear rate equation is based on Equation (7) for the particle with the cut diameter, i.e.,

where vt is the terminal velocity in the centrifugal field of a particle with the cut diameter D*. In Stokes' flow, the terminal velocity of a particle of diameter D* and sphericity φ under a centrifugal field is given by:

where K1 is a shape factor which takes into account the particle sphericity (Pettyjohn and Christiansen, 1948),

where the sphericity, φ, is defined as

and r is the particle radial position in the hydrocyclone. In the present work, particles are considered to flow very close to the equipment wall (i.e., r = Rc ). The angular velocity ω can be expressed by:

where the parameters Ne , Va and also Rc depend on the hydrocyclone geometry. The cut diameter D* is calculated as suggested by Svarovsky (1981) from the following equation:

Inserting Equations (10) and (12) into Equation (9), and the resulting equation into Equation (8), and also noting that

, the following expression for λ* is obtained:

or

Equation (15) provides the form of the shear rate that characterizes globally the separation process of the particles in the centrifugal field established in the interior of the hydrocyclone. This equation is a function of the cut diameter, the fluid velocity in the cylindrical section of the equipment, and the parameter β. This parameter, which is actually a function of the particle sphericity and the cyclone geometry, should be determined experimentally using non-Newtonian fluids. Experiments showed that the parameter β apparently depends only upon the equipment configuration.

EXPERIMENTAL

The experimental work was divided into two parts. The first part included experiments with Newtonian fluids aimed at performing the characterization of the hydrocyclone, i.e., to obtain the efficiency relations, cut diameter, and pressure drop following the classical hydrocyclone formulation. The second part was similar to the first one, but experiments were conducted using non-Newtonian fluids and the goal was to study the apparent viscosity so as to establish a link between the two situations under consideration (i.e., Newtonian versus non-Newtonian fluid operation).

The experimental set-up is presented in Figure 1. The apparatus consisted basically of a tank for the suspension connected to a centrifugal pump, responsible for pumping the suspension to the hydrocyclone. Mechanical stirrers were used in order to maintain the homogeneity of the suspension in the tank. The outlet flow rates of the system were redirected to the suspension tank in order to create a closed loop. A by-pass system was used to control the feed flow rate (see Figure 1). The pressure drop was measured by a pressure gauge installed in the feed tubing.


An AKW hydrocyclone (model KRS-98) was used in the experiments. The hydrocyclone presents a diameter of the cylindrical section of 4.5 cm and diameter of the underflow section of 1.4 cm (see Figure 2). The equipment was built of polyurethane.


In order to quantify the hydrocyclone performance in each experiment, the following variables were measured: temperature of the suspension, feed static pressure, feed solids concentration, underflow, overflow, feed and underflow particle size distribution, and the fluid rheograms in the non-Newtonian fluid experiments. The concentration and flow rates were determined by using gravimetric analysis.

In the first part of this work, experiments using water and dolomite, hematite and alumina particles, with densities of 2,800, 4,800 and 3,300 kg/m3, respectively, were performed in order to characterize the hydrocyclone. In the following part, experimental runs using non-Newtonian fluid were carried out using an aqueous solution of CMC. Adding CMC to water, the solution acquired a pseudoplastic behavior. The CMC solutions were prepared by adding pure water over CMC powder previously weighed at different concentrations of 0.5 to 1.5% by weight. This was done inside a small mixer under strong agitation. The mixture was agitated for two hours and left to rest for half an hour. This procedure was repeated three times to ensure that CMC was completely solubilized. The final solution was then transferred to the tank of the experimental hydrocyclone apparatus. Three fluid samples were collected for rheology testing in a capillary viscometer. All these procedures were performed at the same temperature as the hydrocyclone separation. After that, we added solid particles to the non-Newtonian fluid to proceed with the hydrocyclone separation. This suspension was used two or three days in a row and then discarded. As solid particles we used dolomite and alumina. The particle-size distributions are shown in Figure 3.


The particle size distribution of the solids in the flow streams was obtained from aqueous suspension tests in a modified Andreasen pipette. It was observed that all the experimental particle size distribution curves were well fitted by the Rosin-Rammler-Bennet (RRB) model, given by the following equation:

where X is the weight fraction of particles whose diameter is smaller than D. D' and m are the model parameters representing, respectively, the particle diameter corresponding to X=0.632 and the dispersion.

The non-Newtonian fluid rheology was determined by a capillary viscometer. The rheology measurement was performed at the operation temperature of the hydrocyclone. The capillary viscometer consisted of a peristaltic pump that maintained a constant volumetric flow in a tube of known diameter (diameter 2.39x10-3 m and length 1.268 m). The non-Newtonian fluid flow laminar regime inside this tube, where the pressure drop (gauges) and mass flow (scale's accuracy was 0.0001 g), were measured. With the volumetric flow and pressure drop data, we calculated the shear stress and shear rate by classical literature equations for fluid flow in pipelines. Table 1 shows the results obtained for the rheology of the non-Newtonian fluids used in this work. The shear stress and shear rate data given in Table 1 were fit according to the power-law model (S=Mλn), behaving as a pseudoplastic fluid and representing the aqueous solution of CMC without solid particles. The parameter M presents an average deviation of 0.0004 kg/ms2-n and n of 0.006. The symbol A was used to identify the experiments performed with alumina and the symbol D with dolomite. The temperatures of the experiments ranged from 25 to 35 °C.

In total, 34 experimental runs were performed using water and 18 using the non-Newtonian fluid, made of an aqueous solution of CMC with pseudoplastic behavior. The following operational variable ranges were imposed on the hydrocyclone:

• Pressure drop: 103 - 276 KPa;

• Suspension temperature: 25 - 35 °C;

• Feed volumetric solid concentration: 0.5 - 2.0%;

• Feed volumetric flow rate: 5 - 11m3/h;

• Underflow-to throughput (Rf): 0.17 - 0.24.

RESULTS AND DISCUSSION

Reduced Grade Efficiency

For each experiment, the reduced grade efficiency was calculated by Equation (2) and from the results of the grade analyses of the feed and underflow and total efficiency. In order to study the centrifugal separation alone, the particle reduced grade efficiency was calculated from Equation (3), and then the experimental cut diameter that corresponds to the diameter for G' = 50%.

The experimental results of the reduced grade efficiency and cut diameter for both Newtonian and non-Newtonian fluid experiments are shown in Figure 4.


From this figure it is possible to observe that the results obtained for the experiments with water and CMC are very similar to each other, and no clear distinction between the separation curves can be noticed. The dotted line in this figure gives the confidence interval of the fitted curve. Therefore, both Newtonian and non-Newtonian fluid experimental data were used for fitting the curve shown in Figure 4. The dispersion observed in the data is expected and has already been reported in the literature (Svarovsky, 1990). The following expression was obtained for the individual reduced grade efficiency:

The variances of the parameters 0.5 and 0.7 were on the order of 5%.

Cut Diameter

The results obtained for the cut diameter from the Newtonian fluid experiments were used for estimating the constant K in Equation (1). The correlation of Damasceno, Clark and Massarani (1990) for the volumetric concentration of solids in the feed was adopted in the present work. Their empirical correlation was obtained by studying the fluid dynamics of dilute suspensions and is given by:

This result seems not to depend upon the nature of the fluid and the particle's shape.

A correlation to fix the influence of Rf on the cut diameter, f(Rf), may be obtained from experiments by varying the underflow diameter under different operational conditions. Alternatively, it is possible to rearrange Equation (1) as:

where K*(Rf)=Kf(Rf). Therefore, from the experimental data of D* using a Newtonian fluid and from the operational conditions of the hydrocyclone, the following expression for K*(Rf) was obtained:

Pressure Drop

The results obtained for the pressure may be represented by the following correlation:

where

.

where µ is the viscosity of the Newtonian fluid or the apparent viscosity of the non-Newtonian fluids.

Table 2 summarizes the characterization of the AKW model KRS-98 hydrocyclone. It is worthwhile mentioning that the correlation given by Equation (17) is valid for both Newtonian and non-Newtonian fluid operation.

Apparent Viscosity - Centrifugal Separation

This section aims to extend the use of the equations developed for Newtonian fluids for the case of operation with non-Newtonian fluids. As mentioned previously, this may be performed by defining an apparent viscosity, µapp, which is intended to replace the fluid viscosity in the classical hydrocyclone modeling. It is necessary, however, to establish the correlation for λ* (Equation (15)), which relies directly on the particle sphericity and hydrocyclone geometry.

In the experiments using CMC, the cut diameter was obtained from the reduced grade efficiency results, obtained in the hydrocyclone characterization described in the previous sections. Equations (4) and (17), together with the total efficiency and the feed particle size distribution, given by Equation (16), were used in order to obtain D*. From the operational conditions and the knowledge of D*, Equation (19) and (20) were used in the calculation of the apparent viscosity given in Table 3. Finally, with the aid of the non-Newtonian fluid data (Table 1), like the typical rheological curve illustrated in Figure 5, the characteristic shear rate was obtained.


Table 3 presents the characteristic shear rate results obtained from the non-Newtonian fluid experiments. It is possible to note that the apparent viscosities are larger than the water viscosity, which leads to low deformation rates. This result suggests that the separation takes place in the boundary layer near to the internal wall of the hydrocyclone under low rate of shear and high viscosities, as previously suggested by Bloor et al. (1993) and Ingram and Laverack (1980). This behavior is related to a pseudoplastic fluid that has a high apparent viscosity at low shear rates and low apparent viscosity at high shear rates. It is important to highlight that some experiments with non-Newtonian fluids were not used in this determination. In some cases, the characteristic shear rate calculated presented results beyond the range of the same variable obtained experimentally.

Regarding the non-Newtonian fluid experiments using dolomite and alumina particles, the arithmetic average value of λ* was determined and is given by:

The total efficiency can be predicted by Equation (22) with the knowledge of the operational conditions of the experiment, the particle size distribution of the feed flow and the rheological curve of the non-Newtonian fluid.

Table 4 presents the comparison between experimental and calculated values of the total efficiency. One can observe a good fit between the experimental and calculated total efficiency with a deviation of less than 10%.

Apparent Viscosity - Pressure Drop

The experimental pressure drop and fluid flow velocity data in the cylindrical section of the hydrocyclone were used in order to determine the Reynolds number in the experiments using CMC (see Equation (21)). Then, the apparent viscosity was calculated from the definition of the Reynolds number:

In Table 5 the estimates of µapp calculated from Equation (23) are presented. The values obtained for the apparent viscosity are very close to the viscosity of water. This suggests that, as far as pressure drop is concerned, the viscosity is lower than that related to the separation process itself. This result has also been reported by Bloor, Ingram and Laverack (1980).

In this case, the shear rate applied to the flow is high and leads to low apparent viscosity, which is in accord with pseudoplastic fluid behavior. From these results, it would be possible to determine an expression for the characteristic shear rate related to the pressure drop in the equipment, in analogy to the previous section. However, the apparent viscosities obtained from the Reynolds number calculations lead to very high values of the shear rate when calculated by the rheological equations given in Table 1, which were not determined experimentally.

In order to investigate the apparent viscosity behavior at high shear rate, a sample of an aqueous solution of CMC with the same concentration range and rheological behavior as the one employed in the experimental study of a non-Newtonian fluid was prepared. The fluid rheological curve was obtained at an average temperature of 30 °C. Figure 6 presents the results of this test. A continuous decrease can be observed in the apparent viscosity as the shear rate increases, ultimately approaching the viscosity of water. This result supports the behavior observed in the experimental data presented in Table 5.


CONCLUSIONS

Regarding the operational conditions used in this work, an aqueous solution of CMC with a pseudoplastic behavior (n<1), a low concentration of solid particles and the hydrocyclone model provided the theoretical and experimental results that led to the following conclusions:

• The reduced grade efficiency curve as a function of D/D* is not influenced by the non-Newtonian fluid behavior, and is also quite similar to the grade reduced efficiency curve obtained using a Newtonian fluid (see Figure 4);

• The use of the concept of an apparent viscosity in the separation of solid non-Newtonian fluid mixtures was found to be possible. Considering the rheological behavior of pseudoplastic fluids, it was found that the apparent viscosity determined for the cut diameter in the centrifugal separation is greater than the apparent viscosity determined for the study of the relationship between fluid flow and pressure drop;

Regarding the case of centrifugal separation, the characteristic shear rate may be computed from Equation (22). The separation takes place near the internal walls of the hydrocyclone at low deformation rates and high viscosities. The total efficiency of each experiment can be calculated from the expression for λ* and from the operational conditions, particle size distribution, and fluid rheogram.

As far as the pressure drop is concerned, an expression for λ* could not be derived. The reason for this lies in the fact that the apparent viscosities determined from the Reynolds number led to high shear rates, which were outside of the rheological measurement range. It is worth mentioning that, at a given pressure drop, the apparent viscosity results are considerably lower than those determined for the separation, and slightly greater than the viscosity of water.

ACKNOWLEDGMENTS

We gratefully acknowledge the financial support provided by CNPq and CAPES.

REFERENCES

Barrientos, A. and Concha, F., Phenomenological Model of Classification in Conventional Hydrocyclones. In: Comminution - Theory and Practice, American Institute of Mining, Metallurgical and Petroleum Engineers, New York, Chapter 21, p. 287-305 (1992).

Bloor, M. I. G., Ingham, D. B. and Laverack, S. D., An analysis of boundary layer effects in a hydrocyclone. 1st International Conference on Hydrocyclone, Cambridge, UK, p. 49 (1980).

Bradley, D., The Hydrocyclone. Pergamon Press, London (1965).

Brennan, M. S., Narasimha, M., Holtham, P. N., Multiphase modeling of hydrocyclones - prediction of cut-size. Minerals Engineering, 20(4), 395-406 (2007).

Damasceno, J. J. R., Clark, S. and Massarani, G., Rheology of suspension and the effects of particles concentration on the particle dynamic II. XVIII Brazilian Meeting in Porous Media, v. 1, p. 103, Nova Friburgo, Rio de Janeiro (1990). (In Portuguese).

Davailles, A., Climent, E., Bourgeois, F., Majumder, A. K., Analysis of swirling flow in hydrocyclones operating under dense regime. Minerals Engineering, 31, 32-41, (2012).

Dyakowsky, T., Hornung, G. and Williams, R. A., Simulation of non-Newtonian flow in a hydrocyclone. Trans. IchemE, 72, 515 (1994).

Horsley, R. R., Tran, Q. and Reizes, J., The effect of rheology on performance of hydrocyclone. 4th International Conference on Hydrocyclone, Cambridge, UK, p. 215 (1992).

Lilge, E. O., Hydrocyclone fundamentals. Bulletin Institution of Mining and Metallurgy, London, 71, 285-337 (1961-1962).

Lynch, A. J. and Rao, T. C., Studies on the operating characteristics of hydrocyclone classifiers. Indian

J. Technology, 6, 106-114 (1968).

Lynch, A. J., Rao, T. C. and Prisbey, K. A., The influence of hydrocyclone diameter on reduced efficiency curves. Int. J. Mineral Processing, 1, 173-181 (1974).

Lynch, A. J. and Rao, T. C. Modelling and scalle-up of hydrocyclone classifiers. Proceedings 11th Int. Mineral Processing Congress, Paper 9, p. 9-25 (1975).

Laruccia, M. B., Velocity sedimentation in non-Newtonian fluids; form and particles concentration effects. Master Dissertation, UNICAMP, Campinas, Brazil (1990). (In Portuguese).

Massarani, G. and Silva Telles, A., Non-Newtonian fluid flow in the neighborhood of solid particles. Brazilian Journal of Physics, 8(3), 550-562 (1978). (In Portuguese).

Napier-Munn, T. J., Influence of medium viscosity on the density separation of minerals in cyclones. 1st International Conference on Hydrocyclone, Cambridge, UK, p. 63 (1980).

Pettyjohn E. S. and Christiansen, E. B., Effect of particle shape on free-settling rates of isometric particles. Chem. Eng. Progress, 44(2), 157-172 (1948).

Plitt, L. R., The analysis of solid-liquid separation in classifiers. CIM Bulletin, 64, 42-47 (1971).

Rao, T. C., Nageswararo, K. and Lynch, A. J., Influence

of feed inlet diameter on the hydrocyclone behavior. Int. J. of Mineral Processing, 3, 357-363 (1976).

Svarovsky, L., Solid-Liquid Separation. Butterworths, London (1981).

Svarosky, L., Hydrocyclone. Holt, Rinchart & Winston, London (1984).

Svarovsky, L., Solid-Liquid Separation. Butterworths & Co. Ltd, 3rd Ed., London (1990).

Upadrashta, K. R. and Venkateswarlu, D., Tangential flow pattern of power-law fluids in a hydrocyclone. J. Powder Bulk Solids Tech., 7(4), 19-28 (1983).

Upadrashta, K. R., Ketcham, V. J. and Miller, J. D., Tangential velocity profile for pseudoplastic power-law fluids in the hydrocyclone - A theoretical derivation. International Journal of Mineral Processing, 20, 309-318 (1987).

Walker, K. J., Veasey, T. J. and Moore, I. P. T., A parametric evaluation of the hydrocyclone separation of drilling mud from drilled rock chippings. 4th International Conference on Hydrocyclone, Cambridge, UK, p. 121 (1992).

Yasblonskii, V. O., Hydrodynamics of non-Newtonian fluid flow in hydrocyclone. Russian Journal Applied Chemistry, 73(1), 102-107 (2000).

Yasblonskii, V. O., Flow hydrodynamics of non-Newtonian fluid in a cylindrical-conical hydrocyclone. Russian Journal Applied Chemistry, 77(6), 957-963 (2004).

Yasblonskii, V. O., Effect of rheological properties of the dispersion medium on separation of suspensions in hydrocyclones with various working space configurations. Russian Journal Applied Chemistry, 78(8), 1294-1300 (2005).

Yasblonskii, V. O. and Ryabchuk, G. V., Flow of a rheologically complex suspension in a cylindroconical hydrocyclone. Theoretical Foundations of Chemical Engineering 39(4), 333-339 (2005).

Yoshida, H., Takashina, T., Fukui, K., Iwanaga, T., Effect of inlet shape and slurry temperature on the classification performance of hydro-cyclones. Powder Technology, 140(1-2), 1-9 (2004).

(Submitted: May 2, 2012 ; Revised: October 29, 2012 ; Accepted: November 5, 2012)

  • Barrientos, A. and Concha, F., Phenomenological Model of Classification in Conventional Hydrocyclones. In: Comminution - Theory and Practice, American Institute of Mining, Metallurgical and Petroleum Engineers, New York, Chapter 21, p. 287-305 (1992).
  • Bloor, M. I. G., Ingham, D. B. and Laverack, S. D., An analysis of boundary layer effects in a hydrocyclone. 1st International Conference on Hydrocyclone, Cambridge, UK, p. 49 (1980).
  • Bradley, D., The Hydrocyclone. Pergamon Press, London (1965).
  • Brennan, M. S., Narasimha, M., Holtham, P. N., Multiphase modeling of hydrocyclones - prediction of cut-size. Minerals Engineering, 20(4), 395-406 (2007).
  • Damasceno, J. J. R., Clark, S. and Massarani, G., Rheology of suspension and the effects of particles concentration on the particle dynamic II. XVIII Brazilian Meeting in Porous Media, v. 1, p. 103, Nova Friburgo, Rio de Janeiro (1990). (In Portuguese).
  • Davailles, A., Climent, E., Bourgeois, F., Majumder, A. K., Analysis of swirling flow in hydrocyclones operating under dense regime. Minerals Engineering, 31, 32-41, (2012).
  • Dyakowsky, T., Hornung, G. and Williams, R. A., Simulation of non-Newtonian flow in a hydrocyclone. Trans. IchemE, 72, 515 (1994).
  • Horsley, R. R., Tran, Q. and Reizes, J., The effect of rheology on performance of hydrocyclone. 4th International Conference on Hydrocyclone, Cambridge, UK, p. 215 (1992).
  • Lilge, E. O., Hydrocyclone fundamentals. Bulletin Institution of Mining and Metallurgy, London, 71, 285-337 (1961-1962).
  • Lynch, A. J., Rao, T. C. and Prisbey, K. A., The influence of hydrocyclone diameter on reduced efficiency curves. Int. J. Mineral Processing, 1, 173-181 (1974).
  • Lynch, A. J. and Rao, T. C. Modelling and scalle-up of hydrocyclone classifiers. Proceedings 11th Int. Mineral Processing Congress, Paper 9, p. 9-25 (1975).
  • Laruccia, M. B., Velocity sedimentation in non-Newtonian fluids; form and particles concentration effects. Master Dissertation, UNICAMP, Campinas, Brazil (1990). (In Portuguese).
  • Massarani, G. and Silva Telles, A., Non-Newtonian fluid flow in the neighborhood of solid particles. Brazilian Journal of Physics, 8(3), 550-562 (1978). (In Portuguese).
  • Napier-Munn, T. J., Influence of medium viscosity on the density separation of minerals in cyclones. 1st International Conference on Hydrocyclone, Cambridge, UK, p. 63 (1980).
  • Pettyjohn E. S. and Christiansen, E. B., Effect of particle shape on free-settling rates of isometric particles. Chem. Eng. Progress, 44(2), 157-172 (1948).
  • Plitt, L. R., The analysis of solid-liquid separation in classifiers. CIM Bulletin, 64, 42-47 (1971).
  • Svarovsky, L., Solid-Liquid Separation. Butterworths, London (1981).
  • Svarosky, L., Hydrocyclone. Holt, Rinchart & Winston, London (1984).
  • Svarovsky, L., Solid-Liquid Separation. Butterworths & Co. Ltd, 3rd Ed., London (1990).
  • Upadrashta, K. R. and Venkateswarlu, D., Tangential flow pattern of power-law fluids in a hydrocyclone. J. Powder Bulk Solids Tech., 7(4), 19-28 (1983).
  • Upadrashta, K. R., Ketcham, V. J. and Miller, J. D., Tangential velocity profile for pseudoplastic power-law fluids in the hydrocyclone - A theoretical derivation. International Journal of Mineral Processing, 20, 309-318 (1987).
  • Walker, K. J., Veasey, T. J. and Moore, I. P. T., A parametric evaluation of the hydrocyclone separation of drilling mud from drilled rock chippings. 4th International Conference on Hydrocyclone, Cambridge, UK, p. 121 (1992).
  • Yasblonskii, V. O., Hydrodynamics of non-Newtonian fluid flow in hydrocyclone. Russian Journal Applied Chemistry, 73(1), 102-107 (2000).
  • Yasblonskii, V. O., Flow hydrodynamics of non-Newtonian fluid in a cylindrical-conical hydrocyclone. Russian Journal Applied Chemistry, 77(6), 957-963 (2004).
  • Yasblonskii, V. O., Effect of rheological properties of the dispersion medium on separation of suspensions in hydrocyclones with various working space configurations. Russian Journal Applied Chemistry, 78(8), 1294-1300 (2005).
  • Yasblonskii, V. O. and Ryabchuk, G. V., Flow of a rheologically complex suspension in a cylindroconical hydrocyclone. Theoretical Foundations of Chemical Engineering 39(4), 333-339 (2005).
  • Yoshida, H., Takashina, T., Fukui, K., Iwanaga, T., Effect of inlet shape and slurry temperature on the classification performance of hydro-cyclones. Powder Technology, 140(1-2), 1-9 (2004).
  • *
    To whom correspondence should be addressed
  • Publication Dates

    • Publication in this collection
      10 Jan 2014
    • Date of issue
      Dec 2013

    History

    • Received
      02 May 2012
    • Accepted
      05 Nov 2012
    • Reviewed
      29 Oct 2012
    Brazilian Society of Chemical Engineering Rua Líbero Badaró, 152 , 11. and., 01008-903 São Paulo SP Brazil, Tel.: +55 11 3107-8747, Fax.: +55 11 3104-4649, Fax: +55 11 3104-4649 - São Paulo - SP - Brazil
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