Proceedings of the ASME th Joint US-European Fluids Engineering Division Summer Meeting FEDSM2014 August 3-7, 2014, Chicago, Illinois, USA

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Proceedings of the 4th Joint US-European Fluids Engineering Division Summer Meeting ASME-FEDSM2014 August 3-7, 2014, Chicago, Illinois, USA

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Proceedings of the ASME 2014 4th Joint US-European Fluids Engineering Division Summer Meeting FEDSM2014 August 3-7, 2014, Chicago, Illinois, USA FEDSM2014-21613 EXPERIMENTAL AND NUMERICAL INVESTIGATION OF THE EFFECT OF VISCOSITY AND PARTICLE SIZE ON THE EROSION DAMAGE CAUSED BY SOLID PARTICLES A. Mansouri, S. A. Shirazi, B. S. McLaury Erosion/Corrosion Research Center The University of Tulsa 800 S Tucker Drive, Tulsa, OK, 74104 E-mail: amir-mansouri@utulsa.edu ABSTRACT Oil and gas produced from wells usually contain impurities such as sand particles transported by fluid flowing through pipelines. The particles impinge on the pipe walls and fittings removing material from the wall and causes erosion damage. The effect of viscosity and particle size on the local thickness loss and total erosion ratio was investigated by conducting a comprehensive experimental study on the erosion of stainless steel 316 specimens caused by sand entrained in a submerged liquid jet. Two types of sand with sizes of 150 µm and 300 µm were used and added to liquids with 1, 14 and 55 cp viscosities. The tests were carried out for three different nozzle angles: 90 ⁰ (normal to target), 75 ⁰ and 45 ⁰. The results show that for the 90 ⁰ orientation, the total erosion ratio does not change significantly with increase in viscosity. The measurements also show that the erosion ratio for 300 µm sand is approximately two times higher than for 150 µm sand; where the erosion ratio is the mass loss of the target divided by the mass throughput of sand. The local thickness losses on the specimens were measured using a 3D profilometer, and the results show, maximum erosion depth is increasing as viscosity increases. Comparing the Scanning Electron Microscopy (SEM) images of the specimens after the test revealed that the crater sizes do not change very much with increases in viscosity. SEM images for both viscosities of 1 and 55 cp showed that the craters become longer moving radially outward from the the center of the impact zone. Computational Fluid Dynamics (CFD) simulations of erosion patterns are compared with data and they tend to under predict the total erosion ratio and local thickness loss for slurry flows as viscosity increases. NOMENCLATURE d p particle diameter, μm ER erosion ratio, kg/kg M sand sand rate, kg/s Re Reynolds number at the nozzle exit t test duration, second V f average fluid velocity at the nozzle exit, m/s W 1 coupon weight before the test, kg W 2 coupon weight after the test, kg z thickness loss from the coupon surface, μm θ impact angle (angle between nozzle and target surface), degree carrier fluid viscosity, cp μ f INTRODUCTION The erosion phenomenon is the consequence of repetitive impacts of sand particles transported by fluid flow through pipelines, with walls of fittings or other industrial equipment. In the oil and gas industry erosion damage causes leakage and abrupt failure of pipelines, bends and tees without prior warning, and can result in expensive repairs and loss of production time. Therefore, it is extremely crucial to predict the erosion rate and identify the location of the equipment which is most at risk. There are also other types of equipment for operations that involve small particles and consequently experience erosion problem, such as heat exchangers in fluidized bed combustors, steam-turbine blades in electric power generation plants and helicopter engine inlets and blades operating in sandy areas. For decades, significant research has been performed to understand the erosion mechanism and to 1 Copyright 2014 by ASME

develop erosion models for predicting the erosion rate in various pipe fittings and multiphase production situations [1-3]. Modeling and prediction of erosion rate is very challenging, since many factors such as particle impact speed, particle impact angle, particle hardness, shape, diameter, strength and material hardness affect the erosion process. Most of the previous studies of erosion rates were concerned with the effects of materials and particle characteristics including particle velocities and did not consider the effects of fluid medium. For example, Finnie [4] developed a theoretical erosion equation for vacuum conditions and proposed that the erosion mechanism for ductile material is micro-cutting, while material lost during erosion of brittle materials is as a result of lateral and radial cracks. Thereafter, numerous theoretical and empirical equations have been developed and reported in the literature. Bitter [5], Neilson and Gilchrist [6], McLaury et al. [7], Grant and Tabakoff [8], Huang et al. [9], Oka et al. [10] and Zhang et al [2] are among the erosion models most commonly reported in the literature which are either purely theoretical or empirical based but again they did not consider the effects of the fluid medium on the erosion process/models. Traditionally standard laboratory tests using a variety of testing devices Coriolis, slurry pot, toroid wheel, jet impingement or pipe loops have been used by researchers to study the erosion rate and develop empirical models [11]. Computational Fluid Dynamics (CFD) is another powerful tool for predicting particle impact velocity that is a common factor used to calculate erosion rates for different operating conditions and geometries. CFD simulations have been widely used to study the erosion rate, but CFD results must be validated by experimental data before they can be used to predict erosion rates accurately. It has been shown that erosion equations developed from either theory or experimental data can be implemented into CFD codes, and in some cases relatively good agreement between the CFD results and erosion measurements for simple geometries has been observed [2, 11, 12]. For instance, Zhang et al. utilized an erosion ratio equation extracted from erosion tests in air, in a commercially available code to predict erosion rates in gas and water. Relatively good agreement was observed between the experimental measurements and CFD results for flat specimens in water or air flow and 90º elbows in air flow. There are a few studies of wear pattern which are limited to water flows [12-14]. Previously, in order to study the effect of viscosity on erosion damage, Okita, et al. [15] measured the total erosion ratio caused by sand particles transported by liquids with various viscosities and compared to CFD results. The results showed that CFD calculations deviate from experimental measurements as viscosity increases. Nidasanametla [16] also measured the erosion damage caused by glass beads instead of sand particles. Glass beads are rounded and produce less damage compared to sand particles which have angular shapes. Similar to Okita s work, Nidasanametla also indicated that CFD results tend to under predict the erosion ratio as compared to experimental results, but the effect of viscosity on the particle impact speed and angle and consequently the local thickness loss has not been studied in the literature. In this study, the influence of carrier fluid viscosity on erosion damage is investigated experimentally and numerically. EXPERIMENTATION In order to improve the understanding of slurry erosion, a comprehensive experimental study on erosion caused by sand entrained in a submerged impinging jet was performed. The schematic of the flow loop is shown in Figure 1. A series of tests were conducted and total erosion ratio and local thickness loss (wear pattern) of the stainless steel (SS316) samples were measured. Two types of sand were used: Oklahoma #1 and California 60 with average sizes of 150 μm and 300 μm. The sand particles were added to liquid with viscosities of 1, 14 and 55 cp. The viscous liquid is prepared in a reservoir tank prior to experiments by mixing CMC (Carboxymethyl Cellulose) and water. CMC increases the viscosity of the liquid without a significant change in the density. Viscosity of the carrier fluid was measured by a vibrational viscometer before and after each test. Then, sand particles were mixed with the solution prepared for the desired viscosity in the reservoir tank. During the experiment, a slurry mixer was used to prevent the settling of the sand particles and maintaining the homogeneity of the mixture. Two pumps were used to maintain an average nozzle exit velocity of 14 m/s during the experiment. Pumps By Pass Valve Slurry Mixer Figure 1. Schematic of Experimental Facility (Submerged Impinging Jet Test). The prepared sand concentration inside the reservoir tank measured by weight was 1%; however, the actual sand concentration measured at the nozzle exit (by passing the mixture through a filter) was less than the sand concentration inside the tank. The sand concentration measured at the nozzle exit was used in the erosion ratio calculations. The total erosion ratio ER is obtained from Eqn. 1. kg W2 W1 ER( ) (1) kg M t sand Nozzle Coupon Reservoir Tank Where, W 1 (kg) and W 2 (kg) are the weight of the coupon before and after the erosion test, respectively. 2 Copyright 2014 by ASME

M sand (kg/s) is the sand rate and t (s) represents the duration of the test. The inner diameter of the nozzle used in the test loop was 8 mm, and the distance between the nozzle and coupon was 12.7 mm for all tests. In order to obtain measurable local erosion depth and total erosion ratio for all the tests, each test was performed for 6 hours. The key parameters in the experiments are summarized in Table 1. Figure 2 illustrates the effect of sand size on the erosion ratio, which indicates that the erosion ratio caused by 300 μm sand is approximately twice as high as that for 150 μm sand particles. The results also show that the erosion ratio does not change significantly as viscosity increases. For the results shown in Figure 2 the angle between the nozzle and target surface is maintained at 90º. Table 1. Key Parameters in experimental conditions Volumetric flow rate 0.000704 m 3 /s Average nozzle exit velocity (V f ) 14 m/s Nozzle diameter Nozzle-coupon distance 8 mm 12.7 mm Sand concentration in reservoir tank 1% Sand concentration at nozzle exit 0.5%±0.1 Impact angle (θ) Sand size (d p ) 90, 75 and 45 deg 150, 300 μm Coupon material Stainless Steel 316 Carrier fluid viscosity (μ f ) Test duration (t) 1, 14 and 55 cp 6 hours Based on the results shown in Figure 3, there is no significant difference between the erosion ratio measured for nozzle angles of 75º and 90º, but in the case of 45º, the erosion ratio decreases as viscosity increases. In addition to total erosion ratio calculated by measuring the total mass loss, local erosion depth (wear pattern) was also measured using a 3D profilometer instrument. A sample 3D scan of the specimen after an erosion test is shown in Figure 4. As the slurry flow reaches the target wall, the carrier fluid velocity reduces to zero at the wall. Since the carrier fluid velocity and consequently particle impact speed significantly decrease in this zone, less erosion is observed in this zone which is the called stagnation zone. As shown in Figure 5, after the stagnation zone, the fluid flow and particle impact speed increase and produce a highly eroded zone which is shown in Figure 4. There is also a slight thickness loss on the surface of target material, outside of the highly eroded zone which is marked in Figure 4. A symmetrical wear pattern is expected for normal impingement, but profilometry measurements show that the wear pattern on the specimen for some of the test conditions is not symmetrical (Figure 6). Two reasons might cause this non-symmetrical behavior: (1) small misalignment between the nozzle and specimen, (2) there is also swirling flow inside the nozzle which might be another reason for this behavior. Since studying the overall behavior of the radial erosion pattern is important, in this study a circumferential average of scanned profile every 5º is performed. This average profile for normal impingement, sand size of 300 μm and nozzle velocity of 14 m/s is plotted in Figure 7. As explained earlier, it is also assumed that the erosion depth at the stagnation point is nearly zero. This assumption is used for other results presented below. Error bars in this graph represent the variability of the erosion depths at different angles (as measurements for every 5 degrees are averaged). Figure 8 illustrates the effect of viscosity on the averaged erosion depths measured by 3D profilometry. It is expected that carrier fluids with higher viscosities exert higher drag forces on sand particles and reduce the particle impact speed and consequently cause less erosion damage. In despite of what is expected, the experimental results show that the maximum erosion depth for a carrier fluid with viscosity of 55 cp is higher than 1 cp (Figure 8). The reason for this observation can be explained by the difference in velocity profiles resulting from laminar and turbulent flows within the nozzle. In the case of higher viscosities, for the same average velocity of 14 m/s, the Reynolds number for flow in the nozzle reduces to 2100 which corresponds to laminar flow. For laminar flow at the nozzle exit, the velocity profile is parabolic, and this parabolic velocity profile contributes to higher sand particle speeds at the center of the nozzle which may cause higher impact speeds and consequently higher erosion depths for the case of higher viscosity carrier fluids. As mentioned earlier, one of the factors which can affect the erosion ratio is the particle size. In Figure 9, the effect of particle size on the thickness loss is investigated, and the results show that the maximum thickness loss for d p = 300 μm is approximately twice as high as the thickness loss caused by 150 μm sand particles. This confirms the ER results presented earlier in Figure 2. Erosion is a very complex phenomenon, and it is very important to obtain experimental results which are repeatable. To ensure the results are repeatable, each test is repeated two or three times. For instance, the repeatability of the wear pattern for θ=90º, d p =300 μm and μ f =1 cp is shown in Figure 10. This figure shows that the wear patterns for three different experimental tests with similar test condition are similar. Repeatable results are also obtained for θ=45º, d p =300 μm and μ f =1 cp which are shown in Figure 11. Because the wear patterns especially for non-normal impact angles are not symmetrical, it is better to examine the 3D contour of wear patterns, which are shown in Figure 12, Figure 12, Figure 13 and Figure 14 for different test conditions. The elevation of different zones (stagnation zone, highly eroded zone and coupon surface zone) is also shown in the figures. Comparing the wear pattern of μ f = 1 cp with μ f = 55 cp for normal impingement reveals that higher viscosities can cause higher thickness losses than water. As discussed earlier, the difference between the nozzle velocity profiles of laminar and turbulent flow is the reason of this observation. Wear patterns 3 Copyright 2014 by ASME

for θ=45º show that the stagnation point moves off the center of the coupon and oval-shaped profiles are produced. Instead of producing a highly eroded zone with circular shape, the eroded zone moves to the sides for θ=45º. Thickness loss also decreases for θ=45º compared to normal impingement. Stagnation Point Coupon Surface Highly Eroded Zone Figure 4. Different Zones of a Coupon Scanned After the Erosion Test Figure 2. Effect of Sand Size on Erosion Ratio Nozzle Stagnation Zone Highly Eroded Zone Figure 5. CFD Simulation of the Flow Field for the Submerged Impinging Jet Figure 3. Effect of Nozzle Angle on the Total Erosion Ratio Figure 6. Wear Pattern for Normal Impingement (μ f = 1 cp, d p =300 μm and V f =14 m/s) 4 Copyright 2014 by ASME

Figure 7. Circumferential Average of the Erosion Depth Profile Figure 10. Repeatability of Wear Profile (θ=90º, d P =300 μm) Viscosity increases Figure 11. Repeatability of Wear Profile (θ=45º, d P =300 μm) Figure 8. Effect of Viscosity on Erosion Depth (d P =300 μm, V f =14 m/s) Figure 9. Effect of Particle Size on Erosion Depth (μ f =1 cp, θ=90º) CFD SIMULATION CFD simulations have been performed for the same conditions as the measurements mentioned in Table 1. In the simulations, the length of the nozzle should be long enough to have a fully developed flow at the outlet of the nozzle. V f =14 m/s is used at the inlet of the nozzle for the inlet boundary condition. No-slip wall boundary condition is also imposed for the coupon surface and nozzle wall. For the cylinder surrounding the nozzle and coupon, a pressure outlet boundary condition is specified. The schematic of the computational domain is shown in Figure 16. The Shear- Stress Transport SST k-ω turbulence model is used for the simulations. In the simulations, the one-way coupling between the sand particles and carrier fluid is assumed, because in dilute suspensions sand particles slightly affect the fluid flow. But it is also worth mentioning that Matas et al. showed that suspended particles can influence the flow field and transition to turbulence [17]. The erosion equation used in this paper to predict erosion was generated at the Erosion/Corrosion Research Center of the University of Tulsa [2] and is provided in Eqns. (2-4): kg 0.59 n ER( ) Fs. C( BH ). V. F( ) (2) kg ( H 0.1023) BH V 0.0108 (3) 5 Copyright 2014 by ASME

(a) (a) (b) Z= 0 μm Z= -11.5 μm (b) Z= 0 μm Z= -8.6 μm Z= -166 μm Z= -118 μm Z= -198 μm Figure 12. Wear Pattern for (θ =90º, d P =300 μm and μ f = 1 cp) (a). Top View, (b). 3D Contour (a) Figure 14. Wear Pattern for (θ =90º, d P =300 μm and μ f = 55 cp) (a). Top View, (b). 3D Contour (a) (b) Z= 0 μm Z= 0 μm (b) Z= 0 μm Z= -27 μm Z= -87 μm Z= -129 μm Z= -84 μm Z= -90 μm Figure 13. Wear Pattern for (θ=45º, d P =300 μm and μ f = 1 cp) (a). Top View, (b). 3D Contour Figure 15. Wear Pattern for (θ =45º, d P =300 μm and μ f = 55 cp) (a). Top View, (b). 3D Contour 6 Copyright 2014 by ASME

Table 2. Constants for Erosion Equation (Stainless Steel 316) Parameter Value C 1.42E-7 n 2.41 H V (GPa) 1.5 F s 1 A -0.05065 B 0.04065 C 0.000539 D -3.97E-5 E 5.14E-7 F -2.07E-9 Figure 16. The Direct Impinging Jet Geometry, Dimensions and Boundary Conditions Applied in CFD Simulation F s is the sharpness factor of the sand particles, which ranges from 0.2 to 1, but for this type of sand F s =1. BH is the Brinell hardness of the target material which is calculated by H V, Vicker s hardness. V is the particle impact speed and F(θ) is the impact angle function. For these simulations, a polynomial function is used for the particle impact angle function: 2 3 4 5 A B C D E F (4) F( ) C and n are the empirical constants. The values for the constants in the erosion equation are shown in Table 2. The erosion patterns predicted by CFD simulation and measured by 3D profilometry are compared in Figure 19 and Figure 20. As experimental measurement show in the case of θ =90º, a ring of high erosion is generated which is also predicted by the CFD simulation. Figure 19 and Figure 20 show the predicted pattern and measured thickness loss, respectively for θ =45º. In this case, instead of a highly eroded ring, erosion depth increases on the sides of the center plane. As shown, in the case of θ =45º the CFD simulation also agrees well with the experimental data. Figure 21 shows the velocity profile at the jet exit for μ f =1 cp and μ f =55 cp. The results imply that μ f =55 cp leads to laminar flow and parabolic velocity profile at the jet exit. The higher velocities at the center of the jet exit, contributes to higher particle impact speeds and consequently higher erosion depth for the case of higher viscosity carrier fluids. Figure 22 compares the predicted total erosion ratio for μ f =1, 14 and 55 cp with experimental data. In agreement with literature [15, 16], CFD simulations of the present work also under predict the experimental data. This figure also shows that the velocity profile at the jet exit has an important effect on the total erosion ratio calculated by CFD For the CFD results mentioned in [14], [15] uniform velocity profile was assumed at the jet exit, while the current study reveals that solving the fluid flow inside the nozzle and obtaining a fully developed velocity profile at the jet exit can improve the erosion predictions. These results still indicate that CFD simulations predict that erosion rate and ratios are decreasing as fluid viscosity is increased, but the experimental data does not. This difference requires further research and investigation. Erosion rate (kg/m 2 s) Elevation (μm) Figure 17. Erosion Pattern Predicted by CFD Simulation (θ =90º, d P =300 μm and μ f = 1 cp) Figure 18. Thickness Loss Measured by 3D Profilometry (θ =90º, d P =300 μm and μ f = 1 cp) 7 Copyright 2014 by ASME

Erosion rate (kg/m 2 s) Elevation (μm) MICROSTRUCTURE Post-test analysis of the coupon surface is performed to investigate the shape and size of the craters in different zones of the coupon. As mentioned earlier, three different zones in terms of thickness loss are produced on the target materials which are shown in Figure 23. Elevation (μm) Stagnation zone Highly eroded zone Figure 19. Erosion Pattern Predicted by CFD Simulation (θ =45º, d P =300 μm and μ f = 55 cp) Figure 20. Thickness Loss Measured by 3D profilometry (θ =45º, d P =300 μm and μ f = 55 cp) Coupon surface Figure 23. Different Zones Produced on Coupon Surface after Erosion Test (θ=90º, μ f =55 cp) Figure 21. Velocity Profile at the Jet exit (μ f =1 cp, μ f =55 cp) Electron Scanning Microscope (SEM) images of the coupon, near the center are shown in Figure 24 and Figure 27and which represent the stagnation zone. Comparing the images for viscosities of 1cP and 55cP reveals that in this region the crater sizes do not change very much with varying fluid viscosity. Figure 25 and Figure 28 are SEM images of the coupon 6 mm from the center representing the highly eroded zone. Figure 26 and Figure 29 are the images of the coupon far enough form the center of the coupon to be considered representative of the coupon surface region. Two points are concluded from the SEM images: (1) crater size and shape for the same distance from the center of the impact area are similar for various viscosities. (2) by moving far away from the center of the impact area, craters become longer and sharper in comparison to the craters caused by sand particles near the stagnation zone. Figure 22. Comparison of Erosion Ratio Predicted by CFD Simulation with Experimental Data 8 Copyright 2014 by ASME

Figure 24. SEM Image of Coupon after the Erosion Test near the Center (Sand Size=150 μm, μ f = 1 cp) Figure 27. SEM Image of Coupon after the Erosion Test near the Center (Sand Size=150 μm, μ f = 55 cp) Figure 25. SEM Image of Coupon after the Erosion Test on 6 mm From the Center (Sand Size=150 μm, μ f =1cP) Figure 28. SEM Image of Coupon after the Erosion Test on 6 mm From the Center (Sand Size=150 μm, μ f =55cP) Figure 26. SEM Image of Coupon after the Erosion Test on 12 mm From the Center (Sand Size=150 μm, μ f = 1cP) Figure 29. SEM Image of Coupon after the Erosion Test on 12 mm From the Center (Sand Size=150 μm, μ f = 55 cp) 9 Copyright 2014 by ASME

CONCLUSIONS AND SUMMARY 1) A comprehensive experimental study of the influence of the carrier fluid viscosity and sand size on erosion damage is performed. It is found that increasing the viscosity does not have a significant effect on the total erosion ratio, while it increases the maximum erosion depth. Increasing the sand size also increases the erosion damage. 2) CFD simulations were conducted to predict the erosion ratio and erosion pattern for the same conditions that experimental tests were performed. It is shown that CFD simulations are capable of predicting the wear pattern for different impact angles (θ =45º, θ =90º), but CFD tends to under predict the total erosion ratio. It is also found that obtaining a fully developed velocity profile at the jet exit predicts the erosion ratio better, compared to assuming a uniform velocity profile at the jet exit. 3) Post-test analysis of the coupon surface reveals that crater size and shape for the same distance from the center of the impact area do not change for various viscosities. By moving far away from the center of the coupon, craters become longer and sharper as compared to the craters caused by sand impacts near the stagnation zone. ACKNOWLEDGMENTS The authors would like to thank Ed Bowers for his invaluable technical expertise. The authors wish to acknowledge financial support of many oil and gas and service companies that have supported E/CRC research for many years. REFERENCES [1] Chen, X., McLaury, B. S., and Shirazi, S. A., 2004, "Application and Experimental Validation of a Computational Fluid Dynamics (CFD)-Based Erosion Prediction Model in Elbows and Plugged Tees", Comput. Fluids, 33, 1251 1272. [2] Zhang, Y., Reuterfors, E.P., McLaury, B.S., Shirazi, S.A., Rybicki, E.F., 2007, "Comparison of Computed and Measured Particle Velocities and Erosion in Water and Air Flows", Wear, 263. [3] Mazumder, Q., Shirazi, S., McLaury, B., Rybicki, E., Shadley, J., 2005, " Development and Validation of a Mechanistic Model to Predict Solid Particle Erosion in Multiphase Flow ", International Journal of Wear, 259, 203-207. [4] Finnie, I., 1972, "Some Observations on the Erosion of Ductile Materials", Wear, 19. [5] Bitter, J.G.A., 1963, "A Study of Erosion Phenomena Part I", Wear, 6. [6] Neilson, J.H., Gilchrist, A., 1968, "Erosion by a Stream of Solid Particles", Wear, 11. [7] McLaury, B.S., Shirazi, S.A., Shadley, J.R., Rybicki, E.F., 1996, "Modeling Erosion in Chokes", ASME Fluids Engineering, 236(1). [8] Grant, G., Tabakoff, W., 1973, "An Experimental Investigation of the Erosive Characteristics of 2024 Aluminium Alloy", Wear. [9] Huang, C., Chiovelli, S., Minev, P., Luo, J., Nandakumar, K., 2008, "A Comperhensive Phenomenological Model for Erosion of Materials in Jet Flow", Powder Technology, 187(3). [10] Oka, Y.I., Okamura, K., and Yoshida, T., 2005, "Practical Estimation of Erosion Damage Caused by Solid Particle Impact, Part 1: Effects of Impact Parameters on a Predictive Equation", Wear, 259. [11] Gnanavelu, A., Kapur, N., Neville, A., Flores, J.F., 2009, "An Integrated Methodology for Predicting Material Wear Rates Due to Erosion", Wear, 267. [12] Gnanavelu, A., Kapur, N., Neville A., Flores J.F., Ghorbani, N., 2011, "A Numerical Investigation of a Geometry Independent Integrated Method to Predict Erosion Rates in Slurry Erosion", Wear, 271. [13] Wang, M.H., Huang, C., Nandakumar, K., Minev, P., Luo, J., Chiovelli, S., 2009, "Computational Fluid Dynamics Modeling and Experimental Study of Erosion in Slurry Jet Flows", International Journal of Computational Fluid Dynamics, 23(2). [14] Benchaita, M.T., Griffith, P., Rabinowicz, E., 1983, "Erosion of Metallic Plate by Solid Particles entrained in a liquid jet", ASME, 153(8). [15] Okita, R., 2010, "Effect of Viscosity and Particle Size on Erosion Measurements and Predictions", Masters of Science Thesis, The University of Tulsa. [16] Nidasanametla, A. S., 2012, "Effects of viscosity, Particle Size and Shape on Erosion Measurements and Predictions", Masters of Science Thesis, The University of Tulsa. [17] Matas, J. P., Morris, J. F., Guazzelli, E., 2003, "Transition to Turbulence in Particulate Pipe Flow", Physical Review Letters, 014501(90). 10 Copyright 2014 by ASME