PHYSICAL MODEL FOR MASS TRANSFER INA PACKED ” BED ' Thesis for the Degree of Ph. D. MiGHiGAN STATE UNWERSHY RAYMOS‘D LEON PORTER 1973 V ll lllll/llllllll 3 1293 01100 5703 This is to certify that the thesis entitled PHYSICAL MODEL FOR MASS TRANSFER IN A PACKED BED presented by RAYMOND LEON PORTER has been accepted towards fulfillment of the requirements for egree in (ABM/(a/ 3;" ._ 1.12m .-‘ I“ rai' I1;- EIIHKIL' If: Uni Jets: ty 1‘ Ely/1086”}? gamma, # Major profcér Z/,///73 0-7 639 .. JUngmo ABSTRACT PHYSICAL MODEL FOR MASS TRANSFER IN A PACKED BED By Raymond Leon Porter A new method for calculating mass, heat and momentum transfer between particles of a fixed bed and the fluid flowing through it is shown. Overall mass and heat transfer coefficients and pressure loss per unit length of bed are computed from fluid preperties--viscosity, heat capacity, superficial velocity, thermal conductivity, density, diffusion coefficient of active component through the fluid; and the bed characteristics--porosity, particle size, specific surface per unit volume and an index defining the distribution of passage cross sections within the bed. Values calculated for gases in the Reynolds number range from 5 to 33,000 show an average deviation of 3% from literature correlations [5, 8, 15, 31, 40, S4, 58]. Values for liquids in the Reynolds number range from 0.003 to 33,000 and for Schmidt numbers up to 70,600 deviate an average of 5% from literature results [15, 27, S4, 59, 60]. These figures are for fixed beds with voids fractions ranging from 0.38 to 0.70. It is believed that the values calculated in ranges not corrob- orated by experimental investigators are of equivalent accuracy. This is because the method deve10ped in this thesis is not a simple Raymond Leon Porter correlation of experimental data, but is based on a theoretical treatment of a reasonable physical model for a packed bed using principles of fluid dynamics and transport phenomena. The physical model consists of a network of passages arranged in parallel and series with complete mixing assumed at the passage junctions. The passages are assumed to have a distribution of cross sections as described by the index mentioned above. This distribution of cross sections has an effect on coefficients computed for the complete Reynolds number range. Its effect is greatest at extremely low Reynolds numbers where it gives Nusselt and Sherwood numbers which are considerably lower for the bed than for the limiting values of the individual passages. . In the region of fully developed velocity profiles through the passages, treatment of the passages as cylinders with lengths equal to packing size proved to be satisfactory and convenient. In the region of developing boundary layers the length was taken to be half the packing size to allow for boundary layer separation over surfaces curved in the direction of flow. Typically it occurs at about 90 degrees around the curve for surfaces such as cylinders or spheres. The method presented here is in the form of a computer program due to the complexity of handling different cross sections in parallel_ with different flow patterns in the various cross sections. PHYSICAL MODEL FOR MASS TRANSFER IN A PACKED BED BY Raymond Leon Porter A THESIS Submitted to Michigan State University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Department of Chemical Engineering 1973 ACKNOWLEDGMENTS The author would like to thank Dr. Carl M. Cooper for his expert guidance during the writing of this thesis. The patience and understanding of Dr. Cooper, the other members of the Michigan State University Chemical Engineering Department faculty and my family are appreciated very much. ii TABLE OF CONTENTS ACKNOWLEDGEMENT . . . . . . . . . . LIST OF TABLES . . . . . . . . . LIST OF FIGURES . . . . . . . . . . INTRODUCTION ... . . . . . . . . . . LITERATURE SURVEY PACKED BEDS . . . . . . . . . . FLOW PHENOMENA . . . . . . . THEORETICAL ANALYSIS MODEL OF A PACKED BED . . . . . 'MODEL EQUATIONS . . . . . . . . OPERATION OF MODEL. . . . . . . RESULTS . . . . . . . . . . . . . DISCUSSION OF RESULTS . . . . . . . SUMMARY . . . . . . . . . . . . . . CONCLUSIONS . . . . . . . . . . . . RECOMMENDATIONS FOR FUTURE WORK . . APPENDIX A. DERIVATION OF MODEL EQUATIONS B. DISTRIBUTION INDEX . . . . . . c. (VY2)m VARIATION WITH REYNOLDS iii NUMBER 21 . 24 . 38 89 . 102 . 104 . 107 . 114 . 119 Page D. SUMMARY OF MODEL EQUATIONS . . . . . . . . . . . . . . . . 122 E. COMPUTER PROGRAMS . . . . . . . . . . . . . . . . . . . . . 125 F. SHERWOOD NUMBERS, UNIFORM AND NON-UNIFORM PASSAGES . . . . 132 TABLE OF NOMENCLATURE . . . . . . . . . . . . . . . . . . . . . 134 BIBLIOGRAPHY . . . . . . . . . . . . . . . . . . . . . . . . . . 139 iv 13. 14. 15. l6. l7. 18. 19. 20. Comparison Comparison Comparison Comparison Comparison Comparison Comparison Comparison Comparison Comparison Comparison Comparison [59] . . Comparison of Model of Model of Model of Model of Model of Model of Model of Model of Model of Model of Model of Model of Model [59] . . . . . . Comparison Comparison Comparison Comparison Comparison Comparison Comparison of Model of Model of Model of Model of Model of Model of Model LIST OF TABLES with Chu, Kalil and Wetteroth [8] . with Chu, Kalil and Wetteroth [8] . with Chu, Kalil and Wetteroth [8] . . . with Thoenes with Thoenes with Thoenes with Thoenes with Thoenes with Bennett and Kramers [54] . and Kramers [54] ..... and Kramers [S4] . . . . . and Kramers [S4] . . . . . and Kramers [S4] . and Bradshaw [3] . . . . . with Kasik and Happel [31]. . . . . . . with Kusik and Happel [31]. . . . . . . with Williamson, Bazaire and Geankoplis with Williamson, Bazaire and Geankoplis with Wilson with Wilson with Wilson with Wilson with Wilson with Wilson with Wilson 0 O O O O O I O O O O O O O and Geankoplis [60] . . . . and Geankoplis [60] . . . and Ceankoplis [60] . . . . and Geankoplis [60] . . . . and Geankoplis [60] . . . . and Geankoplis [60] . . . . and Geankoplis [60] . . . . ,so 51 $2 53 .54 S6 S7 58 60 Table Page 21. Comparison of Model with Wilson and Geankoplis [60] . . . . 69 22. Comparison of Model with Galloway and Sage, Spheres [15]. . 72 23. Comparison of Model with Galloway and Sage, Spheres [15]. . 73 24. Comparison of Model with Galloway End Sage, Spheres [15]. . 74 25. Comparison of Model with Galloway and Sage, Spheres [15]. . 75 26. Comparison of Model with Galloway and Sage, Commercial Packing [15] . . . . . . . . . . . . . . . . . . . . . . 76 27. Comparison of Model with Galloway and Sage, Commercial Packing [15] . . . . . . . . . . . . . . . . . . . . . . 77 28. Comparison of Model with Galloway and Sage, Commercial _ Peeking [15] O I O O O O O O O O O O O O I O O O I O O O 78 29. Comparison of Model with Galloway and Sage, Commercial PaCking [15] O O O O O I O O O O O O I O O O O O O O O O 79 30. Comparison of Model with Galloway and Sage, Commercial PaCking [15] O O O O O O O O O O O O O O I O O O O O 0 O 80 31. Comparison of Model with Petrovic and Thodos [40] . . . . . 82 32. Comparison of Model with Jolls and Hanratty [27]. . . . . . 83 33. Comparison of Model with Wilkins and Thodos [58]. . . . . . 84 34. Summary of Results for Cases. . . . . . .......... 85 35. Summary of Results for Liquids. . . . . . . . . . . . . . . 86 36. Example Using Model . . . . . . . . . ........... 88 37. Constants for Equation 44 . . . . . . . . . . . . . . . . . 120 38. (W2 Variation with Reynolds Number ........... 121 )m 39. Computer Program Listing for Table 2 . . . . ....... 126 40. Computer Program Listing for Table 36 . . . . . . . . . . . 128 41. Sherwood Numbers, Uniform and Non-Uniform Passages ..... 133 vi 10. 11. 12. 13. 14. 15. LIST OF FIGURES Random Packed Bed of Spheres . . . . . . . . . . . . . Model of a Random Packed Bed . . . . . . . . . . Distribution Index . . . . . Flow in a Passage . . . . . . . . . . Nusselt Number in Tubes . . . . . . . . . . . Effect of Schmidt Number on Mass Transfer at Low Reynolds Nmnbers O O O O O O O O O O O O O O O O O O O O Sherwood Numbers for Uniform and Non-Uniform Passages Comparison of Model with Wilson and Geankoplis [60], Low Reynolds Numbers . . . . . . . . . . . . . . . . . . . Comparison of Model with Wilson and GeankOplis [60], High Reynolds Numbers . . . . . . . . . . . . . . . . . . . Comparison of Model with Literature Correlations . . . . Comparison of Model with Literature Correlations . . . Comparison of Model with Literature Correlations . . . Comparison of Model with Data of Wilson and Geank0plis [60] . . . . . . . Simple Cubic Array of Spheres Rhombohedral Array of Spheres . . . . . . . . . . . . . vii Page 24 25 30 32 36 43 44 92 93 95 96 116 117 118 INTRODUCTION A large number of chemical processes, especially catalytic processes, are carried out in packed bed reactors. With improvements in catalytic reactors, ion exchange columns, leaching beds, chromat- ographic columns and gas adsorbers, it has become increasingly important to predict accurately the performance of packed beds. Proper design involves a knowledge of heat, mass and momentum transport between fluid and solid surfaces. Mass transfer between the packing and the flowing fluid can occur in either direction depending upon the process. In either case the physical phenomena is similar. There is a transfer of some chemi- cal specie to and from the phase boundary through a series of resist- ances. Resistances may be due to diffusion in either phase, laminar or turbulent convection in the fluid, or due to slow chemical formation or reaction of the active chemical substance. In some processes the controlling resistance is in the flowing fluid, such as in a catalytic reactor where there is a slow flow rate and a fast chemical reaction rate. In such a case the size of the equipment is determined by the mass transfer rate between the fluid and solid particles. When the fluid flow rate is rapid and the reaction rate is slow, chemical kinetics dictates the design. Knowledge of the mass transfer rate for a particular process is essential for design and it is dependent upon the type of heterogeneous system. 2 Mechanism of mass transfer has been explained by several theories. The film concept assumes that most of the resistance to mass transfer occurs in a stagnant layer next to the solid surface. Mass transfer through the film is by diffusion. Boundary layer studies show that there is also considerable resistance in the bulk flow stream and in the buffer region next to the film adhering to the solid surface. Another completely different explanation called the 'penetration theory' holds that the flowing fluid is a mass of eddies which continually expose fresh surfaces of fluid to the solid. No matter which theory is followed mass transfer rates are generally expressed in terms of a mass transfer coefficient, kc, just as heat transfer rates are given in terms of a heat transfer film coefficient, h. Variables influencing mass transfer coefficients in packed beds are size and shape of the voids, viscosity and density of the flowing fluid, and the diffusivity of the active substance in the fluid. As with many other chemical engineering processes, correlations are effected using dimensionless groups. The common ones for mass transfer are Reynolds number, Schmidt number and Sherwood number. Reynolds number is a measure of fluid flow rate. Schmidt number contains only the physical prOperties of the fluid and its active component which makes it similar to the Prandtl number of heat transfer. Sherwood number contains the mass transfer coefficient and the diffusivity and is analogous to the Nusselt number of heat transfer. For packed beds particle diameter is commonly used in place of effective diameter of voids and fluid velocity based on empty cross sectional area is used in place of interstitial velocity. For flow through pipes the analogy between heat and mass transfer exists because they both occur due to molecular diffusion and 3 convective mixing. Thus heat transfer correlations can be used to calculate numerical values for mass transfer rates to or from pipe walls. There is, however, less literature data concerning heat transfer in packed beds than there is for mass transfer. Momentum transfer, in terms of pressure drop, in a packed bed can easily be determined from existing equations. However, attempts to show the analogy between momentum and mass transfer have not been successful. Most of the correlations for mass transfer in packed beds are given in the literature by a relationship between Reynolds number and Sherwood number divided by Schmidt number to the one-third power. Recent correlations give mass transfer rates which are in reasonable agreement with reliable reported data. The best corre- lations are for liquids flowing at high Reynolds numbers. For gases at lower Reynolds number flow rates, correlations are more difficult because diffusion coefficients are so much higher for gases than for liquids. Equations necessarily have to be more complicated. Keeping in mind all of the complexities of packed beds it was decided to formulate a physical model for a packed bed which would take into account factors such as fluid properties, packing arrange- ments, nature of flow and the inter-relationships among these factors. Due to the ready availability of digital computers it was thought that a fairly sophisticated model could be devised which could be readily solved by the computer for desired results. For simplicity reasons it was decided to derive the model on the basis of heat transfer and then make the necessary analogies for application to mass transfer. It was also thought that some 4 correlation could be obtained between mass and momentum transfer in packed beds, namely an equation in which mass transfer coefficient is a function of pressure loss per unit length of bed. LITERATURE SURVEY PACKED BEDS The scientific means by which mass transfer occurs in packed beds has been investigated by many persons. One of the first investigations was by Colburn [9] in 1933 who wrote an analogy between frictional resistance to fluid flow, heat transfer and mass transfer which was based on flow through tubes and across tube banks. He reported the equation: Nu = 0.33 Re'6 pr1/3 for heat transfer across tube banks. Using the same analysis Chilton anlColburn [7] later suggested as a basis for correlation of heat transfer data the following equation: 2/3 h/CG Pr = J = f(Rep) h and for mass transfer a similar equation: 2/3 . . ~Graphs of J versus Reynolds number were presented for turbulent flow inside tubes, across tube banks and parallel to flat plates. They reported that the mass transfer equation disregarded free convection at low Reynolds numbers and any liquid film resistance at the gas- liquid interface on the tubes. Mass velocity was for the relative motion between the two phases. By using water evaporation data from a through circulation dryer experiment Gamson, Thodos and Hougen [19] reported values of Jd averaged about 8% lower than Jh values. They assumed in the calculations that the surface temperature of the particles was equal to the adiabatic saturation temperature. One of their recommended equations was: Jd = 16.8 (Rep)'1 for Rep< 40 Sherwood [50] pointed out that if the surface temperature were not at the adiabatic saturation temperature the Jd values could vary widely whereas the J values would vary little. h Wilke and Hougen [57] used the same type of experiment as Gamson et. al. and by controlling heating conditions and changing the method of wetting the packing arrived at a different equation. J . 1.82 (Re )'-$1 for Re < 100 d p p They also assumed the surface temperature to be equal to the adiabatic saturation temperature. Hurt [25] used different sizes and shapes of packing and measured the height of a transfer unit for gas controlled systems. He showed good agreement between heat and mass transfer factors when employing cylindrical particles. The relationship between height of a transfer unit and Jd is: Jd - Sc2/3/(Ht)a where a is the specific surface area per unit volume. The agreement was poor for other packing shapes. Hurt did not, however, report the surface area or the voids fraction of his packed beds. Resnick and White [45] ran experiments with fixed and fluidized beds of naphthalene particles. Results showed Jd values lower than those of Gamson et. al. which was attributed to the use of smaller particles. McCune and Wilhelm [36] obtained data for the mass transfer in both fixed and fluidized bed between flakes of P-naphthol and flowing water. Gamson [18] collected data for water evaporation from porous particles into a flowing air stream. Hobson and Thodos [24] observed data during mass transfer to water or methyl ethyl ketone adsorbed on fixed bed particles. BrStz [6] analyzed these authors' data and came up with the equations: -.41 Jd I 1.46 (Rep) (1 - c)’61 for Rep/(l - c)> 100 _ -l _ 1.2 _ Jd 17 (Rep) (1 e) for Rep/(1 c)< 100 using an equivalent diameter for particle diameter. By changing temperature and pressure, the effect of gas properties on the mass transfer coefficient was studied by Shulman and Margolis [51]. They reported that J was independent of pressure d in their equation: Jd - 1.195 [Rep/(l - an"36 Robson and Thodos [24] measured evaporation rates of water and organic compounds from spherical packing into air, carbon dioxide, ammonia and nitrogen. It was found that the temperature of the bed decreased linearly in the direction of flow but the Schmidt number remained practically constant, so the temperature effect was disregarded. Ergun [12] correlated a mass of experimental data and arrived at an equation for pressure drop in packed beds in terms of dimensionless groups. (-AP)chpe3/[pu2L(l - 5)] 150(1 - e)/Rep + 1.75 At low Reynolds numbers the 1.75 is negligible and at high Reynolds numbers it is dominant. Chu, Kalil and Wetteroth [8] correlated data on heat and mass transfer in liquid-solid and gas-solid systems and arrived at the equation: Jd - 1.77 [(Rep/(l - e)]'-44 for 30 < Rep/(l - e) < 5000 . Epatein [ll] determined an axial mixing factor to correct heat and mass transfer coefficients to account for non-plug flow in packed beds. The fixed bed is treated as a series of perfect mixers in his mathematical treatment. ‘ Thoenes and Kramers [54] determined mass transfer coefficients for fluids flowing around single active Spheres surrounded by similar inactive spheres using eight different packing arrangements. The acive Spheres were either soluble in the flowing fluid or were porous and soaked with liquid “thich evaporated into a gas stream. :Graphs of [Shp/Sc1/3][e/(1 - 2)] (which is equivalent to eJdRep/[l - 2]) versus Rep/(l - S) were presented. A review of 438 mass transfer measurements was expressed by the equation: Shp[e/(l - e)] . 1.0 Sc1/3[Rep/(1 - an”2 which was said to be good for a Rep /(1 - e) range between 40 and 4000, a voids fraction range between 0.25 and 0.50 and a Schmidt number range between 1 and 4000. It was said to have a mean deviation of t 10%. An even better correlation was obtained by assuming that the total mass transfer was due to three contributions: laminar convective transfer, turbulent convective transfer and one for diffusion in stagnant areas. The latter is important for gas flows at Reynolds numbers less than 500. For gases the stagnant regions near the contact points of adjacent spheres are important because diffusion coefficients for gases are so much larger than for liquids. The following equation was correlated: Shple/(I - c)] . 1.26 Sc1/3[Rep/(1 - 5)]1/3 + 0,054 Sc-4[ReP,(1 _ 6)].8 * 0.8 [Rep/(1 - e)].2 in which the first term is for laminar convection, the second for turbulent convection and the last for diffusion. Al-Khudayri [1] made a correlation for predicting the mass trans- fer coefficient in packed beds. The correlation is a plot of [Shp/Sc1/3][e/(l f 5)] versus Rep/(l - e). For liquid-solid systems the deviation of experimental data of other investigators was 30% and was higher for gas-solid systems. His experimental work consisted of the absorption of ammonia fvom a helium-ammonia flow stream onto -the surface of 0.726 cm. diameter alundum spheres coated with copper II chloride. Laminar flowsware used amd mass transfer coefficients were calculated from the data. His results checked closely with those of other investigators for gases at low flow rates. Al Khudayri pointed out that void volume and void surface area are more valid to use than packing diameter when expressing the mass lO transfer characteristics of the bed. If packing diameter is used, a correction needs to be made to compensate for variations in voids fraction. DeAcetis and Thodos [10] made careful temperature measurements of air and packing surface during the evaporation of water from the surface of porous ceramic spheres into an air stream. They found that contrary to usual assumptions, temperature of the packing sur- face is not the same as the wet-bulb temperature of the entering air, unless high air flow rates are used. They summarized their data and that of other investigators up to 1960 in graphs of Jh and Jd versus Rep. The ratio of Jh to Jd reported was 1.51 compared to the value of 1.08 given by Gamson, Thodos and Hougen which was obtained on the assumption that the temperature of the evaporating surface was that of the wet-bulb temperature of the air entering the bed. Bradshaw and Bennett [5] measured mass transfer coefficients for air flowing through short beds of naphthalene Spheres and cylinders. They reported the equation: 1/3 J . 2.0/Re Sc + 1.97/Re 1’2 d p p which was said to cover the Reynolds number range from 40 to 10,000. Sen Gupta and Thodos [22] analyzed the data of other workers -and found Jd to be inversely proportional to voids fraction for mass transfer to flowing gases in packed beds. Kusik and Happel [31] made a theoretical study of gas diffusion rates in packed beds using a free-surface model (spherical particle surrounded by a spherical envelope) with boundary layer theory. 11 The Reynolds number (Rep/e) range covered was from 100 to 1000 with voids fractions of 0.3 to 1.0. Simplified forms of momentum and diffusion equations were solved to predict dissolution rates in a particle bed and to analyze the effects of molar velocity perpendicular to the spherical catalytic surface. Boundary layer equations were solved by using Pohlhausen's method of introducing polynomials describing velocity and density distributions. One equation arrived at was : Sh/Sc1/3=O.93[e - 0.75(1 - e)(e - 0.2)]‘1/2Rep1/2 The authors confirm that the change in boundary layer thickness due to normal convective velocity was the same for boundary layers on spheres as for flat plate geometry. The results Of the study showed that the assumption in film theory that the film thickness does not change with mass transfer rate is correct. This means that film theory can be used for the bulk of chemical engineering problems involving heterogeneous catalysis. Williamson, Bazaire and Geankoplis [59] obtained liquid phase mass transfer coefficients for packed beds of benzoic acid spheres with water passing through. The recommended equations were: St SCo53 = 2.40 (Rep/;)'-66 for Rep]: from 0.08 to 125 and: St Sc-58 - 0.442(Rep/E)'°31 for Rep/e from 125 to 5000. 12 Galloway and Sage [16] developed analytical expressions for heat and mass transport from Spheres to a turbulent air stream taking into account Reynolds number, sphere diameter, and level of turbulence. Sphere size ranged from draplets to 1 ft. in diameter and superficial Reynolds number values ranged from 2 to 1.33 x 106. By analyzing the works of other investigators it was shown by graphi- cal means that the assumption of Nusselt number to be a single valued function of the square root of Reynolds number leads to an average deviation of 60%. Their analysis begins with the Frossling [14] equation for macroscOpic transfer from spheres with zero turbulence: Nu . 2.00 + 0.552 Re 1/2Pr.1/3 P“ Relationships derived for predicting convective thermal and material transport were: [(Nu - 2.00)]/Re l/Zpr.1/3 - 0.538 + 0.1807 01/2 + 0.323 a (a + 0.0405)Re 1/2 t t p [(Sh - 2.00)1/Repa1/25c.1/3 . 0.439 + 0.1807 01/2 + 0.234 a (a + 0.0500)Re 1/2 t t p where d is sphere diameter and at is the longitudinal level of turbulence. I Mickley, Smith, Korchak [37] measured velocity profiles and turbulence parameters in the voids of a 1 ft. square bed of rhombohedrally arranged 1.5 in. diameter table tennis balls. A hot wire anemometer was used and the superficial Reynolds number 13 range covered was from 4780 to 7010. Turbulence energy spectra showed that eddy shedding behind the particles did not occur in the voids between spheres. Since high heat transfer coefficients are known to be caused by eddy shedding and high turbulence level, the high local heat transfer coefficients in the voids characteristic of rhombohedral packing must be explained by a high level of turbu- lence intensity. The mean void velocity showed a maximum within 1.5 particle diameters from the wall. There was a 10% difference in the mean velocity at the center of the bed compared with the maximum region. Rhodes and Peebles [46] determined local mass transfer rates at room temperature by measuring radius changes in 1.5 in. diameter benzoic acid spheres by passing water around them at various flow rates using simple cubic and rhombohedral packing arrays. The Reynolds number range covered was from 166 to 3410 based on superficial velocity. Mass transfer tests were carried out by placing the test sphere in an assembled array of inert, insoluble spheres. Analysis of results for the cubic array (voids fractionw-0.4764), in terms of Sherwood number versus degrees from the front stagnation point, suggested that the flow pattern around the test sphere had the following characteristics: (a) The region around the forward contact point (0 to 10 deg.) showed the minimum mass transfer rate. (b) The over-all maximum mass transfer rate occurs between 50 to 80 degrees forward from the front stagnation point. It was suggested that this is the ring of attachment of the boundary layer of the sphere above. In this region mass transfer rates are 2.2 to 3 times the over-all 14 average. A streamline arriving at this location splits into two streamlines: one circling upward forming the principle eddy of the wake of the preceding sphere and the other streamline attaching itself as a boundary layer that follows along the sphere surfaee until it reachasa ring of separation between 103 and 122 degrees depending upon the Reynolds number. (c) A region of essentially zero mass transfer occurs where there is a point of contact between spheres. (d) The region to the rear of the separation ring is a wake region where the local mass transfer rates are less than the average over the entire sphere. In the rhombohedral array (voids fraction m 0.2595) the orientation of packing was such that each sphere was entirely behind another sphere in the flowing stream, thus giving the limiting case for investigating extremes of local mass transfer rates. Considerably higher maximum Sherwood numbers were reported between 30 and 50 degrees from the front stagnation point than for the cubic array. Wilson and Geankoplis [60] reported studies of mass transfer and reviewed earlier works. They used a bed of randomly packed benzoic acid spheres with an average diameter of 0.251 in. Water or propylene glycol were allowed to flow down through the bed. For superficial Reynolds numbers between 55 and 1500 and voids fractions between 0.35 and 0.75 they recommend: 0.31 eJ d I 0.250/Rep Between superficial Reynolds numbers of 0.0016 and 55 the equation given was: _ 2/3 eJd 1.09/Rep 15 This eqUation was shown to correlate data over a Schmidt number range of 165 to 70,600. Petrovic and Thodos [40] determined mass transfer factors in a packed bed by vaporizing water and heavy hydrocarbons from the surface of 0.0721 to 0.370 in. diameter random packed spheres into air. Using this data and recalculating various other studies by Thodos and coworkers to correct the data for axial mixing, their recommended equation is: I I The results of this study covered the superficial Reynolds number range between 3 and 230 for voids fractions between 0.416 and 0.778 and were said to hold for solid-gas systems subjected to either upward or downward flow. Satterfield [48] compared the equations of Wilson and Geankoplis and Petrovic and Thodos and found that they only differ 15% or less over a range of superficial Reynolds numbers between 55 and 1500. Gillespie, Crandall, and Carberry [20] measured local and overall heat transfer coefficients in two random packed beds of l in. diameter brass Spheres. Air was passed through the packing at flows corresponding to a Reynolds number range of 120 to 1700, based on superficial velocity and Sphere diameter. Local heat .transfer coefficients were measured in the first, second and nine- teenth layers of packing. Average heat transfer coefficients were determined at 25 places in the bed. By examining the local heat transfer distribution the existence of a laminar boundary layer was verified. Highest values of heat transfer coefficient were obtained 16 for the surface perpendicular to the bulk flow in the bed. It was also observed from heat transfer coefficient profiles that at high Reynolds numbers the flow may rejoin the sphere and begin to build another boundary layer which subsequently separates. The effect of repacking of the bed was to change the range of local heat transfer coefficients, but the variation within the range was about the same. The entrance effect of the bed has been shown to result in a lower heat transfer coefficient in the tOp layer than in the bulk of the bed. This has been attributed to a lower incident flow rate and turbulence intensity. The effect of lateral position on average heat transfer coefficient showed higher coefficients near the wall than at the center of the bed. Wilkins and Thodos [58] studied the evaporation of n-decane in- to air from the surface of 0.1 in. diameter celite spheres in both a random packed bed and a fluidized bed. Using their results and those of other investigators they obtained the relationship: cJ - 0.589/Rep°°427 d Jolls and Hanratty [27] used electrochemical techniques and studied details of flow around an instrumented l in. diameter nickel plated brass-bronze ball located 7 to 8 inches from the top in a dumped bed (voids fraction - 0.41) of l in. diameter glass spheres. .Reynolds number (based on empty cross—section) ranged from 5 to 1100 and the Schmidt number of the flowing fluid was 1700. A transition from laminar to turbulent flow was found to occur in this system over a Reynolds number range from 110 to 150. The electrochemical reaction consisted of the reduction of the ferricyanide ion on the nickel cathode (test Sphere) and oxidation of the ferrocyanide ion 17 on a nickel pipe anode located outside the column. Electrode lead wires were placed at various points arOund the sphere. With the exception of the very rearward portion of the Sphere the effect of Reynolds number on the local mass transfer rate was the same as that predicted by boundary layer theory. At the rear of the sphere local mass transfer measurements indicated a larger variation with Reynolds number, apparently due to separation. The effect of Reynolds number on the overall mass transfer to a sphere in either a bed of inert or active spheres indicates a slightly higher power on the Reynolds number dependency than that predicted by boundary theory. This research showed that the flow pattern varied from sphere to sphere. In order to make meaningful results it was necessary to average measurements from a large number of experiments. Reasonable correlation was obtained by assuming the Sherwood number varied with Re 0°57 and Sco'ss. P Galloway and Sage [17] used an instrumented 1.5 in. diameter copper sphere in a 12 in. diameter, 20 in. long column containing a rhombohedral array of 1.5 in. uniform diameter spheres in order to make local heat transfer measurements. Inert spheres were made of celluloid and partial spheres were used on the inside surface of the cylindrical wall to fill out the array and reduce wall effects. The study concerned determination of local heat transfer coefficients .as a result of steady flow of air and covered a range of superficial Reynolds numbers from 875 to 3618 with the effect of turbulence being noted. Local air velocities in flow passages were measured directly. Analyzing available literature data their model provided an analytical expression which was found to represent transport 18 from Single cylinders and spheres, and arrays of cylindrical, spherical, and commercial packing. Overall deviation was 9.8%. The model also predicted the height of a gas phase transfer unit in commercial packed columns being irrigated with liquid within 12% for twelve cases involving absorption and vaporization. .The basis of their boundary layer model was that the local Frassling number l”Sci/3]) was independent of surface (Fs, equivalent to [Sh-2]][Re shape and configuration of packing. Consequently such a model should apply equally well to any packing material. Their general equation was 3 u/kc - (Ht)a - ReSc/Sh - Rel/28c2/3/[Fs + 2/(Rel/28c1/311 Galloway [15] presented results of earlier analyses of data using uniform Spheres, cylinders and commercial packing. The expression given for mass transfer in beds of spheres was: A 1 3 2 sap . 2/[1 - (1 - cp) / 1. °°55[(°pG/")(€p _ 6b)11/ Sc1/3 1/3 + 0.30 Zt(Zt + 0.05)(DpG/uep)5c in whick SP is the voids fraction of the packing, ch is the voids fraction of relatively stagnant regions in the bed, and 2t is the turbulence level. Haring and Greenkorn [23] dev010ped a statistical model of a porous medium with non-uniform pores which matched experimental capillary pressure, permeability and dispersion data. The model was constructed with two parameter distribution functions for pore radius and pore length. Orientation of pores was considered random in all directions. Various properties of a porous medium were found 19 by integrating over joint distributions resulting from the model. Dimensionless quantities were used for pore length and radius so they varied from O to 1. To make the model non-uniform the dimensionless terms were each assumed to be diStributed according to the beta function. The permeability of the model was found by relating the average velocity in an individual pore to the average velocity of all pores. The permeability-porosity ratio, which causes dissipation due to entrance-exit effects, was found to be a function of the average pore radius squared and the pore radius distribution. For most flow situations of interest to engineers, the residence time of the fluid in the individual pore is much smaller than the time needed for appreciable mixing due to molecular diffusion within that pore. Neglecting molecular diffusion, expressions for dispersion coefficient were found by determining the probability distribution of the position of a marked particle after a random walk of inde- pendent steps through the model. The diSpersion coefficient was found to be dependent on both pore radius and length distributions. Wegner, Karabelas, Hanratty [56] made studies of the motion of dye streamers in a rhombohedral array (voids fraction -«O.26) of 3 in. diameter Plexiglas spheres. The test sphere containing the dye taps was located in the tenth layer of a fifteen layer bed. Similar flow patterns were observed at superficial Reynolds numbers .0f 82 and 200. Nine distinct regions of reverse flow were noted. Flow was described as steady at the lower flow rate and unsteady at the higher one. 1 Van Der Merwe and Gauvin [55] investigated flow deveIOpment in packed beds by setting up an experimental apparatus using a regular 20 arrangement of ten banks of seven centimeter diameter spheres. A skewed arrangement was also tested where the spheres were arranged on 0.375 in. rods at an angle where the mean flow direction made equal angles with the three principal axes of the packing. The pressure drag coefficients on the central Sphere of each bank were determined for air having Reynolds numbers of 27,000 and 10,000. It was found from the distribution of local pressure measurements, which allowed determinations of the separation and reattachment points of the boundary layer on the central sphere of each bank, that the boundary layer behavior on a sphere in a packing is similar to that of a Single Sphere. The skewed arrangement showed a lower pressure drag coefficient than did the regular arrangement at the same Reynolds number. Karabelas, Wegner and Hanratty [28] studied the effect of Grashof, Reynolds and Schmidt numbers on mass transfer rates to liquids (Sc . 1600) from cubic arrays of spheres. For Reynolds below Rep - 110, the correlation equation was: Shp a 0.46 (Gr Sc)-25 They also give a summary of other authors' correlations for heat and mass transfer data. 21 FLOW PHENOMENA Graetz [21] in 1883 made the first analysis for the development of the temperature profile in a round tube. He assumed the velocity profile was fully developed at the tube entrance for the two cases of uniform and parabolic velocity. Nusselt substantiated Graetzls solutions independently in 1910. Pohlhausen [42] solved the problem of heat transfer to a fluid in laminar flow parallel to a flat plate. The velocities and temperatures are approximated by polynomials in y having coefficients that are functions of x. The coefficients are determined by satisfying the boundary conditions at the plate and at the edge of the boundary layer using integral forms of the equations of continuity, motion and energy for the boundary layer. Leveque [33] modified the problem of heat transfer to a fluid in laminar flow in a pipe with constant temperature walls. He assumed the parabolic velocity profile to be completely developed before the fluid enters the section of pipe where the heating begins. A thermal boundary layer is then assumed to develOp, superimposing itself on the already developed velocity profile. The following equation was -formulated: Nu . 1.077 [0 Re Pr/L]1/3 This equation gives the same values for Nusselt number in the region [0 Re Pr/L] greater than 100 as the more complicated Graetz equation. 22 The Leveque equation is not valid beyond the length where the thermal boundary layer reaches the center of the pipe. Norris and Streid [38] analyzed the problem for laminar flow in flat rectangular ducts and suggested that entrance region Nusselt num- bers for simultaneously develOping velocity and temperature profiles might be obtained using results for heat transfer from a flat plate. Langhaar [32] postulated that the pressure gradient in the transition length of a tube is higher than in a region of laminar flow because of increased frictional loss and increased kinetic energy if fluid as it passes downstream. He used linear approximation methods to solve the Navier-Stokes motion equations involving frictional flow for the case of steady flow in the transition length of a straight tube. A family of velocity profiles was determined which were defined by means of Bessel functions. The pressure function was then derived from the computed velocity field by means of the general energy equation. Sparrow [53] studied the simultaneous develOpment of temperature and velocity profiles in flat rectangular ducts. Laminar flow and constant wall temperature were assumed. Thermal and velocity boundary layer calculations were made using the Pohlhausen method. Nusselt numbers were reported for the Prandtl range from 0.01 to 50. By plotting D Re Pr/L (Graetz.number, 02) versus Nusselt number it was found that there is a separate curve for each Prandtl number in the entrance region. In contrast when a parabolic profile is assumed at the entrance, there is a single curve which satisfies all Prandtl numbers. In order to compare his results with those of Norris and Streid, the Pohlhausen solution gave the equation: 23 Nu = [0.664/¢][D Re Pr/L11/2 For Prandtl numbers equal to or greater than one, many investigators have found 0 - PSI/6. For Pr less than one Sparrow has a plot of e vs. Pr. Kays [30] studied the problem where the thermal and hydrodynamic boundary layers develop at the same time by combining Langhaar's results for the developing velocity profile with a numerical solution of the differential energy balance. His solutions were limited to fluids with a Prandtl number of 0.7. Kays pointed out that for high Prandtl number fluids, such as oils, the assumption of a fully developed velocity profile at the tube entrance does not affect the heat transfer mechanism because the velocity profile is established much more rapidly than the temperature profile at the place where heating begins. However, for fluids with Prandtl numbers near unity, such as gaSes, the velocity and temperature profiles develop at nearly the same rate along the tube. As a result experimental data Showed considerably higher Nusselt numbers than predicted by the assumption of a parabolic profile throughout the tube. The Graetz parabolic velocity solution provided lower limit Nusselt numbers, while the Graetz slug flow solution gave upper limiting values. Kays showed that the Pohlhausen flat plate solution using Langhaar ‘velocity profiles gave intermediate Nusselt numbers to those with parabolic and slug flows. As D/L approaches zero, Nusselt number approaches a minimum value of 5.75 for slug flow and 3.656 for parabolic flow. Kays postulates that the Pohlhausen solution should approximate actual performance near the tube entrance. THEORETICAL ANALYSIS MLQAEAQKEDEED Packed beds are commonly made by packing tubes or cylindrical vessels with solid particles such as cylindrical catalyst pellets, Raschig rings, spheres, etc. These beds are generally used to effect mass transport between the bulk of a fluid flowing through the bed and the fluid-solid interface (or the interface with a second fluid which wets the solid). Usually the solid particles which make up the bed distribute themselves in a random fashion, but sometimes, especially in research on the characteristics of packed beds, the packing is placed in the bed in a regular pattern. Figure 14 and 15 in Appendix B Show the spatial arrangement for two types of regular fixed beds. Figure 1. Random Packed Bed of Spheres The mass, momentum, and heat transport characteristics of packed beds have been investigated by others in a vast number of experiments resulting (after correction for wall and and effects) in a large 24 25 number of correlating equations for transport in the bulk of the packed bed. These equations are generally expressed in terms of a packed bed Reynolds number together with a Sherwood and Schmidt number (or alternatively a Nusselt and Prandtl number). The tacit assumption is commonly made that these correlating equations may be used to design beds with a different packing material and a different random packing arrangement as long as the dimensionless variables are in the same range as the experiments. While such extension of the correlating equations could lead to erroneous results (for example, when cylindrical packing happens to arrange itself in a manner which blocks the fluid) they have been used in this manner with some success. As might be expected, the corre- lating equations are extended more successtlly when the dimensionless variables are defined in terms of the average interstitial velocity u]: rather than superficial velocity u, and interstitial hydraulic radius e/a, or c Dp/6(l - e), rather than the spherical packing diameter DP' Thus a packed bed may be viewed more appropriately as a network of channels of varying Shapes and sizes rather than as an aggregate of solids. The active part of the bed is the voids. It is the solids which are inert. Figure 2. Model of a Random Packed Bed 26 This thesis grows out of the concept that the transport characteristics of a random packed bed can be computed from a physical model consisting of a simplified network of channels. Al-Khudayri [I] assumed a network of uniform cylindrical channels with mass transport in the individual channels governed by the Graetz [21] equation. McCabe and Smith [35] use a similar model to derive the Ergun [12] equation for pressure drOp in packed beds. The model used here is more SOphisticated than these. It includes channels of varying diameters, thus simulating the stagnant and active flow regions which occur in real packed beds. And it provides for mass transfer in the regimes of boundary layer formation and separation, and incipient turbulence. Specifically, this model, or combination of models, may be described as follows: 1. For computing velocity distribution in the bed and for computing mass transfer at low velocities, the physical model used is a network of cylindrical channels all of a length equal to the diameter of equivalent spherical pack- ing. On the average these channels are at an angle of 45° with the axis of the bed, and the distribution of diameters is described by a parameter XS. The void volume per unit bed volume and the surface per unit bed volume are the same as in the real bed. 2. The distribution of velocities in the bed is computed assuming that all channels have the same pressure drop and that that pressure drOp may be computed from Langhaar's analysis [32] of the entrance of a circular pipe. This 27 'gives very low velocities in low diameter channels, and high velocities in large diameter channels. Mass transfer in the channels is computed in accordance with the type of flow occurring. At the lowest velocities with fully developed velocity and concentration profiles the asymptotic Sherwood number for cylindrical tubes is used. At somewhat higher velocities with developed veloc- ities and developing concentrations the Leveque equation is used to compute the Sherwood number. Both of these equations derive from rigorous application of basic fluid dynamic and transport principles to the flow regimes described. I At higher velocities and diameters both the velocity profile and the concentration profiles are developing. The treatment developed by Blasius and Pohlhausen [42] for flow over a surface parallel to the direction of flow is applicable here except that the real surface formed by spheres and cylindrical packing curves in the direction of flow. Since boundary layer separation occurs at about half way around a sphere or cylinder, the length of the boundary layer in_the Pohlhausen equation is taken as half the length of the channel. At still higher velocities a somewhat different physical model is used to simulate mass transport in a packed bed. Instead of regarding the fluid as flowing through a network of cylindrical passages, it is regarded as flowing normal to a bank of cylinders, again with the same void fraction and surface as the real bed. This model gives incipient turbu- lence at much lower velocities than cylindrical passages 28 and in this respect behaves more like a real packed bed. The Colburn [9] equation developed for heat transfer in fluids flowing across banks of tubes is applicable to this model. 6. In this thesis a single equation is used to compute the Sherwood number in all the flow regimes described above and in the transition regions between them. This equation states that the Sherwood number in any case is equal to the feurth root of the sum of the fourth powers of Sherwood numbers computed by all the equations described above. This is a somewhat arbitrary combination of these equations, but it does give values which are in pretty good agreement with the transition between developing concentrations and developed concentrations as derived rigorously by Graetz [21]. 7. Overall mass transfer in the bed is then computed on the basis that all the concentrations leaving a given layer of channels mix to an average concentration before entering the next layer of channels. Obviously what is described above is not a rigorous derivation of transport in a randOm packed bed from the equations of continuity, motion, energy, and mass transfer. It is, however, a combination of _ rigorous analysis and reasonable approximation to the transport behavior of a fluid flowing through a physical model designed to simulate many of the phenomena which occur in packed beds. Mass transfer coefficients computed from this model are therefore a priori predictions as to how random packed beds Should behave over a wide range of operating conditions. This is much different from 29 correlating equations which represent a posteriori fits to limited range data taken on a particular packed bed. The model equations are derived on the basis of heat transfer for simplicity reasons and then converted to mass transfer by substituting the appropriate dimensionless variables. DERIVATION Q2 MODEL EQUATIONS Primary units for quantities used in the derivations are: heat H, mass M, length L, time t, force F, and temperature T. Consider that the flow cross-section is distributed among the various diameters so that: S/sIll - (D/Dm)s (l) where: S total cross-sectional area of passages having diameters less than 0 sm - total cross-sectional area of all passages D - diameter of a given passage D - maximum passage diameter present 5 - exponent which depends upon the distribution of passages The average passage diameter Dav is determined from equation 1 by multiplying 4 times the average hydraulic radius. Average hydraulic radius is calculated by dividing SIn by the total perimeter of all passages. Since the perimeter of a given circular cross-section 30 is ND = 4S/D: Dav ' F.1— (2) D After integration (See Appendix A): Dav 3 Lil on (3) Let: XS = l/S Dav = (1 - x3) 0In (4) When X5 = 0, S = c, all passages have the same diameter. When XS 3 1, Dav . 0. This requires that substantially all of the surface to be located in passages of infinitesimal diameter. Dh‘yxs. 0.01 O S 5m Figure 3. Distribution Index Ordinary packed bed parameters are: u a superficial fluid velocity, based on empty cross section (L/t) e a voids fraction, voids volume/total bed volume (L3/L3) a a packing surface area per unit bed volume (L2/L3) 31 Dp - particle diameter (L) p a fluid viscosity (M/Lt) p a fluid density (M/L3) k a thermal conductivity of fluid (H/LtT) C a heat capacity of fluid (H/MT) J- diffusion coefficient of active component in fluid (L2/t) Volumetric hydraulic radius in terms of fixed bed parameters is the volume of voids divided by the packing surface area. Therefore the average equivalent diameter of a cylindrical passage is: Dav = 45/8 (5) Consider the fluid to be perfectly mixed before entering a given layer of passages so that the entering temperature T1 is the same for all passages. Consider the wall temperature Tw constant throughout the layer so that (T1 - T") 8 ATI is also uniform. However, since different temperatures are reached at the end of different passages, T2 and (T2 - T") 2 AT are not uniform. Assume the length 2 of a passage L to be equal to a particle diameter D , and the average angle between the flow direction in the passages and the axis of the bed to be 0. In order to determine the ATZ/ATl ratio for a given passage a heat energy balance per unit of time is made: m C dTp a - h (TP - Th) e D dL (6) where: m . mass flow rate of fluid in a passage (M/t) T a temperature of fluid at any point in a passage (T) 32 h a fluid film heat transfer coefficient (H/thT) Figure 4. Flow in a passage Rearranging equation (6) and integrating over the length of the passage: L 1;. 111C (Iii-IIWDIOL r-T T. ' V) O In [BIZ/1T1] - - 5.3.1:. The mass velocity of the fluid is G = m/(nD2/4). 1 AT AT s-flL '11 2/ 1] 600 The dimensionless groups--Reynolds number, Re a DG/u; Nusselt (7) (8) (9) number, Nu s hD/k; and Prandtl number, Pr = Cu/k--are then substituted into equation (9). ._ 4NuL (10) 33 It is then convenient to introduce Y = D Re/L, a parameter given in Langhaar's article [32]. ‘41'u ln [ATZIATI] =- - Y? (11) V Solving for ATz/ATI: Mm AT /AT- 2 e V (12) 2 1 In terms of dimensionless groups the average Reynolds number of the fluid, based on the superficial velocity direction, is defined as: 1 g)! 035 .S Reav I D... I. R. ‘0‘. D J 5:- (13) The average temperature change ratio is calculated by integrating equation (12) over the distribution of passages. ‘Nm ‘ . 'F D s f a Re case "' <13;- (ATZ/AT1)av = 3* ._________ (14) R. case 23 135; e A relationship for Y is determined from the mechanical energy balance of a fluid streamline at the entrance of a tube, the pressure loss equation for fully developed laminar flow, and a correction to account for the pressure loss in the transition length. Disregarding elevation effects and assuming a fluid of con- stant density, the Bernoulli equation [35] for potential steady-state 34 flow along a streamline is: -‘{-+-'£wdw=0 (15) where: P a static pressure of fluid (F/Lz) 9 . density of fluid (M/L3) w a velocity component perpendicular to the cross section of channel (L/t) gc - gravitational constant (LM/th) Since the average velocity in the tubes is u/e and w in the mixing sections between layers is negligible: (16) I. By dividing both sides of equation (16) by 2l’:,:,,‘!..and defining V (the number of 'Velocity heads') :- muff—:13; , then at the tube entrance. Beyond the transition length where the laminar flow pattern is fully developed the Hagen-Poiseuille equation [35] for pressure loss in a round tube applies. - AP = flit“ (13) $ t>IAQ Since Y 3 D RE/L 3 W V = 64/Y (19) 35 Therefore the equation V I l + 64/Y or its equivalent, Y I \IVYZ + 1024 - 32 (See Appendix A), satisfy the limiting conditions at high Y and at low Y, but in the intermediate region (transition length) a correction is needed. This region is important to the model because of the distribution of passages. Langhaar [32] made a theoret-I ical study of the pressure losses in the flow develOping region of a tube and his results are used in this thesis to make the needed correction. Langhaar's analysis begins with the Navier-Stokes differential equation of motion for flow perpendicular to the channel cross section. He solves the differential equation using the equation of continuity and valid approximations. The solution is a family of velocity profiles defined by Bessel functions. The pressure function is then determined from the computed velocity field by means of the general energy equation. From these equations then Langhaar calculates a table of values for 4/Y versus V. For purposes of this thesis the table is converted into the equation: 2 B a 4 - - ——_——.—_ Y (‘Ivv +102 32)(1 ".N") (20) where: B,A I constants RT = (W2)°25 (21) By analyzing Langhaar's data the best fit seems to be when: B = 5.8, A I 175. The Nusselt number in a given passage is determined by combining the limiting value and three other equations using the fourth power averaging method. 36 Nu - ((3.656)4 + (1.615)4(Y Pr)4/3 + (0.664(2 nuzprl”)4 e (22) 1/3 4 .25 (0.33 Re-6 Pr ) ) Equation 22 is a continuous equation and represents a weighted average of the limiting Nusselt number for fully developed laminar flow in tubes [30], the Leveque equation for developed velocity and developing temperature laminar flow profiles [33], the Pohlhausen equation for developing laminar velocity and temperature profiles [42], and the Colburn equation for heat transfer in turbulent flow across tube banks [9]. The factor 2 in the Pohlhausen equation compensates for the formation of two boundary layers in one length of channel as previously described. log-tog P393? 51/ 3* N“ W c Q 6V0? Jaga!$:1%’ vgyove FWiII 3.55 - L ID I The Figure 5. Nusselt Numbers in Tubes As is seen in equation 22 the Nusselt number for boundary layer formation, developed laminar flow and turbulent flow is proportional to the one-third power of the Prandtl number times Reynolds number to a power which depends upon flow conditions. 37 For the analogy between heat and mass transfer the following terms are defined: Nu I average Nusselt number, Dth/k 8V kc Shav I average Sherwood number, Davkc/‘V I mass transfer coefficient based on superficial velocity (L/t) Shp I Sherwood number based on particle diameter, Dpkc/J? . . f‘ Sc I Schmdt number of fluid, Q5 Rep I Reynolds number based on particle diameter, DquVr Relationships derived in Appendix A are: Rep - 1.5(1 - e)Reav Shp - 1.5(1 - c)Shav/c e 6Kc‘ Shp'7:1: *' auar (23) (24) (251 (26) For mass transfer Sherwood number and Schmidt number are similar, respectively, to Nusselt number and Prandtl number of heat transfer. Therefore: 1/3 ... 1/3 Shav/Sc -—-Nuav/Pr In terms of mass transfer then: 1/3 x Shav/ Sc (1: Rem, with the value of x depending upon the type of flow. follows that: (27) (28) It then (29) 38 where C1 is a proportionality constant. Equation 29 expresses the mass transfer characteristics Of a packed bed in terms of voids volume and voids surface area and many of the literature correlations use varying forms Of this equation. For a bed of spherical particles the following relationship is derived in Appendix A. L - Op - 6(l - c)/a (30) OPERATION 9f Lg MODEL The general procedure used to mathematically solve for .891 and ‘3ng Tg—z from the model is: (A) Bed porosity (e) and Pr (Sc) are set at desired values. The angle 9 is assumed to be 45’, so case- I 0.707. (B) XS is assigned a value of 0.3 (See Appendix B). (C) A value for (W2)m is assumed, the magnitude of which depends upon the voids fraction and the desired value for Rep/(1 - a) (See Appendix C). (D) Reav and (ATz/ATl)av are evaluated from equations 13 and 14 by integration. Dav/0m is calculated from equation 4. For each value of S/Sm, the following sequence of equations is used: (a) DID. from equation 1 (b) W2 from (VY2)n(D/Dm)4 (31) 39 (c) RT from equation 21 (d) Y from equation 20 XS (e) From Appendix A: Re I 1.5 Y 1'7! (ii—'9) (I-XS) (32) (f) Nu from equation 22 (E) Rep/(1 - c) is then determined from equation 23. (F) Nuav is calculated from (See Appendix A): é PrReAv 1 (AI: 3" ' - 5(:-£)cose :1 AT, M (33’ (6) Finally by combining equations 25 and 27: Se"; .- 5 “0’3 Model equations are summarized in Appendix D. The mass transfer coefficient can then be determined from equation 26. a 551;.“ ShF G 1‘c" —_"“ [Sch Te] The pressure loss per unit length of bed can be calculated from the model and the Ergun equation (See Appendix A). q {730 - 010- X5)+(VY‘)- (35) -AP AL I / IZG 3e e‘ 2 D. A correlation between mass transfer coefficient and pressure loss per unit length of bed can be made by combining equations 28 and 35: 40 1: '-AP [64.61 93: 50,1!» [Eh—'1‘] 36 c' TC zvar‘u-e 0"0- X5)7"(VY") 56° '-‘ I ) The heat transfer coefficient can be determined by combining the definition of Nuav and equation 5. h - Nuavka/«t e (37) Computer programs showing the Operational steps of the model are given in Appendix E RESULTS The principal advantages Of the computerized model of this thesis compared to previous correlations are its flexibility and its coverage of larger ranges Of Reynolds and Schmidt numbers and bed perosities. Literature correlations are generally for data Obtained from specially constructed laboratory beds. Graphs of data are usually in the form of Colburn 'J' factors versus Reynolds number which are easily compared with results of this model. Authors' equations containing Colburn 'Jd' factors are changed to equations containing Sherwood number by: J . kc/(u.Sc2/3) d Si ce: R I D n ep p u p/u SC = u/(plfl Sh IDk P P c”r Then: Shp/(Rep Sc) I kc/u 1/3 I Shp/(Rep Sc ) Correlation equations Often contain specially defined axial mixing or turbulence correction factors and apply only for limited ranges of packed bed parameters. Data have been Obtained by evaporating various liquids from porous solid particles into gas 41 42 streams, dissolving pellets of slightly soluble solids into flowing liquids or extracting liquids from porous solids into flowing water. Correlations for gases at relatively low Reynolds numbers (below 250) are most difficult because mixing in the axial direction becomes increasingly significant and it is hard to avoid essentially equilibrium conditions at the exit even in a short packed bed. In this work boundary layer theory is considered by using the Pohlhausen equation in the model to account for the development of temperature, concentration and velocity profiles in the entrance region of a conduit. The model also contains the Leveque equation for developing temperature and developed velocity profiles. These are important for gases because the temperature, concentration and velocity profiles develop simultaneously whereas for viscous liquids the velocity profile develops first. For gases, therefore, heat and mass transfer occur at a much greater rate in this region than downstream where profiles are fully developed. {Figure 6 shows the effect of a low Schmidt number (gases) on the model at low Reynolds numbers. It can be seen that mass transfer is much greater than for a liquid with a high Schmidt number. Figure 7 shows the effect of distributed cross-sections on the rate of heat and mass transfer. A distribution index (XS) of 0.3 .gives Nusselt and Sherwood numbers at extremely low Reynolds numbers which are only about one-third of the amount they would be if all passages were of the same diameter. Data for the graph are given in Table 41 in Appendix F. An equation to account for turbulence is also incorporated into the model. It is based on the Colburn equation for turbulent flow 43 Voids Fraction I .4 X8 = .3 0.001 0.01 0.1 1.0 322 g 6'49. l"‘ an” Figure 6. Effect of Schmidt Number on Mass Transfer at Low Reynolds Numbers 44 newsman.— Eomgcaéez 13 30.3.5 new whose—.2 100335 .5 omen: l4 vs? .ooo.o~ .OOOA .ooH .o— o.~ ~.c Ao.o moo.o n >4Nk ~n~.~ 2 52.5.: o.m v.mv~ 45 heat transfer across tube banks. Jolls and Hanratty [27] and Karabelas, Wagner and Hanratty [28], using electrochemical techniques report that in a dumped bed of l in. spheres having a voids fraction of 0.41 that a transition from laminar to turbulent flow occurred over the Reynolds number range of 110 to 150 (Rep/(l - e) I 186 - 255). Table 1 shows the results of the model not using the turbulence equation. The model equations used were identical with those of Table 2 with the exception of the omission of the turbulence equation. Comparison of the two tables shows that turbulence affects the results above a Reynolds number of 260. Tablesl to 33 compare Shp/Sc1/3Ic/(1 - e)] - 315233.17,- - ORE/ADS (computer print-out) values from the model with those obtained by using various authors' equations and graphs. The Reynolds numbers given are Rep/ (1 - e) I 6 u Q/af I OUR/AZ (computer print-out). Table 39 is an example computer program used to compute Table 2 and is found in Appendix E. (W2)In values were selected from Appendix C to produce the Reynolds number range desired at the voids fraction of the bed. The equations listed in the headings are those of the authors and the Reynolds number ranges given are in terms of Rep/ (1 - 6). Tables 2 and 3 compare the model results with those of Chu, Kalil and Wetteroth [8]. Their correlation equation is for mass transfer in packed and fluidized beds to a gas, Schmidt number of 2.57, covering a Rep/(l - c) range from 30 to 5000 and bed porosities of 0.38 and 0.64. Jd - 1.77[Rep/(l - an"44 46 TABLE 1. COMPARISON OF MODEL WITH CHU, KALIL AND WETTEROTH [8] CHU I KALIL + HETTEROTH (19531 EQUATION J 8 1.77/REEII.44 SCHMIDT NUMBER 8 2.57 (GASES) VOIOS FRACTION = 0.38 REYNOLDS NUMBER RANGE = 30 - 5000 XS 3 0.3 REYNOLDS I6UR/AZ) 29.7577 40.4643 54.3287 72.0920. 94.6633 123.1697 159.0187 203.9735 260.2463 330.6098 418.5302 528.3253 665.3528 836.2363 1049.1404 1314.1057 1643.4611 2052.3297 2559.2521 3186.9540 3963.2883 4922.3948 MODEL CHU DEVIATION (6KE/ADS) (6KE/ADS) FRACTION 5.2150 4.4975 0.1375 5.9654 5.3421 0.1044 6.7986 6.3004 0.0732 7.7186 7.3819 0.0436 8.7323 8.5984* 0.0153 9e8490 909641 ‘000116 11.0793 11.4965 '0.0376 12.4354 13.2165 -0.0628 13.9321 15.1485 -0.0873 1505866 1703210 ”0.1112 17.4186 19.7662 -0.1347 19.4506 22.5206 -0.1578 2107076 2506251 -001804 24.2168 29.1246 -0.2026 27.0080 33.0692 “0.2244 30.1131 37.5136 -0.2457 3305668 4205189 “002666 3704066 4801521 -002872 41.6733 5404879 -003075 4604115 6106094 -0032?“ 51.6702 69.6094 -0.3471 57.5034 78.5915 -0.3667 47 TABLE 2. COMPARISON OF MODEL WITH CHU, KALIL AND WETTEROTH [8] CHU + KALIL + HETTEROTH (1953) EQUATION J 8 1.77/REEIO.44 SCHMIDT NUMBER 8 2.57 (GASES) VOIDS FRACTION 8 0.38 REYNOLDS NUMBER RANGE 3 30 - 5000 XS 8 0.3 REYNOLDS I6UR/AZ) 29.7577 40.4643 54.3287 72.0920 94.6633 123.1697 159.0187 203.9735 260.2463 330.6098 418.5302 528.3253 665.3528 836.2363 1049.1404 1314.1057 1643.4611 2052.3297 2559.2521 3186.9540 3963.2883 4922.3948 MODEL CHU DEVIATION (6KE/ADS) (ORE/ADS) FRACTION 5.3352 4.4975 0.1570 6.1447 5.3421 0.1306 7.0588 6.3004 0.1074 8.0872 7.3819 0.0872 9.2432 8.5984 0.0697 10.5422 9.9641 0.0548 12.0020 11.4965 0.0421 13.6425 13.2165 0.0312 15.4874 15.1485 0.0218 17.5643 17.3210 0.0138 19.9058 19.7662 0.0070 22.5495 22.5206 0.0012 25.5381 25.6251 -0.0034 28.9198 29.1246 ‘0.0070 32.7488 33.0692 -0.0097 41.9954 42.5189 -0.0124 47.5545 48.1521 -0.0125 53.8453 54.4879 -0.0119 69.0052 69.6094 -0.0087 78.0956 78.5915 *0.0063 48 TABLE 3. COMPARISON 0? MODEL WITH CHU, KALIL AND NETTEROTH [8] REYNOLDS IbUR/AZ) CHU + KALIL + HETTEROTH (1953) EQUATION J 8 1.77/REE*!.44 SCHMIDT NUMBER 8 2.57 (GASES) VOIDS FRACTION 8 0.64 r REYNOLDS NUMBER RANGE 8 30 - 5000 30.6966 40.0189 51.7523 66047391 84.9081 107.9628 136.7743 172.7587 217.6751 273.6998 343.5172 430.4298 538.4942 672.6872 839.1108 1045.2445 1300.2556 1615.3801 2004.3909 2484.1720 3075.4214 3803.5146 4699.5597 XS = 0.3 MODEL CHU DEVIATION (6KE/ADS) (6KE/ADS) FRACTION 8.5324 7.7076 0.0966 9.6402 8.9417 0.0724 10.8636 10.3265 0.0494 12.2154 11.8805 0.0274 13.7110 13.6258 0.0062 1503684 1505878 ’0001‘2 1702084 1707957 “000341 19.2550 20.2824 -0.0533 21.5353 23.0848 -0.0719 2400789 2602438 ‘000899 2609188 2908046 “001072 30.0909 33.8172 -0.1238 33.6344 38.3366 -0.1398 37.5924 43.4238 -0.1551 42.0125 49.1464 -0.1698 46.9470 55.5795 “0.1838 52.4542 62.8071 -0.1973 58.5991 70.9229 -0.2103 65.4544 80.0319 -0.2227 73.1013 90.2516 -0.2346 8106313 10107137 -002460 91.1471 114.5663 -0.2569 101.7643 128.9749 -0.2673 49 This equation converts to: Shp/Sc1/3[c/(l - c)]I 1.77 e[Rep/(l - c)]'S6 Table 4 shows a comparison of one equation of Thoenes and Kramers [54] and the model. They measured the rate of mass transfer between a flowing fluid and the surface of one active Sphere in the middle of a regular bed of spheres. Eight different geometric configurations of spherical packing were used. They present graphs interpreting their data, but do not list the data in tabular form. One equation given is: sup e/(l - c) . 1.26[Rep/(1 - 5)]1/3 Sal/3 + o.os4[aep/(1 - c)]°8 Sc°4 + 0.8[Rep/(l - .)]'z The first term is said to be for laminar convective transfer, the second for turbulent convective transfer and the third for diffusion in the stagnant regions near contact points of adjacent spheres. The last.term is said to account for a large part of mass transfer in gases at Reynolds numbers less than 500. Another equation listed in this same article is: Shp C/(l - E) a l'olkep/(l _ 6)]l/2 SCI/3 ' which they say checks within 1 10% for all of their 438 mass transfer measurements. The ranges for this equation are given as: voids fraction, 0.25 to 0.50; Schmidt number, 1 to 4000; Reynolds number, 40 to 4000. Tables 5 through 8 compare this equation with the model. Table 9 shows the equation of Bradshaw and Bennett [5] who measured mass transfer coefficients for air passing through various TABLE 4. COMPARISON OF MODEL WITH THOENES AND KRAMERS [54] THDENES C KRAMERS EQUATION SCHMIDT NUMBER VOIDS FRACTION REYNOLDS NUMBER R XS = 0.3 REYNOLDS (6UR/AZ) 39.9038 54.1952 72.6815 96.3457 126.3956 164.3293 212.0186 271.8090 346.6431 440.2082 557.1130 703.0961 885.2755 1112.4486 1395.4568 1747.6302~ 2185.3349 '2728.6450 3402.1703 4236.0747 50 (19581 SH/SCIII/3 = 1.26 REE**l/3 + .054 REE**.B SC*0.067 + .8 REE**.2/SC**1/3 = 1.0 (GASES) = 0.32 ANGE = 40 - 4000 MODEL THOENES IbKE/ADS) (6KE/ADS) 5.4498 7.0087 6.2858 7.8628 7.2529 8.8089 8.3596 9.8574 9.6171 11.0220 11.0419 12.3193 12.6556 13.7704 14.4823 15.4002 16.5496 17.2393 18.8897 19.3235 21.5400 21.6954 24.5441 24.4050 27.9519 27.5106 31.8200 31.0800 36.2119 35.1921 41.1983 39.9385 46.8582 45.4261 53.2794 51.7792 60.5602 59.1428 68.8104 67.6867 DEVIATION FRACTION -0 0 2860 -0.2508 -002145 -001791 “001460 -0.1156 -0.0880 -000633 -0.0416 -0.0229 -000072 0.0056 0.0157 0.0232 0.0281 0.0305 0.0305 0.0281 0.0234 0.0163 TABLE 5. COMPARISON OF MODEL WITH THOENES AND KRAMERS [54] THOENES 8 KRAMERS (1958) EQUATION SH 3 1.0 RE**1/2 SCIIII3 SCHMIDT NUMBER 3 1.0 (GASES) VOIDS FRACTION * 0.40 REYNOLDS NUMBER RANGE = 40 - 4000 XS 8 0.3 REYNOLDS (6UR/AZ) 40.6615 54.3969 71.9472 94.2029 122.2702 157.5324 201.7237 257.0198 326.1454 412.5041 520.3302 654.8720 822.6120 1031.5341 1291.4520 1614.4116 '2015.1856 2511.8839 3126.7029 3886.8476 MODEL THOENES DEVIATION (6KE/ADS) (6KE/ADS) FRACTION 602981 603766 ’000124 7.2164 7.3754 -0.0220 802533 804821 '000277 9.4165 9.7058 -0.0307 10.7198 11.0575 -0.0315 12.1816 12.5511 -0.0303 13.8236 14.2029 -0.0274 15.6701 16.0318 -0.0230 17.7488 18.0594 -0.0175 20.0921 20.3101 -0.0108 22.7369 22.8107 -0.0032 25.7253 25.5904 0.0052 29.1049 28.6812 0.0145 32.9285 32.1175 0.0246 37.2553 35.9367 0.0353 42.1509 40.1797 0.0467 47.6885 44.8908 0.0586 53.9497 50.1186 0.0710 61.0260 55.9169 0.0837 69.0199 62.3445 0.0967 52 TABLE 6. COMPARISON OF MODEL WITH THOENES AND KRAMERS [54] REYNOLDS THOENES 8 KRAMERS (1958) EQUATION SH 3 1.0 RE001IZ SC**1/3 SCHMIDT NUMBER 8 4000. (LIQUIDS) VDIDS FRACTION 8 0.40 REYNOLDS NUMBER RANGE 8 40 - 4000 XS 3 0.3 (6UR/AZ) 40.6615 54.3969 71.9472‘ 94.2029 122.2702 157.5324 201.7237 257.0198 326.1454 412.5041 520.3302 654.8720 822.6120 1031.5341 1291.4520 1614.4116 2015.1856 2511.8839 3126.7029 3886.8476 MODEL THOENES DEVIATION (6KE/ADS) (6KE/ADS) FRACTION 6.5896 6.3766 0.0323 7.5172 7.3754 0.0188 8.5594 8.4821 0.0090 9.7288 9.7058 0.0023 11.0404 11.0575 “0.0015 12.5116 12.5511 “0.0031 14.1628 14.2029 -0.0028 16.0181 16.0318 “0.0008 18.1055 18.0594 0.0025 20.4576 20.3101 0.0072 23.1118 22.8107 0.0130 26.1103 25.5904 0.0199 29.5005 28.6812 0.0277 33.3357 32.1175 0.0365 37.6747 35.9367 0.0461 42.5833 40.1797 0.0564 48.1347 44.8908 0.0673 54.4106 50.1186 0.0788 61.5023 55.9169 0.0908 69.5127 62.3445 0.1031 53 TABLE 7. COMPARISON OF MODEL um: THOENES AND was [54] REYNOLDS THOENES 8 KRAMERS (1958) EQUATION SH 8 1.0 REOIIIZ SCI81/3 SCHMIDT NUMBER 8 1.0 (GASES) VOIDS FRACTION 8 0.50 REYNOLDS NUMBER RANGE 8 4O - 4000 XS 8 0.3 (6UR/AZ) 39.6532 52.2723 68.2434 88.3577' 113.6052 145.2278 184.7829 234.2199 295.9704 373.0563 469.2186 589.0736 738.3027 923.8861 1154.3883 1440.3116 1794.5291 2232.8186 2774.5188 3443.3339 4268.3221 MODEL THOENES DEVIATION (6KE/ADS) (6KE/ADS) FRACTION 7.3841 6.2970 0.1472 8.3994 7.2299 0.1392 9.5265 8.2609 0.1328 10.7772 9.3998 0.1278 12.1676 10.6585 0.1240 13.7167 12.0510 0.1214 15.4457 13.5934 0.1199 17.3790 15.3042 0.1193 19.5443 17.2037 0.1197 21.9731 19.3146 0.1209 24.7011 21.6614 0.1230 27.7678 24.2708 0.1259 31.2173 27.1717 0.1295 35.0983 30.3954 0.1339 39.4648 33.9762 0.1390 44.3770 37.9514 0.1447 49.9018 42.3618 0.1510 56.1140 47.2527 0.1579 63.0978 52.6737 0.1652 70.9478 58.6799 0.1729 79.7704 65.3323 0.1809 54 TABLE 8. COMPARISON OF MODEL WITH THOENES AND KRAMERS [S4] REYNOLDS THOENES 5 KRAMERS (1958) . EQUATION SH 8 1.0 RE981/2 SC'81/3 SCHMIDT NUMBER 8 4000. (LIQUIDS) VOIOS FRACTION 8 0.50 REYNOLDS NUMBER RANGE 3 4O “ 4000 X5 3 003 (6URIAZ) 39.6532 52.2723 68.2434 88.3577' 113.6052 145.2278 184.7829 234.2199 295.9704 373.0563 469.2186 589.0736 738.3027 923.8861 1154.3883 1440.3116 1794.5291 2232.8186 2774.5188 3443.3339 4268.3221 MODEL THOENES DEVIATION (6KE/ADS) (6KE/ADS) FRACTION 7.6487 6.2970 0.1767 8.6622 7.2299 0.1653 9.7893 8.2609 0.1561 11.0424 9.3998 0.1487 12.4365 10.6585 0.1429 13.9894 12.0510 0.1385 15.7218 13.5934 0.1353 17.6582 15.3042 0.1333 19.8265 17.2037 0.1322 22.2586 19.3146 0.1322 24.9899 21.6614 0.1331 28.0603 24.2708 0.1350 31.5139 27.1717 0.1377 35.3994 30.3954 0.1413 39.7710 33.9762 0.1457 44.6887 37.9514 0.1507 50.2196 42.3618 0.1564 56.4388 47.2527 0.1627 63.4301 52.6737 0.1695 71.2884 58.6799 0.1768 80.1198 65.3323 0.1845 55 size naphthalene spheres and cylinders. Beds were randomly packed, 4 in. diameter and 5 to 10 in. high. .Their correlation equation is: 1/3 1/2 Jd I 2.0/Rep Sc . 1.97/Rep which is said to cover the Rep range from 400 to 10,000. In terms Of this work the equation is: Shp/Sc1/3te/(1 - efl' 2.0 E/(l _ e)Sc1/3 + 1.97 6/(1 - e)1/2 [Rep/(1 - c)]'5 with a Rep/(l - 2) range from 667 to 16,667. A theoretical study of gaseous diffusion rates in packed beds using a free surface model (spherical particle surrounded by a spherical envelope of fluid) and boundary layer theory was made by Kusik and Happel [31]. They give the equation: Shp/Sc1/3 Repl/Z a 0.93/(e _ 0.75(1 _ €)(e - .2))0.5 which they say is applicable for Rep]: range of from 100 to 1000 and a voids fraction range from 0.3 to 1.0. The Reynolds number range converts to Rep/(l - e) between 67 and 667 at a porosity of 0.4 and between 233 and 2330 at a porosity of 0.7. Tables 10 and 11 are for voids fractions of 0.4 and 0.7. Liquid mass transfer coefficients fOr randomly packed beds Of benzoic acid spheres and water were measured by Williamson, Bazaire and GeankOplis [59]. Two equations are reported, each covering a different Reynolds number range. The equation: 58 s: Sc' - 2.4(Rep/e)"66 56 TABLE 9. COMPARISON OF MODEL WITH BENNETT AND BRADSHAW [3] BRADSHAW 8 BENNETT (1961) EQUATION J 8 2.0/(RE SCIIII3) + 1.97/RE'*.5 SCHMIDT NUMBER 8 2.57 (GASES) VOIDS FRACTION 8 0.40 REYNOLDS NUMBER RANGE 8 667 - 16667 XS 8 0.3 REYNOLDS MODEL BRADSHAW DEVIATION (6URIAZ) (6KE/ADS) (6KE/ADS) FRACTION 673.5189 26.2911 27.3747 “0.0412 845.8481’ 29.7285 30.5601 “0.0279 1060.4576 33.6169 34.1015 -0.0144 1327.4116 38.0163 38.0375 “0.0005 1659.0617 42.9933 42.4097 0.0135 2070.5549 48.6220 47.2641 0.0279 2580.4587 54.9854 52.6506 0.0424 3211.5306 62.1762 58.6243 0.0571 3991.6634 70.2983 65.2462 0.0718 4955.0464 79.4691 72.5835 0.0866 6143.5903 89.8206 80.7107 0.1014 7608.6738 101.5020 89.7104 0.1161 9413.2845 114.6816 99.6743 0.1308 11634.6421 129.5498 110.7038 0.1454 14367.4106 146.3218 122.9116 0.1599 17727.6347 165.2408 136.4224 0.1744 57 TABLE 10. COMPARISON OF MODEL WITH KUSIK AND HAPPEL [31] KUSIK a HAPPEL (1962) EQUATION SH = 0.93/(E-O.75(l-E)(E-0.2))II.5 REII.5 SCIIl/B SCHMIDT NUMBER I 1.0 (GASES) VOIDS FRACTION 0.40 REYNOLDS NUMBER RANGE 8 67 - 667 XS = 003 REYNOLDS MODEL KUSIK DEVIATION (6UR/AZ) IbKE/ADS) (6KE/ADS) FRACTION 66.1489 7.9246 7.0153 0.1147 76.94301 8.5270 7.5660 0.1127 89.2338 9.1685 8.1480 0.1113 103.2058 9.8513 8.7627 0.1105 119.0673 10.5783 9.4120 0.1102 137.0542 11.3526 10.0979 0.1105 157.4337 12.1777 10.8226 0.1112 180.5085 13.0574 11.5887 0.1124 206.6214 13.9954 12.3986 0.1140 236.1608 14.9961 13.2553 0.1160 269.5664 16.0640 14.1618 0.1184 307.3356 17.2039 15.1214 0.1210 350.0301 18.4214 16.1376 0.1239. 398.2840 19.7220 17.2140 0.1271 452.8119 21.1121 18.3546 0.1306 ‘514.4185 22.5984 19.5634 0.1343 584.0083 24.1880 20.8447 0.1382 662.5978 25.8885 22.2029 0.1423 TABLE 11. COMPARISON OF MODEL WITH KUSIK AND HAPPEL [31] REYNOLDS (6UR/AZ) 232.1225 262.9783 297.7868 337.0403 381.2897 431.1519 487.3167 550.5560 621.7330 701.8132 791.8767 893.1315 1006.9285 1134.7789 1278.3733 1439.6023 1620.5811 1823.6756 2051.5325 2307.1125 KUSIK 8 HAPPEL EQUATION (1962) SH = 0.93/(E-0.75(1-E1(E-0.2)1".5 RE*|.5 SCii1/3 SCHMIDT NUMBER = VDIDS FRACTION = REYNOLDS NUMBER RANGE MODEL (6KE/ADS) 25.0388 26.6128 28.2842 30.0589 31.9433 33.9440 36.0679 38.3225 40.7154 43.2549 45.9495 48.8034 51.8412 55.0582 58.4704 62.0892 65.9269 69.9967 74.3124 78.8888 (GASES) 233 - 2330 KUSIK (6KE/ADS) 23.6251 25.1464 26.7589 28.4680 30.2791 32.1982 34.2311 36.3845 38.6650 41.0796 43.6360 46.3419 49.2057 52.2362 55.4428 58.8352 62.4240 66.2201 70.2353 74.4819 DEVIATION FRACTION 0.0564 0.0551 0.0539 0.0529 0.0520 0.0514 0.0509 0.0505 0.0503 0.0502 0.0503 0.0505 0.0508 0.0512 0.0517 0.0524 0.0531 0.0539 0.0548 0.0558 59 is said to cover a Rep/e range from 0.08 to 125 for a bed porosity of 0.4 and a Schmidt number of 1000. This converts to: .09 Shp/Sc1/3fc/(l - ci . 2.4 Sc 81°66/(l - e)'66 [Rep/(1 _ eH.354 for Rep/(l - e) from 0.053 to 83. Table 12 analyzes this equation. The other equation listed is: 58 1 St Sc‘ 3 0.442(I?.ep/e).'3 covering a Rep/c range from 125 to 5000. This equation converts to: 1/3 .09 61.31 [e/(l - 5)]: 0.442 Sc /(1 - e)°31 [Rep/(l - e)]°69 Shp/Sc at a Rep/(l - 2) range between 83 and 3333 for a voids fraction of 0.4. Table 13 compares the equation with the model. Two equations are reported by Wilson and Geank0plis [60] for mass transfer from randomly packed beds of benzoic acid spheres to water and prepylene glycol solutions. They report the equation: 6 Jd - 1.09 Rep’2/3 for the Rep range from 0.0016 to 55, Schmidt numbers varying from 950 to 70,600 and bed porosities between 0.35 and 0.75. This converts to the equation: 1/3 1/3 Shp/Sc [e/(l - e)]= 1.09/(1 - 6) Rep for a Rep/(l - 6) range from 0.0027 to 92 at a bed porosity of 0.4 and 0.0053 to 183 at a bed porosity of 0.7. Tables 14 through 18 compare the model results with this equation. The other equation: a .1d - 0.25 Rep’°31 60 TABLE 12. COMPARISON OF MODEL WITH WILLIAMSON, BAZAIRB AND GEANKOPLIS [59] NILLIAMSON 5 BAZAIRE 8 GEANKOPLIS (1963) EQUATION ST SC'*.58 8 2.4 (RE/E)**-.66 SCHMIDT NUMBER 8 1000 (LIQUIDS) VOIDS FRACTION 8 0.40 REYNOLDS NUMBER RANGE 8 0.053 - 83 XS 3 003 REYNOLDS MODEL WILLIAMSON DEVIATION 16UR/AZ) (6KE/AOSI (6KE/AOS1 FRACTION 0.0528 0.5484 0.5034 0.0820 0.0789 0.6308 0.5769 0.0855 0.1177 0.7268 0.6609 0.0906 0.1755 0.8376 0.7570 0.0961 0.2614 0.9647 0.8669 0.1014 0.3889 1.1105 0.9922 0.1065 0.5778 1.2779 1.1352 0.1116 0.8569 1.4702 1.2979 0.1172 1.2675 1.6912 1.4827 0.1233 1.8690 1.9455 1.6920 0.1303 2.7443 2.2380 1.9280 0.1385 4.0072 2.5745 2.1929 0.1482 5.8102 2.9613 2.4881 0.1597 8.3509 3.4053 2.8147 0.1734 11.8776 3.9137 3.1729 0.1892 16.6937 4.4938 3.5622 0.2073 23.1624 5.1532 3.9817 0.2273 31.7142 5.8997 4.4307 0.2489 42.8610 6.7420 4.9085 0.2719 57.2182 7.6897 5.4151 0.2957 75.5354 8.7540 5.9514 0.3201 61 TABLE 13. COMPARISON OF MODEL WITH WILLIAMSON, REYNOLDS BAZAIRE AND GEANKOPLIS [59] WILLIAMSON 8 BAZAIRE 8 GEANKDPLIS (19631 EQUATION ST SC'*.58 8 0.442 (RE/E1**-.31 SCHMIDT NUMBER 3 1000 (LIQUIDS) VOIDS FRACTION 8 0.40 REYNOLDS NUMBER RANGE I 83 - 3333 XS = 0.3 I6UR/AZI 83.6600 108.9902 140.8616 180.8422 230.8992 293.4984 371.7243 469.4210 591.3615 743.4491 932.9637 1168.8604 1462.1372 1826.2865 2277.8505 2837.1057 3528.9034 MODEL WILLIAMSON (6KE/ADS) I6KE/ADSI 9.1886 6.1578 10.4353 7.3908 11.8335 8.8218 13.4021 10.4816 15.1635 12.4066 17.1440 14.6400 19.3742 17.2324 21.8891 20.2428 24.7289 23.7395 27.9387 27.8008 31.5691 32.5162 35.6763 37.9883 40.3230 44.3338 45.5790 51.6864 51.5220 60.1985 58.2389 70.0451 65.8272 81.4264 DEVIATION FRACTION 0.3298 0.2917 0.2545 0.2179 0.1818 0.1460 0.1105 0.0752 0.0400 0.0049 -0.0300 -0006‘08 “000994 -001339 -00 168‘. ”002027 ’002369 62 TABLE 14. COMPARISON OF MODEL WITH WILSON AND GEANKOPLIS [60] WILSON 8 GEANKOPLIS (I966) EQUATION E J = 1.09/RE*'2/3 SCHMIDT NUMBER = 950 (LIQUIDS) VOIDS FRACTION = 0.40 REYNOLDS NUMBER RANGE = 0.0027 - 92 XS = 0.3 REYNOLDS MODEL WILSON DEVIATION (6UR/AZ) (6KE/ADSI I6KE/ADS) FRACTION 0.0027 0.2416‘ 0.2134 0.1166 0.0053 0.2785 0.2686 0.0357 0.0107 0.3314 0.3379 -0.0195 0.0424 0.5082 0.5343 -0.0511 0.1665 0.8214 0.8431 -0.0262 0.3290 1.0459 1.0578 ~0.0113 0.6473 1.3298 1.3255 0.0032 1.2662 1.6898 1.6576 0.0190 2.4532 2.1472 2.0665 0.0376 4.6819 2.7284 2.5632 0.0605 8.7345 3.4650 3.1555 0.0893 15.7971 4.3926 3.8445 0.1247 27.5323 5.5482 4.6266 0.1661 46.1803 6.9723 5.4971 0.2115 74.7931 8.7131 6.4556 0.2590 63 TABLE 15. COMPARISON OF MODEL WITH WILSON AND GEANKOPLIS [60] WILSON 8 GEANKOPLIS (1966) EQUATION E J = 1.09/RE'i2/3 SCHMIDT NUMBER = 70600 (LIQUIDS) VOIDS FRACTION = 0.40 REYNOLDS NUMBER RANGE = 0.0027 - 92 XS = 003 REYNOLDS MODEL WILSON DEVIATION (6UR/AZ) (6KE/ADS) (6KE/ADS) FRACTION 0.0027 0.2070 0.2134 -0.0309 0.0053 70.2633 0.2686 -o.ozoo 000107 003342 003379 “000111 0.0213 0.4234 0.4250 -0.0037 0.0424 0.5355 0.5343 0.0023 0.0841 0.6764 0.6713 0.0075 0.1665 0.8537 0.8431 0.0124 0.3290 1.0770 1.0578 0.0178 0.6473 1.3591 1.3255 0.0247 1.2662 1.7163 1.6576 0.0341 2.4532 2.1701 2.0665 0.0477 4.6819 2.7475 2.5632 0.0670 8.7345 3.4805 3.1555 0.0933 15.7971 4.4049 3.8445 0.1272 27.5323 5.5579 4.6266 0.1675 46.1803 6.9799 5.4971 0.2124 74.7931 8.7192 6.4556 0.2596 64 TABLE 16. COMPARISON OF MODEL WITH WILSON AND GEANKOPLIS [60] WILSON 8 GEANKOPLIS (1966) EQUATION E J = 1.09/RE**2/3 SCHMIDT NUMBER = 950 (LIQUIDS) VOIDS FRACTION = 0.70 REYNOLDS NUMBER RANGE = 0.0053 - 183 XS = 0.3 REYNOLDS MODEL WILSON DEVIATION (6UR/AZ) (6KE/ADS) (6KE/ADS) FRACTION 0.0050 0.3839 0.4183 ~0.0896 0.0101 0.4783 0.5260 -0.0996 0.0200 0.6051 0.6610 '0.0924 0.0397 0.7706 0.8302 -0.0774 0.0786 0.9814 1.0420 -0.0616 0.1548 1.2478 1.3062 -0.0467 0.3034 1.5850 1.6345 -0.0312 0.5896 2.0120 2.0396 -0.0137 1.1306 2.5520 2.5339 0.0071 2.1237 3.2320 3.1264 0.0326 3.8752 4.0802 3.8204 0.0636 6.8225 5.1235 4.6130 0.0996 11.5576 6.3869 5.4992 0.1389 18.8821 7.8977 6.4767 0.1799 29.9160 9.6911 7.5505 0.2208 46.2762 11.8153 8.7322 0.2609 70.3346 14.3362 10.0399 0.2996 105.5814 17.3412 11.4957 0.3370 157.1198 20.9410 13.1245 0.3732 65 TABLE 17. COMPARISON OF MODEL WITH WILSON AND GEANKOPLIS [60] WILSON 8 GEANKOPLIS (1966) EQUATION E J = 1.09/RE'52/3 SCHMIDT NUMBER = 70600 (LIQUIDS) VOIDS FRACTION = 0.70 REYNOLDS NUMBER RANGE = 0.0053 - 183 XS = 0.3 REYNOLDS MODEL WILSON DEVIATION (6UR/AZ) (6KE/AOS) (6KE/ADS) FRACTION 0.0050 0.3979 0.4183 -0.0513 0.0101' 0.5035 0.5260 -0.0446 0.0200 0.6362 0.6610 -0.0390 0.0397 0.8030 0.8302 -0.0339 0.0786 1.0129 1.0420 -0.0286 0.1548 1.2777 1.3062 -0.0223 0.3034 1.6122 1.6345 -0.0137 0.5896 2.0358 2.0396 *0.0018 1.1306 2.5721 2.5339 0.0148 2.1237 3.2483 3.1264 0.0375 3.8752 4.0932 3.8204 0.0666 6.8225 5.1335 4.6130 0.1013 11.5576 6.3946 5.4992 0.1400 18.8821 7.9037 6.4767 0.1805 29.9160 9.6958 7.5505 0.2212 46.2762 11.8191 8.7322 0.2611 70.3346 14.3394 10.0399 0.2998 105.5814 17.3441 11.4957 0.3371 157.1198 20.9436 13.1245 0.3733 TABLE 18. COMPARISON OF MODEL WITH WILSON AND GEANKOPLIS [60] REYNOLDS (6UR/AZ) 92.6051 115.0941 142.2887 175.1088 214.6648 262.2967 319.6189 388.5730 471.4868 571.1448 690.8685 834.6116 1007.0720 1213.8246 1461.4782 1757.8623 2112.2491 2535.6173' WILSON 8 GEANKOPLIS EQUATION E J SCHMIDT NUMBER VOIDS FRACTION 3 0.40 REYNOLDS NUMBER RANGE 8 92 - 2500 XS = 0.3 MODEL (6KE/ADS) 9.6456 10.7156 11.8924 13.1871 14.6124 16.1827 17.9146 19.8266 21.9396 24.2767 26.8637 29.7285 32.9020 36.4179 40.3129 44.6272 49.4048 54.6939 (1966) 0.25/RE'&.31 (LIQUIDS) WILSON (6KE/ADS) 6.6633 7.7417 8.9619 10.3417 11.9022 13.6672 15.6642 17.9245 20.4836 23.3812 26.6621 30.3764 34.5799 39.3351 44.7115 50.7870 57.6484 65.3929 DEVIATION FRACTION 0.3091 0.2775 0.2464 0.2157 0.1854 0.1554 0.1256 0.0959 0.0663 0.0368 0.0075 -0.0217 -0.0509 '0.0801 '0.1091 -0.1380 -0.1668 -001956 TABLE 19. COMPARISON OF MODEL WITH WILSON AND GEANKOPLIS [60] REYNOLDS (6UR/AZ) 92.6051 115.0941 142.2887 175.1088 214.6648 262.2967 319.6189 388.5730 471.4868 571.1448 690.8685 834.6116 1007.0720 1213.8246 1461.4782 1757.8623 2112.2491 2535.6173 WILSON 8 GEANKOPLIS EQUATION E J SCHMIDT VOIDS FRACTION = 0.40 REYNOLDS NUMBER RANGE XS = 0.3 NUMBER MODEL (6KE/ADS) 9.6513 10.7209 11.8973 13.1917 14.6169 16.1870 17.9188 19.8305 21.9439 24.2807 26.8679 29.7328 32.9061 36.4223 40.3172 44.6318 49.4093 54.6977 (1966) 0.25/RE**.31 (LIQUIDS) 92 * 2500 WILSON (6KE/ADS) 6.6633 7.7417 8.9619 10.3417 11.9022 13.6672 15.6642 17.9245 20.4836 23.3812 26.6621 30.3764 34.5799 39.3351 44.7115 50.7870 57.6484 65.3929 DEVIATION FRACTION 0.3095 0.2778 0.2467 0.2160 0.1857 0.1556 0.1258 0.0961 0.0665 0.0370 0.0076 ’000216 -0.0508 -000799 ‘001089 ”001379 ”001667 -0.1955 68 TABLE 20. COMPARISON OF MODEL WITH WILSON AND GEANKOPLIS [60] REYNOLDS (6UR/AZ) 181.3178 227.8180 285.7430 357.8186 447.3915 558.5660 696.3739 866.9824 1077.9505 1338.5433 1660.1180 2056.5974 2545.0501 3146.4014 3886.3040 .4796.2047 WILSON 8 GEANKOPLIS (1966) EQUATION E J = 0.25/RE09.31 SCHMIDT NUMBER 950 (LIQUIDS) VOIDS FRACTION 0.70 REYNOLDS NUMBER RANGE = 183 - 5000 XS = 0.3 MODEL WILSON DE (6KE/ADS) (6KE/ADS) FR 22.4266 13.1327 25.0308 15.3733 27.9346 17.9744 31.1730 20.9922 34.7842 24.4910 38.8100 28.5439 43.2961 33.2348 48.2931 38.6597 53.8570 44.9288 60.0503 52.1685 66.9420 60.5240 74.6098 70.1625 83.1405 81.2761 92.6312 94.0858 103.1907 108.8460 114.9411 125.8496 VIATION ACTION 0.4144 0.3858 0.3565 0.3265 0.2959 0.2645 0.2323 0.1994 0.1657 0.1312 0.0958 0.0596 0.0224 -0.0157 ”0.0548 ’0009’99 TABLE 21. COMPARISON OF MODEL WITH WILSON AND GEANKOPLIS [60] REYNOLDS (6URIAZ) 181.3178 227.8180 285.7430 357.8186 447.3915 558.5660 696.3739 866.9824 1077.9505 1338.5433 1660.1180 2056.5974 2545.0501 3146.4014 3886.3040 ~4796.2047 WILSON 8 GEANKOPLIS EQUATION E J SCHMIDT NUMBER 8 70600 VOIDS FRACTION REYNOLDS NUMBER RANGE 0.3 MODEL (6KE/ADS) 22.4291 25.0332 27.9367 31.1755 34.7864 38.8115 43.2987 48.2949 53.8578 60.0525 66.9437 74.6112 83.1416 92.6330 103.1971 114.9396 (1966) 0.25/RE'*.31 (LIQUIDS) 183 - 5000 WILSON (6KE/ADS) 13.1327 15.3733 17.9744 20.9922 24.4910 28.5439 33.2348 38.6597 44.9288 52.1685 60.5240 70.1625 81.2761 94.0858 108.8460 125.8496 DEVIATION FRACTION 0.4144 0.3858 0.3566 0.3266 0.2959 0.2645 0.2324 0.1995 0.1657 0.1312 0.0958 0.0596 0.0224 -000156 “0.0547 -000949 70 is for a Rep ranging from 55 to 1500 with Schmidt numbers and voids fractions being the same as for the other equation. This equation converts to: sup/5c1/3fe/(1 - £)1- 0.25/(1 - 2) Rep'69 for a Rep/(1 - 5) range from 92 to 2500 at a porosity of 0.4 and 183 to 5000 at a bed porosity of 0.7. Tables 18 through 21 show com- parison of results of the model with the equation. In his thesis Galloway [15] reports equations containing turbulence factors and graphs of c Jd versus ReP for beds of spheres, cylinders and commercial packing. Tables 22 through 30 show results obtained by estimating equations from his graphs and using these equations for comparison with the model. Estimated equations for spheres are: e Jd - 0.85 Rep"5° for a Rep range between 3 and 10,000 and a Schmidt number of 1000. This converts to: Shp/Scl/3[e/(l - c)]- 0.850 - e)"5[aep/(1 - e)]'5 for a Rep/(l - a) range between 5 and 16,700 for a bed porosity of 0.4' and between 10 and 33,333 for a voids fraction of 0.7. c Jd - 0.95 Rep"51 for a Rep range between 10 and 10,000 and a Schmidt number of 1. This converts to: Shp/Sc1/3[€/(l - 6)]. 0.95(1 _ €)'051[Rep/(1 _ 5)].49 71 for a Rep/(l - c) range between 17 and 16,700 for a bed porosity of 0.4 and between 33 and 33,333 for a voids fraction of 0.7. Tables 22 to 25 analyze these equations. Estimated equations for commercial packing are: e Jd - 0.7 Rep“48 for a Rep range between 35 and 2000 and a Schmidt number of 1. This converts to: 5 /S<=1/3 E/(l - 611- 0.7(1 - e)’°48[ge /(1 - c)]'52 hp P for a Rep/(1 - c) range between $8 and 3333 for a bed porosity of 0.4 and between 117 and 6667 for a voids fraction of 0.7. -e32 c Jd I 0.23 Rep for 3 Rep range between 2000 and 10,000 and a Schmidt number of 1000. This converts to: sup/SCUSIC/(l - c)] I 0.230 - £)-'32[Rep/(1 - “1.68 for a Rep/(1 - a) range between 3333 and 16,667 for a bed porosity of 0.4. c ad - 0.50 aep"4l for a Rep range between 35 and 2000 and a Schmidt number of 1000. This converts to: sup/scum“: - .)]- 0.500 - .y-“mepm , 01-59 72 TABLE 22. COMPARISON OF MODEL WITH GALLOWAY AND SAGE, SPHERES [15] REYNOLDS (6UR/AZ) GALLOWAY 8 SAGE (1967) ESTIMATED EQUATION FOR BEDS OF SPHERES E J 8 0.95/REOO.51 SCHMIDT NUMBER 8 1 (GASES) VOIDS FRACTION 8 0.40 REYNOLDS NUMBER RANGE 8 17 - 16700 16.0226' 27.8987 46.7518 75.6586 118.9646 182.9820 276.9902 414.6284 615.7833 909.1413 1335.7102 1953.7778 2845.9635 4129.2699 5969.3868 8600.9973 12356.5448 17706.9452 XS 8 0.3 MODEL GALLOWAY DEVIATION (6KE/ADS) (6KEIADS) FRACTION ‘02321 ‘07993 -0013‘0 5.3202 6.2980 -0.1837 6.7193 8.1108 ‘0e2070 8.4574 10.2685 -0.2141 10.5737 12.8180 -0.2122 13.1487 15.8287 -0.2038 16.2933 19.3942 ‘0.1903 20.1469 23.6330 '0.1730~ 2‘08866 28.6870 '001527 3007331 3‘07212 ‘001297 37.9542 41.9242 'OeIO‘b 46.8719 50.5120 -0.0776 57.8739 60073‘9 ’000‘9‘ 71.4299 72.8860 “0.0203 88.1137 87.3116 0.0091 108.6299 104.4228 0.0387 133.8460 124.7084 0.0682 164.8315 148.7499 0.0975 73 TABLE 23. COMPARISON OF MODEL WITH GALLOWAY AND SAGE, SPHERES [15] REYNOLDS (6UR/AZ) GALLDWAY 8 SAGE (1967) ESTIMATED EQUATION FOR BEDS OF SPHERES E J 8 0.95/RE88.51 SCHMIDT NUMBER 2 1 (GASES) VOIDS FRACTION 8 0.70 REYNOLDS NUMBER RANGE 8 33 - 33333 34.3932 52.8744 80.0105 119.7385 177.7973 262.4626 385.5627 563.9079 821.3252 1191.5570 1722.3868 2481.4956 3564.7579 5107.9823 7303.5199 10423.7565 14854.3412 21141.1899 30056.9690 XS 8 0.3 MODEL GALLDWAY DEVIATION (6KE/ADS) (6KE/ADS) FRACTION 10.0932 9.9371 0.0154 12.3347 12.2682 0.0053 14.9978 15.0291 -0.0020 18.1788 18.3116 '0.0073 21.9951 22.2256 -0.0104 26.5873 26.8989 -0.0117 32.1195 32.4771 ’0.0111 38.7822 39.1276 “0.0089 46.7982 47.0439 -0.0052 67.9957 67.6232 0.0054 81.8735 80.8725 0.0122 98.5255 96.5798 0.0197 118.5122 115.1950 0.0279 142.5150 137.2532 0.0369 171.3632 163.3893 0.0465 206.0669 194.3568 0.0568 247.8578 231.0495 0.0678 298.2387 274.5268 0.0795 74 TABLE 24. COMPARISON OF MODEL WITH GALLOWAY AND SAGE, SPHERES [15] REYNOLDS (6UR/AZ) 7.2776’ 13.2947 23.4360 39.7536 65.0221 103.1153 159.6190 242.7263 364.4930 542.5527 802.4290 1180.7022 1729.4439 2522.5093 3664.5050 5303.5616 7649.4773 10999.4387 15774.4283 MODEL (6KE/ADS) 3.2283 4.0952 5.1789 6.5186 8.1595 10.1587 12.5910 15.5542 19.1772 23.6257 29.1067 35.8728 44.2276 54.5361 67.2397 82.8762 102.1049 125.7371 154.7732 GALLDWAY 8 SAGE ESTIMATED EQUATION FOR BEDS OF SPHERES E J 3 0.85/RE89.50 SCHMIDT NUMBER 3 1000 VOIDS FRACTION 3 0.40 REYNOLDS NUMBER RANGE 3 5 - 16700 XS 3 003 (1967) (LIQUIDS) GALLDWAY (6KE/ADS) 2.9603 4.0011 5.3123 6.9188 8.8485 11.1430 13.8639 17.0962 20.9501 25.5602 31.0846 37.7062 45.6348 55.1137 66.4279 79.9147 95.9752 115.0876 137.8224 DEVIATION FRACTION 0.0830 0.0229 -0.0257 80.0613 "0e0844 '0.0968 -0.1010 -0.0991 -000924 -000818 -0e0679 -000511 -0.0318 ‘0. 0105 0.0120 0.0357 0.0600 0.0846 0.1095 TABLE 25. COMPARISON OF MODEL WITH GALLDWAY AND SAGE, SPHERES [15] REYNOLDS (6UR/AZ) 13.3576 21.6167 33.9899 52.2805 79.1400 118.4652 175.9381 259.7546 381.6315 558.2222 813.1324 1179.7914 1705.5391 2457.4278 3530.4414 5059.1272 7234.0508 10325.0707 14714.2601 20942.4748 29775.2226 SPHERES SCHMIDT VOIDS FRACTION 3 0.70 REYNOLDS NUMBER RANGE 8 10 - 33333 XS 8 003 GALLDWAY 8 SAGE ESTIMATED EQUATION FOR BEDS OF E J = 0.85/RE8*.50 NUMBER MODEL (6KE/ADS) 6.7951 8.3831 10.2660 12.4967 15.1469 18.3106 22.1053 26.6711 32.1721 38.7982 46.7716 56.3548 67.8620 81.6717 98.2436 118.1347 142.0238 170.7337 205.2717 246.8614 296.9975 (1967) (LIQUIDS) GALLDWAY (6KE/ADS) 5.6718 7.2152 9.0475 11.2209 13.8056 16.8909 20.5844 25.0115 30.3165 36.6658 44.2526 53.3041 64.0898 76.9305 92.2088 110.3814 131.9924 157.6902 188.2467 224.5806 267.7847 DEVIATION FRACTION 0.1653 0.1393 0.1186 0.1020 0.0885 0.0775 0.0688 0.0622 0.0576 0.0549 0.0538 0.0541 0.0555 0.0580 0.0614 0.0656 0.0706 0.0763 0.0829 0.0902 0.0983 76 TABLE 26. COMPARISON OF MODEL WITH GALLDWAY AND SAGE, COMMERCIAL PACKING [15] GALLDWAY 8 SAGE (1967) ESTIMATED EQUATION FOR COMMERCIAL PACKING E J 3 Oe7/RE..e#8 SCHMIDT NUMBER 3 1 (GASES) VOIDS FRACTION 8 0.40 REYNOLDS NUMBER RANGE ‘ 58 - 3333 X5 8 0.3 REYNOLDS (6URIAZ) 59.4799 78.4085 102.3652 132.5366 170.4078 217.8417 277.1744 351.3298 443.9556 559.5844 703.8279 883.6104 1107.4541 1385.8291 ~1731.5826 2160.4675 2691.7937 3349.2280 MODEL GALLDWAY (6KE/ADS) (6KEIADS) 7.5302 7.4861 8.6058 8.6427 9.8115 9.9280 11.1626 11.3553 12.6788 12.9407 14.3824 14.7034 16.2989 16.6654 18.4574 18.8519 20.8915 21.2912 23.6398 24.0146 26.7462 27.0562 30.2597 30.4537 34.2353 34.2479 38.7340 38.4834 43.8238 43.2091 49.5802 48.4786 56.0881 54.3509 63.4420 60.8915 DEVIATION FRACTION 0.0058 -000042 -000118 -000172 -0.0206 '0.0223 -00022‘ -0.0213 -0.0191 -0.0158 -0001 15 -00006‘ -0.0003 0.0064 0.0140 0.0222 0.0309 0.0402 77 TABLE 27. COMPARISON OF MODEL WITH GALLDWAY AND SAGE, COMMERCIAL PACKING [15] GALLOWAY 8 SAGE (1967) ESTIMATED EQUATION FOR COMMERCIAL PACKING E J 8 0.7/RE58.48 SCHMIDT NUMBER 8 1 (GASES) VOIDS FRACTION 8 0.70 REYNOLDS NUMBER RANGE 8 117 - 6667 XS 8 0.3 REYNOLDS (6UR/AZ) 120.1870 151.5724 190.7316 239.5497 300.3476 375.9781 469.9422 586.5336 731.0155 909.8388 1130.9102 1403.9211 1740.7517 2155.9658 2667.4182 3296.9977 4071.5381 5023.9338 6194.5064 MODEL GALLDWAY (6KE/AOS) (6KEIAOS) 18.2114 15.0524 20.3618 16.9825 22.7569 19.1381 25.4265 21.5459 28.4033 24.2350 31.7229 27.2373 35.4241 30.5874 39.5495 34.3235 44.1459 38.4876 49.2648 43.1262 54.9635 48.2905 61.3058 54.0378 68.3626 60.4314 76.2135 67.5419 84.9474 75.4479 94.6639 84.2367 105.4746 94.0057 117.5047 104.8630 130.8944 116.9292 DEVIATION FRACTION 0.1734 0.1659 0.1590 0.1526 0.1467 0.1413 0.1365 0.1321 0.1281 0.1246 0.1214 0.1185 0.1160 0.1137 0.1118 0.1101 0.1087 0.1075 0.1066 78 TABLE 28. COMPARISON OF MODEL WITH GALLDWAY AND SAGE, COMMERCIAL PACKING [IS] GALLDWAY 8 SAGE (1967) ESTIMATED EQUATION FOR COMMERCIAL PACKING E J 8 0.50/RE88.41 SCHMIDT NUMBER 8 1000 (LIQUIDS) VOIDS FRACTION 8 0.40 REYNOLDS NUMBER RANGE 8 58 - 3333 XS 8 0.3 REYNOLDS (6URIAZ) 59.4799 78.4085 102.3652 132.5366 170.4078 217.8417 277.1744 351.3298 443.9556 559.5844 703.8279 883.6104 1107.4541 1385.8291 1731.5826 2160.4675 2691.7937 3349.2280 MODEL GALLDWAY (6KE/ADS) (6KE/ADS) 7.8287 6.8676 8.9100 8.0835 10.1229 9.4605 11.4831 11.0180 13.0089 12.7792 14.7218 14.7717 16.6471 17.0275 18.8143 19.5839 21.2574 22.4832 24.0153 25.7732 27.1319 29.5075 30.6564 33.7459 34.6437 38.5549 39.1548 44.0085 44.2578 50.1891 50.0283 57.1888 56.5509 65.1107 63.9206 74.0705 DEVIATION FRACTION 0.1227 0.0927 0.0654 0.0404 0.0176 -0.0033 -000228 -0.0409 80.0576 “Go 0731 -0.0875 -0.1007 -0.1128 -0.1239 ”0.1340 -00 1431 -0.1513 -0.1587 79 TABLE 29. COMPARISON OF MODEL WITH GALLDWAY AND SAGE, COMMERCIAL PACKING [15] GALLDWAY 8 SAGE (1967) ESTIMATED EQUATION FOR COMMERCIAL PACKING E J 8 0.23/RE8*.32 SCHMIDT NUMBER 8 1000 (LIQUIDS) VOIDS FRACTION 8 0.40 REYNOLDS NUMBER RANGE 8 3333 - 16667 XS 8 0.3 REYNOLDS (6UR/AZ) 3419.3315 3770.5474 4156.7638 4581.3815 5048.1279 5561.0876 6124.7370 6743.9821 7424.1993 8171.2809 8991.6844 9892.4867 10881.4438 11967.0551 13158.6356 14466.3931 15901.5144 17476.2585 MODEL GALLDWAY (6KE/ADS) (6KE/ADS) 64.6694 68.5171 68.3292 73.2275 72.1945 78.2479 76.2764 83.5982 80.5869 89.2993 85.1385 95.3735 89.9444 101.8448 95.0186 108.7383 100.3758 116.0810 106.0317 123.9015 112.0026 132.2304 118.3061 141.1000 124.9604 150.5449 131.9852 160.6019 139.4007 171.3100 147.2289 182.7108 155.4928 194.8487 164.2157 207.7707 DEVIATION FRACTION ”000594 '0.0716 -0.0838 -0.0959 “0.1081 -001202 “001323 '001443 “001564 -001685 -0.1806 -001926 -0.2047 “0.2168 -0.2289 -0e2409 °0.2531 -0.2652 80 TABLE 30. COMPARISON OF MODEL WITH GALLOWAY AND SAGE, COMMERCIAL PACKING [15] GALLDWAY 8 SAGE (1967) ESTIMATED EQUATION FOR COMMERCIAL PACKING E J 8 0.50/RE88.41 SCHMIDT NUMBER 8 1000 (LIQUIDS) VOIDS FRACTION 8 0.70 REYNOLDS NUMBER RANGE 8 117 - 6667 X5 8 0.3 REYNOLDS (6UR/AZ) 120.1870. 151.5724 190.7316 239.5497 300.3476 375.9781 469.9422 586.5336 731.0155 909.8388 1130.9102 1403.9211 1740.7517 2155.9658 '266704182 3296.9977 4071.5381 5023.9338 6194.5064 MODEL GALLDWAY (6KE/ADS) (6KE/ADS) 18.4361 13.8186 20.5849 15.8458 22.9782 18.1467 25.6457 20.7583 28.6203 23.7218 31.9377 27.0829 35.6369 30.8927 39.7602 35.2081 44.3547 40.0928 49.4720 45.6183 55.1695 51.8648 61.5108 58.9226 68.5671 66.8936 76.4176 75.8925 85.1519 86.0486 94.8687 97.5080 105.6806 110.4352 117.7119 125.0161 131.1033 141.4601 DEVIATION FRACTION 0.2504 0.2302 0.2102 0.1905 0.1711 0.1520 0.1331 0.1144 0.0960 0.0778 0.0599 0.0420 0.0244 0.0068 -000105 -0.0273 '0e0‘49 ~0.0620 -000789 81 for a Rep/(1 - c) range between 58 and 3333 for a bed porosity of 0.4 and between 117 and 6667 for a voids fraction of 0.7. Tables 26 to 30 show these equations. Data for mass transfer in randomly packed beds of spheres to gases at low Reynolds numbers is given by Petrovic and Thodos [40]. The values given are corrected for axial mixing. Their recommended equation is: e Jd - 0.357/Rep'359 and is recommended for a Rep between 3 and 230. This converts to the equation: Shp/Scl/sfc/(l - c)]- 0.357 Rep’641/(1 - c) with a Rep/(1 - e) range from S to 390. Comparison of this equation with the model is in Table 31. Table 32 compares the model with the equation of Jolls and Hanratty [27]. They used electrochemical techniques to study mass transfer rates to an active sphere in a dumped bed. They report the equation: 1/3 _ .58 Shp/Sc 1.44 Rep _ to be good for a Schmidt number of 1700, voids fraction of 0.41 and a Re range between 35 and 140. This converts to: P 5hp/5c1/3[e/(1 - e)]- 1.44 c/(l - 6) Rep'58 at a Rep/(1 - 0) range between 59 and 237. 82 TABLE 31. COMPARISON OF MODEL WITH PETROVIC AND THODOS [40] PETROVIC 8 THODOS (1968) EQUATION E J 8 0.357/RE8*.359 SCHMIDT NUMBER 8 3 (GASES) VOIDS FRACTION 8 0.40 REYNOLDS NUMBER RANGE 8 5 - 390 XS 8 0.3 REYNOLDS MODEL PETROVIC DEVIATION (6URIAZ) (6KE/ADS) (6KE/ADS) FRACTION 4.9733 2.6797 1.1991 0.5525 7.1760 3.0551 1.5168 0.5035 10.2537 3.5051 1.9067 0.4560 14.4859 4.0366 2.3794 0.4105 20.2101 4.6556 2.9456 0.3672 27.8271 5.3662 3.6159 0.3261 37.8124 6.1719 4.4012 0.2868 50.7344 7.0783 5.3138 0.2492 67.2819 8.0954 6.3678 0.2134 88.3002 9.2360 7.5800 0.1792 114.8381 10.5147 8.9707 0.1468 148.2052 11.9482 10.5641 0.1158 190.0427 13.5558 12.3895 0.0860 242.4094 15.3604 14.4813 0.0572 307.8858 17.3888 16.8798 0.0292 ' 389.6970 19.6724 19.6321 0.0020 83 TABLE 32. COMPARISON OF MODEL WITH JOLLS AND HANRATTY [27] REYNOLDS (SUR/Al) 58.8424 66.6772 75.3981 85.0932 95.8594 JOLLS 8 HANRATTY (1969) EQUATION SH/SC881/3 8 1.44 RE88.58 SCHMIDT NUMBER 8 1700 (LIQUIDS) VOIDS FRACTION 80.41 REYNOLDS NUMBER RANGE 8 59 - 237 XS 8 0.3 107.8039 121.0455 135.7153 151.9587 169.9367 189.8276 211.8288 236.1587 MODEL JOLLS DEVIATION (6KE/ADS) (6KE/ADS) FRACTION 7.9148 7.8308 0.0106 8.8847 9.0418 -0.0176 9.4082 9.6990 '0.0309 9.9591 10.3928 '0.0435 10.5389 11.1254 -0.0556 11.1491 11.8986 -0.0672 11.7914 12.7149 80.0783 13.9287 15.4467 -0.1089 15.5500 17.5326 -0.1274 84 TABLE 33. COMPARISON OF MODEL WITH WILKINS AND THODOS [58] REYNOLDS (6UR/AZ) 30.5370 41.3359 55.2024 73.0405 95.5950 124.0220 159.7301 204.4754 200.4010 330.4450 417.0749 527.0341 003.2337 033.0319 1044.5050 1307.5790 1034.4309 ‘2040.0195 2542.0420 3104.7524 WILKINS 8 THODOS (1969) EQUATION E J 3 0.589/RE88.427 SCHMIDT NUMBER 8 3 (GASES) VOIDS FRACTION 8 0.40 REYNOLDS NUMBER RANGE 8 33 8 3333 X5 3 003 MODEL WILKINS (6KE/ADS) (6KE/ADS) 5.5967 5.1958 6.4317 6.1801 7.3700 7.2988 8.4226 8.5643 9.6028 9.9915 10.9258 11.5989 12.4092 13.4086 14.0731 15.4469 15.9415 17.7445 18.0426 20.3371 20.4093 23.2650 23.0791 26.5740 26.0949 30.3151 29.5045 34.5448 33.3614 39.3260 37.7251 44.7281 42.6617 50.8281 48.2448 57.7118 54.5568 65.4746 61.6895 74.2231 DEVIATION FRACTION 0.0716 0.0391 0.0096 80.0168 -000404 -000616 -000805 “000976 80.1131 80.1271 -001399 -001514 80.1617 80.1708 -001787 80.1856 ’001914 80.1962 80.2001 -002031 85 TABLE 34. SUMMARY OF RESULTS FOR GASES REYNOLDS DEVIATION AVERAGE TABLE VOIDS NUMBER FRACTION DEVIATION NUMBER FRACTION RANGE RANGE FRACTION 31 0.40 5-390 .55 -.- 0 +0.15 22 0.40 17-16,700 -.13-+- -.21-.- .10 -0.02 2 0.30 30-5000 .16 -.- -.01 +0.03 3 0.64 30-5000 .10 +-.27 -0.15 33 0.40 33-3333 .07 + -.20 -0.10 23 0.70 33-33,333 0 +.07 +0.02 4 0.40 40-4000 -.29 ->- .02 -0.04 5 0.40 40-4000 -.03 -e- .10 +0.04 7 0.50 40-4000 .14 —>- .12—>.10 +0.14 26 0.40 50-3333 0+ -.02 4.04 +0.01 10 0.40 67-667 .11 ->- .14 +0.12 27 0.70 117-6667 .17 + .11 +0.13 11 0.70 233-2330 .05 +.06 +0.05 9 0.40 667-16,667 -.04 +.17 +0.00 AVERAGE PERCENTAGE DEVIATION 8 +34 86 TABLE 35. SUMMARY OF RESULTS FOR LIQUIDS REYNOLDS DEVIATION AVERAGE TABLE VOIDS NUMBER FRACTION DEVIATION NUMBER FRACTION RANGE RANGE FRACTION 14 0.40 0.0027-92 .12+-.05 —+-.26 +0.06 Sc=950 15 0.40 0.0027-92 -.03 —>- .26 +0.06 56-70600 16 0.70 0.0053-103 -.09 + .37 +0.05 Sc-9SO - 17 0.70 0.0053-183 -.05 -—+-.37 +0.06 Sc-70600 12 0.40 0.053-03 .00 —0- .32 +0.15 24 0040 5-16.700 008+ -010 + 011 70002 25 0.70 10-33,333 .16 -+- .05 -+ .10 +0.00 6 . 0.40 40-4000 .03—0- 0 -—.- .10 +0.04 0 0.50 40-4000 .10-0- .13 ->- .10 +0.15 20 0.40 50-3333 .12—> -.16 - - -0.04 32 0.41 59-237 . .01....- -.13 -0.03 13 0.40 83-3333 .33 +-.24 +0.03 10 0.40 92-2500 .30 -e--.20 +0.05 30 0.70 117-6667 ‘ L25 + -.00 +0.05 20 0.70 103-5000 ‘ .41->- -.10 +0.14 29 0.40 3333-16,667 -.O6 +-.27 +0.15 AVERAGE PERCENTAGE DEVIATION 8 +54 87 In order to demonstrate the usefulness of the computer model the results of an example problem, taken from Satterfield [48], are shown in Table 36. Table 40 in Appendix E is the program listing for Table 36. This program calculates h, kc and pressure loss per unit length of bed by reading in the standard packed bed parameters and fluid properties. Actual Reynolds number (REI) is the Rep/(l - a) calculated from bed parameters and fluid properties. Calculated Reynolds number (REE) is the Rep/(1 - 6) calculated from (VY2)m. The (W2)m used is calculated from the actual REI. Since the relationship between (VYZ)m and the Reynolds number changes with the porosity of the bed, the constants A1 through A9 have to be changed accordingly. The values for these constants are given in Table 37, Appendix C. 88 TABLE 36. EXAMPLE USING MODEL GIVEN FLUID PROPERTIES VISCOSITY (V15) 8 0.092 LB/(FT.HR) HEAT CAPACITY (CP) 8 0.90 BTU/(LBoDEG F) SUPERFICIAL VELOCITY (VEL) 8 1320 FT/HR THERMAL CONDUCTIVITY (AK) 8 0.131 BTU/(FToHRcDEG F) DENSITY (RHO) 8 1.05 L8/(CU FT) DIFFUSION COEFFICIENT (DIF) 8 0.0296 SQ FT/HR GIVEN BED CHARACTERISTICS BED POROSITY (EP) 8 0.40 SPECIFIC SURFACE (ASP) 8 311 SQ FT/(CU FT) PARTICLE DIAMETER (DPA) 8 0.01285 FT COMPUTER RESULTS ACTUAL CALCULATED SCHMIDT REYNOLDS REYNOLDS VYSM NUMBER NUMBER NUMBER 165593.6539 2.9601 322.6467 322.1269 HEAT MASS TRANSFER TRANSFER DP/DL COEFFICIENT COEFFICIENT PSI/FT 433.9091 98.0404 0.0397 DISCUSSION OF RESULTS The model equations of this thesis simulate heat and mass transfer rates in a randomly packed bed better over a wide range parameters than any of the empirical equations we found in the literature. This is because the equations are derived from basic fluid dynamics and transport phenomena principles. Other authors' equations are obtained by drawing arbitrary straight lines through scattered data points and in some cases using special mixing or turbulence factors to fit their data. Some of the earlier authors did not recognize that Jd was inversely proportional to voids fraction. ch, and not Jd, is shown to be a function of Reynolds number by Thoenes 0 Kramers [54], Gupta 8 Thodos [22], Wilson 8 Geankoplis (60], and others. The model equations also cover the entire range of Reynolds numbers, Schmidt or Prandtl numbers, and , voids fractions whereas literature equations are for limited ranges. Comparisons between the model and empirical equations are given in Tables 2 to 33 and summarized in Tables 34 and 35. The equation of Chu, Kalil and Wetteroth [8] is analyzed in ‘Tables 2 and 3. Their equation is said to apply to both packed and fluidized beds and shows no dependency of Jd on voids fraction. In the article they show data for fixed beds with voids fractions of about 0.4 and expanded beds of higher porosities. Table 2, which is for a voids fraction of 0.38, shows a much better correlation than Table 3, which is for a porosity of 0.64. The equation of Chu, 89 90 et. a1., gives mass transfer rates that are proportional to voids fraction compared to the model equations which indicate less dependency. For example, at an interstitial Reynolds number of 3900, the increase in mass transfer by the Chu equation is 0.64/0.38 whereas the model equations show an increase of only the square root of this ratio. In addition mass transfer rates are necessarily higher in fluidized beds due to the increased surface contact between solid and fluid which is the case in Table 2.. Thoenes and Kramers [54) present the equation shown in Table 4, which contains three additive terms. One term is for mass transfer in laminar flow, one for turbulent flow and one for stagnant areas. The packing was arranged in a body-centered cubic configuration. Analysis of results indicates that mass transfer was better in the bed at low Reynolds numbers than the model shows. This could be accOuntable to regular packing. In a regular packed bed there are bottlenecks in which the fluid flows at a much higher rate than the average velocity. Consequently mass transfer is greater in these areas. The effect on overall transfer rate would reasonably be greatest at lower Reynolds numbers. Tables 5 to 8 compare a simplified formula presented by Thoenes and Kramers in the same article which they say has a mean deviation of t 10%. Agreement is reasonably goOd for beds with porosities of -0.4 but model resUlts average about 15% higher than the given formula for a voids fraction of 0.5. No tabular data is listed, but lines on graphs presented fOr packed beds with porosities of 0.48 generally show higher rates of mass transfer than for the lower porosities. 91 The equation of Bradshaw and Bennett [5] shown in Table 9 is in terms of Jd instead of EJd. Also the data from which the equa- tion was derived shows a 25% standard deviation. Kusik and Happel [31] use a free surface model to derive their equation which is compared to the model in Tables 10 and 11. They used boundary layer theory in the derivation. As the Tables indicate, correlation is better at a voids fraction 0.7 than for 0.4. This would seem reasonable for a free surface model which is described as a Sphere surrounded by a spherical enveIOpe of fluid. Williamson, Bazaire and Geankoplis [59] present two equations, one for low and one for high Reynolds numbers. These comparisons are shown in Tables 12 and 13. Agreement is not too good, especially in the Reynolds number region where the two equations coincide. There is considerable scattering of the data and these two equations seemed to be the best fit. Wilson and Geankoplis [60] used the data of the previous article by the senior author and new data to present two new equa- tions which are analyzed in Tables 14 to 21. The first four Tables are for void fractions of 0.4 and the others for 0.7. It can be seen that changing the Schmidt number from 950 to 70,600 affects the results only at low Reynolds numbers. Figures 8 and 9, which follow, show graphically the answers in Tables 14 and 18. The model results follow closely the authors' equations, except in the inter- secting region. Again in order to divide the data into two correlating equations, it was necessary to have larger deviations at intermediate Reynolds numbers. Similar graphs would result by plotting Tables 15 and 19, etc. 92 —--- Model -- Table 14 Figure 8. Comparison of M0001 with Wilson and G0ankoplis [60] Low R0ynolds Numbers 93 100 10 1.0 ---- Model Tables 14 8 18 Reg ‘ 61.42 I-e hf Figure 9. Comparison of Model with Wilson and Geankoplis [60] High Reynolds Numbers 94 Galloway [15] presents graphs in his thesis that are correlations of his data and other authors. The equations presented contain turbulence intensity factors and are difficult to compare with the model. Two of the graphs given are plots of Sh/Scl/S versus Reynolds number; so equations were estimated from them that are comparable to the model. Tables 22 to 25 are for beds of spheres and the results compare reasonably well with the model. Tables 26 to 30 are for commercial packing. Again the results compare favorably. Petrovic and Thodos [40] give an equation for mass transfer to gases. Table 31 shows poor correlation at low Reynolds numbers but the data presented in the article shows considerable scattering especially at low Reynolds numbers. He also uses axial mixing factors of Epstein [11] in his analyses. Wilkins and Thodos [58] use the previous data of the senior author and others and give a new equation for mass transfer to gases which varies considerably from the previous equation. These results are given in Table 33. This equation gives higher mass transfer rates at corresponding Reynolds numbers. Jolls and Hanratty [27] give an equation for mass transfer for an isolated sphere in a bed of inert spheres. Table 32 shows that - mass transfer is slightly better than for the model. This would seem logical since the model is for a randomly packed bed of active spheres. Figures 10, 11, and 12 compare the model results with literature equations for gases and liquids at voids fractions of 0.4 and 0.7. These Figures show that the model equations agree with the various 95 Schmidt Number = 1 (Cases) Voids Fraction = 0.4 ---- Model Table Table Table Table 10 Table 22 Table 31 Table 33 10 100 1000 10,000 Re : ‘uQ 41-2 ar Figure 10. Comparison of Model with Literature Correlations 96 Schmidt Number I 1000 (Liquids Voids Fraction 8 0.4 ---— Model Table 6 - Table 13 - Table 18 - Table 24 - Table 28 - Table 29 - Table 32 - R -6 7—35“Tur‘ Figur0 11. Comparison of Model with Literature Correlations 97 Schmidt Number 8 1000 (Liquids) = 7 Voids -—-- Model 1 Table 20 - Re£.f601 2 Table 25 - Ref.[|51 3 Table 30 - Ref.C'5J Figure 12. Comparison of Model with Literature Correlations 98 authors' correlations better than the correlations do with each other. For this reason the deviation fractions in Tables 2 to 33 are based on results of the model equations. As is indicated in Tables 34 and 35 the average deviation for gases and liquids are +34 and +51, respectively. Root mean square deviation, which is a measure of data scattering, is not applicable. Root mean square deviations were determined to be 13.0% for gases and 14.2% for liquids. Satterfield [48] uses the equation of Petrovic and Thodos (40] and calculate. heat and mass transfer coefficients for a hydrode- sulfurization reactor packed with cylindrical catalyst pellets. Table 36 shows results using the model of this thesis. Units for the answers are: heat transfer coefficient-+8tu/ft2hroF; mass transfer coefficient-~ft/hr; pressure drop per unit length of Dede-pounds force per square inch per foot. Agreement between the computer answers and those of Satterfield is about 10% due to the use of the Petrovic equation. SUMMARY Through the years a very large number of articles have appeared in the literature, representing a huge expenditure of research time and effort in the study of heat, mass and momentum transfer in packed beds. Many of the authors have presented correlation equations for mass transfer coefficients covering varying ranges of fluid flow rates, physical properties and bed characteristics. The method of computing mass transfer coefficients develOped here differs from most of these correlations, since it is based on a physical model and does not employ arbitrary empirical constants to fit a specific set of data. If we compare the values predicted by the literature correlations with those computed by this new model, we find that the root-mean- square deviation for the literature correlations studied is about 13.5%, whereas the average deviation between the physical model results of this thesis and these same correlations is about 4%. In other words the mass transfer results from the model agree better with authors' results than a comparison of authors' results with 'one another. The physical model is derived from basic principles of fluid flow and transport phenomena. The bed is considered to be randomly packed with spheres. The channels between the spheres are treated at low'loymolds mulbers as parallel cylindrical tubes with different 99 100 cross sections. The distribution of cross sections is described by a distribution index, XS. The bed is assumed to be divided into layers of these parallel passages with the length of each passage equal to the diameter of the spheres used. The fluid from all of the tubes in each layer mix before entering the next layer. Flow in the passages is treated as laminar and the pressure drop across each layer is the same through each of the parallel conduits. Mhss transfer coefficients computed using this model are the ones for equimolal counter-diffusion, for low concentrations, or for other cases where J is equal to N. These coefficients are therefore entirely analogous to heat transfer and the latter may be computed by substituting Pr for Sc and Nu for Sh. Also in deriving the model most of the basic transport phenomena equations used-~Leveque, Pohlhausen, Colburn--were originally derived for heat transfer. For simplicity, therefore, the model was derived on the basis of heat transfer and converted to mass transfer by substitution of the apprOpriate dimensionless variables. Starting equations are heat and mechanical energy balances across a passage with constant temperature walls. A correction is added to account fer the higher pressure gradient in the transition length. Nusselt number is calculated (a) from a weighted average of the limiting value fer fully developed laminar flow, (b) from the Leveque equation for developed velocity and developing temperature profiles, to) from the Pohlhausen equation for developing velocity and temperature profiles and (d) from the Colburn equation for heat transfer acress tube banks. These are all combined into a continuous equation which smooths out the transition ranges between the regimes 101 described by the individual equations. Average Nusselt and Reynolds numbers are then determined by integrating over the distribution of the cross sections in the layer. Overall Nusselt and Prandtl numbers of heat transfer are converted to Sherwood and Schmidt numbers of mass transfer. Since most of the literature correlations are in terms of Sherwood number divided by Schmidt number to the one-third power, they are easily compared with the model. Due to the complexity of doing the mathematics of the model equations, they are solved by means of a computer program. The model equations cover a much broader range of Reynolds and Schmidt numbers and bed porosities than do any of the literature correlations. The Colburn equation is used to account for turbulent heat and mass transfer at high Reynolds numbers. At low Reynolds numbers the distribution of cross sections is particularly important since uniform passages would give higher Sherwood numbers than experimental results show. This should be particularly important for gas chromatography where mass transfer occurs at extremely low flow rates in packed beds containing finely divided particles. CONCLUSIONS The results and conclusions of this research are summarized as follows: Overall mass and heat transfer coefficients and pressure loss per unit length of bed can be predicted with reasonable accuracy using the physical model of this thesis. Fluid properties that need to be specified are: viscosity, heat capacity, superficial velocity, thermal conductivity, density, diffusion coefficient of active component through the fluid. Bed characteristics which have to be known are: porosity, particle size, specific surface per unit volume and an index defining the distribution of passage cross- sections within the bed. The model equations cover wider Reynolds and Schmidt number ranges than do any of the literature correlations. Mass transfer results using the model equations show deviations from literature correlations of 3% for gases and 5% for liquids in the Reynolds and Schmidt number ranges reported. Mass transfer values calculated in.Reynolds and Schmidt number ranges not corroborated by experimental investigators are believed to be reasonably accurate because basic principles of fluid dynamics and transport phenomena are used in developing the model. 102 103 The distribution of cross-sections introduced into the model has an effect upon coefficients computed over the entire Reynolds number range. The effect is greatest, however, at extremely low Reynolds numbers where it gives Sherwood and Nusselt numbers which are much lower for the bed than for the limiting values for individual passages. Treatment Of the passages between the spheres as layers of parallel tubes with mixing between layers proved to be satisfactory and convenient. The Pohlhausen and Leveque equations adequately describe transfer in the flow develOping regions and the Colburn equation simulates the turbulence flow results. For simplicity reasons the model was derived on the basis of heat transfer. RECOMMENDATIONS FOR FUTURE WORK After analyzing the results of this thesis the following suggestions are made for future investigations: a. Design carefully controlled experiments to cover a wide range of Schmidt, Reynolds numbers and bed porosities to further verify the results of the model. Investigate Reynolds number regions not previously explored. With more controlled experiments we would be justified in making a more sophisticated model. Using turbulent boundary layer theory or some other theoretical method, investigate the turbulent region in more detail to obtain a better theoretical model. Determine the effect of distributed cross sections on results using cylinders or commercial packing, such as Raschig rings, instead of spheres. Refine the fourth power method of evaluating the transition regions when calculating Nusselt number. Investigate the effect of particle shape on the distribution coefficient, XS, at low Reynolds numbers. Design experiments for gas flow mass transfer in beds of finely divided particles. Assume venturi shaped cross sections or passages with flat walls to see if a better model can be formulated. 104 105 g. A theoretical model could be attempted assuming passages with non-isothermal walls. The partial differential equations involved, however, would be more difficult to solve. APPENDICES 106 APPENDIX A 107 APPENDIX A DERIVATION 0F MODEL EQUATIONS DERIVATION 95 D .3! 45m 890 4 ”,1 Dds Total perimeter from: 2170 855.39.- d8 0 Since: 8 n.3— D5 D S m s d8 -._2. s 05-1 d0 D5 I) 4 sm ”v ' 5.5713119...) . 0“» s ”111 /s l)avflg 1571—" Ds 2 d0 s ”111 /s D 8 av D 5'1 III (s-l) D v = [(5 - l)/S] Dm 108 (1) (3) 109 DERIVATION 95,; V 8 1 + 64/Y VY2 8 Y2 + 64 Y 72 + 64 v + 1024 - w2 + 1024 2 (Y + 32)2 - vv + 1024 v . (w2 + 1024)”2 - 32 MODEL EQUATIONS ASSUMING PARTICLES ARE SPHERES The parallel cylindrical passage model is related to spherical particles using the subscript p to represent such particles. Volume of sphere . i 11' D: l- l SCI-Race area of sphere f p" T 0 Dp 8 6(1 - c)/a (30) Since: a . 4 s/Dav (5) 0p - 1.5 Dav(l - c)/c I (30) Rep .. 831.393 (24) Since: Rem, - Dav 11 Q]: [I Dav 8 4 e/a (S) 414! v R°av . (39) 110 Rep 8 1.5(1 - c)Reav Since: Shav = Dav kc/JV D :- 6.: 3" 1571-01 Shp . Dp kc/e _ .51 5"“ fin. Since: Dp 8 6(1 - c)/a G 6310 5"? vs T 0+5 Re a Y L/D Since: L . Dp . 1.5 Dave—31+) -=--.—-'-°~ (44 Since: Dav - (1 - XS)DIn (23) (38) (25) . (30) (26) (38) (4) 111 Re I 1.5 Y(1 - XS)[(1 -e)lc](Dm/D) Since: D/Dm = (S/sm)XS (1) XS ' Re = 1.5 Y(1 - XS)[(1 - c)/c](Sm/S) (32) The average Nusselt number is calculated from an energy balance over a layer of passages. For one passage at the angle 6 it has been previously shown that: Nu . - [(0 Re Pr)/(4 L)][ln(AT2/AT1)] (10) A similar equation can be written for the average Nusselt number of heat flow perpendicular to the superficial velocity direction. Nuav I . [(DavReavPr)/(4 L cos 0)][ln(AT2/8Tl)av] (40) Since: L = 1.5 Dav [(1 - E)/c] (38) Nuav = - {[ReavPr c]/[6 cos 6(1 - c)]}[1n(AT2/ATl)av] (33) The average Stanton number 15 defined as: Stav I Nuav/(Reavpr)+ Stav I - {8/[6 cos 6(1 - e)]}[ln(AT2/AT1)av] (41) 112 MOMENTUM'EQUATION The pressure loss per unit length in terms of the parameters of the model is determined by the fellowing procedure from the Ergun [12] equation. ZEEELS‘ 0’ ‘3 ——— an ."'(L") .0 138‘ {Leeseu‘fl-B R0, Ergun equation: . -AP 10 0' 6) be" By ' Q 1. cos 0 1541-4) -(;9‘5—1¢‘=L)° ‘ ,, L) (VIZ). - szm/D)‘ (31) 4- M2) . -AP 21.29: I r“ BIY‘BmII' 1.19.5 H z. 2" of en 0 a‘h-e) Since: L I 01) I 6(1 - c)/a (30) BY Iatvv‘). 2"?qu g Q 0. u a to: 0 Since: Dav/DI I (1 - XS) (4) 113 4-‘5 :g m‘). c‘n-mo-xss r H t D” «so a" :0 Q‘ Since: Dav ' 4 5/8 (S) 1 (VP)... (Iv ¢)(c-xs)‘s‘r" EY- ._ 11.0 1 use uq The Ergun Equation in terms of the model is then: O o £19 0' c’ - “"3" ("‘x"”qr—) 43’! . '"7Mt‘ +1.1: (42) QLe-south-é me ”sou Solving for pressure loss per unit length of bed: , , u‘r‘ “-60.4346,”Ill “W W, + (35) APPENDIX B ‘ 114 APPENDIX B DISTRIBUTION INDEX XS was assigned a value of 0.3 by comparing model results with other authors' results from random packed beds. Figure 13 compares the equation of Wilson and Geankoplis with the model for X8 values of 0, 0.25 and 0.50. After studying this graph and other similar plots from other authors it was decided to use XS - 0.3 in all cal- culations. Dm/DP ratios for simple cubic (Figure 14) and rhom- bohedral (Figure 15) arrays or any other regular arrangement of Spherical packing can be approximated by the following method. Dav - (1 - ‘xsmm (4) XS 3 l - Dav/0m Since: Dp - 1.5 Dav(1' e)/e (33) "S’l'fiifin‘a Since in regular packing the passage cross sections would be uniformly distributed (X880): l. D.’% = m ‘4” 115 116 Voids Fraction - .4 0.001 0.01 0.1 1 Reg .3 bug l-G & Figure 13. Comparison of Model with Data of Wilson and Geankoplis [60] 117 fi ‘4 Volume of Cube - Dp no ‘ Solid Volume in Cube - “7;:- Voids Fraction (e) - :45 s 0.41s DI: ,, cheat 9' " ISM-0.415) z °'“°" Figure 14. Simple Cubic Array of Spheres 118 Volume of Pyramid - 'é' (Area of Base) (Altitude) 'I D ‘ a . ‘- °' - flaw-Wm (5%;- 1 - 0.118 Ops | .2: Solid Volume in Pyramid - 4 (a) t". ) - 0.0373 01,3 - . M1) = Vaids Fraction (c) m 0'". 0.260 D_n z 0.2; ~ , 1.50-0.24.) " 0'2.“ Figure 15. Rhomhohedral Array of Spheres APPENDIX C 119 APPENDIX C (VYZ)In VARIATION WITH REYNOLDS NUMBER As is shown in Table 38 the (VYZ)m value to use to produce a desired Reynolds number depends upon the porosity of the bed. Equation 44, which is in the form: In (W2) - Al + A2 (ln REI) + A3 (ln REUZ + -----+ A9(ln mans can be used to predict the correct (VY2)n. Using the data from Table 38 the average constants--Al, A2, A3, °'-, A9--were determined by a least squares technique using the Gauss-Jordan elimination method. TABLE 37 CONSTANTS FOR EQUATION 44 EP I 0.3 EP 8 0.4 EP 3 0.5 EP 3 0.6 EP I 0.7 A1 .4124SE+01 .45844E+01 .500618+01 .SSllGE+01 .58816E+01 A2 .104068001 .10358E+01 .10360Efi01 .123085+01 .1058SE+01 A3 -.8546BE-02 -.61421E-02 .104385-02 -.7829ZE-02 .27823E-01 A4 -.30444E-04 .40949E-02 .726988—02 -.90$07E-02 .111835-01 AS .260675-02 .236346-02 .188415-02 .322178-02 .49379E-03 A6 -.S6269£-04 -.l8728E-03 -.2606SE-03 .891635-04 -.30353E-03 A7 -.62718£-04 -.43577E-04 -.2726SE-O4 -.5966SE-04 .63015E-06 A8 .698415-05 .618365-05 .530918-05 .392528-05 .354458-05 A9 -.22253£-06 -.21780£-06 -.2074l£-06 -.76254E-07 -.188535-06 120 VYSH 0.5005 0.1005 0.2005 0.4005 0.8005 0.1605 0.3205 0.6405 0.1285 0.2565 0.5125 0.1025 0.2045 0.4095 0.8195 0.1635 0.3275 0.6555 0.1315 0.2625 0.5245 0.1045 0.2095 0.4195 0.8385 0.1675 0.3355 0.6715 0.1345 0.2685 0.5365 0.1075 0.2145 0.4295 0.8585 0.1715 0.3435 0.6875 0.1375 0.2745 00 01 01 01 01 02 02 02 03 03 03 04 04 04 04 05 05 05 06 06 O6 07 07 07 07 08 08 08 09 09 09 10 10 10 10 11 11 11 12 12 TABLE 38. (VYZ)In VARIATION WITH REYNOLDS NUMBER 5P=0.3 0.8725-02 0.1735-01 0e34SE‘01 006866-01 0.1365 00 0.2695 00 0.5325 00 0.1045 01 0.2045 01 0.3965 01 0.7565 01 0.1405 02 0.2545 02 0.4415 02 0.7395 02 0.1195 03 0.1875 03 0.2885 03 0.4365 03 0.6535 03 0.9705 03 0.1435 04 0.2105 04 0.3075 04 0.4485 04 0.6505 04 0.9405 04 0.1355 05 0.1945 05 0.2785 05 0.3985 05 0.5695 05 0.8105 05 0.1155 06 0.1645 06 0.2335 06 0.3305 06 0.4695 06 0.6655 06 0.9425 06 121 Ep30e4 0.5615-02 0.1115-01 0.2225-01 0e441E'01 OeBTSE'Ol 0.1735 00 0.3425 00 0.6735 00 0.1315 01 0.2545 01 0.4865 01 0.9055 01 0.1635 02 0.2845 02 0.4755 02 0.7685 02 0.1205 03 0.1855 03 0.2805 03 0.4205 03 0.6245 03 0.9215 03 0.1355 04 0.1975 04 0.2885 04 0.4185 04 0.6045 04 0.8705 04 0.1255 05 0.1795 05 0.2565 05 0.3655 05 0.5215 05 0.7415 05 0.1055 06 0.1495 06 0.2125 06 0.3015 06 0.4275 06 0.6065 06 5.0.6.0.? EP'OeS 0e37‘E'02 0e74‘E'02 0.1485-01 0.2945-01 OeSBBE'OI 0.1155 00 0.2285 00 0.4495 00 0.8775 00 0.1695 01 0.3245 01 0.6035 01 0.1085 02 0.1895 02 0.3175 02 0.5125 02 0.8055 02 0.1235 03 0.1875 03 0.2805 03 0.4165 03 0.6145 03 0.9025 03 0.1315 04 0.1925 04 0.2785 04 0.4025 04 0.5805 04 0.8345 04 0.1195 05 0.1705 05 0.2435 05 0.3475 05 0.4945 05 0.7035 05 0.9985 05 0.1415 06 0.2015 06 0.2855 06 0.4045 06 VOID FRACTIONS (5P) OF 0.3.0.4.0. EP'Oeb 0e249E‘02 0e‘966-02 0.9875-02 0.1965-01 0.3895-01 0.7705-01 0.1525 00 0.2995 00 0.5855 00 0.1135 01 0.2165 01 0.4025 01 0.7265 01 0.1265 02 0.2115 02 0.3415 02 0.5365 02 0.8255 02 0.1245 03 0.1865 03 0.2775 03 0.4095 03 0.6015 03 0.8795 03 0.1285 04 0.1855 04 0.2685 04 0.3875 04 0.5565 04 0.7965 04 0.1135 05 0.1625 05 0.2315 05 0.3295 05 0.4685 05 0.6655 05 0.9455 05 0.1345 06 0.1905 06 0.2695 06 EP'0e7 0.1605-02 0.3195-02 0.6345-02 0.1265-01 0.2505-01 0.4955-01 0.9785-01 0.1925 00 0.3765 0.7285 0.1385 0.2585 0.4665 0.8115 0.1355 0.2195 0.3455 0.5305 0.8025 0.1205 0.1785 0.2635 0.3865 0.5655 0.8235 0.1195 0.1725 0.2485 0.3575 0.5125 0.7325 0.1045 0.1485 0.2115 0.3015 0.4285 0.6075 0.8615 0.1225 0.1735 The values in the 5 columns to the right are Reynolds numbers, Rep/(l - a), calculated from the model using (VYZ). values in the left column. APPENDIX D 122 APPENDIX D SUWARY OF IDDEL EQUATIONS Given Data: Voids Fraction (6) Schmidt number (Pr) cos 0 a 0.707 XS I 0.3 Assume a value for (W2)In depending upon the Rep/(l - e) desired. By graphical integration solve for: a.” - (1 - XS) cosI f ‘4 (-‘-£-)”4(‘3:) d‘ir -:—:: R, (...ng m LR g. Tx‘déi'» The sequence used for the graphical integration is: (AT2/AT1)‘V ' For SIS“ values between 0 and 1, determine: vvz - (wz). (seams) Y I ( VY + 1024 - 32)(l - 5.8/(RT + 175IRT)) Re - 1.5 Y(l - x3)(.'L.!.) ‘53.)” 123 (l3) (14) (31) (21) (20) (32) 124 1/2 1/3 4 4 . 1.6154(v pr)"3 + (.664 (2 Y) Pr ) Nu I ((3.656 .6Pr1/3 4 .25 + (.33 Re ) ) After Reav and (ATZ/ATl)aV have been determined: Rep/(l - c) I 1.5 Reav 1e Fk'lhe £5129) nuav. - fill-0‘98. 5'1 AT. MI 8 e 1.: Na '35 1-0 ' PC" k-"‘°"’ Ea: +3] c .’ 6»! 1 a? r";. - (1"(1- xs)4( v v), - L . Ap/A ‘26 ‘6 a? D? h I Nuav k a/(4 e) (22) (23) (33) (34) (26) (35) (37) APPENDIX E 125 .3 C) (1 rs (5C! (3 (1 OMWCI (1 F5 (5F! r1 (5 (5 APPENDIX E TABLE 39. COMPUTER PROGRAM LISTING FOR TABLE 2 HRITEISoII FORMATIIHI) MRITEISeZI FORMATII4I/121X'CHU + KALIL + HETTEROTH (19531'./21X I'EQUATION J 3 1.77/REEII.44'./21X Z'SCHMIDT NUMBER 8 2.57 (GASESI'o/ZIX 3'VOIDS FRACTION I 0.38'./21X 4'R5YNOLDS NUMBER RANGE I 30 - 5000'0/21X 5'XS I 0.3'/////) HRIT51593I FORMATI9X 1'R5YNOLDS MODEL CHU DEVIATION 2'I9X 3'16UR/AZ) (6K5/ADS) (6KE/ADSI FRACTION' 4el/I FORMATI4FI7.4) COSINE THETA CT‘eTO.’ CONSTANT IN LANGHAAR CORRECTION B’Sea SCHMIDT NUMBER EQUALS VISCOSITY DIVIDED BY DENSITY AND OIFFUSIVITY PR32e57 BED VOIDS FRACTION EPI.38 EPRIII.-5P)/EP DISTRIBUTION INDEX XS'.3 V TIMES Y SQUARED MAXIMUM VYSM82600. DO 12 NIlg22 VYSMIVYSMII.5 S DIVIDED BY S SUBSCRIPT M SR 3 1e0625 START GRAPHICAL INTEGRATION TO FIND AVERAGE REYNOLDS NUMBER AND AVE TEMPERATURE DIFFERENCE RATIO 00 10 I 3 1116 SRISR-.0625 D DIVIDED BY 0 SUBSCRIPT M OR I SRIIXS V TIMES Y SOUARED VYSI VYSM I ORG-4 VARIABLE IN LANGHAAR CORRECTION RT 3 VYS..e25 Y EQUALS DIAMETER TIMES REYNOLDS NUMBER DIVIDED BY LENGTH Y I ((1024.+VYSIII.5 - 32.1'11. - B/IRT + 175./RTI) REYNOLDS NUMBER IN A PASSAGE REIl.SIYIEPR/DRI(l.-XS) 126 IS 10 12 127 TABLE 39 (cont'd,) NUSSELT NUMBER IN A PASSAGE AA=3.656**4+1.615**4*(Y*PR)**1.33333 BB=(.664*(2.*Y)**.S*PR**.33333)**4 CC=(.33*RE**.6*PR**.33333)**4 GNU=(AA+BB+CC)**.25 IF(I-1)15,15,9 LOGARITHM OF MAXIMUM TEMPERATURE DIFFERENCE RATIO, SR - 1 ALXM=-4.*GNU/PR/Y STARTING VALUE FOR INTEGRAL TO FIND AVERAGE REYNOLDS NUMBER SUMRI-RE/Z . STARTING VALUE FOR INTEGRAL To FIND AVERAGE TEMPERATURE RATIO SXOMRI-RE/Z. ; SUM OF REYNOLDS NUMBERS ‘ SUMR-SUMR+RE/UR I TEMPERATURE DIFFERENCE RATIO DIVIDED BY MAXIMUM RATIO XOXMIEXP(-4.*GNU/PR/Y-ALXM) SUM OF TEMPERATURE DIFFERENCE RATIOS DIVIDED BY MAXIMUM RATIO SXOMR=SXOMR+XOXM*RE/DR CORRECTION FOR THE INITIAL VALUE SUMR=SUMR+RE/DR/2. CORRECTION FOR THE INITIAL VALUE SXOMR=SXOMR+RE/DR/2. AVERAGE REYNOLDS NUMBER FOR A GIVEN VYSM REAI(l.-XS)*CT*SUMR/l6. AVERAGE TEMPERATURE DIFFERENCE RATIO DIVIDED BY MAXIMUM RATIO DTAOMISXOMR/SUMR AVERAGE TEMPERATURE DIFFERENCE RATIO FOR A GIVEN VYSM XXI-(ALOG(DTAOM)+ALXM) AVERAGE STANTON NUMBER STAIXX/6./EPR/CT PARTICLE REYNOLDS NUMBER DIVIDED BY (1 - VOIDS FRACTION) - 6UR/AZ REE=1.S*REA AVERAGE NUSSELT NUMBER GNUAISTA*REA*PR 6KE/ADS FROM MODEL EQUATIONS SSTIl.S*GNUA/PR**.33333 DRE/ADS FROM THE EQUATION 0F CHU, KALIL AND NETTEROTH CHU=1.77*EP*REE**.S6 DEVIATION FRACTION BASED ON MODEL 6KE/ADS DEVG=(SST-GRU)/SST WRITE(S,4)REE,SST,CHU,DEVC CONTINUE CALL EXIT END 128 TABLE 40. COMPUTER PROGRAM LISTING FOR.TABLE 36 HRITEI59II FORMATIIHIYIZI/II WRITEISgSI FORMATIZTX'GIVEN FLUID PROPERTIES'e/IIZX 'VISCOSITY IVISI = 0.092 LB/IFToHRI'p/IZX 'HEAT CAPACITY (CF) 3 0.90 BTU/ILBTDEG FI'v/IZX (1 (T O n n on N 2 3 . 4 'SUPERFICIAL VELOCITY (VEL) : 1320 FT/HR'./12X 5 'THERMAL CONDUCTIVITY (AK) 8 0.131 HRITEISob) BTU/(FT.HR.D5G FI'I FORMATIIZXI'DENSITY IRHOI 8 1.05 LB/(CU FTI'a/IZX I 'DIFFUSION COEFFICIENT IOIFI 3 0.0296 SQ FT/HR'o/l/ZSX 2 'CIVEN BED CHARACTERISTICS'QFIIZX 3 'BED POROSITY (EP) = 0.40'0/12X 4 'SPECIFIC SURFACE (ASP) 3 311 SQ FT/ICU FTI'o/IZX 5 'PARTICLE DIAMETER IDPAI 3 0.01285 FT'I HRITEISeTI FORMATI/////3OX'COMPUTER RESULTS.) HRITEISQZI FORMATII/IIX I. ACTUAL CALCULATED' Zc/IIX 3' SCHMIDT REYNOLDS REYNOLDS. Re/IOX ‘ 5'VYSM NUMBER NUMBER NUMBER.) COSINE THETA CT‘oTOT CONSTANT IN LANGHAAR CORRECTION 835e8 DISTRIBUTION INDEX XS=.3 VISCOSITY OF FLUID VIS=.O92 HEAT CAPACITY OF FLUID CP=.9 SUPERFICIAL VELOCITY OF FLUID VEL=I3ZO. THERMOCONDUCTIVITY OF FLUID AK=.13I DENSITY OF FLUID RHO=1.05 DIFFUSIVITY OF ACTIVE COMPONENT 0153.0296 BED VOIDS FRACTION EP=.4 SPECIFIC SURFACE OF PACKING ASP=3II. DIAMETER OF PARTICLE 0 00 0 00 D mm o O 129 TABLE 40 (cont‘d.) DPA=.01285 GRAVITATIONAL CONSTANT GC=4.17E+08 EPR=(l.-EPl/EP SCHMIDT NUMBER EQUALS VISCOSITY DIVIDED BY DENSITY AND DIFFUSIVITY SC=VISIDIFIRHO PRISC ACTUAL PARTICLE REYNOLDS NUMBER REO=DPAIVELIRHOIVIS ACTUAL REYNOLDS NUMBER = OUR/Al REI=REO/(I.-EPI CONSTANTS FROM TABLE 31 Al=.4584425+01 AZ=.1035827E+01 A3=-.6142123E-02 A4=.40949ISE-02 A5=.23b3402E-02 Abs-.187284E-03 A7=-.4357685E-04 A8=.6183554E-05 A9I-.21780075-06 EQUATION TO FIND V TIMES Y SQUARED MAX' FROM ACTUAL REYNOLDS NUMBER A=ALOGTREII AZIAI+AZIA+A3IAII2 AZIAZ+A4IAI53+ASIAII4+A6IAIIS AZIAZ+A7IAII6+A8IAII7+A9IAII8 V TIMES Y SQUARED MAX VYSM=EXPTAZT S DIVIDED BY S SUBSCRIPT M SR 2 1.0625 START GRAPHICAL INTEGRATION TO FIND AVERAGE REYNOLDS NUMBER AND AVE TEMPERATURE DIFFERENCE RATIO DO 10 I 3 ler SRISR-.0625 D DIVIDED BY 0 SUBSCRIPT M OR = SRIIXS V TIMES Y SQUARED VYS= VYSM . DRII4 VARIABLE IN LANGHAAR CORRECTION RT : VYS'.025 Y EQUALS DIAMETER TIMES REYNOLDS NUMBER DIVIDED BY LENGTH Y = ((1024.+VYS)II.5 - 32.1!(1. - B/(RT + 175./RT!) REYNOLDS NUMBER IN A PASSAGE RE=I.SIYIEPRIDRI(l.-XS) NUSSELT NUMBER IN A PASSAGE n on on a On an on 000000 (7 (7f? (7 (700 O H H .- ‘0 130 TABLE 40 (cont'd.) AA=3.656**4+1.615**4*(Y*PR)**1.33333 BB=(.664*(2.*Y)**.S*PR**.33333)**4 CC=(.33*RE**.6*PR**.33333)**4 GNU=(AA+BB+CC)**.25 IF(I-1)Is,15,9 LOGARITHM OF MAXIMUM TEMPERATURE DIFFERENCE RATIO, SR = 1 ALXM=-4.*GNU/PR/Y STARTING VALUE FOR INTEGRAL TO FIND AVERAGE REYNOLDS NUMBER SUMRa-RE/Z. STARTING VALUE FOR INTEGRAL TO FIND AVERAGE TEMPERATURE DIFFERENCE RATIO SXOMRs-RE/Z. SUM OB REYNOLDS NUMBERS SUMR=SUMR+RE/DR TEMPERATURE DIFFERENCE RATIO DIVIDED BY MAXIMUM RATIO XOXM=ExP(-4.*GNU/PR/Y-ALXM) SUM OF TEMPERATURE DIFFERENCE RATIOS DIVIDED BY MAXIMUM RATIO SXOMR=SXOMR+XOXM*RE/DR CORRECTION FOR INITIAL VALUE SXOMR=SXOMR+RE/DR/2. CORRECTION FOR INITIAL VALUE SUMR=SUMR+RE/DR/2. AVERAGE REYNOLDS NUMBER FOR A GIVEN VYSM REA-(1.-XS)*CT*SUMR/16. AVERAGE TEMPERATURE DIFFERENCE RATIO DIVIDED BY MAXIMUM RATIO DTAOM=SXOMR/SUMR AVERAGE TEMPERATURE DIFFERENCE RATIO FOR A GIVEN VYSM XX--(ALOG(DTAOM)+ALXM) AVERAGE STANTON NUMBER STA=XX/6./EPR/CT PARTICLE REYNOLDS NUMBER DIVIDED BY (1. - VOIDS FRACTION) a 6UR/AZ REE=1.S*REA ' AVERAGE NUSSELT NUMBER GNUA-STA*REA*PR 6KE/ADS FROM MODEL EQUATIONS SST=1.S*GNUA/PR**.33333 HEAT TRANSFER COEFFICIENT AH=GNUA*AK*ASP/4./EP MASS TRANSFER COEFFICIENT AKC=ASP*DIF*SC**.33333/6./EP*SST PRESSURE LOSS PER UNIT LENGTH OF BED DPDL-9.*ASP**2*VIS**2*(I.-EP)**2 DPDLaDPDL*(1.-XS)**4*VYSM/128. a}; 131 TABLE 40 (cont'd.) DPDL=DPDLlGC/EP**4/RHO/DPA/144. HRITEIS.3)VYSM,PR.REI.REE FORMATI/4F17.4) HRITEISI4I FORMAT(/////6X W I 1' HEAT MASS TRANSFER COEFFICIENT 2' TRANSFER 3' COEFFICIENT FORMATI/9X3Fl7.4) HRITEI5.8)AH9AKCVDPDL CALL EXIT END 0) F URES SUPPORTED 1F T E NDED PRECISIJN (I A x 0 s R E E I :9 E REQUIREMENTS FOR “OHMDN O VARIABLES 172 PROGRAM EVD OF COMPILATION [I XEQ 'o/BX 1312 DP/DL'9/7X PSI/FT') I I n . APPENDIX F 132 APPENDIX F TABLE 41. SHERWOOD NUMBERS, UNIFORM AND NON-UNIFORM PASSAGES REYNOLDS (4UR/AZ) 0.0002 0.0004 0.0009 0.0018 0.0037 0.0074 0.0147 0.0293 0.0582 0.1154 '0.2279 0.4483 0.8785 1.8971 3.2358 8.0289 10.8788 18.9190 31.8884 51.1938 80.4313 123.8393 187.0805 279.9594 415.8919 813.8238 901.4041 1318.3273 1920.0885 2785.5598 4028.4345 5800.9157 8333.1087 1 1940.4843 1‘I072.5998 SCHMIDT NUMBER 8 1 VOIDS FRACTION 8 .4 SHERWOOD (XS303’ 1.1300 1.1302 1.1310 1.1320 1.1337 1.1364 1.1410 1.1493 1.1646 1.1937 1.2459 1.3294 1.4542 1.6377 1.9065 2.2956 2.8416 3.5732 4.5129 5.6792 7.0988 8.8263 10.9363 13.5222 16.7032 20.6271 25.4737 31.4590 38.8428 47.9403 59.1366 72.9045 89.8261 110.6193 136.1690 133 REYNOLDS I4UR/AZI 0.0007 0.0015 0.0030 0.0060 0.0120 0.0239 0.0476 0.0945 0.1872 0.3698 0.7278 1.4240 2.7603 5.2708 9.8294 17.7197 30.6258 50.6487 80.5665 124.4274 188.4019 281.8330 418.5266 618.4262 909.9348 1333.2542 1945.2162 2826.2189 4090.1040 5898.1543 8478.8974 12156.1121 17388.4383 24825.4019 35386.6635 SHERHDOD (X5801 3.6560 3.6560 3.6560 3.6560 3.6560 3.6561 3.6563 3.6568 3.6580 3.6611 3.6690 3.6890 3.7392 3.8611 4.1339 4.6595 5.5049 6.6785 8.1774 10.0291 12.3023 15.1029 18.5683 22.8646 28.1877 34.7702 42.8924 52.8964 65.2029 80.3305 98.9195 121.7597 149.8247 184.3144 226.7064 {3 .‘Il..- _. TABLE OF NOMENCLATURE 134 ‘4, TABLE OF NOMENCLATURE Primary Quantities §ZEB£1. Dimension Name F Force H Heat L Length M Mass T Temperature t Time Secondary Quantities Symbol Name Dimensions r—- "“‘ H L M T t 8 Packing area per unit volume of -1 bed C Heat capacity of flowing fluid 1 -l -1 D Diameter of a given passage 1 Dav Average diameter of a passage 1 Dn Maximum diameter of any passage 1 Dp Particle diameter ,1 Diffusivity of solute in flowing 2 -l ‘5 fluid G Mass velocity of fluid in a -2 l -1 given passage Gav Average mass velocity of fluid -2 I -1 LL perpendicular to cross-section 135 136 TABLE OF NOMENCLATURE (cont'd.) Symbol Name Dimensions ' F II L M T t gc Gravitational constant -1 l l -2 h Average Fluid film heat transfer I -2 —l -1 coefficient parallel to the bed axis k Thermal conductivity of fluid 1 -1 -l -1 k Average mass transfer coefficient 1 -1 L Length of parallel passages l m Mass flow rate in a given passage 1 -l P Pressure exerted by fluid 1 -2 S Total cross-sectional area of all 2 passages having diameters less than D - Sm Total cross-sectional area of 2 all‘passages T1 Temperature of fluid entering l a passage T2 Temperature of fluid leaving 1 a passage T Temperature of fluid at any 1 p point in a passage Tw Temperature of the passage wall 1 u Average linear velocity of fluid, 1 -1 based on empty cross-section, perpendicular to the cross- section of the bed w Velocity component perpendicular l -1 to the cross-section p Fluid density -3 l u Fluid viscosity -1 1 -l SSZbeol l\,J3 (21.x LIKES I! ‘eav II ep 137 TABLE OF NOMENCLATURE (cont'd.) chsrl‘sns Name Voids fraction (voids volume/total bed volume) Average angle between passages and average flow direction in bed (degrees) Constants in Langhaar [32] correction factor for Y Constant and exponent in: ShPIScl/3 [c/(l - 8)] 3 C1[Rep/(l - 6)]x Exponent which depends upon the distribution of passages l/s Dimensinnlessfima Name Graetz number Colburn mass transfer factor Colburn heat transfer factor Nusselt number in a passage Average Nusselt number in all passages Prandtl number of fluid Reynolds number in a passage Average Reynolds number in all passages Reynolds number based on particle diameter Basic Formula Cu/k 0 Ch: Dav Gav," Dp uQ/u EESZELOI IQFT 138 TABLE OF NOMENCLATURE (cont'd.) Dimensignlgss 919335 Name Variable in Langhaar [32] correction factor Schmidt number Average Sherwood number Sherwood number based on particle diameter Average Stanton number Velocity head Maximum VY2 factor Parameter of Langhaar [32] Basic Formula (vyz).25 .11. u! Dav kc/D DP kc/D h/C Gav - P Q Iiélu’dd VY2(Dm/D)4 D Re/L BIBLIOGRAPHY 139 10. 11. 12. 1&3. 11%. 15. 11L 17h BIBLIOGRAPHY Al-Khudayri, T., Ph.D. dissertation, Michigan State University (1960). Barker, J. J., Ind. Engng. Chem., 57 (4), 43 (1965). Bennett, C. 0. and Myers, J. E., Momentum, Heat, and Mass Transfer, McGraw-Hill Book Co., N. 7. (1962). Bird, R. 8., Stewart, N. E. and Lightfoot, E. N., Transport Phenomena, Riley, N. Y., (1960). Bradshaw, R. D. and Bennett, C. 0., Am. Inst. Chem. Engrs. Jl., Z; 48, (1961). Brotz, W., Fundamentals of Chemical Reaction Engineering, Addison-NesIey, Rea31ng,‘Mhss. (19355. ., Chilton, T. H. and Colburn, A. P., Ind. Engng. Chem., 36, 1183 (1934). Chu, J. C., Kalil, J. and Netteroth, M. 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