.V..._. DRYER " NT I‘COGUR” 7?... I1 .I ......x a. 2 Hi. V...” (...; «u... A»... .......:».V...V .....I. .... ... «:3 .va: ....Zfiiz fVVV: .r.. . ..re ., 1...... 2.2.. {V :r 1.. ... €31.95... In... t . L. Inhv ‘5 l I... . . ...”..m... 3.... LIBRARY Michigan Stan: Unim ‘ISity This is to certify that the thesis entitled SIMULATION AND OPEN-LOOP CONTROL OF A COCURRENT DRYER presented by Wayne Howard Clifford has been accepted towards fulfillment of the requirements for Ph.D. Engineering degree in MM i; major professor Date Feb. 10, 1972 0-7 639 ABSTRACT SIMULATION AND OPEN—LOOP CONTROL OF A COCURRENT DRYER BY Wayne Howard Clifford The dynamic simulation of a cocurrent moving bed dryer for shelled corn involves at least three independent variables: time, distance along the bed, and whatever is used to model the moisture gradient within an individual corn kernel. The first problem is to simulate a thin layer of drying corn—-the mathematical equivalent of simulating a single kernel. In this case the diffusivity of water in corn is available as a function of average moisture content and average temperature of the kernel. Also the Biot number is small enough so that temperature gradients within the kernel may be neglected. The model divides the kernel into three concentric regions with the same dry mass in each region. Geometric parameters in the model were fitted from experimental thin-layer drying data, using a hill-climbing parameter optimization program. The parameter optimization requires that the model be solved many times, so a highly efficient integration Wayne Howard Clifford routine is important in order that the cost of the opti- mization not be prohibitive. A method is presented where a set of a few nonlinear differential equations is solved by linearizing and solving the linearized equations by Laplace transforms. For accuracy the linearization must be done at the center of the interval, but in practice it is done at the front and end and the average of the two is used. Iterations are needed since the values at the end of the interval are not known. Once the geometric parameters have been found, the convective heat and mass transfer coefficients are needed. The steady—state equations correSponding to the thin layer model were derived and solved. This solution made use of the same technique as the thin‘layer solution. Parameter optimization was again used, this time to find the convective heat and mass transfer coefficients. The dynamic corn dryer model consists of 6 non- linear partial differential equations. The backward dif— ference approximation was used for the time partials, and then the equations were solved by the same technique used above. The dynamic solution was used to evaluate the net cost during the transition from one steady—state to another, corresponding to changing from one batch of corn to another at 5% higher moisture. The goal was to find the best input air temperature function during the trans- ition. Several one— and two-parameter functions were Wayne Howard Clifford tested and optimized in terms of their own parameters. Since the best control found was not significantly better than a single—step (or bang—bang) control, the latter would be the best to use under current normal operational conditions. SIMULATION AND OPEN~LOOP CONTROL OF A COCURRENT DRYER Wayne Howard Clifford A THESIS Submitted to Michigan State University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Department Cf Chemical Engineering 1972 ACKNOWLEDGMENTS The author wishes to express his thanks to Dr. George A. Coulman for his guidance and help through— out the course of this work. The author is indebted to Dr. Fred W. Bakker-Arkema for his assistance and interest. Appreciation is also extended to the other members of his committee: Dr. Myron H. Chetrick, Dr. Donald K. Anderson and Dr. William G. Bickert. Thanks are due to several of Dr. Bakker's graduate students for help with various aspects of this work, especially Daniel Elzinga for thin-layer experiments, Ralph Gygax for steady—state data, Dave Farmer for intro- ducing the author to Rosenbrocks hill—climbing program, and Lloyd Lerew for getting programs into the computer. The understanding and patience of the author's family, especially his wife, Mary Kay, is sincerely appreciated. ii TABLE OF CONTENTS Page ACKNOWLEDGMENTS. . . . . . . . . . . . . . ii LIST OF TABLES . . . . . . . . . . . . . . iV LIST OF FIGURES. . . . . . . . . . . . . . v LIST OF SYMBOLS. . . . . . . . . . . . . . vi INTRODUCTION. . . . . . . . . . . . . . . 1 LITERATURE REVIEW . . . . . . . . . . . . . 3 APPROACH TO THE PROBLEM . . . . . . . . . . . 6 NUMERICAL TREATMENT OF THE DIFFUSION EQUATION IN APPROXIMATELY SPHERICAL PARTICLES . . . . . . . 13 A THIN-LAYER MODEL FOR SHELLED CORN . . . . . . . 22 STEADY- STATE SIMULATION AND CONVECTIVE HEAT AND MASS TRANSFER COEFFICIENTS IN THE DEEP BED. . . . . 37 DYNAMIC SIMULATION OF A COCURRENT DRYER FOR SHELLED CORN . . . . . . . . . . . . . 43 (DPEN-LOOP NEAR-OPTIMAL TEMPERATURE CONTROL. . . . . 61 CONCLUSIONS . . . . . . . . . . . . . . . 74 REFERENCES . . . . . . . . . . . . . . . 77 APPENDICES . . . . . . . . . . . . . . . 80 10. ll. 12. 13. LIST OF TABLES Thin-layer data and simulation average moisture contents as a function of time. . . Thin-layer moisture contents as a function of time for low temperature Troeger data . . Thin—layer moisture contents as a function of time for medium temperature Troeger data 0 O O O O O O O O O O O 0 O Thin-layer moisture contents as a function of time for high temperature Troeger data . . Differential equations for a steady—state deep bed corn dryer . . . . . . . . . . . Values of the proportionality constant between convective coefficients for heat and mass transfer . . . . . . . . . . . . . Steady—state dryer data and best fit simulation results . . . . . . . . . . . . Dynamic equations for a cocurrent corn dryer. . Substitutions used in the linearization of the cocurrent dryer dynamic equations. . . . . Linearized cocurrent dryer dynamic equations. . Open-loop temperature control results, Runs 1—22. . . . . . . . . . . . . Open-loop temperature control results, Runs 22—38 . . . . . . . . . . . . Additional single—step temperature control results . . . . . . . . . . . . . iv Page 30 33 34 35 38 41 42 48 57 58 65 68 72 .10. LIST OF FIGURES Page Cocurrent corn dryer diagram . . . . . . . 7 Division of a spherical particle into pyramidal segments . . . . . . . . . . . . . l4 Locating diagram for thin-layer model parameters . . . . . . . . . . . . 20 Flow chart of the method used for single-step integration for initial value problems . . . 25 Thin-layer moisture contents as a function of time for Data Set #3 . . . . . . . . 31 Variation of moisture content with time for selected sets of Troeger data . . . . . . 36 The linearization used for the previous time step . . . . . . . . . . . . . . 50 Input temperature function for the best single-step and overall . . . . . . . . 69 Exit moisture contents in response to the best single—step and the best overall input temperature functions. . . . . . . . . 70 Variation in penalty with time of single—step . 73 AorA LIST OF SYMBOLS 3 area of corn kernel in ftZ/ft , 239.0 at e = 0.5. area enclosing regions 1 or 2 in ft2/ft3 ratio of area to Ar, ft heat capacity of corn, air, Btu/lb of dry matter/°F diffusivity of water inside the corn kernel, ftz/hr diffusivity of water in air, ftz/hr equivalent particle diameter, ft mass flow rate of corn, air, lb of dry matter/ hr/ft absolute humidity of air, lb of water/lb of dry air heat transfer coefficient, Btu/hr/ft2/°F mass transfer coefficient based on moisture content differences, lb of water/hr/ft2 heat of vaporization of water, Btu/lb thermal conductivity, Btu/hr/ft/°F ratio of heat to mass transfer for coef— ficients, 16°F/Etu proportionality constant in Equation 44 dry basis moisture fraction, lb of water/lb of dry corn average moisture content over region 1, 2, 3 moisture content in equilibrium with air relative humidity vi radial distance inside the corn kernel, ft Laplace Transform variable temperature of corn, air, °F time, hours overall mass transfer coefficient, lb of water/hr/ft2 volume, ft3 length along the dryer, ft ratio of area to Ar for region 1, 2 void fraction of the bed dry basis particle density of corn, 72 lb/ft3 density of air, lb of dry air/ft3 viscosity, lb/sec/ft vii INTRODUCTION As mankind moves toward the last quarter of the twentieth century, the message of R. Buckminster Fuller,7 ". . . the physical resources of earth can support all of a multiplying humanity at higher standards of living 3 than anyone has ever experienced or dreamed,‘ presents both an optimistic outlook for the future and the largest challenge ever to our technology: ”So it is also part of the great message to humanity . . . that the world's problems cannot be solved by politics and can only be solved by a physical invention-and-design revolution."7 Mr. Fuller even mentions part of the method of approach. "We find that man is deveIOping an increas- ing confidence in the way in which computers are re- solving heretofore vexing and seemingly unsolvable problems."7 This work represents the author's concept of the next steps to be taken so that computers may be used to bring about one part of that invention-and—design revolu— tion. *Footnote numbers refer to Bibliography entries. A cocurrent corn dryer was chosen for this re— search for several reasons. Corn is a very important raw material for various foods; therefore any method of in— creasing the supply, such as improving methods used in its preservation, has humanitarian as well as economic value. Most optimal control work has involved linear systems, so a nonlinear system was sought. In addition, relatively little control work has been done with distributed systems such as tubular reactors or moving bed dryers. Also, most optimal control uses the minimum time to reach steady state, a minimum amount of control action, or the time integral of the squared error from some desired value as the objective function, and all of these seem rather artificial. On the other hand, a straight economic objec— tive function can easily and accurately be applied to a corn dryer. Finally, the strong interest in corn drying over the years has produced a wealth of basic technology. The author feels that the following are important contributions in this thesis. First, a new thin layer model is presented based on a different way of looking at the corn kernel. Next, this model is used with some steady state data to find heat and mass transfer coeffi- cients for the deep bed dryer. The corresponding dynamic deep bed dryer equations are derived and solved to find a practical optimum open loop control. In addition, a highly efficient method of solving sets of a few differential equations is presented and demonstrated. LITERATURE REVIEW The most significant factor in any simulation of corn drying is the method used to treat the drying of a single kernel of corn. Single kernel drying is also known as thin‘layer drying since in a thin layer, each kernel will be exposed to the same drying air. Many reviews are available for such work, such as Bakker-Arkema and Lerew.l Two approaches are used in single particle models: single— lump models and moisture—gradient models. In single—lump models the results of thin—layer drying tests are summarized in empirical expressions. l3 express the drying rate as a function Troeger and Hukill of equilibrium moisture content (which is a function of air temperature and humidity), temperature, initial moisture content, current moisture content, and air velocity. Thompson et a1.ll use an empirical expression to calculate the time required for a certain amount of drying as an explicit function of all the same above parameters except air velocity. In each case the empiri- cal constants found in the model have very little physi- cal meaning. A moisture gradient model with results like a Single-lump model was used by Chittenden and Hustrulid.5 They used a prefectly spherical model with no surface‘ resistance and a constant moisture diffusivity. Under those assumptions, a closed form solution can be found 'for moisture content versus time, involving an infinite series of exponentials.* Their main conclusion was that the diffusivity is not constant. The work of Chu and Hustrulid6 represents an advancement in that the requirement of a constant dif— fusivity was dropped; however, the perfect sphere and no surface air resistance assumptions were kept. The dif- fusivity was then estimated from short-time drying results. This model is a pure internal moisture gradient type. However, it also uses a "dynamic equilibrium moisture content" and a " seudo initial moisture content." While each of these is a plausible physical phenomenon and each is useful for making the data fit their model, they are both somewhat difficult to determine except in terms of a specific model. The "dynamic equilibrium moisture content" may arise from physical changes in the corn at different temperatures and moisture contents, perhaps related to the hysteresis effects found in re— peated equilibrium moisture sorption isotherms. The "pseudo initial moisture content" is said to arise from *This solution is then used in the same manner as the completely empirical models, but the constants have physical meaning, e.g. the equivalent spherical radius or diffusion coefficient. the fact that the kernel is somewhat cooler than the dry- ing air for the first part of the drying. 15 which does not The work of Whitaker et_al., involve corn directly, uses a variable diffusion coeffi- cient on a spherical body with finite surface resistance. They divided the sphere into ten shells numerically and used a linear function of moisture content for the diffu- sion coefficient. This work was performed to prove the method before attempting to apply it to biological systems. The most important work found on control of a cocurrent dryer for corn is that of Zachariah.l6 He controlled the flow rate of corn in response to exit moisture content using four different control systems, and concluded that a proportional—integrated controller with on-off override would be best. APPROACH TO THE PROBLEM The goal of this work is to find a control scheme for a cocurrent corn dryer. In such a dryer, as is depicted in Figure l, the wet corn and drying air enter at the same end. Although any configuration is possible, the flow generally is downward. An unloading mechanism is provided at the bottom to control the corn flow rate. Plug flow will be assumed for both corn and air, as well as perfect insulation at the sides, so there will be no gradients in planes orthogonal to the direction of flow and the cross-sectional shape will not be important. The independent variables in a mathematical description of the dynamic operation of a deep bed corn dryer will be time and distance along the bed as well as whatever is used to model the moisture gradient inside the corn kernels. It is clear, then, that a thin—layer model must form the basis for any deep bed simulation. Once it is established, the extensions to a steady—state deep bed dryer and from there to the dynamic dryer are mostly straightforward. The thin—layer model used here has three internal zones to determine the moisture gradient. Since each zone adds a differential equation to the steady-state ____> Grain Flow --——9 Air Flow Wet Corn Storage H, Air Heater Drying Air Entrance \\\\N\‘Qd i \ )\ ’A// ’\/\ / \ é ¢ ‘\Z.m/ Air Exits J, /~Z/,Corn Unloading Mechanism Figure l.—-Cocurrent corn dryer diagram. W h simulation (and a partial differential equation to the dynamic simulation), the number of zones should be kept to an absolute minimum. It was decided that the diffusiv— ity of Chu and Hustrulid6 would be used, but that it would be based on the average moisture content rather than the average between each pair of zones. The assumption of zero surface transport resistance was dropped, as was the spherical shape requirement. The resulting model has three shape parameters and the two outside tranSport coefficients, all of which must be determined by fitting experimental data. The thermal conductivity in the kernel is high enough so the Biot number (th/k, the ratio of internal to external resistance to heat transfer) is small. For this reason temperature gradients inside the kernel are neglected. Since most chemical engineering processes are carried out in counter current fashion, a brief explana- tion of the use of a cocurrent dryer is in order. One benefit of cocurrent operation is the tempering effect of the end portion of the dryer, making control easier and the product more uniform. There are two drawbacks in countercurrent operation. The first is the tendency of a countercurrent dryer to heat the exit product. This can damage the starch so it cannot be used for certain appli— cations. It also wastes energy since the corn should be stored cool and so must be cooled in a subsequent opera- tion and since the heat could be used to evaporate water. The other difficulty with countercurrent dryers is the tendency of the exit air to become saturated so that moisture is actually added to entering corn by condensa— tion. The method used here for solving sets of nonlinear ordinary differential equations is analogous to the improved Euler method, but the exact solution to the linearized set is used where a simple Euler step would be made. The set of nonlinear differential equations is linearized over short intervals and the exact solution to the linearized equations is used. The intervals, although short, are an order of magnitude longer than would be used for a corresponding numerical technique such as the pre- dictor corrector. For good results the linearization must be dOne at the center of the interval. In practice it is done at both ends and the average value of each lineariza- tion coefficient is used. This requires that an estimate of the final values for the interval be available, so the method iterates until the values just calculated agree with their estimate. The value of this method is that it is both fast and accurate. The drawback is that it is complicated to program, requiring the "hand" calculation of the solution to the linearized equations. In addition to the thin—layer and dynamic dryer simulations described 10 here, a steady—state program was written and implemented. It ran about 50 times faster than the corresponding pro- gram using the Bulirsch-Stoer (4) method. Control of a cocurrent distributed system is dif- ficult due to the long time lags involved. For a corn dryer the air-side dynamics are very fast—-generally 1000 or so times faster than the product dynamics—~50 that the air is very nearly at steady—state with respect to the instaneous corn temperature and moisture distribution. Consider an attempt to read the exit corn moisture content continuously and use this to control the input air temper— ature. If the exit corn is too wet, the input air temper— ature must be raised. However this causes the corn near the entrance to dry faster, so the air near the exit becomes both cooler and more humid, making the exit corn wetter still. Lowering the input air temperature instead would be worse yet, since corn near the entrance would be dried less. When that corn reached the exitythe dryer would probably be incapable of recovering to properly dry it; certainly the control would be asking for still lower temperatures. For the above reason an Open loop control was used, where the input corn moisture content is used to control the input air temperature. It was assumed that a certain production rate is required, so corn flow is not manipulated. The input corn temperature has little ll effect, since sensible heats are small compared to heats of vaporization. The air flow rate is determined by the fan and motor used and these are difficult to change. The only input variable left is the air temperature, which is easily controlled. The specific control problem is as follows: find the input air temperature as a function of time during the period when a new steady-state is achieved. It is thought that a given batch of corn would be fairly uniform in moisture content so a single input air tempera- ture would achieve steady state drying for an economic optimum. The problem concerns the input air temperature over the time of transition from one batch to another; what is sought is the economic Optimum. The problem is well—posed once the simulation model is available. However, at this time optimal control theory has advanced only to the point where systems of order 10 or maybe 15 can be handled. The model would result in a system of 300 order if the dryer is divided into 50 length segments. In addition, this system is very highly nonlinear, while most of the optimal control work has been with linear systems. For this reason it is Virtually impossible to apply current optimal control techniques; and, therefore, the results should not be termed an optimal control. The term "near—optimal" best describes the practical optimum which is actually found. 12 One possible solution would be to set up the input temperature profile as a parameter vector where each com- ponent is the temperature used in the numerical method at the time step in question. This would give a vector of about 150 elements. The excellent parameter optimiza— tion technique used in the thin-layer section takes about 50 function calls for each component, so 7500 calls would be required. Since the resulting program takes 5 minutes to carry out each approach to steady state when using the CDC 6500 computer, over 26 days straight would be required for this computation. The more practical method used to find a near optimal control was to express the input temperature profile as a function of 2 parameters and find the optimum of those parameters. NUMERICAL TREATMENT OF THE DIFFUSION EQUATION IN APPROXIMATELY SPHERICAL PARTICLES The purpose of this section is to give the thin- layer method a stronger theoretical basis. Consider a particle which starts with a uniform moisture content and is treated in such a way that conditions at its sur— face vary only in time but are identical over the whole surface at any instant. Such a particle may be considered pseudo-spherical if there is a single point within, called the center, where the moisture gradients are zero in each direction (VM=O), and if all net moisture transfer occurs in the radial direction. While corn may not fit these conditions exactly, one may assume that it comes close enough so that the results will apply. The particle is divided into n2 pyramid—shaped segments, each segment having angular widths 2fi/n, as is shown in Figure 2. Then each segment is divided into m zones in such a way that each zone within a segment con— tains the same amount of material. Note that n will tend to be large, while m is usually between 3 and 10. In what follows the first subscript refers to the segment, 13 l4 / The iEE \ Segment \ —"/ Zone 3 + 4 5 4 r1,3 1 1 r. r 1 1,2 i,l Figure 2.—-Division of a spherical particle into pyramidal segments. lil||V||ll ; A 15 the second to the zone, so rin will be the outside radius of the j—th zone in the i—th segment, Min will be the average moisture content, and Ai,j will be the outside surface area of the same zone. As n is made larger the moisture moving between segments becomes negligible com- pared to that moving along a segment. Then each will behave as if it were part of a sphere of radius ri,m' If D, the diffusivity, is independent of r then D 8M1 2 BMi :3?— = 7 (r a?" ‘1’ r HP’ The average moisture content of the j—th zone will be: r. — l i 1’] 47Tr2 i . — r 1 ——7— dr (2) ’3 1,] i,j-l n where V. . = 4“ (r? . - r3 . ), the volume of the j—th ll] 31.12 1!] 113—]- zone in the i—th segment. Of course, ri 0 = O for all i. I Next each side of equation 2 is differentiated with respect to time. lrj o der3 = 1 iIEI (3M ) dr (3) at V. . 2 5t 1’3 r R 1,3—1 But the aMi/at is given by equation 1, so on substitution 17 Consider the case where there is a bulk outside moisture content, Me’ which is the equilibrium moisture content of the product at the temperature and humidity of the bulk air flowing past the product. In addition, there is a convective mass transfer coefficient, hé. The subscript m is used to denote a mass transfer coefficient and the prime is used to differentiate between this co— efficient which is based on moisture content differences and hm, the one more commonly used, which is based on humidity differences. Then the rate of mass transfer per unit area is given by: where Dq:is the inside moisture conductivity and Mi 5 I is the moisture content at the surface. After some algebraic manipulation, Equation 9 yields 3M1 hr; — (——-) = —— (M — M. ) (10) Sr ri,m D0 + h’ Ar. e l’m c m i,m where Ari m is the distance between the surface and the I point where Mi = Mi m' Substituting this into Equation 5 I results in l6 _ ri J dMi,j _ 1 41Tr2 D a 2' 3M1 T‘v Tics” 5T)dr} (4) i,j n r r. . 1,3-1 Carrying out the indicated integration dMi,j 4WD {(r2 aMl) _ (r2 8M1 dt _ 2 8r r. . r r. . } n Vi,j 1,3 1,3-1 (5) Next ri’j is defined as the radial center of mass of I its zone: Then ri’j is the best available estimate of the point I where M. = M. ., 1 1,3 ference form of the partial: and is used to construct a divided dif- 3M. Mi '+l _ P.1 i (——l) =—',3'—— :J,j=l,2...m—1 (7) 8r r. r. . - r . 1,] l,j+l 1,] Noting that A. . = 4nr2 /n2, and substituting into 1,] i,j’ Equation 5 there results dM.. M. . -1\—4. . M. .—H.. 1,] = D {A. i,j+l 1,3 _ A. . 1,1 1,3-1} d Vi,j 1,3 rin+l - ri,j 1,3-1 ri,j - ri,j-1 for j = l, 2 ... m—l (8) 17 Consider the case where there is a bulk outside moisture content, Me, which is the equilibrium moisture content of the product at the temperature and humidity of the bulk air flowing past the product. In addition, there is a convective mass transfer coefficient, hé. The subscript m is used to denote a mass transfer coefficient and the prime is used to differentiate between this co- efficient which is based on moisture content differences and h the one more commonly used, which is based on ml humidity differences. Then the rate of mass transfer per unit area is given by: 3M. Do Do (—-—l . c 8r ri m m e l,S Arim I I (9) where Dq:is the inside moisture conductivity and Mi 5 I is the moisture content at the surface. After some algebraic manipulation, Equation 9 yields 8Mi hr; - (gr—4r = -——— (Me — Mi,m) (10) i,m DpC+ hé Ari m I where Ari m is the distance between the surface and the I point where Mi = Mi m' Substituting this into Equation 5 I results in 18 —1 m l hmDAi m Mi m- Mi m l d”, = { _,_z____ (M — M. )-DA. —J—;—' "} dt Vi,j Dpc+ hm Ari,m e i,m i,m l ri m ri,m-l The quantities of interest will be the m average moisture contents throughout all n2 j—th zones. This is denoted by dropping the first subscript. M. = ____2_____._ (12) n volume, 2 V. . = V/m, then i v dM. n2 mi]. 5 dt =21 (Vi,j ‘ dt) (14) 1—1 For j = 1,2 ... m-l, the result from Equation 8 is 1% = 7 {A31 (Mj+1 — Mj) — Aj_l (Mj - Mj_l)} (15) where n2 Ai . A]. = ;_ f,—-—;—3f.——, j = 1,2, m-l. (16) 1-1 l,j+l 1,] And for j = m, dfim m DhglA _ _ _ t V .{Dp + h Ar (Me _ Mm) _ DAm—l (Mm Mm-l)} c m m (17) where A is the total outside area and DD _ A _ ‘c Ar — ‘2 h'—r (18) n Ai m m h‘ E ———-—-+————— m i=1 DQ2+ hmAri,m The result of the above is that the effects of particle geometry on diffusion are captured in m parameters, Ai, Ag, ... Aé_l, and Arm. Of course, it is not practical to determine these parameters directly. Instead, they are estimated by fitting the model to experimental thin—layer drying data. Another way of looking at this model of the corn kernel is as in Figure 3. Here the kernel is divided into three concentric layers with the same dry mass in each % . X: \\‘ Ar3A Figure 3.—-Locating diagram for thin—layer model parameters. 21 layer, and with iso—moisture content surfaces between the layers. The solid lines in the figure denote these sur- faces. Then within each layer there is another iso— moisture content surface where the moisture content is the mass average for that layer, denoted by dotted lines in the figure. The Ar values will be some kind of average separation between the average moisture content surfaces in the two layers. The same set of geometric parameters will result. A THIN—LAYER MODEL FOR SHELLED CORN Using the techniques of the previous section, the corn kernel is divided into three concentric Spherical layers with the same dry mass in each layer. To aid in visualizing the process and for ease in applying the re- sults to deep bed work, a calculation basis of a cubic foot of corn kernels with a void fraction of 0.5 is used. Heat and mass balances inside the corn yield the following equations: dMl 3Ai dM2 3A2 3AiD = V D (M3 — M2) - V (M2 - M1) (20) dM3 3A hé D 3A’ dt = VTDp + H7 Ar )(Me _ M3) - V D (M3 _ M2) c In 3 (21) dTC hfg A hé D dt=CV(Dp+h7Ar)(M—M3) CV(TC-T) pC c 3 c (22) 22 23 In the above set of equations the value of A/V is taken from Bakker—Arkema et a1.,2 namely 239 ft-l. Chu and Hustrulid6 provide a formula for D as a function of M and T . c 4523.4 } ..3 _' D — 1.629 x 10 EXP {(0.025 TC + 6.008) M - Tc + 459.7 (23) where TC is in °F, and M is the average dry basis moisture fraction. Three other quantities are assumed constant, p = 72 lb of dry matter per cubic foot, Cp = 0.6 Btu per c °F per pound of dry matter, and hfg = 1040 Btu per pound of water. It is understood of course that the heat capacity is a function of moisture content. However, it was decided that the extra accuracy in using the function would not offset the difficulties encountered by the added nonlinearity in the system. For this reason all heat capacities here and in the deep bed sections are ”stream” values, based on average moisture contents and pounds of dry matter in each stream. This value of Cp corresponds to M = 0.2081. C The unknowns are Ai/V, Aé/V, Ar3, hé, and h, the heat transfer coefficient. Although estimates of hé and h are available, the use of such estimates would mean that any error in the estimate would color the determination of the three geometric parameters. _______________:J-IIIII-IIIIIIIIIIlI-l-I"Il 24 The five unknowns were determined by fitting solutions of the differential equations to three sets Of experimental data in a weighted least squares sense. The hill climbing method Of parameter optimization Of Rosenbrock9 was used tO minimize the function E = z t [174' (t) — M (t)] (24) CALC The squared error at each point was multiplied (or weighted) by the time to that point because the moisture content changes fastest early in the drying and because errors in measuring time are relatively less significant at longer times. Since each evaluation Of the error represents 36 hours Of system time (3 runs at 12 hours each) and a 5— parameter Optimization normally requires over 200 trials, it is important that the solution be carried out as efficiently as possible. The equations are "almost" linear, so a Laplace transform may be used over short time intervals when the coefficients (diffusivity actually) are the average Of the endpoints. As may be seen in Figure 4, a front or starting :point diffusivity is calculated from the known tempera- ‘ture and average moisture content at the start Of the time interval. Next the moisture content at the end Of the interval is estimated. This estimate need not be 1. Calculate coefficients Of the linearized equations at the front Of the interval from known initial values. 2. Estimate values Of the dependent variables at the end Of the interval. 3. Calculate the coefficients at the end from the current estimate Of the end values. 4. Use the average Of front and end coefficients tO perform an exact solution Of the linearized equations to the end Of the interval. Laplace transforms are used here. 5. Is the step complete? Need either prOper number Of trials or convergence Of the end value estimates. YES 6. GO on tO the next step. Figure 4. Flow chart of the method used for single- step>integraton for initial value problems. 26 particularly good, in fact, the values at the front may be used. The one used here was M. = M. — 0.2 At (M. 1! l, t+At l, t — Me)' (25) t The end diffusivity is calculated from this estimate and the coefficients are calculated from the average Of the front and end diffusivities. Next, a single step is made. This provides much better values for the end moisture content and temperature, from which a much better end diffusivity is calculated. A new average diffusivity provides new coefficients so a second step may be made over the same interval. This loop is continued until it converges. For these runs the second and third trials always agreed within :rlO_5 moisture fraction. The following substitutions were made to simplify the Laplace transform solution. 3A’D 3A’D _ l _ 2 _ a- V b— V OL—a‘i'b D h’ c — 35 m B = c + b (26) ._fL- =.—h__A___ pc Ccpcv 27 So the equations are H2 (27) “I fl ll m 3 N I m 3 H N% - b M3 - a M2 + a M1 (28) Q) fl. CL 2 w — CMe — 8M3 + bM2 (29) Q.) r... Q19: ('i'I-Zl = dMe - dM - 6T + dTa (30) 3 A bar over a variable will denote its Laplace transform, a O superscript will denote value at the front of the interval, and S will be the transform variable. Then the transformed equations are SMl — M1 = aM2 — aMl (31) _ _ o = _ _ _ _ 8M2 M2 bM3 dMZ + aMl (32) _ CMe _ _ SM3 - M3 = —§— — 8M3 + sz (33) _ dMe + dTa _ _ ST - T° = ————§———— — dM3 - ST (34) 28 Solving these (Cramer's rule works rather well) s [(S+d)(S+B) — b2] M: + s(s+s) aME + ab(SM§ + CM ) M = e l s [(S+a)(S+d)(S+B) — b2 (S+a) - a2 (s+B)] (35) M = as (8+8) M: + s (s+a)(s+B) M3 + b(s+a)(SM§ + CMe) 2 s [(S+A) (S+d) (5+8) - b2 (S+a) - a2 (s+s)] (36) O O 2 O M = abSMl + bS (S+a) M2 + [(S+a) (S+O(.) - a ] (5M3 + CMe) 3 s [(S+a) (S+d) (s+s) — b2 (S+a) — a2 (s+B)] (37) -d {abSM° + bS(S+a) Mo + [(S+a) (S+O() —a2] (SMo + CMe)} T = + [(S+a)(S+d)(S+B)—a2(S+B)-b2(S+a)](ST° + dMe+STa) 2 (s+a) -a2 (s+B)] s(s+6) [(S+a)(S+d)(S+B) -b (38) Writing the Heaviside expansion theorem in this notation, If u (s) = gig} where Q(S) = (S-al)(S—a2) ...... (S-am) and P(S) is a polynomial of degree m—l or less In Then U(t) = Z —d—§-— e i 29 So the only difficulty in the solution was finding the roots of the polynomial (s + a) (s + a) (s + s) - b2 (s + a) — a2 (s + B). It should be clear that these roots are all real and negative, so a special subroutine was written to solve a general cubic with all real roots. The programs used to perform the integrations and the optimization are shown in Appendix A. Experi- mental thin layer drying data taken by D. G. Elzinga were thus fitted to the model. The results are shown in Table l and a representative set of results is plotted in Figure 5. The drying was carried out with air at 98°F and 50% relative humidity. The air flow rate was not determined, but was quite high. The resulting values were: Ai/V = 12.58 x 104 ft—2 Aé/V = 9.46 x 104 ft—2 3 Ar3 = 3.931 x 10‘ ft h = 12.33 Btu/hr/ft2/°F hé = 1.193 lb of water/hr/ftz. There are two problems with the data Of Elzinga. First, the whole set was taken with the same drying air temperature. Second, the air flow rate was not recorded. In order to give the model a broader foundation eleven 30 TABLE l.—-Thin—layer data* and simulation average moisture contents as a function of time. Time, Set 1 Set 2 Set 3 hours EXP SIM EXP SIM EXP SIM 0 .3605 .3605 .3377 .3377 .3813 .3813 0.5 .2863 .2916 .2712 .2805 .2895 .3007 1 .2619 .2582 .2493 .2510 .2649 .2639 2 .2243 .2195 .2143 .2155 .2263 .2226 3 .2003 .1965 .1929 .1938 .2017 .1984 4 .1810 .1806 .1747 .1787 .1817 .1821 5 .1712 .1690 na .1675 .1720 .1701 6 .1607 .1600 .1555 .1589 .1612 .1608 8 .1454 .1470 .1421 .1463 .1464 .1476 12 .1330 .1318 .1312 .1314 .1339 .1321 * The data were taken by Mr. Daniel G. Elzinga Of the Michigan State University Department Of Agricultural Engineering on September 11, 1969. Dry Basis o 6 Moisture Content, 31 40 C) Experimental —— Simulation 32— 28- 24- 20 16 A . 1 i l I l I 0 2 4 6 8 10 12 12 Drying Time, Hrs. Figure 5.—-Thin—1ayer moisture contents as a function of time for data set #3. ————' 32 selected runs from the data of Troeger12 were also used. Three of these were at about 90°F, five at about 125°F, and three more at about 160°F. All were at an air velocity of 160 ft/sec. In checking the Troeger data with his thin layer model, errors of up to 1.6% were found. Also, his raw data could not be used since they were not taken at the same times for each run. Therefore, a correction factor was applied to the model assuming that the error would be a linear function of time between the data points. The first action taken with this data was to fit it in the same manner as the Elzinga data, both grouped by temperature and with all eleven runs together. The results by temperature group varied a great deal from one group to the other, not only in geometric parameters, but also in the convective coefficients. For all eleven together the result was a very poor fit. Finally, the geometric parameters found from the Elzinga data were used and only the convective transfer coffficients were adjusted to fit the set of data at each temperature. This gave a better fit of the data. The results of fitting the Troeger data are shown in Tables 2, 3, and 4, with selected runs plotted along with their raw data in Figure 6. 33 TABLE 2.--Thin—layer moisture contents as a function of time for low temperature Troeger data.* Run #1404310 Run #1404410 Run #1504310 Time, min. Sim Troeger Sim Troeger Sim Troeger O .3458 .3548 4276 .4276 .3481 .3481 10 .3462 .3418 .4128 .4074 .3409 .3350 20 .3393 .3309 .4031 .3939 .3348 .3239 30 .3330 .3217 .3950 .3825 .3292 .3158 40 .3273 .3146 .3876 .3729 .3240 .3091 50 .3219 .3080 .3807 .3645 .3191 .3033 70 .3116 .2961 .3677 .3496 .3099 .2928 90 .3021 .2857 .3555 .3364 .3012 .2848 110 .2931 .2768 .3440 .3245 .2930 .2766 130 .2845 .2691 .3329 .3139 .2853 .2694 150 .2764 .2614 .3224 .3043 .2780 .2629 200 .2578 .2452 .2984 .2831 .2613 .2490 250 .2415 .2314 2772 .2653 .2467 .2375 300 .2272 .2200 .2586 .2503 .2339 .2274 350 .2145 .2104 .2422 .2375 .2228 .2187 400 .2034 .2014 .2278 .2253 .2130 .2114 500 .1850 .1870 .2039 .2065 .1970 .1987 600 .1706 .1757 .1854 .1909 .1846 .1889 700 .1591 .1667 .1709 .1790 .1750 .1811 800 .1500 .1594 .1594 .1701 .1675 .1748 900 .1427 .1535 .1502 .1626 .1615 .1696 *Using h = 2.054, hé = .1002. E x o mmaa. u .a m4 4 u : anamo4 nova. nova. mmva. mova. mvma. mnna. Nona. mmoa. mvma. vmva. oom aoma. mnma. omma. mnma. bmom. mnma. vvma. Nona. omoa. mooa. omm whoa. aana. mmoa. aaha. omam. mmma. Nvma. moma. whoa. hvha. omm moma. anma. amha. anma. mvmm. mvam. vmom. nmma. vmma. mama. ovm huma. omom. ooma. ooom. mmmm. hmmm. mmam. mmam. mmam. omam. oom vmam. momm. mham. momm. vmnm. mmmm. oomm. mamm. aomm. momm. ooa momm. mvvm. momm. ovvm. wmmm. mmom. nmvm. mmvm. aomm. ammm. ova mmvm. aoom. mmvm. aoom. vmmm. mvmm. momm. mvmm. mmom. omom. oma mmmm. mhhm. nmmm. momm. mvam. haom. whom. whom. oamm. onmm. ooa whom. momm. ammm. momm. momm. momm. aamm. mmmm. maom. mnom. om ommm. Nmam. aoom. mmam. onvm. vam. ommm. mmmm. mamm. momm. oo vmom. mnmm. mmom. mnmm. ammm. vamm. amom. onom. mamm. oovm. mm M omam. anmm. omam. Nnmm. Nmom. oaom. omom. nvam. movm. momm. vv mmmm. mwvm. momm. mnvm. omnm. aanm. nmam. ommm. mamm. moom. om mavm. whmm. vmvm. mnmm. vamm. oamm. mvmm. momm. mmom. ammm. mm ammm. mmom. mmmm. mmom. mmmm. ommm. ammm. mmmm. momm. mmmm. om mmmm. ovum. Nmom. ovum. mmmm. vmmm. movm. mmvm. mmmm. oomm. oa Baum. momm. manm. momm. nvov. vvov. movm. mmvm. oamm. vomm. Na momm. momm. momm. momm. aaav. ooav. ammm. mmmm. aoov. amov. m vomm. mmmm. momm. vmmm. nnav. mnav. onmm. anmm. omov. moav. v moov. moov. voov. voov. ovmv. ovmv. Naom. Naom. mmav. mmav. o i Hmmmons Sam Hmmmoae 8am Hmmmone Eam Hmmmoab Sam Hmmmone Eam .QHE _ .mEaB ovvvammw qsm omvvammv ssm oavvammm com oamvamm# ssm oavvommv csm . «.mamo HommOHB mndumnmméwp EdanE MOM wfiau mo coapoc3m m mm mpcmpcoo musumaofi mommalcanell.m mamde 35 TABLE 4.——Thin-1ayer moisture contents as a function of for high temperature Troeger data.* time Run #3204310 Run #3204410 Run #3404320 Time, min. Sim Troeger Sim Troeger Sim Troeger 0 .3630 .3630 .4314 .4314 .3665 .3665 2.33 .3591 .3535 .4244 .4201 .3629 .3600 '4.67 .3541 .3443 .4166 .4092 .3581 .3538 7.0 .3483 .3354 .4084 .3986 .3527 .3478 9.33 .3422 .3272 .4002 .3882 .3468 .3421 11.67 .3359 .3197 .3921 .3782 .3408 .3367 16.33 .3235 .3053 .3764 .3606 .3288 .3266 21.0 .3115 .2917 .3615 .3441 .3172 .3156 25.67 .3002 .2798 .3474 .3286 .3063 .3045 30.33 .2895 .2703 .3341 .3150 .2959 .2941 35.0 .2794 .2614 .3215 .3033 .2862 .2844 46.67 .2565 .2420 .2931 .2773 .2641 .2626 58.33 .2367 .2259 .2684 .2563 .2451 .2439 70 .2195 .2115 .2471 .2386 .2286 .2293 81.67 .2045 .1995 .2285 .2234 .2143 .2169 93.33 .1913 .1890 .2124 .2097 .2018 .2044 116.67 .1695 .1696 .1859 .1867 .1812 .1856 140.0 .1523 .1565 .1652 .1698 .1651 .1699 163.33 .1384 .1448 .1488 .1555 .1522 .1575 186.67 .1269 .1355 .1356 .1439 .1417 .1471 210.0 .1174 .1275 .1246 .1338 .1331 .1382 *Using h = 9.623, hé = 0.4188. 2.. ....“- _a~o-T-_‘:--—— ...... . .a- -..-r 36 .mamo Hmmmoue mo mumm pmaomaom paw mEau Saaz ucmuzoo mHasmaoE mo coaumaam>an.o madman oom mmuscaz .mEaB mcamao com com 004 com com D r _ _ _ G O mcsm coaumazfiam moooa .ommvovm a cam .mumo 36m momma .oaqqomm # cam .mme 36m moam .oavvova # cum .mumo 36m '1uequ03 eansrow sIseg Ala dues 18d STEADY-STATE SIMULATION AND CONVECTIVE HEAT AND MASS TRANSFER COEFFICIENTS IN THE DEEP BED Once a thin-layer model is established the dynamic equations for a deep bed may be derived assuming plug flow of both air and corn and no kernel to kernel heat or mass transfer. This is done in the next section. The steady— state equations are found by setting the time partial derivatives to zero and making the distance partial deriva— tives into total derivatives. This results in the set of equations shown in Table 5. Generally input conditions are known and the problem will be to determine temperatures, moisture contents and the humidity along the bed. For a cocurrent dryer the input conditions may be located at z = 0, making the simulation an initial value problem of six non-linear ordinary differential equations. This set of equations is similar to the thin-layer set, except that air temperature and humidity equations are added. The same technique was used to solve them. Since it is illustrated in both the thin—layer section and the dynamic simulation section, it will not be repeated here. The program to do this is found in SUBROUTINE MBCDS in Appendix B. 37 38 TABLE 5.--Differentia1 equations for a steady-state deep bed corn dryer. d Ml 2'8 Dalpc (M —M ) dz GC 1 2 0M2 _ 3 DdlpC (M _M ) - 3 DdzpC (M _M ) az _ G 1 2 G 2 3 c c U _ D pc hm M 2 V 1n (l-RH) _ D p + h7 Ar ’ e —O.382 (T + 50) C m 3 a dz G 2 3 G 3 c c dT UA h C h A _ _ ____§q _ dz 7 G c (T Tc) G C (M3 Me) pc c pa dlI _ UA _ d? _ G_ (M3 Me) a d Ta _ _ hA (T _ T ) az — G C a c a pa _ —3 — 4523.4 D _ 1.629 x 10 EXP {(0.025Tc + 6.008)M — Tc + 459.7} R = H ' PTOT , M'— M1 + M2 + M3 H (H + 0.622) - P “ 3 sat 39 The only things needed at this point are values for the convective heat and mass transfer coefficients in the deep bed. A great deal of work has been done on heat and mass transfer in packed beds, as may be seen in the review of Barker.3 The work which most closely parallels a corn dryer is by Gamson et a1.8 and Wilke and Hougen,l4 since they involve drying. There are two results from these papers. First, a relationship has been found for the heat transfer coefficient by dimensional analysis: 0 u . D G _ D G h = 1.064 ch (—E—)‘2/3 (JUL) 0'41, _E_ > 350 (39) cu_ DG_ h=1.95CG (—p—) 2/3 (—E-) 0'51 P k u I D G 4;; < 350 (40) Using the following constants at 1200F C = 0.24 Btu/lb°F u = 0.0461 1b/hr ft Dp = 0.0322 ft, from Bakker et_al.2 C U 312—: 0.735 and for G in 1b/hr ft2, these formulas yield 40 h = 0.363 G'59, G > 500 (41) .49 h = 0.690 G , G < 500 (42) This last formula will be of most use, since G will usually be less than 500. Roughly speaking, the top formula corre— sponds to turbulent flow and the second to the transition region. If a continuous function is required, then a G of 615.78 should be used as the break point instead of 500. For G less than 60, corresponding to laminar flow, the heat transfer coefficient should be constant at its value for G = 60. Under the assumption that the log mean partial pressure of air in the boundary layer, the mean molecular weight of the air water mixture and the Schmidt number “D a w are all constant, the mass transfer coefficient should be directly proportional to the heat transfer coefficient, so h' = K - h (43) m Then K may be estimated from the thin—layer results. The h various values of Rh determined from the thin—layer data are shown in Table 6. In the absence of more direct esti— mates Equations 41, 42, and 43, along with a value of Kh from Table 6, could be used to estimate these coefficients for deep bed work. To obtain better values of h and hfi for deep bed work, however, it is advisable to use deep bed data directly. 41 Steady—state deep bed data were available from R. Gygax, so a program was written, using Rosenbrock's9 hill—climbing subroutine, to find the best values of Kh in Equation 43 and KG in Equation 44: h = K - G ' (44) Here the objective function was based on the absolute value of the moisture content error and the temperature error, summed over all five runs, . . _ 4 _ _ Objective — 2 x 10 Z I MEXP — MSIM' and weighted so that a 0.1% error in moisture content counted as much as a 200E error in temperature. TABLE 6.-—Values of the proportionality constant between convective coefficients for heat and mass transfer. Data Source h hi Kh = h$/h Elzinga Data 12.33 1.193 0.0967 Troeger-—Low Temp. 2.054 0.1002 0.0488 Troeger——Med. Temp. 4.430 0.1955 0.0441 Troeger—-High Temp. 9.623 0.4188 0.0435 Troeger——Average 0.0455 The results of this work are shown in Table 7, along with the experimental data. The best values of Kh and KG were found to be 0.0553 and 0.2803, respectively. The theoretical value of KG in Equation 42 is 0.69. Since that 42 TABLE 7.——Steady—state dryer data and best fit simulation results.* Run Number 6 8 11 14 15 GC, Corn flo rate lb/hr/ft dry basis 193 216.5 144 115.4 140.8 Ga’ Air flowzrate 1b/hr/ft dry basis 560 408 357 338 336 Entrance Conditions: TC, Corn Temp CF 42.5 65 42 53 50 M, dry basis moisture fraction .3141 .3141 .3403 .2697 .2697 Ta, Air Temp, OF 350 300 350 250 300 H, Abs. Humidity .0047 .0045 .0043 .0048 .0048 Experimental Exit Conditions (2 ft of bed length) Ta, Air Temp, OF 134 107 112 102 106.5 M, Moisture Content .2213 .2557 .2498 .2136 .2194 Simulation Exit Conditions: Ta, Air Temp, OF 141 113 117 113 122 M, Moisture Content .2301 .2601 .2498 .2120 .2132 * = I = . o For KG .2803 and (h 0553 value refers to fixed beds of spheres, the results here may be considered to be in agreement with the theoretical values. The final optimization program executed in about 85 seconds and used 25 trials. Since each trial needed 5 SOJJitions of the steady—state equations, each solution for 2 feet of bed length took about 0.68 seconds of CDC 6500 running time. DYNAMIC SIMULATION OF A COCURRENT DRYER FOR SHELLED CORN Several assumptions are used in deriving the equa— tions for a cocurrent corn dryer. First are plug flow of both corn and air, and perfect insulation at the dryer walls; the result of these is that there will be no radial gradients inside the bed. Also heat and mass transfer by conduction along the bed (z—axis) are assumed negligible. Each region of the corn is treated as a continuum rather than as individual kernels. To do this the geometric parameters are expressed per cubic foot of dryer. Here 0i is substituted for the Ai/V of the thin—layer section. Since the thin-layer calculations were based on a value of 8 of 0.5 they are 4 -2 col = 12.58 x 10 (2) (l-e) ft (46.) 4 —2 . a2 = 9.46 X 10 (2) (l—s) ft (47) —1 A = 239 (2) (1—8) ft (48) A moisture balance on the innermost (Ml) region from z to z + Az is as follows (FLOW INPUT AT 2) - (FLOW OUTPUT AT Z + AZ) - (OUTPUT BY DIFFUSION) = (ACCUMULATION RATE) 43 44 C) O _ M ) C — - M — §—-M D alpcAz (M1 2 l I Z+Az 1) (49) ——( Note that each term is in units of pounds of water per hour per square foot of bed cross-section. Each term is divided by Az and the limit is taken as Az-+0: G M - M (3 8M _g lim 1 z+Az 1 z _ _ = _g _ 1 (3 ) A240 {" L‘T—‘Lz } D O‘1"c (M1 M2) 3‘1 E)at (50) which gives G 8M 9 (1-e) 3M c 1 _ _ _ _ c __1. In a similar manner, a moisture balance is made on the M2 segment Gc Gc M + D d p Az(M -M ) - —— M - D d p AZ(M -M ) 3" 2]z 1c 1 2 3 2|Z+AZ 2c 2 3 O — d—t (AZT (1 e) M2), (52) which gives 45 GC 8M2 pc(1-s) 3M2 3— 8—2 = D O‘1‘3c (M1’M2) ’ D O‘2"c (M27M3) ' 3 at (53) The overall moisture transfer coefficient at the edge of the kernel, U, is defined as c h _ D p + h Ar (54) Then a moisture balance on the outer segment is G G l C C 2 z+Az _ d 0c , — 3E (AZ?- (1-8) M3); (55) where Me is the equilibrium moisture content of corn at the bulk air conditions. This gives 0 c 8M3 pc(l—€) 3M 3_ 32 = D OL200 (M2_M3) _ UA (Ms—N2) 3 at 3. (56) Under the assumption that the temperature is essentially uniform inside a kernel, a heat balance is made on the corn. Here the units of each term are Btu's per hour per square foot. 46 GCCpCTq/Z+ h A AZ(Ta-Tc) - GCCche/Z+Az- UAhngz(M3-Me) = d—- (C p (l—€)Az T ) (57) dt pc C c g which gives 8T 8T0 CpCGC F = h A (Ta-TC) - U Ahfg (M3—Me) Cpcpc(l—g).§.E_ (58) Note here that the heat capacity of the corn is a dry basis "stream" value of 0.6 Btu/lb/OF. This corresponds to about 21% moisture content dry basis. The only value of the heat balance equation is to estimate the corn temperature needed in the expression for diffusivity of moisture in the kernel, so it was felt that the gain by having a linear equa— tion would offset the loss in accuracy. A moisture balance on the air is _ d GaHI + UA Az(M3"Me) - G HI — dt (paeAzH) z z+Az (59) xvhich gives 8H _ _ _ 29. Ga ——Z— — UAMO (94) dt 0.0936(MO-M). MEMO where MO is the target moisture content. Note that since the air flow rate is constant the cost of blowing air through the bed will not depend on the exit moisture content. The following function was used as a normalized input temperature: _ T - 155.71 Y " 176.02 — 155.71 (95) The first type of control tried was of the ”bang—bang" or single—step type. Here y is zero until the switching time, ts’ is reached, after which y = 1. There are three reasons for choosing this type of control: (1) It is simple to hnplement. (2) Many control situations have such a control as the Optimum. (3) It is easy to evaluate the temperature integral for this control. The temperature integral will represent the total amount of heat energy applied to the system, so it is expected that I will be approximately the same at the T optimum for various control functions. The second type of control function used was an "S-curve" of two parameters: B (B+l) _ B (97) y=_ eat+B Note that this function is zero at t = 0 and approaches 1.0 as t increases. The value of IT for this function is B + 1 ‘ a (98) IT: When the value of IT is held constant the S-curve becomes a single—parameter function. The results of the 5 bang—bang control trials are shown in Table 11, Runs 1-5. These were fitted to a quad— ratic least squares of the same type as in the linearization of the previous time—step on page 49. Here the two smallest values were fitted exactly and the others were weighted by one over the square of their X—distance from the average of the two lowest points. The result was that the best estimate of the minimum was at IT = 0.0361. 65 TABLE llr-Open-loOp temperature control results, Runs 1-22. Run # Parameters IT Penalty* 1 tS = 0.025 .0125 7.522501E-4 2 tS = 0.05 .0375 7.473014E—4 3 tS = 0.075 .0625 7.449360E-4 4 tS = 0.1 . .0875 7.829919E-4 5 t8 = 0.2 .1875 1.230722E-3 6 a = 40 B = 0.8370035 .0361 7.390341E-4 7 a = 30 B = 5.69979 .0361 7.366338E-4 8 a = 28.38209 B = 20 .0361 7.361246E-4 9 a = 27.83887 B = 100 .0361 7.359437E-4 10 a = 27.76997 B = 200 .0361 7.359203E-4 11 a = 27.71468 B = 1000 .0361 7.359016E-4 12 a = 27.70269 B = 7000 .0361 7.358974E-4 13 a = 28.57334 .035 7.365738E-4 14 a = 27.02884 .037 7.353200E-4 15 a = 25 .04 7.332408E-4 16 a = 20 .05 7.277053E-4 17 a = 15 .0667 7.194253E-4 18 a = 10 .1 7.130775E-4 19 a = 5 .2 1.299459E-3 20 a = 9 .101 7.184637E-4 21 a = 11 .0909 7.131513E-4 22 a = 10.23 .09775 7.127858E-4 Runs 1-5 are single-step; Runs 6-12 are S-curve; Runs 13—22 are exponential. *The penalty is in cent—hours per pound of dry corn. . '-.zir'_'7'g';:c:_.—_;v; i. . - .__ 66 Next IT was held constant at 0.0361 and various pairs of a and B were run for the S-curve. This series appears as Runs 6—12 in Table 11. The penalty decreased as larger and larger values of B were used. It is clear that for very large values of B Equation 97 could become unstable, so this search was stOpped at B = 7000. Then Equation 97 was rearranged to y=B {_:§_Ei_l__ 1} = fin _ {at}, (99) e + B e + B For very large B, this reduces to the following: y = 1 - e’at, I = 1/a (100) T so this exponential was tried. Runs 13-22 used this function; the Optimum was estimated with the quadratic fit as above to be at a = 10.23. The final set of functions used started out to be simple time lag, followed by the exponential of Equation 100. If te is the time lag this is y -{0' t i te (101) T e a 67 However, this equation actually went the wrong way, so instead an equation was tried which keeps y above some minimum value, ym, and approaches one exponentially: -at y = ym + (l-ym) (l-e ) (103) _ _ .1 104 IT _ (l ym) a ( ) This function was used in the final optimization. First IT was held constant at 0.09775 as shown in Runs 22-28 in Table 12. Here the Optimum was estimated at a = 6.45. Then a was held constant at 6.45 and IT was varied for Runs 29-34. The Optimum for that was estimated to be at IT = 0.076. Finally, Runs 35 and 36 show that the best value Of a was still near 6.45. The last trial, Run 38, is very near the Optimum for these functions. The input temperature for this Optimum is shown in Figure 8. The exit moisture content _as a function Of time is shown in Figure 9 for this run and for the best single-step. 68 TABLEJJL-—Open-lOOp temperature control results, Runs 22-38. Rgn Parameters IT Penalty* 22 A = 10.23 ym = 0 0.09775 7.127858E-4 23 A = 9.5 ym = 0.071375 0.09775 7.045864E-4 24 A = 8.0 ym = 0.2180 0.09775 7.065060E-4 25 A = 5.0 ym = 0.5125 0.09775 7.065060E-4 26 A = 7.38 ym = 0.278605 0.09775 6.839579E-4 27 A = 5.7 ym = 0.442825 0.09775 6.879560E-4 28 A = 6.45 ym = 0.3695125 0.09775 6.814373E-4 29 A = 6.45 ym = 0.3550 0.1 6.840006E-4 30 A = 6.45 ym = 0.38725 0.095 6.787003E-4 31 A = 6.45 ym = 0.4840 0.08 6.716968E-4 32 A = 6 45 ym = 0.6775 0.05 6.834780E-4 33 A = 6.45 ym = 0.9355 0.01 7.355592E—4 34 A = 6.45 ym = 0.525925 0.0735 6.715480E-4 35 A = 7.0 ym = 0.4855 0.0735 6.724805E-4 36 A = 6 0 ym = 0.5590 0.0735 6.725858E-4 37 A = 4 0 ym = 0.7060 0.0735 7.274961E-4 38 A = 6.45 ym = 0.5098 0.06 6.710516E-4 These control functions are from Equations 100 and 1014 *The penalty is in cent—hours per pound of dry corn. f" ‘ "‘"m‘m “" y Of Equation 95 69 1.0 _____ 1 /// // // / 0.8 a // / //’ Nr\‘Best Overall / / / / 0.6 — / / / / 0.4 v 0.2 A kQ//// Best SingleaStep 0 I I I I I 0 0.1 0.2 0.3 0.4 0.5 0.6 Time, Hrs. Figure 8.—-Input temperature function for the best Single-step and overall. ' _fifi-fia~ 70 18.35 18.3 _ 18.2 a Best / \\Vp//Overall \ 18.1 — EXIt Average Moisture Content, % Dry Basis 18.0 '— ' 17. l 1 95 T I O 1.0 2.0 3.0 3. “I" Time, Hrs. . Figure 9.—-Exit moisture contents in response tO the best SlIKJle-Step and the best overall input temperature functions. 71 The cost penalty shown is in cent—hours per pound Of dry corn. At a flow rate of 15 lb of dry corn per hour the net penalty at the optimum (6.710516 x 10-4 calculated penalty) is 0.010066 cents while for the best single step (calculated penalty 7.449360 x 1074) it is 0.011174 cents. Since this was for 3.75 hours Operation, 56.25 pounds of dry corn were processed or 1.0045 bushels. Then the Optimum here shows a net cost of 0.01002 cents per bushel while the best single step net cost is 0.0111 cents per bushel. In View of this, the best practical control probably is to change the input temperature set point as soon as the new moisture content corn reaches the bed. TO implement this control policy the Operator (either human or automatic) must estimate the time when a new batch Of corn will reach the drying zone. Additional single-step trials were run to test the sensitivity Of the penalty to errors in this estimate. The results of these trials are Shown in Table 13, and plotted along with Runs 1—5 in Figure 10. If a 50% increase in the penalty is 3), there is a 25 minute allowed (to approximately 1.1x10_ band during which the step may be made, from about 14 minutes before to about 11 minutes after the new corn reaches the drying zone. 72 TABLE 13.-—Additional single—step temperature control results. Time Of Step Penalty tS=-0.3 1.226E-3 t3=-0.2 1.044E-3 tS=-0.l 0.885E-3 tS=—O.05 0.819E-3 ts: 0.0 0.769E—3 t = 0.3 3.400E-3 73 Of Dry Corn cent-hours/lb. 1000 x Penalty, -.3 -.2 -.1 0 .1 .2 .3 Time Of Single—Step, Hrs. Figure 10.--Variation in penalty with time of single-step. ww— -..---" 1_ii__ CONCLUSIONS The quality of a corn dryer simulation is limited by its weakest link—-the thin—layer model. Although a great deal Of work has been done, this problem may be con- sidered unsolved in that no model accurately predicts known thin—layer drying behavior. The author feels strongly that a good model must carry the internal moisture gradient, especially so for modeling nonstandard dryers such as cocurrent—countercurrent or intermittent air flow where the external history Of the kernel is vastly differ- ent than in thin—layer experiments. On the other hand, if too many internal segments are used the model is expensive .tO run. The best number is probably in the range of three to five; at three some Of the gradient is probably lost, and at five it would be very difficult to apply the integra- tion method used here tO the dynamic deep bed model. Future thin—layer work along the lines of this model should be pointed toward finding a better estimate of the diffusivity, D. The one used here was determined with a model where the convective mass transfer coefficient, hfi, was assumed to be infinite. From the thin—layer results here it appears that the D is tOO small at high moisture contents and too large at lower moisture contents. 74 75 The values Of the convective heat and mass transfer coef- ficients were higher for the high temperature Troeger data than the low temperature data, so D is probably too small at higher temperatures also. Convective heat and mass transfer coefficients are difficult to measure in the deep bed. The method used here-—finding the set which best fits experimental data—- is easy to apply if there is enough computer time available or the model runs efficiently so that many trials may be made. The result will, of course, depend on the thin-layer model upon which the steady—state model is based. Future work in this area should concentrate on Obtaining more accurate and complete steady-state data, with several replicates or redundant measuring systems for each variable. The control work done here demonstrates one Of the good properties Of the cocurrent dryer--it is relatively stable to changes in inputs. The control results make it clear that little would be gained in the use of a compli— cated Open-lOOp control. The best choice might be to measure the incoming moisture content, look up the needed input air temperature, and reset the air temperature controller to that value. This could be either manual or automatic——even computerized. Future work along this line could make use Of a more sophisticated objective function where sensible heats are accounted for as well as the heat of vaporization. Such work might also involve other Sizes —_—-i .21.. 76 of changes in input moisture content, a decrease instead Of an increase, or multiple changes. Other types Of controls, probably corn flow rate manipulation, could also be simulated with this program. That control has the interesting property that the corn flow rate may always take its maximum value for the input air temperature being used. REFE RENCE S 77 10. REFERENCES Bakker-Arkema, F. W., and L. E. Lerew (1970). Single Particle Cooling and Thin Layer Drying Simulation. Proceedings of the Institute Of Simulation of Cooling and Drying Beds of Agricultural Products. Michigan State University, November 2-4, 1970. Bakker-Arkema, F. W., J. R. Rosenau and W. H. Clifford (1969). Measurement of Grain Surface Area and its Effect on Heat and Mass Transfer Rates. ASAE Paper NO. 69-356. Barker, J. J. Heat Transfer in Packed Beds, Industrial and Engineering Chemistry 57(4),43, April, 1965. Bulirsch, R., and J. Stoer. Numerical Treatment Of Ordinary Differential Equations by Extrapolation Methods. Proceedings Of the 1965 IFIP Congress, Vol. 2, Spartan Books, Washington, D.C. Chittenden, D. H., and A. Hustrulid (1966). Determining Drying Constants for Shelled Corn. Trans. ASAE 9(2), 52-55. Chu, S. T., and A. Hustrulid (1968). Numerical Solution of Diffusion Equations. Trans. ASAE 11(5), 705. Fuller, R. Buckminster. Utopia or Oblivion: The PrOSpects for Humanity. Bantam Books (1969), New York. I Gamson, B. W., G. Thodcs and O. A. Hougen. Heat, Mass and Momentum Transfer in the Flow of Gases Through Granular Solids, Trans. AIChE, Vol. 39 (1943), P. l. Rosenbrock, H. H., and C. Storey. Computational Techniques for Chemical Engineers. Pergamon Press (1966), pp. 64-68. Scott, John T., Jr. "Economics of Corn Conditioning and Storage Alternatives for Farmers." Ag. Exp. Station Bulletin, University of Illinois, January, 1969. 78 ll. 12. l3. 14. 15. 16. 79 Thompson, T. L., R. M. Peart and G. H. Foster (1968). Mathematical Simulation Of Corn Drying-~A New Model. Trans ASAE 11(4), 582. Troeger, J. M. (1967). DevelOpment of a Mathematical Model for Predicting the Drying Rate Of Single Layers Of Shelled Corn. Ph.D. Dissertation, University Microfilms, Number 67-13,006. Troeger, J. M., and Hukill, W. V. (1970). Mathe— matical Description Of the Drying Rate Of Fully Exposed Corn. ASAE Paper NO. 70-324. Wilke, C. R., and O. A. Hougen. Mass Transfer in the Flow Of Gasses through Granular Solids Extended to Low Modified Reynolds Numbers. Trans AIChE, Vol. 41 (1945), P. 441. Whitaker, T., H. J. Barre, and M. Y. Hamdy (1969). Theoretical and Experimental Studies of Diffusion in Spherical Bodies with a Variable Diffusion Coefficient. Trans ASAE 12 (5) 668. Zachariah, G. L. and G. W. Isaacs (1966). Simulating a moisture—control system for a continous—flow drier. Trans. ASAE 9 (3) 297. APPENDICES 80 APPENDIX A THIN LAYER PROGRAM 81 APPENDIX A THIN LAYER PROGRAM This program is used tO find A’, A’ Ar h’, 2’ 3' m and h from thin layer data by parameter Optimization. The calling program, TL4F, is used to initialize the hill climbing search. It calls HCLMB, the subroutine which uses Rosenbrock's9 method. HCLMB calls DEL4Q, the sub- routine tO calculate the total error from the experi— mental data for a given set Of the 5 parameters. The other subroutines are DIFF, which calculates the dif- fusivity Of water in corn from Equation 23, and CUBIC, which finds the roots Of a cubic equation. Some of the variables in DEL4Q and their cor- .respondence in Equation 26 are as follows: AA = a DB = d ALF = d QUE = d ° M + 0 ° T e a BB = b DEL = 0 SEA = C DIFUS = D BET = 8 VOL = V AREA = A RHO = p HFG = h CPP = C fg pc 82 83 In addition, the denominator polymonial 2 2 (s+a)(s+0I)(s-I-B)-6(s+a)-a (8+8) is transtrmed into s3 + 52 - (BZ2) + s - (BZW) + (BZZ) where BZ2 = a + d + B BZW = a (d + B - a) + d - B - b2 BZZ = a (B (d — a) - b2) 84 mNomzaur Nmomxaur aNOQZJU: ONomzauI maomxaur maomxaur Naomzauz OaOQZJUI maomzauz vaomzauz Maomzauz Naomtauz aaOQtJUI anmzaur ooomzaux moomzaur hoomzauz ooongur moomxhur voomZAQI moomzauz Noomzaux aoomxgox .zqeeoxe oz_330 ewo~>oxe we ems: ruezz .ex :emzma eo meopom> xeoxn ex.z.m.o.em .mxoeom> m< omeoem mmumeeqx ex >e ex >3343eo< me< >wxp .xeeooxe cz_33m ome~>oee mm ems: xo_:: .~**ex :eezmx eo meoeow> xeoz: >.e< zo_eez mzo~e<23<>m zoaeozoe eo xmmzoz x:z.x emmwem e>emmmooom zmmzemm zo_e moqezmueme emm¢e e2mozmemaz_ eo emezozn ex memewzqeqe eo zoaeeeeummo mmam HZmOZwmmoza ax mo zoahuzam < mo zazazaz th Dzmu Oh wmoaxaa mzaux wzaknommam *************%*******%#%*%**%%%*** 021 hexw 33.z.m.o.em.e<.me>ez.meemz.mem.zzeue.ex.mzno: 334g \me.oo~.o.oo~u.o.o.m\me>ez. meemz.mew.zzeoe.ex «bee \mvemm.- .m¢m~o~.~ .mummeo~¢o.m.m.emm¢e .e.ooem~1\e eeeo \mmm.m*m.o.o*m\e:x.m3x «pee .m.e ..memox ..m.m3x ..mcem zonmzmzeo .mmcmx ..m~.e< ..m.z ..m.m ..m.e ..m~.> zoemZmzao ovamo aqzemexm evxe zeeooee UUUUUUUUUUUU UUUUUUUUUUQ . _. ..J-fi." 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[ S”‘1 "BI 0 0 0 0 .A-7M171 _szMi + sclMI:z + clMED-fi '31 S+A2 ‘32 0 0 0 M2 52M; + sclngz + C114:D O 782 8”3‘3 'B3C2 O 0 M3 1 52M3 + SCIMEZ + CIMED (9].) 0 0 -B4 s+A4 0 0 H 52 s H° + SC4HPZ + C4HPD 0 0 BS 'Bscz S+A5 “C5 Tc SZT° + SClT:z + clT:D 0 0 0 0 -c6 s+A6 Ta LS2T° + SC4T:Z C4T:D — .4- .4 —( The top four rows Of this equation are independent, so they can be solved by themselves for Mi, Mé, M3' and H. 75+A1 “Bl 0 0 7 FFQ_7 FSZMi + sceri’Z + clM‘ED-1 ’Bl S+A2 -82 0 M2 — 1 S2M§ + SClMgZ + ClMgD O ’32 S+A3 ‘B3C2 M3 82 82M; + SClMgZ + ClMgD 0 0 -B4 S+A4 H ' 52H° + SC4HPZ + C4HPD i _ e 1 e. _ 108 109 Each will be expressed as the ratio of two polynomials in S. theproduct of 82 (S+Al) {(S+A2 + B {- B 1 (S+A )(S+A )( 1 2 ._ E32 2(S+Al ((S+Al)(S+A2) 2 - B2(S+Al The denominator polynomial for each will be the same, and the determinate of the left matrix. )(S+A4) E S+A2 ~13j 0 -B1 0 0 i O 1 I . | = 82 (S+Al) -Ii S+A3 -B3C2 j+ His2 -82 S+A3 -B3C2 0 -B4 S+A4 0 —B4 S+A4 I 2 )(S+A3)(S+A4) - B4B3C2(S+A2) — B2(S+A4)} l(S+A3)(o+A4) + BlB4B3C2} S+A3)(S+A4) - B4B3C2(S+Al)(S+A2) )(S+A ) - B2(S+A )(S+A ) + BZB B C 4 1 3 4 1 4 3 2 - B2}{(S+A )(S+A ) - B B c } l 3 4 4 3 2 110 _ 2 4 3 — S [S + S (Al+A2+A3+A4) + A A -B2 + A A - B B C - B 4) 1 2 1 3 4 4 3 2 } 2 2 +8 {(Al+A2)(A3+A 2 2 2 +5 {(AlAZ-Bl)(A3+A4)+(A3A4-B4B3C2)-BZ(A1+A4)} + {(A A -B2)(A A -B B C ) — 52 A A I] 1 2 1 3 4 4 3 2 2 1 4 Then the denominator polynomial is S (S + S ° BM3 + 82 ° BM2 + S ° BMW + BMZ) = Denominator where BM3 = A + A + A + A 1 2 3 4 BM2 _ A +A — 52 + A +A - B B C - 32 + A A + A A ‘ 1 2 1 3 4 4 3 2 2 1 2 3 4 BMW — (A A -B2) (A +A ) + (A A - B B c ) (A +A ) - B2(A +A ) ’ 1 2 1 3 4 3 4 4 3 2 1 2 2 1 4 BMZ — (A A -B2) (A A — B B C ) -‘B2 A A ‘ 1 2 1 3 4 4 3 2 2 1 4 As an example the numerator polynomial for M1 is as follows: Numerator Of M1 = 82M° + SC MPZ + C MPD —B S+A -B3C S H0 + SC H + C H 0 -B S+A 111 S+A2 -32 0 = (82M: + SClM]:Z + CIMID) -B2 S+A3 —B3C2 0 -B4 S+A4 82M° + SClMPZ + ClMPD "B2 ' + 131 S2M° + SClMPZ + ClMPD S+A3 -B3C2 52H° + SC4HPZ + C4HPD -B4 S+A4 = (s2M°+sclM§Z+clmiD){(S+A2)(S+A3)(S+A4)—B§(S+A4)—B4B3G§S+A2)I + (SZME + SClMgZ + ClMgD)°Bl°{(S+A3)(S+A4) — B4B3C2} + (SZME + SClM§Z + ClMgD)-Bl° B2 (S+A4) + (82H° + SC4HPZ + C4HPD) - Bl . B2B3C2 This will be put in the form of a power series in S. Here the coefficient subscript refers to the dependent variable. 5 o 4 3 . 2 m = S ~Ml + S -TP4(1) + S -TP3(1) + S °TP2(1)+-S-TPW(1)+-1PZ(1) TP4(1) - C MPZ + (A + A + A ) - M° + B - M° — l 1 2 3 4 l l 2 112 _ PD . PZ TP3(1) — ClMI + (A2+A3+A4) ClMl + M° (A A - B B C - B2 + A (A +A )) l 3 4 4 3 2 2 2 3 4 + B (C MPZ + (A +A ) - M° + B - M°) 1 1 2 3 4 2 2 3 TP2(1) = (A +A +A )°C MPD + (A A -B B C -B2+A (A +A ))-C MPZ 2 3 4 l l 3 4 4 3 2 2 2 3 4 1 l - _ _ 2. _ o . PD . PZ +(A2(A3 A4 B4B3C2) 82 A4) Ml-I-Bl (ClM2 + (A3+A4) C1M2 + (A °A -B B c )- M° + B (c MPZ + A M° + B C °H°)) 3 4 4 3 2 2 2 l 3 4 3 3 2 TPW(1) = (A A - B B c - 32 + A (A +A )) . c MPD 3 4 4 3 2 2 2 3 4 1 1 2 PZ + (A2(A3A4 B4B3C2) ‘ B2 A4) C1M1 PD ’ PZ + Bl ((A3+A4) C1M2 + (A3A4 — B4B3C2) ClM2 PD PZ PZ + B2 -(ClM3 + A4 C1M3 + B3 C2C4H )) —— ' _ ._ 2 0 PD TPZ(l) — (A2(A3A4 B4B3C2) B2A4) ClMl PD + Bl ((A3A4 B4B3C2) ClM2 PD . PD + B2 (A4 C1M3 + B312 C4H )) The other three numerator polynomials for M2, M3 and H are found in the same manner. Then the last two equations are solved in terms Of M3 and H. Again Cramer's Rule is used. The solution below is for T5. 113 I— "'I ”r1 7‘ 2 o P Z PD 2 —_ — '1 S+A5 C5 1;) S T + SClTC + ClTC + S (B5C2H B5M3) . _1 “‘2' 2 o PZ PD - + J C6 S+A6 ITa S S Ta SC4Ta + C4Ta I. -J >- —I) >-- --I 2,,o . .Pz , PD . 2 0 P2 ,PD 2 — _ — T = (S+A6)(S 1C + SCllC + Cllc I + CSIS Ta + SC4Ta + C41a } + S BS(C2H M3) C 2 2 S (S + (A5+A6) - S + A5A6 - C5C6) The term involving H and M3 is as follows SS(C H° — M°) + S4(C :P4(4) — TP4(3)) + --~ + (C -TPZ(4) - TPZ(3)) .2 — — - 2 3 2 2 S (C I—M ) - 2 3 4 3 2 S - S - BM3 + S - 8M2 + s - BMW + BMZ Then in order to make this substitution the top and bottom Of the Té equation are multiplied by the denominator above. Then the denominator of Té and Ta is Denominator 2 2 _ _ = S -(S + (A.+A ) . S + A A - C C ) of Tc' Ta 5 6 5 6 5 6 °(S4 + BM3 ° S3 + BMZ ° 82 + BMW ° 8 + BMZ) And the numerator of TC may be found 114 — _ 2 o PZ PD Numerator of Tc — ((S+A6)(S TC + SClTC + Cch ) 2 o PZ PD + c5 (S Ta + SC4Ta + C4Ta )) 4 3 2 - (s + BM3 - s + BMZ - S + BMW - S + BMZ) + B 85(C H° - M°) + s4(c - TP4(4) — TP4(3)) 5 2 3 2 + ... + (C2 - TPZ(4) — TPZ(3)) The numerator is then put in a polynomal form Numerator of TC = S2 ”1‘: +56 - TQ6(l) +55 - TW5(l} + s4 - TQ4(l) + S3 °TW3(l)-+82 °TW2(l)+-S' TQW(l))4—TQZ(1) where j TQ6(l) = TCW + BM3 . T2 TQ5(l) = TCT + TCW ' BM3 + BM2 - T° TQ4(l) = TC3 + TCT - BM3 + TCW ° BMZ + BMW - T2 TQ3(l) = TC3 ' BM3 + TCT ‘ BMZ + TCW ' BMW + BMZ ' T2 TQ2(l) = TC3 - BMZ + TCT - BMW + TCW - BMZ TQW(l) = TC3 - BMW + TCT - BMZ TQZ(l) = TC3 - BMZ 115 and TCW = A ' T° + C . T° + C TPZ 6 C 5 a l c TCT = A6 ' ClTiz + CszD + C5C4T:Z TC3 = A6 - ClTED + c5 . C4T:D The inverse Laplace transformation is as given in Equations 90 and 91. 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