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KNOWLEDGE STRUCTURE

THE BASIC CONCEPTS IN TRANSPORT PHENOMENA

R. BYRON BIRD University of Wisconsin-Madison Madison, WI 53706-1691 ing of the next larger scale. At the microscopic scale, some information about he transport phenomena can be described at the constitutive equations can be obtained from the three scales: the molecular, the microscopic of irreversible processes. This ap­ (continuum), and the macroscopic. At each T proach is particularly important in understanding scale the conservation laws for , , multicomponent and the "cross-effects" in , and play a key role. energy and mass transport. Also, at each scale empiricisms have to be intro­ duced to complete the description of the systems: an For the most part, the notation and sign conven­ intermolecular potential expression at the molecu­ tions here will be those used in references 1, 2, 3, 4, lar scale, the expressions (constitutive equa­ and 5, hereinafter referred to as TrPh, DPLl, DPL2, tions) at the microscopic scale, and the transfer co­ STTP, and MTGL, respectively. efficient correlations at the macroscopic scale. The three scales are intimately connected, with the re­ The Equations of Change sults for each scale contributing to the understand- The basic equations of transport phenomena are the equations of change for the conserved quantities TABLEl as shown in Table 1: The Equations of Change Based on Conservation Laws (A) Conservation of mass for each species (A) !t Pa= -(V · Pav)-(V • ja) + ra a= 1,2,3, ... TrPh Eq. 18.3-4; MTGL 11.1-1 (B) Conservation of momentum (B) !tpv=-[V -pvv]-[V ·1T]+ L,Paga a TrPh Eq. 18.3-2; MTGL 11.1-3; DPLl, 1.1-8 (C) Jt p([r x v]+ i..) = -[ V -pv([r x v]+ i..)]-[v •A] (C) Conservation of angular momentum MTGL, p. 831, Problem 6 -[V · {r X1T Tr]+ ;[r x Paga]+ ;Pata (D) Conservation of energy TrPh Eq. 18.3-6; MTGL ll.1-4;DPL1, 1.1-12 2 2 (D) !t P(½ v + u) = -(v ·pv[½ v + u])-(V . q) These equations can be obtained by writing conser­ -(V · [1T · v])- I,((pav +ju)· g a) vation statements over a (a) a region fixed in space through which the fluid is pa = mass concentration of species a moving (DPLl, Chapter 1) p = of fluid mixture (b) a material element of fluid (i.e., a "dyed" blob of v = mass-average velocity fluid) moving through space. CGJ t = mass flux of a with respect to v r = mass rate of production ofa by chemical reaction total) stress ,;; = ( "Bob" Bird retired in 1992 after forty years of ga = external per unit mass acting on a teaching-one year at Cornell and thirty-nine r = position vector years at Wisconsin. The book Transport Phe­ nomena, which he wrote with colleagues Warren L = internal angular momentum per unit mass Stewart and Ed Lightfoot, was the first textbook A = couple stress tensor on the subject specifically prepared for under­ t a= external torque per unit mass acting on a graduate chemical students. He also coauthored Dynamics of Polymeric Liquids, with 0 = internal energy per unit mass Bob Armstrong (MIT), Ole Hassager (0TH), and q = flux vector Chuck Curtiss (UW).

102 Education KNOWLEDGE STRUCTURE The equations of change have been written in Table describing the interconversion of external and inter­ 1 in terms of the total stress tensor rt which is nal angular momentum. In textbooks, conventionally split into two parts: 7t = p8 + 't it is usually assumed that the stress tensor is sym­ (where 8 is the unit tensor); p is the "thermody­ metric (rt = rtT), so that the external and internal namic "; and 'tis the "(extra) stress tensor" angular momentum are conserved separately, since which vanishes in the absence of velocity gradients. [E:rtT] is then identically equal to zero. The so-called No assumption has been made here that the stress "proofs" that the stress tensor is symmetric (such as tensor be symmetric. Equations (A) through (D) in Problem 3.L in TrPh, pages 114-115) tacitly as­ have to be supplemented with the thermal equa­ sume that there is no interconversion of external tion of state p = p(p,T,co") and the caloric equation and internal angular momentum, and that the ex­ 'of state -0 = U(p,T,cocx), where co" stands for the ternal angular momentum is conserved in the fluid. mass fractions of all but one of the chemical The kinetic theory of dilute monatomic gases yields species a in the mixture. a symmetric stress tensor, as does the kinetic theory By adding the equations in Eq. (A) over all spe­ for dilute solutions of flexible and rodlike . cies, one gets the equation of continuity for the fluid So far there is no experimental evidence that a mixture {TrPh, Eq. 3:1-4]. By forming the cross prod­ nonsymmetric stress tensor is needed. uct of the position vector r with the equation of When all species are subjected to the same exter­ motion, Eq. (B), one obtains Eq. (E); when the latter nal (so that all g" equal g), and when it is is subtracted from Eq. (C) (the equation of conserva­ assumed that the stress tensor is symmetric, Eqs. tion of total angular momentum), the equation for (B) and (D) simplify to Eqs. 3.2-8 and 10.1-9 in internal angular momentum, Eq. (F), is obtainedP 1 TrPh. If all species are subjected to the same exter­ Similarly, by forming the of the fluid nal torques so that all t" are equal to t , a similar velocity v with the equation of motion, Eq. (B), one simplification occurs in Eq. (C). obtains Eq. (G), the equation of change for the ki­ We emphasize that the equations in Table 1 are to netic energy; when the latter is subtracted from Eq. be considered the fundamental equations at the mi­ (D), the equation of change for the internal energy, croscopic scale, whereas those in Table 2 are de­ Eq. (H), is obtained. These various derived equa­ rived from those in Table 1. As explained in TrPh, tions are tabulated in Table 2. the equations of change may be put into many alter­ As pointed out in TrPh (page 314), the term native forms; for example, they may equally well be (rtT:Vv) appears in Eq. (G) with a plus sign and in written in terms of the "substantial" (or "material") Eq. (H) with a minus sign; it describes the derivative operator D/Dt (TrPh Eq. 3.0-2). The en­ interconversion of mechanical and thermal energy. ergy equation has always been a special problem Similarly, the term [E:rtT] appears with a plus sign because it can be written in so many different ways in Eq. (E) and with a minus sign in Eq. (F), thus (see TrPh, pages 322-323, 582, for useful tabular summaries). TABLE2 Equations of Change for Nonconserved Quantities The Flux Expressions (Also Called "Constitutive Equations")

(E) Jt p[ r xv]= -[V · pv[ r xv]] - [ V . {r x 1r T} T] In order to get solutions to the equations of change, we need to have expressions for the j"· 't, and + I,[rx paga J+[e:1rT] q. The standard expressions for these are the "lin­ a ear laws," in which the fluxes are proportional to (F) ftpL =-[V -pvi]-[V•A]- L,Pat a - [e:1rT] gradients, as shown in Table 3. a 2 2 Equation (I) for the mass-flux vector is shown only ·• (G) ftp( ½v ) = - (v -pv( ½v ))-(v ·[1r -v]) for the binary system A-B, and the thermal diffu­ +(nT:vv)- I,(v ·paga) sion, pressure diffusion, and forced diffusion terms a have been omitted (see Eq. (Z) for the complete ex­ (H) ft pU = - (V -pvU) -(V-q)- (1r T :Vv)+ I,(v ·paga) pression). Equation (K) shows the conductive and a diffusive contributions to the heat-flux vector, but the diffusion-thermo (Dufour) effect has been omit­ NOTE: On page 831 ofMTGL, Eq. (E) is given for a ted. In Eq. (J ) we have included the two symmetric stress tensor, but [r x p] should be re­ coefficients µ and K, although the latter is omitted placed by [r x p]T. in most fluid dynamics texts since it is zero for mona- Spring 1993 103 KNOWLEDGE STRUCTURE tomic gases (we know this from kinetic theory-see breadth of the field of transport phenomena and the MTGL, Chapter 7) and since for liquids incompress­ extremely great importance of the equations of ibility is often assumed, so that div v = 0 and the change. All these topics are active research fields term containing K is zero anyway. in which chemical are obligated to play The flux expressions do not have the exalted sta­ an important role. tus accorded to the conservation laws in Table 1. The Macroscopic Balances They are empirical statements, proposed as the sim­ plest possible linear forms; they also emerge from The statements of the laws of conservation of mass, the when one works to the momentum, angular momentum, and energy can be lowest orders in the gradients of concentration, ve­ written down for a typical macroscopic engineering locity, and (see MTGL, Chapter 7). It is system, with one entry port ("1") and one exit port well known that Eq. (J ) does not describe the me­ ("2"); heat can be added to the system at the rate Q, chanical responses of polymeric liquids (see DPLl, and the system can do work on the surroundings at Chapter 2); various nonlinear expressions, and in­ a rate Wmby means of moving parts (such as pistons deed time-dependent expressions, arise from the ki­ or rotatory devices). These conservation statements netic theory of polymeric liquids (see DPL2, Chap­ are given in Eqs. (L-O) in Table 4. It is assumed ters 13-16, 19-20). Furthermore, for some complex there that the fluid velocities at the inlet and outlet materials it is found that the thermal conductivity planes are parallel to the directions of flow n 1 and and diffusivity are rather than scalars, so n 2 • It is also assumed that the extra stress tensor that the fluxes and forces are not collinear. In order does not contribute to the work done on the system to use Eqs. (l,J,K), one needs numerical values for at the entry and exit planes. It is further assumed the diffusivity, viscosity, and thermal conductivity; that there are no mass-transfer surfaces in the mac­ these are preferably obtained from experiments, but roscopic system; such surfaces are considered in in the absence of experimental values kinetic theory TrPh , Chapter 22, and in STTP, Chapter 1. results can be used. Of course, Eqs. (L-O) can also be obtained by inte­ Once the flux expressions have been substituted grating the equations of change in Eqs. (A,B,E,D) into the equations of change, we then have a set of over the entire volume of the flow system; in doing equations which, when solved, will give the concen­ this we must take into account the fact that the tration, velocity, and temperature distributions as shape of the volume is changing with time because 24 251 functions of time. There are many ways in which of the moving parts.c • The macroscopic mechani­ these important equations can be used: cal energy balance (also called the engineering Ber­ noulli equation) cannot be written down directly since • Analytical solutions can be found (for simple, ideal­ there is no for mechanical energy. ized problems, in which transport properties are assumed to be constant)la- 101 It can be derived by integrating Eq. (G) over the • Approximate solutions can be found with perturba- macroscopic system as outlined in Table 5. For the tion theories1111 sake of simplicity, we take the external forces ga to 112 151 be all the same (g = - , where is the potential • Numerical solutions can be found • • Boundary-layer solutions can be found1161 • Time smoothing can yield the turbulent transport TABLE3 111 191 equations · The Flux Equations (or "Constitutive Equations") • Volume smoothing leads to the equations for po­ rous media1201 (I) j A = -p'DAsVmA (binarysystemofAandB) • Flows with chemical reactions can be analyzed1211 (J ) T=-µ(Vv +(Vv)T)+(iµ - K)(V-v )6 • Approximate solutions can be used for lubrication (K) q =-kv'T + Z:(Ha !Ma )lx flowsllll (l 1221 • Mixing and chaos can be studied 'l)AB = binary diffusivity • Particulate motion, suspensions, and emulsions can O)A p / P = mass fraction of a be described1121 µ viscosity • Interfacial transport equations can be establishedI231 K dilatational viscosity • fluid dynamics and transport phenomena 6 = unit tensor (with components cS .) k = thermal conductivity •i can be studied10PLIJ partial molar enthalpy of a This partial list of topics gives some idea as to the 104 Chemical Engineering Education ------KNOWLEDGE STRUCTURE energy per unit mass, TABLE4 which is considered to be Macroscopic Balances independent of time). In Assumptions: ------doing the integration, we no mass-transfer surfaces; need to use the Gauss di­ all species subj ect to same external forces and external torques; vergence theorem (TrPh, T contributions neglected at "l " and "2" A.5-1) and the 3-dimen­ sional Leibniz formula (TrPh, A.5-5). This leads to Eq. (R), in

which 8 1 and 8 2 are the cross-sectional areas at "1" and "2", Sr stands for the fixed surfaces of the system, and Sm stands for the moving surfaces, by means of which work can be done on the surround­ ings. Since the velocity v of the fluid equals the sur­ face velocity V s on the fixed and moving sur­ (Q) %tUtot=U1w1 - U2w2 + Q + Ec + Ev faces, these surface inte­ grals contribute nothing

, to the first term on the mtot = total mass in flow system w1 w2 =mass rate of flow at entry P tot = total momentum in flow system and exit right side. Also, since the

Mtot =total angular momentum in flow pl' p2 =thermodynamic pressure at fluid velocity v is zero on system entry and exit all fixed surfaces, the SI' S = cross-sectional areas of entry l\,,t = total kinetic energy in flow system 2 fixed-surface contribution tot = total potential energy in flow system and exit conduits to the second term on the Utot =total internal energy in flow system Q =heat added to system right side is zero; the in­ ( ) = averages over tube cross section at through container walls Wm= work done on surroundings tegral over the moving entry and exit surfaces gives the work nl'n = unit vector in flow direction at entry Ee, Ev= quantities defined in Eq. (S) 2 transmitted via these sur­ and exit r l'r2'rc =location of the centers of the entry and exit planes and faces, Wm, (sometimes w a. l'w o2. = mass rate of flow of a at entry and exit the center of mass of the called the "shaft work"). fluid in the system The integrals of the extra

TABLES Intermediate Steps in Deriving the Macroscopic Mechanical Energy Balance

2 2 (R) Xt f (½pv + p}dV =-f(n·(½pv +p}( v - vs )~S- f (n ·[(p6 +T )·v])dS-Ec -Ev V(t) S=S,+S,+S,+Sm(t) S=S,+S,+S,+S m( t)

V(t) = volume of engineering flow system cl> = potential energy per unit mass Sr = fixed surfaces of flow system n = outwardly directed unit normal on surface S Sm = moving surfaces of flow system ,. = (extra) stress tensor

v. = velocity of surface (equals zero on S 1,S2,Sr)

Spring 1993 105 KNOWLEDGE STRUCTURE

stress tensor 't over S1 and S2 are presumed coefficient correlations small and have been omitted here; they are w a can be estimated by using mass-transfer coefficient identically zero for laminar, Newtonian flow correlations when the fluid velocity vectors are parallel to These quantities are given in the form of dimensionless the walls of the entry and exit tubes. The inte­ correlations based on large amounts of experimental data; grals labeled Ec and Ev are not evaluated; the they contain the transport properties and the density and latter gives the rate at which mechanical en­ the heat capacity, as well as quantities describing the char­ ergy is degraded into thermal energy. From acteristic length, velocity, temperature, etc. Eqs. (R) and (S) we get Eq. (T), which is easily rearranged to give the mechanical energy bal­ For steady-state systems, the macroscopic balances form a ance in Eq. (P); the latter includes the two set of algebraic relations; for unsteady-systems they become special cases given in TrPh Eqs. 15.2-1 and 2. a set of differential equations, with time as the independent Equation (P) is particularly convenient for in­ variable. The macroscopic balances are the starting point for compressible fluids for which Ec is exactly zero. calculations involving heat exchangers, separations equip­ Equations (L)-(P) are easily generalized to sys­ ment, chemical reactors, and fluids-handling systems. tems with multiple inlet and outlet ports. The Three Levels of Transport Phenomena NOTE: In some textbooks it is stated that the mechanical energy balance (Eq. P) is an For many engineering applications, one starts with the "alternative form" of the total energy balance macroscopic balances in order to understand the overall (Eq. 0 ). Such a comment seems inappropriate behavior of the system. One can often estimate some of since Eq. (P) comes from the equation of con­ the quantities in the balances by using transfer coefficient servation of momentum, whereas Eq. (0 ) has correlations, photographic or other visualization methods, its origins in the equation of conservation of direct pressure, temperature, and density measurements energy. In other textbooks some thermody­ on the system, etc. Other quantities may be assigned by namic "incantations" are offered to get from crude methods. Eq. (0 ) to Eq. (P). The arguments must essen­ In other problems, one needs to know more about the de­ tially involve Eq. (Q), obtained by subtracting tails of the pressure, velocity, temperature, and concentra­ Eq. (P) from Eq. (0); of course, Eq. (Q ) can also tion distributions within the system. This calls for "moving be obtained from integrating Eq. (H)-which down" one level (see Table 6) and solving the equations of is a consequence of the equations of energy change. Many analytical solutions are available, but there and motion-over the macroscopic flow sys­ are also modern computing techniques if numerical solu­ tem. Certainly Eq. (Q ) cannot be written down tions are needed (usually the case if pressure, temperature, directly, since there is no conservation law for the internal energy in an open system with TAB LE6 dissipative processes. Furthermore, the ther­ The Three "Levels" of Transport Phenomena modynamic arguments cannot yield the expres­ sions in Eq. (S), showing how Ec and Ev are Basic Empirical Equations Expressions Results related to the velocities and stresses in the system. Comments from textbook authors (and Macroscopic Dimensionless Solve to get others) on this point would be welcome; before balances over correlations relations among + -+ commenting, however, it would be advisable engineering f, h, kx. , inlet, outlet, and 6 90 931 to read Whitaker's historical essay.c ,PP · system and e. transfer quantities t dimensional analvsis The Transfer Coefficients t J Although the macroscopic balances can be Equations of Flux u Solve to get change for expressions concentration, used, as shown in Table 4, it is often useful to + -+ conserved for pressure, velocity, estimate some of the terms in them by using quantities ja, T , q and temperature dimensionless correlations: t tf I F can be estimated by using friction factor Equation for Intermolecul ar Solve to get correlations ti me evolution force V A , JC, + -+ 8 µ, and Ev can be estimated by using friction loss of phase-space expression kT in the fl ux factor correlations d.istribution fu nction expressions Q can be estimated by using heat-transfer 106 Chemical Engineering Education ------KNOWLEDGE STRUCTURE and concentration dependence of the physical prop­ servation laws as applied to molecular collisions. As erties have to be taken into account). Dimensional a by-product of this derivation, formal expressions analysis of the equations of change suggests the are obtained for the fluxes in terms of the distribu­ form that the transport-coefficient correlations tion function. In this way expressions are obtained should take, these being needed for the macroscopic for the transport properties in terms of molecular balances. models. It should be recognized that there is still one scale Recently there has been an interesting develop­ smaller than the macroscopic and microscopic scales, ment in connection with the kinetic theory of dilute namely the molecular scale. Although this part of gases and the Boltzmann equation. This famous the subject normally lies in the domain of the theo­ equation, although over one hundred years old, has retical physicist or the theoretical chemist, engineers been found to be in error in that it cannot be ob­ occasionally need some familiarity with the molecu­ tained by starting with the quantum Boltzmann lar aspects of transport phenomena. The basic equa­ equation and letting Planck's constant vanish.l261 The tion at the molecular level is an equation for the new "Boltzmann-Curtiss equation" does not suffer time evolution of a phase-space distribution func­ from this defect since it accounts properly for the tion. One example of this is the Boltzmann equation contributions associated with bound pairs of mol­ for dilute gases (MTGL, Chapter 7), and additional ecules; the added terms in the equation are appar­ examples may be found for dilute polymer solutions ently important at low ; as a result the and polymer melts in DPL2, Chapters 17-19. table in TrPh, page 746, will have to be modified. From the differential equation for the phase-space It is seen in Table 5 that at each of the three distribution function, one can obtain a "general equa­ scales, use is made of the basic conservation laws. tion of change," special cases of which are the usual Also, at each scale some kind of empiricism is intro­ equations of change in Table 1; in developing these duced. Each scale can be better understood by going equations, one makes use of the fundamental con- to the next smaller scale in order better to appreci- ate the origins of the equations TABLE7 and their limitations. Thermodynamics of Irreversible Processes (Binary Systems) Thermodynamics of Irrevers­ (U ) dU = TdS-pd(l/ p)+ µdwA ible Processes If into Eq. (H), the equation (V) %t pS = -(V-pvs) -(V -s)+ cr of change for the internal en­ in which s= J (q - µjA) ergy, we insert the thermody­ 1 namic relation Eq. (U) (see cr = - (( q - µjA )· T2 VT }-(jA · J (Vµ+ (gB -gA)) )- +rAµ-(,-:+ Vv) Table 7) for a binary mixture, we get (after using the equa­ (W) j A = - an t (Vµ. + (gs - g A ))- a 12-½ VT tion of continuity) the result T in Eq. (V)-an equation of (X) q-µ.jA = - a21 t (Vµ. +(gs -gA)) - a22-½ VT change for the entropy. In this T equation we can identify an (Y) q = ( µ. + a12 ) jA -[a22 - ai2 J....1_ VT = ( HA - Rs ) j A + q (x) - kVT entropy flux s as the sum of an an T2 M A Ms two contributions, one associ­ (Z) j A =-p 'DAB(vwA + kTV ln T+kpVln p)+ kF (gs-gA) ated with heat conduction and one with diffusion; we can also s entropy per unit mass identify a rate of entropy pro­ µ. = (GA /MA ) - (Gs /Ms) duction a, which is given as a s = entropy flux sum of terms, each of which is (j rate of entropy production the product of a flux and a phenomenological coefficients force. Dufour effect contribution to heat flux thermal diffusion coefficient Then, according to the ther­ pressure diffusion coefficient modynamics of irreversible forced diffusion coefficient processes, every flux will de­ pend linearly on each of the Spring 1993 107 KNOWLEDGE STRUCTURE forces, with the restriction that fluxes must depend mass, momentum, and energy applied to a large on forces of the same tensorial order, or with order engineering system through which a fluid is flowing differing by 2 (Curie's law). There is also the restric­ lead to the macroscopic balances; the two additional tion that the of coefficients in the flux-force balances for angular momentum and mechanical en­ relations be symmetric (Onsager-Casimir reciprocal ergy can be obtained from the integration of mo­ relations). This leads us to Eqs. (W) and (X ), in ments of the equation of motion. The utility of the which a 12 = a 21 • Then combination of Eqs. (W) and balances is enhanced by the use of empirical corre­ (X ) gives Eq. (Y) for the heat flux vector. In this lations for the transfer coefficients. The five macro­ equation, the coefficient of -VT can be identified as scopic balances are the starting point for many analy­ the thermal conductivity for the mixture. The other ses of unit operations and chemical reactors. They term in Eq. (Y) leads to the second term on the right are invaluable for making order-of-magnitude esti­ side of Eq. (K), the diffusion term, plus one addi­ mates for engineering systems. tional very small term associated with the Dufour The conservation laws, when applied to a small effect. region of space through which a fluid is flowing, The term involving Vµ in Eq. (W) can be expanded lead to the equations of continuity, motion, and en­ by using the chain rule of partial differentiation ergy; the assumption of the symmetry of the stress tensor is usually made, and this assumption makes Vµ =(oµ/ dWA )VwA +(oµ/ aT)VT+(oµ/ op )Vp it unnecessary to deal with the interconversion of The term in VT combines with the other VT term in external and internal angular momentum. The flux Eq. (W), and the final result is Eq. (Z); in this equa­ expressions usually used in the equations of change tion the coefficients kP and kF are completely deter­ are the simplest possible relations that are linear in mined from the thermodynamic properties of the the gradients. The vast literature dealing with solu­ mixture, whereas the diffusivity 'DAB and kT are two tions of the equations of change should be familiar phenomenological coefficients that have to be deter­ to engineers, even though these solutions are for mined experimentally for each gas pair or estimated idealized systems; they are, however, very useful for by kinetic theory. As a result of the Onsager rela­ making order-of-magnitude estimates and for check­ tions, the four phenomenological coefficients in Eqs. ing the computer programs used for obtaining nu­ (W) and (X) have been reduced to the three trans­ merical solutions. port properties: diffusivity, thermal diffusion ratio, and thermal conductivity. The conservation laws applied at the molecular scale are used in kinetic theory developments. Ki­ Equation (Z) shows clearly that a mass flux of netic theory provides expressions for the transport species "A" can result from a concentration gradient properties in terms of intermolecular forces; these (ordinary diffusion), a temperature gradient (ther­ expressions are highly developed for dilute mona­ mal diffusion), a pressure gradient (pressure diffu­ tomic gases. In the last several decades the kinetic sion), and a difference of external forces (forced dif­ theory of polymers has developed rapidly, so that fusion) (TrPh, Chapter 18 and MTGL, Chapter 11). much more is now known about the transport prop­ A concise introduction to the thermodynamics of ir­ erties of polymeric liquids.caoi reversible processes has been given by Landau and Lifshitz;1271 a more thorough discussion can be found The subject of transport phenomena can be useful in the classic text by de Groot and Mazur.1281 The in many fields, including micrometeorology, zool­ thermodynamics of irreversible processes has been ogy, analytical , nuclear engineering, tri­ found to be particularly useful in the systematiza­ bology, , , phar­ tion of the flux expressions for multicomponent dif­ macology, and space science. Chemical engineering fusion as well as in linear viscoelasticity.1291 Although departments are in a good position to provide gen­ this topic is not essential for undergraduate stu­ eral service courses in transport phenomena for other dents, perhaps graduate students can benefit from department on campus. the extra insight provided by the thermodynamic ACKNOWLEDGMENTS approach. The author wishes to thank Professors W.E . CONCLUDING COMMENTS Stewart and T. W. Root, and Mr. Peyman Pakdel of It is essential that students of transport phenom­ the Department of Chemical Engineering at the Uni­ ena recognize the central position occupied by the versity of Wisconsin, and Professor J.D. Schieber at conservation statements. The conservation laws for the University of Houston for valuable suggestions. 108 Chemical Engineering Education KNOWLEDGE STRUCTURE REFERENCES 13. Finlayson, B.A., The Method of Weighted Residuals and Variational Principles, Academic Press, New York (1972) 1. Bird, R.B., W.E. Stewart, and E.N. Lightfoot, Transport 14. Finlayson, B.A. , Nonlinear Analysis in Chemical ­ Phenomena, Wiley, New York (1960) ing, McGraw-Hill, New York (1980) 2. Bird, R.B., R.C. Armstrong, and 0. Hassager, Dynamics of 15. Finlayson, B.A. , Numerical Methods for Problems with Mou­ Polymeric Liquids. Vol. 1: Fluid , 2nd ed. , Wiley, ing Fronts, Ravenna Park, Seattle, WA (1992) New York (1987) 16. Schlichting, H., Boundary Layer Theory, 4th ed., McGraw­ 3. Bird, R.B., C.F. Curtiss, R.C. Armstrong, and 0. Hassager, Hill, New York (1960) Dynamics of Polymeric Liquids. Vol. 2: Kinetic Theory, 2nd 17. Hinze, J.O., , 2nd ed. , McGraw-Hill, New York ed., Wiley, New York (1987) (1975) 4. Bird, R.B., W.E. Stewart, and E.N. Lightfoot, Selected Top­ 18. Tennekes, H., and J .L. Lumley, A First Course in Turbu­ ics in Transport Phenomena, Chem. Eng. Prog. Symp. Se­ lence, MIT Press, Cambridge, MA (1972) ries No. 58, Vol. 61, AIChE (1965) 19. Speziale, C.G., in Ann. Rev. 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•,a•5113.-:::b-:::o:--=o=-:k;:--:re=v:;.ie=w-=------..) Sciences. This chapter is a concise review of natural gas engineering production and underground stor­ age of natural gas. Several subjects are covered, NATURAL GAS ENGINEERING: e.g., the branches of petroleum industry, sources of PRODUCTION AND STORAGE information for natural gas engineering, a brief dis­ by Donald L. Katz, Robert L. Lee cussion of geology and sciences, and earth McGraw Hill, New York, NY 10020; 760 pages, $54.95 temperatures and . (1989) Chapter 2 • Properties of Rocks. This chapter con­ Reviewed by tains some descriptions of the properties of rocks or R. A. Greenkorn porous media, including a description of how these Purdue University properties are measured. The discussion is under­ This book covers most aspects of natural gas engi­ standable and relatively clear-but very terse. neering. It is a survey suitable for a short course to Chapter 3 • Thermodynamics: Flow Equation, introduce practicing engineers to the topic. The book Fluid Properties, Combustion. This chapter is basi­ is descriptive and as such is much too broad to be cally descriptive. It is terse, explaining how the equa­ used as a textbook. The later half of the book is tions are derived and giving some limited informa­ essentially a monograph recording the senior author's tion on how to calculate combustion of natural gas. extensive experience in this area. Chapters 1-7 de­ Chapter 4 • Physical Behavior of Natural Gas scribe the material properties of the system, chap­ Systems: Physical and Thermal Properties, Phase ters 8-13 contain the core of the material concerned Behavior, Analyses. The initial part of this chapter with the production and storage of natural gas, chap­ is a review of pressure, volume, and temperature ters 14-15 mainly discuss operations, and chapters relationships of pure fluids. The phase rule and the 16-17 contain miscellaneous topics. behavior of complex mixtures are briefly discussed. Chapter 1 • Natural Gas Technology and Earth Continued on page 116. Spring 1993 109