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Course: ME 303, Fall 2009
School: W. Alabama
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303 WK5TPCSWEB.TEX ME M.M. Yovanovich Week 5 Lecture 1 Sturm-Liouville Problem SLP Cartesian Coordinates. u = ux; y or u = ux; t. Partial di erential equations. uxx + uyy = 0; 0 x L; 0 y H 1D Di usion Equation: uxx = 1 ut; t 0; 0 x L 1D Wave Equation: uxx = c1 utt; t 0; 0 x L where and c are positive constants. Separation of Variables Method SVM is used to obtain two sets of independent ODES. Let ux; y = X xY...

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303 WK5TPCSWEB.TEX ME M.M. Yovanovich Week 5 Lecture 1 Sturm-Liouville Problem SLP Cartesian Coordinates. u = ux; y or u = ux; t. Partial di erential equations. uxx + uyy = 0; 0 x L; 0 y H 1D Di usion Equation: uxx = 1 ut; t 0; 0 x L 1D Wave Equation: uxx = c1 utt; t 0; 0 x L where and c are positive constants. Separation of Variables Method SVM is used to obtain two sets of independent ODES. Let ux; y = X xY y and let ux; t = X xT t. One very important ODE appears in all three cases. 2D Laplace Equation: 2 2 X 00 + X = 0; 2 0 x L Homogenous BCs at x = 0 and x = L are i X 0 = 0 or ii X 00 = 0 or iii , kX 0 0 = hX 0 where h and k are positive thermophysical parameters. These are homogeneous BCs of the rst kind Dirichlet, of the second kind Neumann, and of the third kind Robin. Similarly i X L = 0 or ii X 0L = 0 or iii , kX 0 L = hX L There are nine combinations of these homogeneous BCs. Solution of ODE. X x = C cos x + C sin x; 0 x L and its derivative is X 0x = ,C sin x + C cos x 1 2 1 2 Eigenfunctions are cos x and sin x Three combinations of the homogeneous BCs. a X 00 = 0 and X L = 0 b X 00 = 0 and X 0L = 0 a X 00 = 0 and , kX 0L = hX L Case a requires that X 00 = ,C sin 0 + C cos 0 = 0 1 2 2 C =0 Therefore C = 0 or = 0. Since = 0 gives a trivial solution, it will be rejected, and we take C = 0. Solution is X x = C cosx and X 0x = ,C sinx 2 2 1 1 Apply second homogeneous Dirichlet condition to get C cos L = 0 Either C = 0 which gives a trivial solution, and therefore this option is rejected, or cos L = 0. This is satis ed when n L = 2n , 1 ; n = 1; 2; 3; : : : 2 1 1 Eigenvalues are n = 2n , 1 2 ; n = 1; 2; 3; : : : L 2 Many math texts call 2 the eigenvalues. Most engineering texts call n the n eigenvalues. Eigenfunctions which satisfy the ODE and the two homogeneous Dirichlet conditions at x = 0 and x = L are x ; n = 1; 2; 3: : : : Xn x = Dn cos 2n , 1 2L where Dn are arbitrary constants. X 00 and X 0L = 0 The rst homogeneous Neumann condition requires C = 0 and X x = C cosx and X 0x = ,C sinx as in Case a. The homogeneous Neumann condition at x = L requires that 2 1 1 Case b X 0L = ,C sinL = 0 1 Both options C1 = 0 and = 0 give trivial solutions, therefore they are rejected. Eigenfunctions for Case b are sinn L = 0; n = 1; 2; 3; : : : which require n L = n ; n = 1; 2; 3; : : : n = n ; n = 1; 2; 3; : : : L Eigenvalues for Case b are Eigenfunctions which satisfy the ODE and the two homogeneous Neumann conditions at x = 0 and x = L are Xn x = Dn cos nx ; n = 1; 2; 3: : : : L where Dn are arbitrary constants. Case c X 00 and , k X 0L = hX L 3 The rst homogeneous Neumann condition requires C2 = 0 and X x = C1 cosx and X 0x = ,C1 sinx as in Case a and Caseb. The homogeneous Robin condition at x = L requires that ,kX 0L = hX L or , k ,C sinL = hC cosL 1 1 The option C1 = 0 gives a trivial solution, therefore it is rejected. Cancel the common C1 and rewrite the relation as h cosL = sinL k The relation is dimensional because both and h=k have the same units m,1 . The argument of the cosine and sine functions is L which must be dimensionless. Characteristic Equation Multiple through by L and de ne dimensionless parameters: = L and Bi = hL 0 k Now the characteristic equation becomes: sin = Bi cos and 0 Bi 1 This is a transcendental equation. Numerical methods are required to obtain its roots for a given value of the parameter Bi. The Newton-Raphson iterative method can be used to obtain the roots. For a given value of Bi the in nite set of roots called eigenvalues are: 1 2 3 n n+1 n+2 Lecture 2 Makeup Lecture Number 2. Discuss Project Number 1. Physical interpretation of equations and the solution. Some Problems from Spiegel's Text: p. 584, A Excercises: 3 4 B Excercises: 2, 3 ******************** p. 592, A Excercises: 1, 3 ******************** P. 593, B Excercises: 2, 3 **************** p. 615, A Excercises: 1, 2, 3, 4, 5 *********************** p. 616-617, B Excercises: 1, 2, 6, 7 ********************** p. 617, C Excercises: 8 ************** Limiting values of parameter Bi. For Bi = 0, the characteristic equation becomes sin = 0. Since cannot be set to zero it gives a trivial solution, we set sin = 0. The roots eigenvalues are n = n ; n = 1; 2; 3; : : : For Bi = 1 write the equation as cos = Bi sin and now set Bi = 1 to give cos = 0. The roots eigenvalues are n = 2n , 1 ; n = 1; 2; 3; : : : 2 Location of Roots Eigenvalues. Location of the roots are easily found graphically. They lie in the intervals: 0 Bi 1 0 =2 1 3=2 2 2 5=2 3 n , 1 2n , 1=2 n 5 Maple, Mathcad and Matlab can nd these roots quickly and accurately. Di erence between two consecutive eigenvalues. as n ! 1 n+1 , n ! Eigenfunctions which satisfy the ODE and the homogeneous Neumann and Robin conditions at x = 0 and x = L respectively are ! n Xn x = Dn cos Lx ; n = 1; 2; 3: : : : where Dn are arbitrary constants. Approximation of the First Eigenvalue, 1. p As Bi ! 0; Bi 1 ! and As Bi ! 1; 1 ! 2 These limits are used to develop the following approximation proposed by M.M. Yovanovich: =2 and m = 2:15 1 = " ! =2 m 1=m 1+ p Bi This correlation is equation valid of all values of Bi, i.e., 0 Bi 1, and it provides acceptable accuracy for the calculation of 1 for most engineering applications. Newton-Raphson Iterative Method. The the nth root n of the arbtrary function f is obtained by means of the relation: k k +1 = nk , f0 nk ; k = 1; 2; 3; : : : n fn where k represents the kth iteration. For the characteristic equation, sin , Bi cos = 0, we have the relation: k k k k +1 = nk , k n sink n , Bi cos n k ; k = 1; 2; 3 : : : n n cos n + 1 + Bi sin n 6 1 The rst guess of the rst root 1 this characteristic equation can be based on the approximation given above. Generally three to four iterations will provide very accurate values for the rst root. The rst guess for the second root should be based on 1 = 1converged value + 2 This process can be followed to calculate all required roots which may be as many as several hundred for a particular problem. Maple and Mathcad can calculate these roots very quickly and accurately. See ME 303 Web site: Maple WS called CECART.MWS. Lecture 4 See Spiegel's Text: Sections 2.1 and 2.2 on pages 585-591. Separation of Variables Method SVM applied to 1D wave equation. uxx = c12 utt; t 0; 0 x L and the system constant is c2 = T= where T is the tension in the elastic string and is the linear density of the string. The units of c2 m2=s2 and c m=s . See the development of PDE in the text. Boundary and Initial Conditions. The ends are xed, therefore the homogeneous boundary conditions of the rst kind Dirichlet are: t 0; u0; t = 0; uL; t = 0 The two initial conditions are based on the initial displacement and the initial velocity: @ux; 0 = gx t = 0; 0 x L; ux; 0 = f x; @t Separated ODES. Let ux; t = X xT t; substitute into the PDE to get the separated relationship: X 00 = 1 T 00 X c2 T The identity must hold for all time t 0 and any value of x in interval 0; L . There are three options: lhs = rhs = i 0; ii , 2 ; iii 2. 7 Option i gives the separated ODEs: X 00 = 0; and their solutions are: T 00 = 0 and X x = C x + C ; 1 2 T t = C t + C 3 4 Both solutions are linear in time and space. Option ii gives the separated ODEs: X 00 + X 2 and and T 00 + c T = 0 2 2 and their solutions are : X x = C cosx + C sinx 1 2 T t = C cosct + C sinct 3 4 Both solutions are periodic functions of space and time respectively. Option iii gives the separated ODEs: X 00 , X; 2 and and T 00 , c T = 0 2 2 and their solutions are : X x = C coshx+C sinhx 1 2 T t = C coshct+C sinhct 3 4 Both solutions are non-periodic functions of space and time respectively. The solutions for option iii can also be written in terms of exponentials: X x = C expx+C exp,x 1 2 and T t = C expct+C exp,ct 3 4 The xed end conditions require: u0; t = X 0T t = 0 = X 0 = 0 and uL; t = X LT t = 0 = X L = 0 These homogeneous BCs require C1 = 0 and C2 = 0 in options i and iii. These solutions are not applicable to the xed ends string. These conditions when applied to option ii solution require: C =0 1 and 8 C sinL = 0 2 Since C2 = 0 leads to a trivial solution, it is rejected...

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W. Alabama - ME - 303
WK9TPCSWEB.TEXME 303 M.M. YovanovichWeek 9Lecture 1Lecture cancelled.Lecture 2Lecture cancelled.Lecture 3Lecture cancelled.
W. Alabama - ME - 303
WK8TPCSWEB.TEXME 303 M.M. YovanovichWeek 8Lecture 1Section 1.2: 1D Di usion equation Heat equation with homogeneous Neumann BCs. Section 1.3: 2D Laplace equation conduction problem in a semi-in nite plate with homogeneous Dirichlet BCs. Demons
W. Alabama - ME - 303
WK2TPCSWEB.TEXME 303 M.M. YovanovichWeek 2Lecture 1Hand out Problem Set 1. ODEs in cartesian, polar and spherical coordinates; TAs will discuss some solutions in the tutorials. Discuss how to obtain solution of homogeneous ODE in spherical co
W. Alabama - ME - 303
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W. Alabama - ME - 303
WKxTPCSWEB.TEXME 303 M.M. YovanovichWeek 10Lecture 1Discussed the physics of the problem of Project 2. Used Maple to show the temperature plots as a function of dimensionless time. Solution procedure is based on the material covered in Sectio
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200 OK400 Bad Request301 Moved Permanently200 OK404 Not Found401 Authorization Required200 OK
W. Alabama - ME - 303
WK12TPCSWEB.TEXME 303 M.M. Yovanovich Week 12 Lecture 1Solution of ODEd + m = n; t 0; IC 0 = i dt where t = T t , T1, and the constants are: m = hA and n = qciA cpV pV where A = surface area, V = volume, qi = incident heat ux. Units are: h W=m
W. Alabama - ME - 303
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W. Alabama - ME - 303
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CLASSIFICATION OF LINEAR PDEs OF SECOND ORDERSecond order linear PDEs with two independent variables x; y have the general form:Au + Bu + Cu + Du + Eu + Fu = Gxx xy yy x ywhere the coe cients A; B; C; D; E; F; and G are functions of x and y or
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W. Alabama - ME - 303
ME 303 Advanced Engineering Mathematics Nondimensional Di usion Equation Boundary Conditions and Initial ConditionM.M. YovanovichDIMENSIONLESS PDE, BCs and ICTo illustrate how a Partial Di erential Equation PDE, and its Boundary Conditions BCs an
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ME 303 Advanced Engineering MathematicsM.M. YovanovichOrdinary Di erential Equations in Spherical CoordinatesWhen certain partial di erential equations formulated in spherical coordinates are separated by the separation of variables method, or th
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ME 303 Advanced Engineering Mathematics Fourier Cosine and Sine SeriesM.M. YovanovichFourier series. The Fourier series of a periodic function f x with period 2Lis de ned as the trigonometric series1 X 1 nx + X B sin nx f x = A0 + An cos L n
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W. Alabama - ECE - 309
DEPARTMENT OF ELECTRICAL ENGINEERING ECE 309 Thermodynamics Electrical EngineeringUNIVERSITY OF WATERLOOMid-Term Examination M.M. Yovanovich NOTE:Spring 1996 June 22, 1996 9:00-11:00 A.M.1. Open book examination. You are permitted to use your
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RADLAWSWEB.TEXECE 309 M.M. YovanovichRadiation LawsPlanck's Distribution LawThe relation for the spectral blackbody emissive power Eb was developed by Planck 1901. The relation is known as Planck's distribution law, and it is expressed asWien
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HEATWEB.TEXHeat Transfer Relationships Conduction, Convection and Radiation Laws of Heat Transfer Fourier's Law of Conduction _ Q = ,k rTA Newton's Law of Cooling _ Q = hATwall , T uid Stefan-Boltzmann Law of Radiation for Black Bodies _ Q = A1T14
W. Alabama - ECE - 309
USUFWEB.TEXECE 309 M.M. YovanovichUniform-State, Uniform-Flow Process USUFThe following assumptions lead to a useful model called the uniformstate, uniform- ow process USUF. The control volume is stationary relative to some coordinate frame. The
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W. Alabama - ECE - 309
GIBBS EQUATIONThe Gibbs equation for a simple compressible substance SCS comes from: = . The di erential change in the speci c entropy is: ! ! = + v u Introducing the thermodynamic de nitions of temperature and pressure: 1 = ! v and ! = u we obt
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PRANDTLWEB.TEXECE 309 M.M. YovanovichTypical Ranges of Prandtl Numbers for Selected FluidsThe Prandtl number is a dimensionless group de ned as Pr = molecular di usion of momentum = = Cp molecular di usion of heat kFluidPrLiquid metals 0:0
W. Alabama - ECE - 309
SYSTEMWEB.TEXECE 309 M.M. YovanovichThermodynamic Systems De nitionA thermodynamic system is a de nite quantity of matter occupying a volume which is bounded by a closed surface which is impervious to the ow of matter. The surface is called the
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TEMPWEB.TEXECE 309 M.M. YovanovichTemperature Scales and ConversionsThere are four thermodynamic temperature scales: Celsius, Fahrenheit, Kelvin, Rankine. The Kelvin and Rankine temperature scales are absolute scales. The relations and conversio
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ZEROWEB.TEXECE 309 M.M. YovanovichZeroth Law of ThermodynamicsWhen two bodies A and B are in thermal equilbrium with a third body C: TA = TC and TB = TC then the two bodies also have equality of temperature:TA = TB
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CONVWEB.TEXECE 309 M.M. YovanovichTypical Ranges of Convective Heat Transfer Coe cients Type of ConvectionFree convection of gases Free convection of liquids Forced convection of gases Forced convection of liquids Boiling and condensation h;W=
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PROJ1S99.TEXUNIVERSITY OF WATERLOO DEPARTMENT OF MECHANICAL ENGINEERING E&CE 309 Thermodynamics ISPRING 1999M.M. Yovanovich Project No. 1, Part 1. This part of Project No. 1 must be handed in at thestart of the next lecture, Friday, May 28. You
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WK5TPCSWEB.TEXECE 309 M.M. YovanovichWeek 5Lecture 1Convection Heat Transfer. See Website for material on convective heat transfer. Overview of Convective Heat Transfer _ Newton's Law of Cooling: Qconv = h A Tw , Tf A is total convective are
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WK11TPCSWEB.TEXECE 309 M.M. YovanovichWeek 11Lecture 1Hand out Tables of Properties of Compressed water. Hand out P , v-diagram for water. Show the critical point, the saturated liquid line and the saturated vapor line. Show locations of the
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