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Course: ME 353, Fall 2009
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OF SUMMARY.TEX SUMMARY CONVECTION CORRELATION EQUATIONS ME 353 Heat Transfer 1 Department of Mechanical Engineering University of Waterloo M.M. Yovanovich November 10, 1997 The attached material is a summary of some of the important results for forced and natural convection heat transfer from isothermal or iso ux surfaces. Correlation equations for local and area-average heat transfer for external and internal...

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OF SUMMARY.TEX SUMMARY CONVECTION CORRELATION EQUATIONS ME 353 Heat Transfer 1 Department of Mechanical Engineering University of Waterloo M.M. Yovanovich November 10, 1997 The attached material is a summary of some of the important results for forced and natural convection heat transfer from isothermal or iso ux surfaces. Correlation equations for local and area-average heat transfer for external and internal ow are given. Many empirical and analytic correlation equations have been developed for the local and area-average values of the Nusselt number for limited ranges of the forced and buoyancyinduced ow parameters: Reynolds, Peclet, Grashof and Rayleigh numbers; for laminar or turbulent ows; and for various uids which are characterized by the Prandtl number. One should consult the course text for the de nitions of the various dependent and independent parameters and the basis for the uid properties evaluation for the particular correlation equation. This summary does not cover the numerous forced and buoyancy-induced internal ows through and within complex con gurations. One should consult the course text or the several handbooks which deal with these topics. 1. Laminar and Turbulent Forced External Flow De nitions of Local and Area-average Values ,k @T x; y = 0 Z 1 L hx = T ,@y , h = L hx dx = 2hx = L T w 1 0 x Nux = hkx , Rex = U1 x ReL = U1 L 1 h NuL = kL , Flat Plate, Laminar Boundary Layer Flow Correlation = 5xRe,1=2 x Cf;x = 0:664Re,1=2 x C f;x = 1:328Re,1=2 x = Pr,1=3 Nux = 0:3387Pr1=3 1=2 Limits 100 100 100 100 100 Conditions 500; 000 500; 000 500; 000 500; 000 500; 000 Local Local Area-Average Local Local, UWT, Pr ! 1 Rex Nux 1=2 1 Rex=2 = 0:564Pr Nu=x2 = h 0:3387Pr1=3 i1=4 1 Rex 1 + 0:0468=Pr2=3 Nux = 0:4637Pr1=3 1 Rex=2 Nu=x2 = 0:886Pr1=2 Re1 x Rex Rex Rex Rex Rex 100 Rex 500; 000 Local, UWT, Pr ! 0 100 Rex 500; 000 Local, UWT, 0 Pr 1 100 Rex 500; 000 Local, UWF, Pr ! 1 100 Rex 500; 000 Local, UWF, Pr ! 0 Nu=x2 = h 0:4637Pr1=3 i1=4 100 Rex 500; 000 Local, UWF, 0 Pr 1 1 Rex 1 + 0:0205=Pr2=3 Nu=2 = h 0:6774Pr1=3 i 100 ReL 500; 000 Average, UWT, 0 Pr 1 L 1 1=4 ReL 1 + 0:0468=Pr2=3 NuL = h 0:9274Pr1=3 i 100 ReL 500; 000 Average, UWF, 0 Pr 1 1 ReL=2 1 + 0:0205=Pr2=3 1=4 Flat Plate, Turbulent Boundary Layer Flow Correlation = 0:37xRe,1=5 x Cf;x = 0:0592Re,1=5 x ,1=5 , 1742Re,1 C f;L = 0:074ReL L = Pr,1=3 100 Rex 500; 000 Nux = 0:0296Re4=5 Pr1=3 100 Rex 500; 000 x 1=3 NuL = 0:037Re4=5 , 871 Pr 100 Rex 500; 000 L 2 Limits 5 105 Rex 108 5 105 Rex 108 Rex;c = 5 105 Conditions Local Local Mixed-Average Local Local, UWT, 0:6 Pr 60 Average, UWT, 0:6 Pr 60 Cross Flow Over Circular Cylinders " 4=5 1=2 1=3 ReD 5=8 ? + " 0:6ReD Pr NuD = SD 2=3 1=4 1+ 282; 000 ? SD Correlation Limits 100 ReD 107 0 L=D 8 Conditions Average; UWT; 0 Pr 1 0 1 4 ? A 1 SD = p @ q 1 1 + 0:5D=L ln2L=D Flow Over Spheres L=D 0:76 4 = 1 + 0::869L=D 05+ 1+ 0:4 Pr ! ReD ! 0 ReD ! 0; Asymptote L=D 8 Correlation 24 CD = 0:4 + ReD + Limits Conditions 6 q 0 ReD 2 105 Total Drag, 10 1 + ReD 4=5 = " Average; UWT; 0:6Re1=2Pr13 1+ ReD 5=8 NuD =2+ " D 2=3 1=4 100 ReD 107 282; 000 0 Pr 1 1 + 0:4 Pr 2. External Flow Over Isothermal Oblate and Prolate Spheroids The following universal correlation equation: 0 p 2 !1=2 3 P 1=2 p NupA = Nu A + 40:15 p RepA + 0:35Re0:5665 Pr1=3 A A was developed by Yovanovich 1988 from two accurate correlation equations proposed by Yuge 1960 for air cooling of isothermal spheres, and the correlation equations developed by several researchers for convection heat and mass transfer from isothermal oblate and prolate spheroids. In the above correlation equation the Nusselt and Reynolds numbers are both based p p on the length scale L = A. The di usive limit Nu0 A corresponding to Re ! 0 is the ? dimensionless shape factor SpA . Yovanovich 1988 blended the two Yuge equations and introduced the parameter P= A which accounts for the blockage of the body as the uid ows around it. Also the Yuge 3 p correlation equations which were developed for air were extended to account for large Prandtl number uids, i.e. Pr 0:7. The correlation equation is valid for the wide Reynolds number range: 0 RepA 2 105 . The general correlation equation is in very good agreement with numerous analytical and experimental correlation equations over various ranges of the Reynolds number for Pr = 0:7. It is also in good agreement with the empirical correlation equation of Pasternak and Gauvin 1960 which was developed from 20 di erent convex body shapes to account for both body shape and orientation. The body length scale which they proposed was based on the ratio of the total surface area of the body divided by the maximum projected area of the body perpendicular to the air ow. They achieved good correlation of their heat and mass transfer data with a single power-law equation which was converted to the body scale p length L = A p NupA = 0:914Re0:514Pr1=3 886 RepA 8860 A This equation correlated data for spheres, nite circular cylinders with axes parallel and perpendicular to the ow, prisms, cubes in various orientations, and hemispheres positioned with the at section at the rear. The turbulence intensity was reported to be in the range: 9 to 10 in all their experiments. The single equation correlated all data with a deviation of only 15 in the speci ed range. The general correlation equation agrees with the Pasternak-Gauvin correlation equation within the given Reynolds number range to within 15 . Therefore, the general equation of Yovanovich can be used for arbitrary convex isothermal bodies over a much wider range of the Reynolds number. 3. Laminar Forced Internal Flow De nitions and Notation Reynolds number: Laminar Flow: Hydraulic Diameter: Dimensionless axial distance: Local, Isothermal Wall, Nusselt number: Mean-value, Isothermal Wall, Nusselt number: Local, Iso ux Wall, Nusselt number: Mean-value, Iso ux Wall, Nusselt number: 4 ReD = UDh ReD 2300 A Dh = 4 P = Cross Section Area Wetted Perimeter x 1 ?= x = x Dh Pe Dh RePr = Gz 4 Nux;UWT = Tw qw xx Dh , Tm k w Num;UWT = Tw ,qTmx Dh k Nux;UWF = Tw x qw Tmx Dh k , Num;UWF = Twx qw Tmx Dh k , Local Nusselt Number for Thermally Developing Flow Churchill and Ozoe 1973 propose the following correlation equations for the local Nusselt number for the developing thermal eld for the UWT and UWF cases: " Nux;UWT + 1:7 = 1 + 388 x?,8=9 3=8 5:357 " Nux;UWF + 1 = 1 + 220 x?,10=9 3=10 5:364 5 5 They developed these expressions based on asymptotic solutions valid for small and large values of x?. Area-Average Nusselt Number for Fully Developed Hydraulic, Thermally Developing Flow following The approximations of Shah 1975 for fully developed hydraulic ow and thermally developing in an isothermal UWT or an iso ux UWF circular pipe are based on the analytic solutions of the Graetz-type problems. Expressions for area-mean Num;UWT ; Num;UWF versus the local dimensionless position x? = x=Dh =RePr are given below. The approximations are quite accurate over the entire range: 0:005 x? 1: The maximum di erence with respect to accurate analytic results is less than 4:4. For very small values x? 0:005 the approximate expressions approach the Leveque asymptotes which were obtained by the method of similarity transformation. For large values x? 0:25, the approximations go to the fully-developed hydraulic and thermal solutions: NuUWT = 3:656 and NuUWF = 4:354 which were obtained by the method of separation of variables which leads to a di erential equation of the Sturm-Liouville type. The solution is presented as an in nite series expansion of eigenfunctions and corresponding eigenvalues. 8 1:615 , 0:2; 0:005 x? 0:03 x?1=3 Num;UWT = : 3:656 + 0:0499 ; x? 0:03 x? 8 1:953 ; x? 0:03 x?1=3 Num;UWF = : 4:354 + 0:0722 ; x? 0:03 x? The circular cylinder results may be used to nd approximate values for isothermal and iso ux tubes having other cross-sections e.g. square or triangular pipes by the use of the hydraulic diameter in the Nusselt and Reynolds numbers. 5 4. Laminar and Turbulent Natural External Flow De nitions of Local and Area-average Values ,k @T x; y = 0 @y y hx = 3 h = 4 hx = L T , T , w 1 x Nux = hkx , h NuL = kL 3 Rax = g Tw , T1 x , 3 RaL = g Tw , T1 L , y Grx = g Tw , T1 x3 , 2 3 y GrL = g Tw , T1 L , 2 Rax = GrxPr RaL = GrLPr y For UWF cases, use the midpoint temperature di erence: Twx = L=2 , T1 Flat Plate, Buoyancy-Induced Laminar Boundary Layer Flow Nux Ra1=4 = 0:5027 x Nu=4 = 0:6004Pr1=4 x Ra1 x Nux 0:5027 Ra1=4 = h1 + 0:492=Pr9=16 i4=9 x Nux Ra1=4 = 0:5627 x Nu=4 = 0:6922Pr1=4 x Ra1 x 104 Grx 109 Local, UWT, Pr ! 1 104 Grx 109 Local, UWT, Pr ! 0 104 Grx 109 Local, UWT, 0 Pr 1 ? 104 Grx 109 Local, UWF, Pr ! 1 ? 104 Grx 109 Local, UWF, Pr ! 0 Nux 0:5627 4 ? 9 Ra1=4 = h1 + 0:437=Pr9=16 i4=9 10 Grx 10 Local, UWF, 0 Pr 1 x NuL = h 0:6703 i 104 GrL 109 Average, UWT, 0 Pr 1 1=4 9=16 4=9 RaL 1 + 0:492=Pr NuL = 0:7503 ? 104 GrL 109 Average, UWF, 0 Pr 1 Ra1=4 h1 + 0:437=Pr9=16 i4=9 L 6 Flat Plate, Buoyancy-Induced Turbulent Boundary Layer Flow NuL = h 92 0:387RaL i = 10,1 RaL 1012 NuL = 0:825 + h 8=27 : 1 + 0:492=Pr9=16 ; 1=6 8 0:150Ra1=3 i L 16=27 1 + 0:492=Pr9=16 109 GrL 1012 Average; UWT; 0 Pr 1 Average; UWT; 0 Pr 1 Long Horizontal Isothermal Circular Cylinders, Laminar and Turbulent Flow 2 NuD = 40:60 + 0:387Ra1=6 D 5 1 + 0:559=Pr9=16 8=27 32 0 Pr 1; 10,5 RaD 1012 Finite Horizontal Isothermal Circular Cylinders, Laminar Flow ? NuD = SD + 1 0:518RaD=4 1 + 0:559=Pr9=16 4=9 0 Pr 1; 0 RaD 109 Isothermal Spheres, Laminar Flow NuD = 2 + 0:589Ra1=4 D ; 1 + 0:469=Pr9=16 4=9 0 Pr 1; 0 RaD 1011 5. General Correlation Equation for Arbitrary Isothermal Convex Bodies NuL = Nu0 + F PrGL Ra1=4; L L 0 Pr 1 0 RaL 1011 where the characteristic body length is L = A and A is the total active or wetted surface area. The universal Prandtl number function valid for all isothermal convex bodies is given by: 0:670 F Pr = 1 + 0:5=Pr9=16 4=9 which for air Pr = 0:71 has the value F Pr = 0:71 = 0:513. The di usive limit Nu0 or L p ? shape factor SL with L = A is a weak function of body shape and its aspect ratio. For 7 p ? example, its range is 3:20 SpA 7:55 for a solid circular cylinder whose length-to-diameter ratio varies from 0 a circular disk to 100 very long cylinder. For long axisymmetric bodies e.g. circular cylinder and long square cuboid the shape factor can be accurately q approximated by SpA = 4 L=D= ln2L=D where D is the diameter of the circular cylinder and it is equal to the geometric-mean of the diameters of the inscribed and circumscribed circular cylinders respectively, and L is the le...

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W. Alabama - ME - 353
WK4TPCSWEB.TEXME 353 M.M. YovanovichWeek 4Hand out Project 1. Due Friday, October 16, 12 Noon. Extended surfaces or ns; temperature is one-dimensional T x when Bi = hte=k 0:2 where the e ective n thickness is de ned as te = A=P ; where P is the
W. Alabama - ME - 353
WK9TPCSWEB.TEXME 353 M.M. YovanovichWeek 9Makeup lecture 3. Week 8 lecture summary and several pages of summary of convective heat transfer correlations are available in Engineering Photocopy Center. Pick up and bring to future lectures. See Ap
W. Alabama - ME - 353
WK7TPCSWEB.TEXME 353 M.M. YovanovichWeek 7Lecture 1Read Chapter 5: Sections 5.1 - 5.8. Lumped Capacitance Model LCM Bi = hL=k 0:2; T ~; t = T t r System parameters: _ _ V; S; ; cP ; k; ; h; Ti; Tf ; Tsurr; qin; Egen; Estorage; Qconv; Qrad Ene
W. Alabama - ME - 353
WKxTPCSWEB.TEXME 353 M.M. YovanovichWeek 11ME 353 Heat Transfer Lab begins on Monday. See signup sheet. Forced internal laminar and turbulent convection in circular and noncircular tubes, pipes and ducts. See handout for de nitions of local and
W. Alabama - ME - 353
WK1TPCSWEB.TEXME 353 M.M. Yovanovich Week 1 Lecture 1Information provided: Instructor: M.M. Yovanovich, CPH 3375C X3588, E3-2133A, X6181 or X4586 email: mmyov@mhtl.uwaterloo.ca Teaching Assistants Mirko Stevanovic, E3-2133A, X6181; email: mirko@mh
W. Alabama - ME - 353
WK2TPCSWEB.TEXME 353 M.M. Yovanovich Week 2 Lecture 1Solutions to problems are available in Engineering Photocopy Center. First makeup lecture: Thursday, 8:30 AM, CPH 3385. Discuss the ME 353 Website. Calendar, Assigments, Projects, Exams, Lecture
W. Alabama - ME - 353
DEPARTMENT OF MECHANICAL ENGINEERING ME 353 HEAT TRANSFER 1UNIVERSITY OF WATERLOODecember 9, 1996 M.M. YovanovichTime: 9-12 A.M.Three-hour Closed Book Final Examination. Two crib sheets both sides are permitted. All questions are of equal val
W. Alabama - ME - 353
SUMTABLE.TEXME 353 HEAT TRANSFER I SUMMARY OF CONVECTION CORRELATION EQUATIONS Laminar and Turbulent Forced External Flow Flat Plate, Laminar Boundary Layer Flow= 5xRe,1=2 x Cf;x = 0:664Re,1=2 x f;x = 1:328Re,1=2 C x = Pr,1=3 Nux = 0:3387Pr1=3 Re
W. Alabama - ME - 353
UNIVERSITY OF WATERLOO DEPARTMENT OF MECHANICAL ENGINEERING ME 353 HEAT TRANSFER 1 October 25, 1991M.M. YovanovichTime: 4:30-6:30 p.m.Two-hour Closed Book Mid-term Examination. You are allowed one crib sheet both sides and the solutions to part
W. Alabama - ME - 353
WK13TPCSWEB.TEXME 353 M.M. YovanovichWeek 13Last lecture of the term. Hand in laboratory writeup to the teaching assistants. Ignore the problems for Chapter 11 which deals with Heat Exchanger Design. This topic will be covered in second heat tr
W. Alabama - ME - 353
WK12TPCSWEB.TEXME 353 M.M. YovanovichWeek 12Lecture 1See website for Maple worksheets for air properties correlation equations, and natural convection calculations. Natural convection across annular space bounded by two isothermal horizontal
W. Alabama - ME - 353
WK10TPCSWEB.TEXME 353 M.M. Yovanovich Week 10 Lecture 1Pick up material on Summary of Convection Correlation Equations. Forced External Convective Heat Transfer. Correlation equations for external natural convection: vertical at plate; horizontal
W. Alabama - ME - 353
WK6TPCSWEB.TEXME 353 M.M. YovanovichWeek 6Lecture 1Cancelled for midterm exam. Friday, October 23, 4:30-6:30 PM in CPH3374 3388.Lecture 2Cancelled for midterm exam.Lecture 3Cancelled for midterm exam.
East Los Angeles College - MATH - 1825
MATH1825 Statistics Through Applications Reading listUniversity of Leeds School of Mathematics Semester 2 20091. Baxter, P. D., (2008), MATH1825 Statistics Through Applications [Online], [Accessed on 10th August 2007], Available from World Wide W
W. Alabama - ME - 353
WK5TPCSWEB.TEXME 353 M.M. Yovanovich Week 5 Lecture 1 Lecture 2Monday, October 12 lecture cancelled for Thanksgiving Day. Resistance of truncated cone of length L, and radii a; b where b a with restriction: b , a=L 1. Thermal conductivity depends
East Los Angeles College - MATH - 3802
MATH3802 Time Series Outline Solutions to Worksheet 2University of Leeds School of Mathematics Semester 2 2009Solution to Question 1 R commands:> births1=ts(scan("http:/www.maths.leeds.ac.uk/pdbaxt/math3802/births1.txt") Read 365 items > ts.plot
W. Alabama - ME - 353
WK8TPCSWEB.TEXME 353 M.M. Yovanovich Week 8 Lecture 1Provide midterm results. Problem 3 of midterm will be re-submitted at start of next lecture. Outline of the solution procedure to be followed.Lecture 2Hand in Problem 3. Half-space solutions
East Los Angeles College - MATH - 1825
MATH1825: Lecture 7Two sample non parametric tests1Two sample problems Suppose that we have two samples of data and we are interested in comparing their averages to see if there is a large difference between them. The samples are small in size
W. Alabama - ME - 353
WK3TPCSWEB.TEXME 353 M.M. YovanovichWeek 3ME 353 Web Site: Summary of week 2 topics are on the Web. Contact resistance: Rc = 1=hc A; see Table 3.1 for typical values of Rt;c; how to get hc, contact conductance, from Table 3.1; hc = 1=Rt;c W=m2K
East Los Angeles College - MATH - 1825
MATH1825 Statistics Through Applications Solutions to ExercisesUniversity of Leeds School of Mathematics Semester 2 2009Solution to Question 1 (a) The mean, median and quartiles are produced using the summary command: summary(midsize) Min. 1st Qu
W. Alabama - ME - 353
RADCONDWEB.TEXME 353 M.M. YovanovichRadiative ConductanceThe radiative conductance is de ned asQ hrad = A T 12 T 1 1, 2The radiative exchange between two isothermal gray surfaces is obtained from 1 Q12 = EbR, Eb2 total where Eb1 = T14, Eb2 =
East Los Angeles College - MATH - 1825
MATH1825: Lecture 4Power and sample size for the one sample t-test1How large a sample is needed? Size of sample affects: ability to detect an effect if it is present; cost of obtaining the information. We seek the smallest sample that will a
W. Alabama - ME - 353
UNIVERSITY OF WATERLOO DEPARTMENT OF MECHANICAL ENGINEERING ME 353 HEAT TRANSFER 1 October 26, 1990 M.M. YovanovichTime: 7-9 p.m.Two-hour Closed Book Mid-term Examination. You are allowed one crib sheet both sides and the solutions to partial di
W. Alabama - ME - 353
POISSONWEB.TEXME 353 M.M. YovanovichGeneral Solution of Poisson Equation for Plane Wall, Long Solid Circular Cylinder and Solid SphereThe general Poisson equation r2T = ,P =k with appropriate boundary conditions, and the general solution which
W. Alabama - ME - 353
DEPARTMENT OF MECHANICAL ENGINEERING ME 353 HEAT TRANSFER 1UNIVERSITY OF WATERLOODecember 8, 1997 M.M. YovanovichTime: 2-5 P.M.Three-hour Closed Book Final Examination. Two crib sheets both sides are permitted. Calculator is allowed. All ques
East Los Angeles College - MATH - 1825
MATH1825: Lecture 6One sample non parametric tests1Making decisions What are the key issues in hypothesis testing? the population and its properties; the hypotheses being tested; the sample properties (e.g. size); the test assumptions.2
W. Alabama - ECE - 309
UNIVERSITY OF WATERLOO DEPARTMENT OF ELECTRICAL ENGINEERING ECE 309 Thermodynamics and Heat Transfer for Electrical Engineering Mid-Term Examination M.M. Yovanovich NOTE:1. Open book examination. You are permitted to use your calculator, the text bo
East Los Angeles College - MATH - 3802
MATH3802 Time Series Background 1 (introduction & time series regression)University of Leeds School of Mathematics Semester 2 2009Types of time series Figure 1 shows that lynx numbers in years close together are similar.Lynx trapped0 182030
W. Alabama - ECE - 309
CONTWEB.TEXECE 309 M.M. YovanovichThermal Interface Joint Conductance and ResistanceDe nitionsThermal interface resistance occurs whenever two solids of di erent materials are brought together to form an interface. When there is steady heat tra
East Los Angeles College - MATH - 1825
MATH1825: Lecture 5Power and sample size for the two sample t-test1Two sample problems Suppose that we have two samples of data and we are interested in comparing their averages to see if there is a large difference between them. If the sample
W. Alabama - ME - 303
Laplace Transform M.M. YovanovichLAPLACE TRANSFORMThe Laplace transform of f x; t is de ned asL ff x; tg =and its inverse is de ned asZ01 ,st e f x; tdt = F x; ss 0L,1 fF x; sg =1 2iZ c+i1c,i1F x; sest ds = f x; tSummary of L
W. Alabama - ME - 303
WK1TPCSWEB.TEXME 303 M.M. Yovanovich Week 1 Lecture 1Information: Instructor: M.M. Yovanovich, CPH 3375C X3588, E3-2133A, X6181 or X4586 email: mmyov@mhtl.uwaterloo.ca Teaching Assistants: Rabih Alkhatib, CIM 2705, X3639; email: rfalkhat@engmail.u
W. Alabama - ME - 303
PROJ1S99SOL.TEXUNIVERSITY OF WATERLOO Department of Mechanical Engineering ME 303 Advanced Engineering Mathematics M.M. Yovanovich Project 1 Solution, June 4, 1999Given the linear, second order nonhomogeneous PDE: ! 1 @ r @T + S = 1 @T ; t 0; 0 r
W. Alabama - ME - 303
WK6TPCSWEB.TEXME 303 M.M. YovanovichWeek 6Lecture 1Midterm week. Lecture cancelled.Lecture 2Midterm week. Lecture cancelled.Lecture 3Midterm week. Lecture cancelled.
W. Alabama - ME - 303
WK13TPCSWEB.TEXME 303 M.M. YovanovichWeek 13Lecture 1Sturm-Liouville Problem. This material is usually covered in an ODE Course. See Spiegel's Text, Chapter 8, Section 2 See ME 303 Web site for Note on Sturm-Liouville Problem This proves the
W. Alabama - ME - 303
WK5TPCSWEB.TEXME 303 M.M. YovanovichWeek 5Lecture 1Sturm-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 Equ
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
WK7TPCSWEB.TEXME 303 M.M. YovanovichWeek 7Lecture 1Return Project 1 Return Midterm Exam Exam and its solution are posted on Web site Examination Statistics Table 1: Midterm Exam Summary Q1 Q2 Q3 Exam Max. 30 40 30 98 Min. 8 8 10 46 Avg. 24.5
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
Neumont - IFT - 3820
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
WK3TPCSWEB.TEXME 303 M.M. YovanovichWeek 3Lecture 1Vibrating String and Membranes Rectangular and Circular. The 1-D wave equation for the string in cartesian coordinates is uxx = c12 utt; t 0; 0 x L It can be modi ed to include vibrations of
W. Alabama - ME - 303
ME 303 Advanced Engineering MathematicsSYMBOLIC MATHEMATICSSymbolic mathematics software packages have been developed over the past 25 years. The best known packages are MACSYMA, MAPLE, MATHEMATICA, MATHCAD, MATHSCRIBE, MuMATH,and DERIVE, REDUCE, S
W. Alabama - ME - 303
LPTTABLE.TEXME 303 Advanced Engineering MathematicsTable of Laplace Transforms Some inverse Laplace transforms for solutions of the one-dimensional di usion equation.F sp e,a s ;f t a01 e,aps; a 0 s 1 ps e,apspa 3 exp, at 4 2 t ! a er
Allan Hancock College - COMP - 3101
Objective of Subject COMP3101 Digital System Design IDr Adam Postula 47-313 Dr Mark Schulz 47-309 adam@itee.uq.edu.au marks@itee.uq.edu.au You will be able to design a small digital system for to the specified functionality . You will be able to use
W. Alabama - ME - 303
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
W. Alabama - ME - 303
STURMLIOUVILLEPROB.TEXSTURM-LIOUVILLE PROBLEM SLPThe separation of variables method when applied to second-order linear homogeneous PDEs frequently leads to second-order homogeneous ODEs of the type:d px dyx + qx + rx yx = 0; dx dx or in the equ
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
W. Alabama - ME - 303
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
W. Alabama - ME - 303
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
W. Alabama - ECE - 309
LUMPWEB.TEXECE 309 M.M. YovanovichLumped Capacitance Model With Ohmic HeatingLumped capacitance model valid for Bi 0:2 for a system long constant cross-section wire which has uniformly distributed heat sources due to ohmic heating, and convectiv
W. Alabama - ECE - 309
30996FESOL.TEXUNIVERSITY OF WATERLOODEPARTMENT OF ELECTRICAL ENGINEERING ECE 309 Thermodynamics Electrical EngineeringFinal Examination Solutions M.M. Yovanovich Problem 1Spring 1996 August 8, 1996 2:00 - 5:00 P.M.Incompressible liquid. 1a a
W. Alabama - ECE - 309
RADEXCHGWEB.TEXECE 309 M.M. YovanovichRadiation Exchange Between Black and Gray SurfacesWhen radiation leaves a black convex surface whose area is A1 at absolute temperature T1, a certain fraction F12 will be absorbed by a second convex surface
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
W. Alabama - ECE - 309
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
W. Alabama - ECE - 309
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
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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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REVIRR WEB.TEXECE 309 M.M. YovanovichReversible and Irreversible ProcessesReversible ProcessesThe following processes are frequently idealized as reversible processes. Restrained compression and expansion Frictionless motion Elastic extension
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PROCESWEB.TEXECE 309 M.M. YovanovichTypes of ProcessesA xed mass simple compressible substance system can undergo di erent types of processes between state 1 and state 2: Some types are given below:Isothermal process - constant temperature = I