Wilson Braz MANE 6630 September 30, 2009 Homework 2 One Dimensional Steady State Heat Conduction 1 Consider a steady state heat conduction through the homogeneous, isotropic wall of a hollow cylindrical shell of thermal conductivity k with internal heat generation inside the wall. Use a differential volume element of radial thickness r, unit length and circumference 2 to obtain the steady state heat equation by performing a differential thermal energy balance on the volume element. For a homogeneous isotropic solid in the steady state condition, k is constant and the general form of the heat equation is: q 2T 0 eq. 1 k In cylindrical coordinates, 2T is given by: 2T 1 T 1 2T 2T 2T 2 r r r 2 2 z 2 r Thus the equation becomes: 2T 1 T 1 2T 2T q 2 2 2 2 r r r r z k The above equation can be derived from inspection of a differential control volume. NOTE: q Heat transfer rate W; q ' ' Heat flux in W/m2; q Heat generation per unit volume W/m3 Given a differential control volume in cylindrical coordinate system ( r , , z ) The volume of the differential element is: 2 V r dr d dz r 2 d dz V r dr r 2 d dz 2 V r rdr dr r 2 d dz 2 2 V r dr dr d dz Developing the basic equation for conservation of energy: Ein E generated Eout Estored Where: Ein qr q q z Eout qr dr q d q z dz E generated q r dr dr d dz Estored c T r dr dr d dz t Substituting into the energy equation: qr q q z q r dr dr d dz qr dr q d q z dz c T r dr dr d dz t --------qr dr qr qr dr ; r q d q q d ; q z dz q z q z dz . z Substitute above equations to obtain: qr q qz q r dr dr d dz qr q qr q T dr q d qz z dz c r dr dr d dz r z t Simplify the above equation: q q q T q r dr dr d dz r dr d z dz c r dr dr d dz r z t Fourier’s Law: qr k r d dz q k dr dz T T EQ Fourier 1 ; r EQ Fourier 2; Tz q z k r dr d r 2 d 2 Tz q z k r 2 rdr dr 2 r 2 d q z k r dr dr d q z k r dr dr d T z T z EQ Fourier 3 Substitute Fourier’s equations into energy balance: q r dr dr d dz q r dr dr d dz q q qr q T dr d z dz c r dr dr d dz r z t T T T T k dr dz d k r dr dr d r dr dr d dz k r d dz dr dz c r r z z t k r T k T T T k c r r dr r r dr z z t Using the chain rule and taking lim dr0 of above equation: 1 T 1 T T T k k kr 2 q c r r r r z z t Since our cylinder is in steady state, T 0 , hence: t 1 T 1 T T k k kr q 0 r r r r 2 z z 2 Consider a steady state heat conduction through the homogeneous, isotropic wall of a hollow spherical shell of thermal conductivity k with internal heat generation inside the wall. Use a differential volume element of radial thickness r, and circumferences 2 in both axial and azimuthal directions to obtain the steady state heat equation by performing a differential thermal energy balance on the volume element. The general form of the heat equation is given as: kT q c T t In spherical coordinates: 1 2 T 1 T 1 T T k q c kr 2 k sin 2 2 2 r r r r sin r sin t 3 Consider the problem of properly insulating a metal pipe that carries a hot fluid inside. The pipe is insulated by covering its outside surface with a hollow shell of an insulating material. Assume convective heat transfer conditions apply both along the inner radius of the metal pipe and the outer radius of the insulation. Use the concept of overall thermal resistance to obtain the critical radius of insulation. Te he Tf hf Tf R1 T0 R2 T1 R3 T2 R4 Te The overall heat flow per unit length of a pipe is given to be: q T f Te , L Rt where Tf is the temperature of the fluid within the pipe, Te is the temperature of the fluid surrounding the system and Rt is the overall thermal resistance of the system. Rt can be written as: Rt 1 2 1 1 1 1 or, R1 R2 R3 R4 Rt 1 2 1 1 r 1 r 1 ln 2 ln 3 h r k r1 k 2 r2 he r3 1 f 1 To find the critical radius, we differentiate Rt with respect to r then set the result equal to zero to find the min/max: dRt 1 1 1 dr 2r k hr 0 1 1 1 1 r 2r k hr h k rcr k h 4 Consider the steady state heat conduction problem inside a homogeneous, isotropic cylindrical shell of wall thickness L = b − a, constant thermal conductivity, with internal heat generation and subjected to Dirichlet conditions: T (r = a) = Ta T (r = b) = Tb Write down the governing equation of the problem. Then, use the finite difference method to obtain a system of simultaneous linear algebraic equations that can produce an approximation to the solution. Solve the problem corresponding to the following data: a = 0.10, b = 0.11, Ta = Tb = 0, k = 20 W/mK, Qv = 103W. The heat equation for a 1-D cylindrical steady-state problem with internal heat generation reduces to: d 2T 1 dT q v 0 dr 2 r dr k The finite difference approximation can be written as: Tm1 2Tm Tm1 1 Tm1 Tm1 q v 0 rm 2r k r 2 This equation can be rearranged to solve for Tm: Tm1 2Tm Tm1 r Tm1 Tm1 qv 2rm k q r r Tm1 1 2 Tm v Tm1 1 2rm 2rm k We can modify the finite difference equation shown above slightly to allow for the solution to be found by using the Gauss-Seidel iterative scheme. q r r Tmi 11m1 1 2 Tmi 1 v Tmi 1 1 2rm 2rm k Where i denotes iteration number. Using a 6 node model; 1 2 3 4 5 6 using the B.C.’s given in the problem and setting initial temperature values of zero, Excel was used to obtain the temperature distribution: 1.200 1.000 iteration 0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 T1 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 0.000 T2 0.000 25.000 43.873 59.683 73.577 83.010 89.218 93.284 95.946 97.688 98.828 99.575 100.064 100.383 100.593 100.730 100.820 100.878 100.917 100.942 100.958 100.969 100.976 100.981 100.984 100.986 100.987 100.988 100.989 100.989 100.989 100.989 100.989 100.989 100.990 100.990 T3 0.000 37.380 68.692 96.211 114.894 127.188 135.241 140.513 143.964 146.223 147.702 148.670 149.303 149.718 149.989 150.167 150.283 150.359 150.409 150.442 150.463 150.477 150.486 150.492 150.496 150.499 150.500 150.502 150.502 150.503 150.503 150.503 150.503 150.504 150.504 150.504 T4 0.000 43.514 82.519 105.901 121.001 130.865 137.320 141.545 144.310 146.121 147.305 148.081 148.589 148.921 149.139 149.281 149.374 149.435 149.475 149.501 149.518 149.530 149.537 149.542 149.545 149.547 149.548 149.549 149.550 149.550 149.550 149.550 149.551 149.551 149.551 149.551 T5 0.000 46.555 65.878 77.460 84.940 89.827 93.024 95.117 96.487 97.384 97.971 98.355 98.606 98.771 98.879 98.949 98.996 99.026 99.046 99.058 99.067 99.073 99.076 99.079 99.080 99.081 99.082 99.082 99.082 99.083 99.083 99.083 99.083 99.083 99.083 99.083 T6 Max Delta Delta T1 0.000 0.000 46.5553 0.000 39.0055 0.000 27.5190 0.000 18.6838 0.000 12.2938 0.000 8.0533 0.000 5.2720 0.000 3.4509 0.000 2.2589 0.000 1.4786 0.000 0.9678 0.000 0.6335 0.000 0.4147 0.000 0.2714 0.000 0.1777 0.000 0.1163 0.000 0.0761 0.000 0.0498 0.000 0.0326 0.000 0.0213 0.000 0.0140 0.000 0.0091 0.000 0.0060 0.000 0.0039 0.000 0.0026 0.000 0.0017 0.000 0.0011 0.000 0.0007 0.000 0.0005 0.000 0.0003 0.000 0.0002 0.000 0.0001 0.000 0.0001 0.000 0.0001 0.000 0.0000 Delta T2 25.0000 18.8731 15.8094 13.8944 9.4335 6.2072 4.0661 2.6618 1.7424 1.1405 0.7465 0.4887 0.3199 0.2094 0.1370 0.0897 0.0587 0.0384 0.0252 0.0165 0.0108 0.0071 0.0046 0.0030 0.0020 0.0013 0.0008 0.0006 0.0004 0.0002 0.0002 0.0001 0.0001 0.0000 0.0000 Delta T3 37.3798 31.3118 27.5190 18.6838 12.2938 8.0533 5.2720 3.4509 2.2589 1.4786 0.9678 0.6335 0.4147 0.2714 0.1777 0.1163 0.0761 0.0498 0.0326 0.0213 0.0140 0.0091 0.0060 0.0039 0.0026 0.0017 0.0011 0.0007 0.0005 0.0003 0.0002 0.0001 0.0001 0.0001 0.0000 Delta T4 43.5136 39.0055 23.3819 15.0997 9.8642 6.4549 4.2250 2.7655 1.8102 1.1849 0.7756 0.5077 0.3323 0.2175 0.1424 0.0932 0.0610 0.0399 0.0261 0.0171 0.0112 0.0073 0.0048 0.0031 0.0021 0.0013 0.0009 0.0006 0.0004 0.0002 0.0002 0.0001 0.0001 0.0000 0.0000 Delta T5 Delta T6 46.5553 19.3222 11.5827 7.4800 4.8864 3.1976 2.0929 1.3700 0.8967 0.5870 0.3842 0.2515 0.1646 0.1078 0.0705 0.0462 0.0302 0.0198 0.0129 0.0085 0.0055 0.0036 0.0024 0.0016 0.0010 0.0007 0.0004 0.0003 0.0002 0.0001 0.0001 0.0001 0.0000 0.0000 0.0000 The above table shows that the Gauss-Seidel method converges to 1e-4 after 35 iterations. 5 Consider the steady state heat conduction problem inside a homogeneous, isotropic flat wall of thickness L = b − a, constant thermal conductivity, with internal heat generation and subjected to Dirichlet conditions T (r = a) = 0 T (r = b) = 0 Use the Galerkin finite element method to obtain a system of simultaneous linear algebraic equations that can produce an approximation to the solution. Solve the problem corresponding to the following data: a = 0.0, b = 1.0, Ta = Tb = 0, k = 1 W/mK, Qv = 20x3 W. The heat equation for a 1-D steady-state problem with internal heat generation reduces to: d 2T q v 0 dx 2 k Integrate the above equation twice to yield: q x 2 T x v C1 x C2 k 0.800 0.600 0.400 0.200 0.000 0.098 0.1 0.1 v b2 a q v a C 2 C1 ; C2 k ; k a b q 1 a q v q v b 2 a b2 a ; ; C1 a 2 C2 k a b a k ab a T x q v x 2 q v b 2 a q v b 2 a x a 2 k k k ab a a b a q v 2 b2 a b2 a x T x x a 2 k ab a a b a 6 Obtain an expression for the temperature distribution of a fin constant cross section A and perimeter P and of finite length L with base temperature Tb and heat transfer coefficient h all over its surface into an environment at T1. Performing an energy balance on the system shown in the above diagram yields: qx qx x qconv EQ. 1. As x 0 , qx x qx dq x and dx qconv hP x xT T EQ. 1 becomes: qx qx dq x hPx xT T dx 0 dq hP x T T EQ. 2. dx From Fourier’s Law: dT q x kA x where Ax is the cross sectional area. dx Substitute Fourier’s Law into EQ 2. d dT hPx T T 0 . Ax dx dx k If Ax const. then Px const. : A d 2T hP T T 0 or dx 2 k d 2T hP T T 0 dx 2 kA