ME 345 Heat Transfer Lecture 14 Lecture Outline: 1) Steady 2-d conduction 2) Analytical solutions 3) Approximate graphical solutions Steady Two-dimensional Conduction You now have T(x,y)! The T (k ) term is back in the equation! The steady 2-d energy equation is: y y T T (k ) (k ) q 0 x x y y IF: q 0 and k = constant, then this becomes: 2T x 2 2T y 2 0 which is also written as 2 T 0 (this is just notation!) How many boundary conditions do we need to fully solve this differential equation? EXAMPLE: a “fat” fin… T=20C Tb=80C There are three basic solution techniques: I. Analytical: (you usually aren’t this lucky…) these you can just look up in books II. Approximate graphical Techniques: use of this depends on the geometry of the situation, is particularly useful for first guesses III. Numerical: the usual way in real problems, especially as computers improve. Analytical: The most commonly used technique is separation of variables. In the text they show you one example… y T2 2T W T(x,y) T1 L T1 x 2 T1 2T y 2 0 x TWO things to note: 1) You have all four boundary conditions, and 2) To solve, they NONDIMENSIONALIZE and NORMALIZE the temperature: i.e. they change the equation variables to something with NO units, AND so that all of the values of are between 0 and 1! T T1 T2 T1 One of the advantages of this is that if you get a value of that is not 0-1, then you know you have done something wrong! The solution for (x,y) is given in Equation 4.19: p. 189: ( x, y) 2 ny ) ( 1) n 1 1 nx sinh( L sin n W n L sinh( n 1 L) the results are also shown graphically in Figure 4.3 on p. 189. NOTE: this solution is only good for this particular problem, with this particular boundary conditions! Other solutions have been done, and are given in various references, but are not useful very often. We will go on to other more useful techniques. Approximate Graphical Techniques: These are useful only for the case of steady state with NO internal generation, and constant k! They are also most useful for cases in which the boundaries are adiabatic or isothermal. FLUX PLOT: a graph showing the direction of travel of q” and the corresponding isotherms. Example: 1-d heat transfer in a wall The horizontal dotted lines are ADIABATICheat DOES NOT flow over them!!!! 70C 20C The vertical solid lines are ISOTHERMSheat flows PERPENDICULAR to them!!!! It is very important to note: isotherms are normal (perpendicular) to heat flow lines and adiabats!!! BASIC TECHNIQUE FOR CONSTRUCTING A FLUX PLOT: 1) Draw the picture and identify if the heat transfer is 1-d or 2-d 2) Identify any physical symmetry: lines of symmetry are adiabatic heat flow lines! 3) Note that isothermal boundaries are normal to the flow of q” 4) Try to draw lines in each direction so that the area consists of “squares” (or at least as close as you can get.) If you do this correctly, the same amount of heat will be flowing in each “lane”. Then all you have to do is add them up. M q q i Mq i where M = number of heat flow lanes Eq. 1 i 1 Tj q i kA i and x is the length of one square, is the depth “into”: the paper, and Tj is the T across one square. x k( y ) Tj where x Also note that T should be equal for each set of squares!!! N This means that the total T T j NT j Eq. 2 j1 Where N = the number of temperature increments Combine eqs. 1 and 2 to get the total q, using the fact that since you have “squares”, x = y and that Tj = T/N then q Mk ( y ) T M q kT x N N CONDUCTION SHAPE FACTOR: This means that: q = S k T where S = M /N S is known as the “shape factor” People have already done the work on this for common geometries. To use the tables in the book, you must be able to assume: 1) steady-state 2) 2-d 3) q 0 , and 4) k = constant. Let’s try some examples (and be sure to go over Example 4.1, pp. 194-196.) Group exercises: 1) Find q for the following shape: let = 1. T=0 Adiabatic T = 100 Adiabatic HINT: It is often helpful to think first about HOW the heat will move (from hot-to-cold) and use that to draw your “heat flow lanes” 2) Find q for the following shape: T = 0 on the inside surface (the circle). The other conditions are as given . Adiabatic T = 100 T = 100 T = 100