CHAPTER 1 BASIC CONCEPTS 1.1 Convection Heat Transfer Examine thermal interaction between a surface and an adjacent moving fluid 1.2 Important Factors in Convection Heat q s T Transfer s Surface temperature is too high. How to reduce it? (1) Use a fan (2) Change the fluid (3) Increase surface area V T Fig . 1 .1 1 Conclusion: Three important factors in convection (1) fluid motion (2) fluid nature (3) surface geometryof the role of fluid motion in convection: Examples Fanning to feel cool Stirring a mixture of ice and water Blowing on the surface of coffee in a cup Orienting a car radiator to face air flow 1.3 Focal Point in Convection Heat Transfer Determination of temperature distribution in a moving fluid T T ( x, y, z, t ) (1.1) 2 1.3 Fourier’s Law of Conduction A (T T ) q L A (Tsi Tso ) qx k L si Ts Ts so i A x qx d (1.2) 0 k = thermal conductivity L x x Fig.1.2 Valid for: (1) steady state (2) constant k (3) one-dimensional conduction 3 Reformulate to relax restrictions. Consider element dx T ( x ) T ( x + dx ) T ( x + dx ) T ( x ) q =k A =k A dx dx dT (1.3) qx = k A dx qx Heat flux qx (1.4) q x A dT (1.5) q x k dx x Generalize (1.5): T q x k , x T q y k , y T q z k z (1.6) 4 (1) Why negative sign? (2) k constant (3) Find T(x,y,z,t), use (1.6) to obtain q (4) Changing fluid motion changes T(x,y,z,t) 1.5 Newton's Law of Cooling qs Ts T q s = surface flux Ts = surface temperature qs h(Ts T ) (1.7) 5 Eq. (1.7) is Newton's law of cooling h is called the heat transfer coefficient h f ( g m p , T ) e (1.8) 1.6 The Heat Transfer Coefficient h Is h a property? Does h depend on temperature distribution? Apply Fourier’s law T ( x ,0 , z ) qs k y T ( x ,0 , z ) y h k Ts T (1.9) Combine (1.7) and (1.9) (1.10) Temperature distribution in needed to determine h 6 Ts Apply Newton’s law to the bulb: q s Ts T h (1.11) Increase V to increase h and lower Ts qs V T Fig. 1.1 Table 1.1 Typical values of h h ( W/m 2 o C ) Process Free convection Gases 5-30 Liquids 20-1000 Forced convection Gases 20-300 Liquids 50-20,000 Liquid metals 5,000-50,000 Phase change 2,000-100,000 Boiling 5,000-100,000 Condensation 7 1.7 Differential Formulation of Basic Laws Three basic laws: conservation of mass, momentum, and energy y v u Formulation w Differential Integral Finite difference Key assumption: continuum x z F 1 i 1.8 Mathematical Background (a) Velocity Vector V V ui v j w k (1.12) 8 (b) Velocity Derivative V u v w i j k x x x x (1.13) (c) The Operator Cartesian: i j k x x x (1.14) Cylindrical: 1 ir i i z r r z (1.15) 1 1 Spherical: ir i i r r r sin (1.16) 9 (d) Divergence of a Vector u v w div .V V x y z (1.17) (e) Derivative of the Divergence u v w V x x x y z or or V u i v j w k x x V V x x (1.18) (1.19) 10 (f) Gradient of Scalar T T T Grad T T i j k x y z (1.22) (g) Total Differential and Total Derivative f = flow field dependent variable such as u, v, p, etc. Cartesian Coordinates: f f ( x, y, z, t ) (a) Total differential of f: f f f f df dx dy dz dt x y z t or df Df f dx f dy f dz f dt Dt x dt y dt z dt t (b) 11 But dx dy dz u, v, w dt dt dt (c) Substitute (c) into (b) df Df f f f f u v w dt Dt x y z t Total derivative: df Df dt Dt Convective derivative: f f f u v w x y z Local derivative: f t (1.21) (d) (e) 12 Apply to velocity component u. Set f u du Du u u u u u v w dt Dt x y z t (1.22) (1.22) represents u u u convective acceleration in the x-direction u v w x y z (f) u local acceleration t (g) Cylindrical coordinates : r , , z dv r Dv r v r v θ v θ v θ2 v r v r vr vz dt Dt r r θ r z t (1.23a) 13 dv θ Dv θ dt Dt v θ v θ v θ v r v θ v θ v θ vr vz r r θ r z t dv z Dv z v z v θ v z v z v z vr vz dt Dt r r θ z t (1.23b) (1.23c) Total derivative of temperature: set f = T in (1.21) dT DT T T T T u v w dt Dt x y z t (1.24) 14 1.9 Problem Solving Format Solve problems in stages: (1) Observations (2) Problem Definition (3) Solution Plan (4) Plan Execution (i) Assumptions (ii) Analysis (iii) Computations (iv) Checking (5) Comments 15 1.10 Units SI units Length (L): meter (m) Time (t): second (s) Mass (m): kilogram (kg) Temperature (T): kelvin (K) Celsius and kelvin scales T(oC) = T(K) - 273.15 (1.25) Derived units: Force: newton (N) One newton = force to accelerate one kilogram one meter per sec per sec: Force = mass acceleration N = kg . m /s2 16 Energy: joules (J) One joule = energy due to a force of one newton moving a distance of one meter J = N. m = kg . m2 /s2 Power: watts (W) One watt = one joule per second W = J/s = N. m/s = kg . m2 /s3 17 Example 1.1: Heat Loss from Identical Triangles Surface temperature: Ts Variable h: C h( x ) x q1 Determine: q2 (1) Observations Newton’s law givesq h varies with x Integration is required (2) Problem Definition. Determine dq for dx of each triangle 18 (3) Solution Plan. Apply Newton's law to element and integrate (4) Plan Execution (i) Assumptions steady state one dimensional uniform T uniform Ts negligible radiation (ii) Analysis Apply Newton’s law dq h( x )(Ts T )dA (a) C h= x (b) 19 Triangle 1: dA1 y1 ( x )dx (c) Triangle 2: dA2 y 2 ( x )dx (d) Geometry: H y1 ( x ) ( L x ) L H y2 ( x) x L (e) (f) (e) into (c), (f) into (d): H dA1 ( L x )dx L (g) H dA2 xdx L (h) (b) and (g) into (a), integrate 20 H L x q1 dq1 C (Ts T ) dx 1 / 2 0 L x L q1 ( 4 / 3 )C (T T ) HL1 / 2 s Similarly (i) H x q2 dq2 C (T T ) dx 1 / 2 0 L x L s q 2 ( 2 / 3 )C (T T ) HL1 / 2 s Ratio of (i) and (j) q1 2 q2 (j) (k) (iii) Checking Dimensional check: (b) gives units of C: C = W/m 3/2 o C 21 (i) gives units of q1 q1 = C(W/m3/2-oC)( Ts - T )(oC)H(m)L1/2 (m1/2) = W Qualitative check: q1 q2 because base of 1 is at x = 0 where h . (5) Comments Orientation is important. Same area triangles but different q Use same approach for other geometries 22