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INTRODUCTION TO CONVECTION

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Presentation on theme: "INTRODUCTION TO CONVECTION"— Presentation transcript:

1 INTRODUCTION TO CONVECTION
Convection Heat Transfer Coefficient Conservation Equations Boundary Layer Approximation Reynolds Analogy Turbulent Flow

2 Forced Convection Free Convection Boiling and Condensation External flows Internal flows Laminar flows Turbulent flows

3 Convection Heat Transfer Coefficient
y T(x,y) y x Ts

4 y T(x,y) y x Ts total heat transfer rate over As If Ts = constant, average heat transfer coefficient:

5 Convection Boundary Layer
Velocity (or momentum) boundary layer wall shear stress: m: dynamic viscosity friction coefficient:

6 Temperature (or thermal) boundary layer
local heat flux: local heat transfer coefficient:

7 Laminar and Turbulent Flows
Viscous sublayer

8 laminar: molecular diffusion
turbulent: eddy motion (fluctuation) Critical Reynolds number external flow: internal flow:

9 Comparison of laminar and turbulent velocity profile in the boundary layer

10 Variation of heat transfer coefficient

11 Conservation Equations Continuity Equation: Mass Conservation
incompressible flow 2-dimensional flow

12 Newton’s 2nd law of motion
Momentum Equations Newton’s 2nd law of motion f : force per unit volume force: body force, surface force body force: gravitational force, centrifugal force, electromagnetic force surface force: viscous force, pressure force

13 incompressible flow with constant viscosity
2-dimensional steady flow

14 1st law of thermodynamics
Energy Equation 1st law of thermodynamics rate change of internal energy = heat transferred in the system + work done on the system by forces + internal heat generation internal energy: thermal energy, kinetic energy heat transfer: conduction, radiation work: work done by body force and surface force

15 energy per unit mass of fluid
thermal energy: e kinetic energy: total energy: Total energy equation

16 Mechanical energy equation
Thermal energy equation : viscous dissipation

17 Thermal Energy Equation
thermal energy equation for enthalpy When it is assumed that (ideal gas) and

18 When pressure work and viscous dissipation are negligible, and internal heat generation is not present, When the fluid is transparent to radiation and its thermal conductivity is constant, steady-state:

19 For a 2-dimensional flow

20 Summary 2-dimensional, steady, incompressible, constant property, transparent to radiation, no internal heat generation

21 Boundary Layer Approximation
2-D Boundary Layer Flow dt(x) T(x,y) y d(x) u(x,y) x Ts L d(x): thickness of velocity boundary layer dt(x): thickness of temperature boundary layer

22 dt(x) y d(x) x u(x,y) Ts T(x,y) L scaling from continuity pressure temperature

23 dimensionless variables
continuity

24 momentum equation in the streamwise direction
for a high Reynolds number flow:

25 momentum equation in the wall-normal direction
→ p = p(x) in the boundary layer

26 flow over a flat plate:

27 energy equation Pr: Prandtl number

28 Summary: 2-D Boundary layer equations
continuity: momentum: energy: Boundary layer approximation Parabolic in the streamwise direction Pressure is constant across the boundary layer.

29 Fundamental Form of Solutions

30 Friction coefficient

31 Convection heat transfer coefficient
Nusselt number local Nusselt number average Nusselt number

32 Reynolds Analogy When and Pr = 1, that is, n = a

33 Let boundary conditions Thus,

34

35

36 Stanton number When Pr = 1, Modified Reynolds analogy or Chilton-Colburn analogy

37 Example 6.5 air coolant channel original conditions Find: 1) heat flux to the blade if the surface temperature is reduced to 700°C 2) heat flux at the same dimensionless location for a similar blade having a chord length of L = 80 mm when T∞ = 1150°C, V = 80 m/s, and Ts = 800°C

38 1) air x*, ReL, Pr are independent on Ts. L and k are also unchanged. Thus, h = h1 original conditions air Case 1

39 2) air x*, Pr are also unchanged. Local Nusselt number remains the same. original conditions air Case 2


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