Download presentation
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,
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
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.