COMPUTATIONAL HEAT
TRANSFER AND FLUID FLOW TRANSFER AND FLUID FLOW
PRADIP DUTTA
DEPARTMENT OF MECHANICAL ENGINEERING DEPARTMENT OF MECHANICAL ENGINEERING
INDIAN INSTITUTE OF SCIENCE BANGALORE
Outline Outline
B i f H t T f
Basics of Heat Transfer
M h i l d i i f fl id fl d h
Mathematical description of fluid flow and heat transfer: conservation equations for mass, momentum energy and chemical species momentum, energy and chemical species, classification of partial differential equations generalized control volume approach in Eulerian
g pp
frame
HEAT TRANSFER HEAT TRANSFER
BASICS
What is Heat Transfer?
What is Heat Transfer?
“Energy in transit due to temperature difference.”gy p Thermodynamics tells us:
How much heat is transferred (Q)
H h k i d (W)
How much work is done (W)
Final state of the system Heat transfereat t ansfe tells us:te s us:
How (by which mechanism) Q is transferred
At what rate Q is transferred
Temperature distribution within the body
Heat transfer complementary Thermodynamics Heat transfer complementary Thermodynamics
MODES MODES
Conduction
- needs matter
- molecular phenomenon (diffusion process) i h b lk i
- without bulk motion of matter
Convection
heat carried away by bulk motion of fluid - heat carried away by bulk motion of fluid - needs fluid matter
Radiation d o
- does not need matter
- transmission of energy by electromagnetic waves
APPLICATIONS OF HEAT TRANSFER
Energy production and conversion
Energy production and conversion
- steam power plant, solar energy conversion etc.
Refrigeration and air-conditioning
D ti li ti
Domestic applications - ovens, stoves, toaster
Cooling of electronic equipment
Manufacturing / materials processing
- welding, casting, forming, heat treatment, laser machining
Automobiles / aircraft design
Automobiles / aircraft design
Nature (weather, climate etc)
(Needs medium, Temperature gradient)
T >T T
.. . .
T
2T
1T
1>T
2. . . . . .
. . . . . . . . . . . . . . . . . . .
q’’
. . . . . . . . .
. . . .. . . . . . . . .
q
. . . . .
solid or stationary fluid
………….. . ..
RATE:
. . . . . . .
solid or stationary fluid
RATE:
q(W) or (J/s) (heat flow per unit time)
Conduction (contd ) (contd…)
x Rate equations (1D conduction):
T1
T
A Differential Form
q = - k A dT/dx, W
k = Thermal Conductivity W/mK
q T2 k = Thermal Conductivity, W/mK
A = Cross-sectional Area, m2 T = Temperature, K or oC
k x = Heat flow path, m
Difference Form
q = - k A (T2 – T1) / (x2 – x1) q k A (T2 T1) / (x2 x1) Heat flux: q” = q / A = - kdT/dx (W/m2)
(negative sign denotes heat transfer in the direction of decreasing temperature)
moving fluid T
s>T
∞moving fluid
T
∞q” T
ss Energy transferred by diffusion + bulk motion of fluid
Rate equation (convection)
y U
q” y T
T(y) U
u(y)
Heat transfer rate q = hA( T T ) W
q T(y)
T
su(y)
Heat transfer rate q = hA( Ts-T ) W Heat flux q” = h( Ts-T ) W / m2
h=heat transfer co-efficient (W /m2K)
not a fluid property alone, but also depends on flow p p y , p geometry, nature of flow (laminar/turbulent),
thermodynamics properties etc.
Convection (contd…)
Free or natural
convection (induced by
buoyancy forces) May occur with phase change (boiling,
Forced convection (induced by external
(boiling,
condensation) (induced by external
means)
Convection (contd…) ( )
Typical values of h (W/myp ( 2K))
Free convection gases: 2 - 25
liquid: 50 - 100 Forced convection gases: 25 - 250
liquid: 50 - 20,000q , Boiling/Condensation 2500 -100,000
T
1q
1”
T
2q
2”
RATE:
q(W) or (J/s) Heat flow per unit time q(W) or (J/s) Heat flow per unit time.
Flux : q” (W/m2)
Rate equations (Radiation)
RADIATION:
Heat Transfer by electro-magnetic waves or photons( no medium required. )
Emissive power of a surface (energy released per unit area):
Emissive power of a surface (energy released per unit area):
E=T
s4(W/ m
2)
= emissivity (property)……..
=Stefan Boltzmann constant
=Stefan-Boltzmann constant
Rate equations (Contd )
(Contd….)
q” d ”
Ts u r
q”co n v.
q r a d.
Area = A
T Area = A
Ts
R di ti h b t l f d
Radiation exchange between a large surface and surrounding
Q” = (T 4 T 4) W/ m2 Q r a d = (Ts4-Tsur4) W/ m2
Substantial derivative Substantial derivative
x
1, x
2, x
3, t
d dx d
dx d
dx
D
1 2 3
dt x
dt x
dt x
t
Dt
1
2
3dx D
dt dx x
t Dt
D i
i
D
local ti l
substantia
i
i x
t u Dt
D
component convective component
oca derivative
substa t a
Conservation principle(s) Conservation principle(s)
• mass is conserved
• momentum is conserved
• energy is conserved gy
• chemical species are conserved
•• …
x
1, x
2, x
3, t
D D D
V
dV
source V
V V
change
dV Dt dV
dV D Dt
D Dt
D
Conservation principle p p
for an elementary volume
dV
:: dV dV
Dt
D
dV
Dt D Dt
dV D Dt dV
D
Dt Dt
Dt
dV
Dt dV D Dt
dV D
dV Dt
u dV D i
x dVDt i
i
Conservation principle
D u
D dV x
u Dt
dV D Dt
D
i i
x dV u u x
t
ii i
i
dV
i
i
u dV
x
t
i i
Conservation principle Conservation principle
for an elementary volume
dV
:: D
i i
x u Dt
D
i d f fi l l V
u
iV
i i
x u t
integrated for a final volume V
bounded by a surface
A
::u
in
idA
dV V A
A
V V
i V i
dV x u
t dV Dt dV
D
called as “Reynolds
Transport Equation
V
V A
i
iu dA dV
n
t dV
(RTE)” - a relation
between a system and control volume.
Conservation of mass Conservation of mass
Total mass remains constant. For a control volume,
the balance of mass flux gives the mass accumulation rate the balance of mass flux gives the mass accumulation rate.
dV 0
D dV 0
Dt
set :
-
density, then
-
mass
V
dV
-
0
no source
Conservation of mass Conservation of mass
continuity equation
for an elementary volume
dV
:: V
i t t d f fi l l
V
b d d bu
in
idA
dV V A
ii
x u
t
integrated for a final volume
V
bounded by a surfaceA
::n
iA
dA u
n t dV
V A
i
i Here (ni ui ) is a scalar quantity:-for outward flow (away from the surface)- positive
V -for inward flow- negative
Incompressible flow Incompressible flow
for an incompressible fluid:
=const
:f p f
written for an elementary volume
dV
::
V
0
i i
x u
or a final volume
V
bounded by a surfaceA
::u
in
idA
dV V A A
0
A
i
i
u dA
n
A
Conservation of momentum Conservation of momentum
Rate of change of momentum will cause fluid acceleration.
For a control volume we consider the balance of momentum fluxes For a control volume, we consider the balance of momentum fluxes.
dVuj
FjDt
D
j
j F
dV Du
j
jDt
th l it
d it
u
force j on
accelerati
mass Dt
set :
momentum
then velocity,
density
- -
j j
dV u
u
e unit volum per
force
-
j V
F
Conservation of momentum Conservation of momentum
momentum equation
for an elementary volume
dV
:
j i
ji
j u u F
u x
t
i ij j
i j i
j u u f x
u x
t
d
p ij
i
j x
x
Conservation of momentum
V u
idV V
integrated for a final volume
V
bounded by a surface
A
::u
in
idA
dV
A
momentum change outletconvectioninlet
( . )
d A
i i j
V
j
dA dA
dV f
dA u
n u
dV
t
u
body forces spherical stress deformation stress
A
i d ij A
j V
jdV pn dA n dA
f
Stress - strain relationship p
xx
22 u1 u1
x2
21xx
22xx
11p d
x dV x
dV p dF x
i ij i
ij i
ij
j
3 3 2
2 3
2 0 0
u
x u x
u u u
1 1 u u u
21 1
1
1 0 u u x
x
u
2 1 2
1 1
2
12 2
1 2
1
x u x
u x
u
Stress-strain relationship Stress strain relationship
for Newtonian fluids :
1
2
u
generalized :
12 2
1
12
2
x
d ij d
ij
2
deformation stress = = 2 X viscosity X deformation strain rate
d ij kk
ij
ij
3 1
j j
j 3
j i k
d u u u
1 2 1
k k ij
j i i
d j
ij x x x
2 2 3
Navier-Stokes equations Navier Stokes equations
p d
i ij j
j i
j i
j x x
f p u
x u
t u
i j i
i d ij
x u x
x
k k ij
i j
i
i x
u x
x u
x
3 2
du 1 u
i i j
i j i
i ij
x u x
x u x
x
3
1
Navier-Stokes equations Navier Stokes equations
j i j i
j
u u p
u x u
t u
1
i i j
i j i
j
j
x
u x
x u x
x
f p
3
1
for an incompressible fluid
=const
with a constant viscosity
=const
with a constant viscosity
const
1 2 jj p u
f u
u u
2i j
j i
j
i u u f x x
x
t
Surface force decomposition Surface force decomposition
p dV dV
dF
d ij
ij
x dV dV x
dF x
i i
ij i
j
since:
j i
ij
x
p x
p
the total stress Fj can be separated into the spherical and deformation components:
dV p dV
dF
d ij
j
x
xj i
j
Work decomposition Work decomposition
dx dx
33
dV dV
dx dx
22u
u
22 11 2
2 dx
x u u
12 dx
dx dx
11xx
11xx
22
12 12 x1 dx1total work done on an elementary volume:
dx dx
11xx
11xx
33total work done on an elementary volume:
12 1 2 3 2 2 1
12 dx
x u u
dx dx x dx
2 3 2 12
1 1
u dx dx
x x
Work decomposition Work decomposition
u
dVdx x dx x dx
u
u x 2 12
1 3
2 1 1
2 12
1 12
2
generalized total work done on an elementary volume can be separated generalized - total work done on an elementary volume can be separated into the kinetic and deformation components:
ij ij
j j ij
j
i
x
F u u
x u
work n deformatio work
kinetic work
total
Conservation of mechanical energy
"change of kinetic energy is a result of work d b t l f "
start with the momentum equation :
done by external forces"
dVuj
FjDt
D
ujDt
ij j
ju f dV dV u
dV u
D
kinetic energy change work by external forces
2 i j
j j
j
j dV u
dV x f
Dt dV
Conservation of thermal (or internal) energy ( ) gy
Net heat flux entering a control volume results in rate of change of internal energy
of change of internal energy
dV q
i ij ijDt
D
q
idV V
j j
x
iDt
k T
n
idA
dV
i
A
i
k x
q
i
j ij i
i x
u x
k T dV x
Dt D
sfer heat tran
n work deformatio
sfer heat tran
conduction change
energy
internal
Conservation of thermal energy
set :
e temperatur heat
specific
-
cT
gy
energy
internal
-
V
T u dV cT
fer heat trans
-
i j ij
i
i x
u x
k T
x
thermal energy equation for an elementary volume
dV
:
i
i
T x cTu
t cT
i j ij
i
i x
u x
k T
x
Conservation of thermal energy
integrated for a final volume
V u
idV V
gy
bounded by a surface
A
: in
idA
dV
A
energy change internalinlet energy outletconvectioninternal
dA u
cTn dV
cT
A i iV
T u
dA u
cTn dV
t cT
d ti d f i k
V i
j ij
A
i i
x dV dA u
x n
k T
sfer heat tran
n work deformatio
sfer heat tran
conduction
Conservation of chemical species
Net species mass transfer across the control volume faces + chemical reaction within the control volume results in a change of concentration of chemicalg f f Species in the control volume
ms dV
qis RsD
q
isdV V
i
x R dV
Dt m
s
n
idA
dV
A
i s s
s
i x
q m
D
chemical to
due
k source/sin
s i
s s
i
s R
x m dV x
Dt m
D
D
reaction chemical to
due transfer
mass
diffusion change
ion
concentrat
Conservation of chemical species
set :
ion concentrat
mass
pecies
-
ms s
mass
species -
s V
s dV
m
reaction
chemical
and diffusion
s -
i s s
i
x R m
x
D
mass transfer equation for an elementary volume
for an elementary volume
dV
:
i
s i
s m u
m x t
s i
s s
i
x R m
x
D
Conservation of chemical species
integrated for a final volume
V q
isdV V
bounded by a surface
A
:n
idA
A
ti i
concentration change speciesinlet convectionoutlet
species
A
i i s V
s dV m n u dA
t m
V s A
i i
s s
A V
dV R
dA x n
m t
D
reaction chemical
to due k source/sin transfer
mass
diffusion
species
V
A i
Class of Linear Second-order PDEs
• Linear second order PDEs are of the form
• Linear second-order PDEs are of the form
h A H f ti f d l
H Gu
Fu Eu
Cu Bu
Au
xx 2
xy
yy
x
y
where A - H are functions of x and y only
• Elliptic PDEs: B
2- AC < 0
( d h i i h h )
(steady state heat equations without heat source)
• Parabolic PDEs: B
2- AC = 0
(t i t h t t f ti )
(transient heat transfer equations)
• Hyperbolic PDEs: B
2- AC > 0
(wave equations) (wave equations)
MODULE 1: Review Questions
• What is the driving force for (a) heat transfer (b) electric current flow and (c) fluid flow?
Whi h f th f ll i i t t i l t ?
• Which one of the following is not a material property?
(a) thermal conductivity (b) heat transfer coefficient (c)emissivity
• What is the order of magnitude of thermal conductivity for (a) metals (b) solid insulating materials (c) liquids (d) gases?
• What are the orders of magnitude for free convection heat transfer coefficient, forced convection and boiling?
• Under what circumstances can one expect radiation heat transfer to be significant?
• An ideal gas is heated from 40ºC to 60ºC (a) at constant volume andg ( ) (b) at constant pressure. For which case do you think the energy required will be greater? Explain why?
• A person claims that heat cannot be transferred in a vacuum. Evaluatep this claim.
MODULE 1: Review Questions (contd )
(contd...)
• In which of the three states (solid/liquid/gas) of a matter, conduction heat transfer is high/low? Explain your claim
heat transfer is high/low? Explain your claim.
• Name some good and some poor conductors of heat.
• Show that heat flow lines and isotherms in conduction heat transfer are
l t h th Will thi diti h ld f ti h t
normal to each other. Will this condition hold for convection heat transfer?
• Distinguish between Eulerian and Lagrangian approach in fluid
h i Wh i th E l i h ll d?
mechanics. Why is the Eulerian approach normally used?
• Derive the Reynolds transport equation.
• Derive the continuity (mass conservation) equation in differential form for incompressible flow.
• Define substantial derivative. What is the physical significance of the substantial derivative in an Eulerian framework?