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Chapter 2: Heat Conduction
Equation
Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
Objectives
When you finish studying this chapter, you should be able to:
• Understand multidimensionality and time dependence of heat transfer,
and the conditions under which a heat transfer problem can be
approximated as being one-dimensional,
• Obtain the differential equation of heat conduction in various
coordinate systems, and simplify it for steady one-dimensional case,
• Identify the thermal conditions on surfaces, and express them
mathematically as boundary and initial conditions,
• Solve one-dimensional heat conduction problems and obtain the
temperature distributions within a medium and the heat flux,
• Analyze one-dimensional heat conduction in solids that involve heat
generation, and
• Evaluate heat conduction in solids with temperature-dependent
thermal conductivity.
Introduction
• Although heat transfer and temperature are
closely related, they are of a different nature.
• Temperature has only magnitude
it is a scalar quantity.
• Heat transfer has direction as well as magnitude
it is a vector quantity.
• We work with a coordinate system and indicate
direction with plus or minus signs.
Introduction ─ Continue
• The driving force for any form of heat transfer is the
temperature difference.
• The larger the temperature difference, the larger the
rate of heat transfer.
• Three prime coordinate systems:
– rectangular (T(x, y, z, t)) ,
– cylindrical (T(r, φ, z, t)),
– spherical (T(r, φ, θ, t)).
Classification of conduction heat transfer problems:
• steady versus transient heat transfer,
• multidimensional heat transfer,
• heat generation.
Introduction ─ Continue
Steady versus Transient Heat Transfer
• Steady implies no change with time at any point
within the medium
• Transient implies variation with time or time
dependence
Multidimensional Heat Transfer
• Heat transfer problems are also classified as being:
– one-dimensional,
– two dimensional,
– three-dimensional.
• In the most general case, heat transfer through a
medium is three-dimensional. However, some
problems can be classified as two- or one-dimensional
depending on the relative magnitudes of heat transfer
rates in different directions and the level of accuracy
desired.
• The rate of heat conduction through a medium in
a specified direction (say, in the x-direction) is
expressed by Fourier’s law of heat conduction
for one-dimensional heat conduction as:
• Heat is conducted in the direction
of decreasing temperature, and thus
the temperature gradient is negative
when heat is conducted in the positive x-
direction.
(W)cond
dT
Q kA
dx
= −& (2-1)
General Relation for Fourier’s Law of
Heat Conduction
• The heat flux vector at a point P on the surface of
the figure must be perpendicular to the surface,
and it must point in the direction of decreasing
temperature
• If n is the normal of the
isothermal surface at point P,
the rate of heat conduction at
that point can be expressed by
Fourier’s law as
(W)n
dT
Q kA
dn
= −& (2-2)
General Relation for Fourier’s Law of
Heat Conduction-Continue
• In rectangular coordinates, the heat conduction
vector can be expressed in terms of its components as
• which can be determined from Fourier’s law as
n x y zQ Q i Q j Q k= + +
r rr r
& & & &
x x
y y
z z
T
Q kA
x
T
Q kA
y
T
Q kA
z
 ∂
= − ∂
∂
= −
∂
 ∂
= −
∂
&
&
&
(2-3)
(2-4)
Heat Generation
• Examples:
– electrical energy being converted to heat at a rate of I2
R,
– fuel elements of nuclear reactors,
– exothermic chemical reactions.
• Heat generation is a volumetric phenomenon.
• The rate of heat generation units : W/m3
or Btu/h · ft3
.
• The rate of heat generation in a medium may vary
with time as well as position within the medium.
• The total rate of heat generation in a medium of
volume V can be determined from
(W)gen gen
V
E e dV= ∫& & (2-5)
One-Dimensional Heat Conduction
Equation - Plane Wall
xQ&
Rate of heat
conduction
at x
Rate of heat
conduction
at x+∆x
Rate of heat
generation inside
the element
Rate of change of
the energy content
of the element
- + =
,gen elementE+ &
x xQ +∆− & elementE
t
∆
=
∆
(2-6)
• The change in the energy content and the rate of heat
generation can be expressed as
• Substituting into Eq. 2–6, we get
( ) ( )
,
element t t t t t t t t t
gen element gen element gen
E E E mc T T cA x T T
E e V e A x
ρ+∆ +∆ +∆∆ = − = − = ∆ −

= = ∆
& & &
,
element
x x x gen element
E
Q Q E
t
+∆
∆
− + =
∆
& & & (2-6)
(2-7)
(2-8)
x x xQ Q +∆−& & (2-9)
gene A x+ ∆& t t tT T
cA x
t
ρ +∆ −
= ∆
∆
1
gen
T T
kA e c
A x x t
ρ
∂ ∂ ∂ 
+ = ÷
∂ ∂ ∂ 
& (2-11)
• Dividing by A∆x, taking the limit as ∆x 0 and ∆t 0,
and from Fourier’s law:
The area A is constant for a plane wall  the one dimensional
transient heat conduction equation in a plane wall is
gen
T T
k e c
x x t
ρ
∂ ∂ ∂ 
+ = ÷
∂ ∂ ∂ 
&Variable conductivity:
Constant conductivity:
2
2
1
;
geneT T k
x k t c
α
α ρ
∂ ∂
+ = =
∂ ∂
&
1) Steady-state:
2) Transient, no heat generation:
3) Steady-state, no heat generation:
2
2
0
gened T
dx k
+ =
&
2
2
1T T
x tα
∂ ∂
=
∂ ∂
2
2
0
d T
dx
=
The one-dimensional conduction equation may be reduces
to the following forms under special conditions
(2-13)
(2-14)
(2-15)
(2-16)
(2-17)
One-Dimensional Heat Conduction
Equation - Long Cylinder
rQ&
Rate of heat
conduction
at r
Rate of heat
conduction
at r+∆r
Rate of heat
generation inside
the element
Rate of change of
the energy content
of the element
- + =
,gen elementE+ & elementE
t
∆
=
∆r rQ +∆− &
(2-18)
• The change in the energy content and the rate of heat
generation can be expressed as
• Substituting into Eq. 2–18, we get
( ) ( )
,
element t t t t t t t t t
gen element gen element gen
E E E mc T T cA r T T
E e V e A r
ρ+∆ +∆ +∆∆ = − = − = ∆ −

= = ∆
& & &
,
element
r r r gen element
E
Q Q E
t
+∆
∆
− + =
∆
& & & (2-18)
(2-19)
(2-20)
r r rQ Q +∆−& & (2-21)
gene A r+ ∆& t t tT T
cA r
t
ρ +∆ −
= ∆
∆
1
gen
T T
kA e c
A r r t
ρ
∂ ∂ ∂ 
+ = ÷
∂ ∂ ∂ 
& (2-23)
• Dividing by A∆r, taking the limit as ∆r 0 and ∆t 0,
and from Fourier’s law:
Noting that the area varies with the independent variable r
according to A=2πrL, the one dimensional transient heat
conduction equation in a plane wall becomes
1
gen
T T
rk e c
r r r t
ρ
∂ ∂ ∂ 
+ = ÷
∂ ∂ ∂ 
&
1
0
gened dT
r
r dr dr k
 
+ = ÷
 
&
The one-dimensional conduction equation may be reduces
to the following forms under special conditions
1 1geneT T
r
r r r k tα
∂ ∂ ∂ 
+ = ÷
∂ ∂ ∂ 
&
1 1T T
r
r r r tα
∂ ∂ ∂ 
= ÷
∂ ∂ ∂ 
0
d dT
r
dr dr
 
= ÷
 
Variable conductivity:
Constant conductivity:
1) Steady-state:
2) Transient, no heat generation:
3) Steady-state, no heat generation:
(2-25)
(2-26)
(2-27)
(2-28)
(2-29)
One-Dimensional Heat Conduction
Equation - Sphere
2
2
1
gen
T T
r k e c
r r r t
ρ
∂ ∂ ∂ 
+ = ÷
∂ ∂ ∂ 
&
2
2
1 1geneT T
r
r r r k tα
∂ ∂ ∂ 
+ = ÷
∂ ∂ ∂ 
&
Variable conductivity:
Constant conductivity:
(2-30)
(2-31)
General Heat Conduction Equation
x y zQ Q Q+ +& & &
Rate of heat
conduction
at x, y, and z
Rate of heat
conduction
at x+∆x, y+∆y,
and z+∆z
Rate of heat
generation
inside the
element
Rate of change
of the energy
content of the
element
- + =
x x y y z zQ Q Q+∆ +∆ +∆− − −& & &
,gen elementE+ elementE
t
∆
=
∆
(2-36)
Repeating the mathematical approach used for the one-
dimensional heat conduction the three-dimensional heat
conduction equation is determined to be
2 2 2
2 2 2
1geneT T T T
x y z k tα
∂ ∂ ∂ ∂
+ + + =
∂ ∂ ∂ ∂
&
2 2 2
2 2 2
0
geneT T T
x y z k
∂ ∂ ∂
+ + + =
∂ ∂ ∂
&
2 2 2
2 2 2
1T T T T
x y z tα
∂ ∂ ∂ ∂
+ + =
∂ ∂ ∂ ∂
2 2 2
2 2 2
0
T T T
x y z
∂ ∂ ∂
+ + =
∂ ∂ ∂
Two-dimensional
Three-dimensional
1) Steady-state:
2) Transient, no heat generation:
3) Steady-state, no heat generation:
Constant conductivity: (2-39)
(2-40)
(2-41)
(2-42)
Cylindrical Coordinates
2
1 1
gen
T T T T T
rk k k e c
r r r r z z t
ρ
φ φ
 ∂ ∂ ∂ ∂ ∂ ∂ ∂   
+ + + = ÷ ÷  ÷
∂ ∂ ∂ ∂ ∂ ∂ ∂    
&
(2-43)
Spherical Coordinates
2
2 2 2 2
1 1 1
sin
sin sin
gen
T T T T
kr k k e c
r r r r r t
θ ρ
θ φ φ θ θ θ
 ∂ ∂ ∂ ∂ ∂ ∂ ∂   
+ + + = ÷ ÷  ÷
∂ ∂ ∂ ∂ ∂ ∂ ∂    
&
(2-44)
Boundary and Initial Conditions
• Specified Temperature Boundary Condition
• Specified Heat Flux Boundary Condition
• Convection Boundary Condition
• Radiation Boundary Condition
• Interface Boundary Conditions
• Generalized Boundary Conditions
Specified Temperature Boundary
Condition
For one-dimensional heat transfer
through a plane wall of thickness
L, for example, the specified
temperature boundary conditions
can be expressed as
T(0, t) = T1
T(L, t) = T2
The specified temperatures can be constant, which is the
case for steady heat conduction, or may vary with time.
(2-46)
Specified Heat Flux Boundary
Condition
dT
q k
dx
= − =&
Heat flux in the
positive x-
direction
The sign of the specified heat flux is determined by
inspection: positive if the heat flux is in the positive
direction of the coordinate axis, and negative if it is in
the opposite direction.
The heat flux in the positive x-
direction anywhere in the medium,
including the boundaries, can be
expressed by Fourier’s law of heat
conduction as
(2-47)
Two Special Cases
Insulated boundary Thermal symmetry
(0, ) (0, )
0 or 0
T t T t
k
x x
∂ ∂
= =
∂ ∂
( ),
2 0
LT t
x
∂
=
∂
(2-49) (2-50)
Convection Boundary Condition
[ ]1 1
(0, )
(0, )
T t
k h T T t
x
∞
∂
− = −
∂
[ ]2 2
( , )
( , )
T L t
k h T L t T
x
∞
∂
− = −
∂
Heat conduction
at the surface in a
selected direction
Heat convection
at the surface in
the same direction
=
and
(2-51a)
(2-51b)
Radiation Boundary Condition
Heat conduction
at the surface in a
selected direction
Radiation exchange
at the surface in
the same direction
=
4 4
1 ,1
(0, )
(0, )surr
T t
k T T t
x
ε σ
∂
 − = − ∂
4 4
2 ,2
( , )
( , ) surr
T L t
k T L t T
x
ε σ
∂
 − = − ∂
and
(2-52a)
(2-52b)
Interface Boundary Conditions
0 0( , ) ( , )A B
A B
T x t T x t
k k
x x
∂ ∂
− = −
∂ ∂
At the interface the requirements are:
(1) two bodies in contact must have the same
temperature at the area of contact,
(2) an interface (which is a
surface) cannot store any
energy, and thus the heat flux
on the two sides of an
interface must be the same.
TA(x0, t) = TB(x0, t)
and
(2-53)
(2-54)
Generalized Boundary Conditions
In general a surface may involve convection, radiation,
and specified heat flux simultaneously. The boundary
condition in such cases is again obtained from a surface
energy balance, expressed as
Heat transfer
to the surface
in all modes
Heat transfer
from the surface
In all modes
=
Heat Generation in Solids
The quantities of major interest in a medium with heat
generation are the surface temperature Ts and the
maximum temperature Tmax that occurs in the medium in
steady operation.
The heat transfer rate by convection can also be
expressed from Newton’s law of cooling as
( ) (W)s sQ hA T T∞= −&
gen
s
s
e V
T T
hA
∞= +
&
Rate of
heat transfer
from the solid
Rate of
energy generation
within the solid
=
For uniform heat generation within the medium
(W)genQ e V=& &
-
Heat Generation in Solids -The Surface
Temperature
(2-64)
(2-65)
(2-66)
(2-63)
Heat Generation in Solids -The Surface
Temperature
For a large plane wall of thickness 2L (As=2Awall and
V=2LAwall)
,
gen
s plane wall
e L
T T
h
∞= +
&
For a long solid cylinder of radius r0 (As=2πr0L and
V=πr0
2
L) 0
,
2
gen
s cylinder
e r
T T
h
∞= +
&
For a solid sphere of radius r0 (As=4πr0
2
and V=4
/3πr0
3
)
0
,
3
gen
s sphere
e r
T T
h
∞= +
&
(2-68)
(2-69)
(2-67)
Heat Generation in Solids -The maximum
Temperature in a Cylinder (the Centerline)
The heat generated within an inner
cylinder must be equal to the heat
conducted through its outer surface.
r gen r
dT
kA e V
dr
− = &
Substituting these expressions into the above equation
and separating the variables, we get
( ) ( )2
2
2
gen
gen
edT
k rL e r L dT rdr
dr k
π π− = → = −
&
&
Integrating from r =0 where T(0) =T0 to r=ro
2
0
max, 0
4
gen
cylinder s
e r
T T T
k
∆ = − =
&
(2-71)
(2-70)
Variable Thermal Conductivity, k(T)
• The thermal conductivity of a
material, in general, varies with
temperature.
• An average value for the
thermal conductivity is
commonly used when the
variation is mild.
• This is also common practice
for other temperature-
dependent properties such as
the density and specific heat.
Variable Thermal Conductivity for
One-Dimensional Cases
2
1
2 1
( )
T
T
ave
k T dT
k
T T
=
−
∫
When the variation of thermal conductivity with
temperature k(T) is known, the average value of the thermal
conductivity in the temperature range between T1 and T2 can
be determined from
The variation in thermal conductivity of a material
with can often be approximated as a linear function
and expressed as
0( ) (1 )k T k Tβ= +
β the temperature coefficient of thermal conductivity.
(2-75)
(2-79)
Variable Thermal Conductivity
• For a plane wall the
temperature varies linearly
during steady one-
dimensional heat conduction
when the thermal conductivity
is constant.
• This is no longer the case
when the thermal conductivity
changes with temperature
(even linearly).

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heat conduction equations

  • 1. Chapter 2: Heat Conduction Equation Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
  • 2. Objectives When you finish studying this chapter, you should be able to: • Understand multidimensionality and time dependence of heat transfer, and the conditions under which a heat transfer problem can be approximated as being one-dimensional, • Obtain the differential equation of heat conduction in various coordinate systems, and simplify it for steady one-dimensional case, • Identify the thermal conditions on surfaces, and express them mathematically as boundary and initial conditions, • Solve one-dimensional heat conduction problems and obtain the temperature distributions within a medium and the heat flux, • Analyze one-dimensional heat conduction in solids that involve heat generation, and • Evaluate heat conduction in solids with temperature-dependent thermal conductivity.
  • 3. Introduction • Although heat transfer and temperature are closely related, they are of a different nature. • Temperature has only magnitude it is a scalar quantity. • Heat transfer has direction as well as magnitude it is a vector quantity. • We work with a coordinate system and indicate direction with plus or minus signs.
  • 4. Introduction ─ Continue • The driving force for any form of heat transfer is the temperature difference. • The larger the temperature difference, the larger the rate of heat transfer. • Three prime coordinate systems: – rectangular (T(x, y, z, t)) , – cylindrical (T(r, φ, z, t)), – spherical (T(r, φ, θ, t)).
  • 5. Classification of conduction heat transfer problems: • steady versus transient heat transfer, • multidimensional heat transfer, • heat generation. Introduction ─ Continue
  • 6. Steady versus Transient Heat Transfer • Steady implies no change with time at any point within the medium • Transient implies variation with time or time dependence
  • 7. Multidimensional Heat Transfer • Heat transfer problems are also classified as being: – one-dimensional, – two dimensional, – three-dimensional. • In the most general case, heat transfer through a medium is three-dimensional. However, some problems can be classified as two- or one-dimensional depending on the relative magnitudes of heat transfer rates in different directions and the level of accuracy desired.
  • 8. • The rate of heat conduction through a medium in a specified direction (say, in the x-direction) is expressed by Fourier’s law of heat conduction for one-dimensional heat conduction as: • Heat is conducted in the direction of decreasing temperature, and thus the temperature gradient is negative when heat is conducted in the positive x- direction. (W)cond dT Q kA dx = −& (2-1)
  • 9. General Relation for Fourier’s Law of Heat Conduction • The heat flux vector at a point P on the surface of the figure must be perpendicular to the surface, and it must point in the direction of decreasing temperature • If n is the normal of the isothermal surface at point P, the rate of heat conduction at that point can be expressed by Fourier’s law as (W)n dT Q kA dn = −& (2-2)
  • 10. General Relation for Fourier’s Law of Heat Conduction-Continue • In rectangular coordinates, the heat conduction vector can be expressed in terms of its components as • which can be determined from Fourier’s law as n x y zQ Q i Q j Q k= + + r rr r & & & & x x y y z z T Q kA x T Q kA y T Q kA z  ∂ = − ∂ ∂ = − ∂  ∂ = − ∂ & & & (2-3) (2-4)
  • 11. Heat Generation • Examples: – electrical energy being converted to heat at a rate of I2 R, – fuel elements of nuclear reactors, – exothermic chemical reactions. • Heat generation is a volumetric phenomenon. • The rate of heat generation units : W/m3 or Btu/h · ft3 . • The rate of heat generation in a medium may vary with time as well as position within the medium. • The total rate of heat generation in a medium of volume V can be determined from (W)gen gen V E e dV= ∫& & (2-5)
  • 12. One-Dimensional Heat Conduction Equation - Plane Wall xQ& Rate of heat conduction at x Rate of heat conduction at x+∆x Rate of heat generation inside the element Rate of change of the energy content of the element - + = ,gen elementE+ & x xQ +∆− & elementE t ∆ = ∆ (2-6)
  • 13. • The change in the energy content and the rate of heat generation can be expressed as • Substituting into Eq. 2–6, we get ( ) ( ) , element t t t t t t t t t gen element gen element gen E E E mc T T cA x T T E e V e A x ρ+∆ +∆ +∆∆ = − = − = ∆ −  = = ∆ & & & , element x x x gen element E Q Q E t +∆ ∆ − + = ∆ & & & (2-6) (2-7) (2-8) x x xQ Q +∆−& & (2-9) gene A x+ ∆& t t tT T cA x t ρ +∆ − = ∆ ∆ 1 gen T T kA e c A x x t ρ ∂ ∂ ∂  + = ÷ ∂ ∂ ∂  & (2-11) • Dividing by A∆x, taking the limit as ∆x 0 and ∆t 0, and from Fourier’s law:
  • 14. The area A is constant for a plane wall  the one dimensional transient heat conduction equation in a plane wall is gen T T k e c x x t ρ ∂ ∂ ∂  + = ÷ ∂ ∂ ∂  &Variable conductivity: Constant conductivity: 2 2 1 ; geneT T k x k t c α α ρ ∂ ∂ + = = ∂ ∂ & 1) Steady-state: 2) Transient, no heat generation: 3) Steady-state, no heat generation: 2 2 0 gened T dx k + = & 2 2 1T T x tα ∂ ∂ = ∂ ∂ 2 2 0 d T dx = The one-dimensional conduction equation may be reduces to the following forms under special conditions (2-13) (2-14) (2-15) (2-16) (2-17)
  • 15. One-Dimensional Heat Conduction Equation - Long Cylinder rQ& Rate of heat conduction at r Rate of heat conduction at r+∆r Rate of heat generation inside the element Rate of change of the energy content of the element - + = ,gen elementE+ & elementE t ∆ = ∆r rQ +∆− & (2-18)
  • 16. • The change in the energy content and the rate of heat generation can be expressed as • Substituting into Eq. 2–18, we get ( ) ( ) , element t t t t t t t t t gen element gen element gen E E E mc T T cA r T T E e V e A r ρ+∆ +∆ +∆∆ = − = − = ∆ −  = = ∆ & & & , element r r r gen element E Q Q E t +∆ ∆ − + = ∆ & & & (2-18) (2-19) (2-20) r r rQ Q +∆−& & (2-21) gene A r+ ∆& t t tT T cA r t ρ +∆ − = ∆ ∆ 1 gen T T kA e c A r r t ρ ∂ ∂ ∂  + = ÷ ∂ ∂ ∂  & (2-23) • Dividing by A∆r, taking the limit as ∆r 0 and ∆t 0, and from Fourier’s law:
  • 17. Noting that the area varies with the independent variable r according to A=2πrL, the one dimensional transient heat conduction equation in a plane wall becomes 1 gen T T rk e c r r r t ρ ∂ ∂ ∂  + = ÷ ∂ ∂ ∂  & 1 0 gened dT r r dr dr k   + = ÷   & The one-dimensional conduction equation may be reduces to the following forms under special conditions 1 1geneT T r r r r k tα ∂ ∂ ∂  + = ÷ ∂ ∂ ∂  & 1 1T T r r r r tα ∂ ∂ ∂  = ÷ ∂ ∂ ∂  0 d dT r dr dr   = ÷   Variable conductivity: Constant conductivity: 1) Steady-state: 2) Transient, no heat generation: 3) Steady-state, no heat generation: (2-25) (2-26) (2-27) (2-28) (2-29)
  • 18. One-Dimensional Heat Conduction Equation - Sphere 2 2 1 gen T T r k e c r r r t ρ ∂ ∂ ∂  + = ÷ ∂ ∂ ∂  & 2 2 1 1geneT T r r r r k tα ∂ ∂ ∂  + = ÷ ∂ ∂ ∂  & Variable conductivity: Constant conductivity: (2-30) (2-31)
  • 19. General Heat Conduction Equation x y zQ Q Q+ +& & & Rate of heat conduction at x, y, and z Rate of heat conduction at x+∆x, y+∆y, and z+∆z Rate of heat generation inside the element Rate of change of the energy content of the element - + = x x y y z zQ Q Q+∆ +∆ +∆− − −& & & ,gen elementE+ elementE t ∆ = ∆ (2-36)
  • 20. Repeating the mathematical approach used for the one- dimensional heat conduction the three-dimensional heat conduction equation is determined to be 2 2 2 2 2 2 1geneT T T T x y z k tα ∂ ∂ ∂ ∂ + + + = ∂ ∂ ∂ ∂ & 2 2 2 2 2 2 0 geneT T T x y z k ∂ ∂ ∂ + + + = ∂ ∂ ∂ & 2 2 2 2 2 2 1T T T T x y z tα ∂ ∂ ∂ ∂ + + = ∂ ∂ ∂ ∂ 2 2 2 2 2 2 0 T T T x y z ∂ ∂ ∂ + + = ∂ ∂ ∂ Two-dimensional Three-dimensional 1) Steady-state: 2) Transient, no heat generation: 3) Steady-state, no heat generation: Constant conductivity: (2-39) (2-40) (2-41) (2-42)
  • 21. Cylindrical Coordinates 2 1 1 gen T T T T T rk k k e c r r r r z z t ρ φ φ  ∂ ∂ ∂ ∂ ∂ ∂ ∂    + + + = ÷ ÷  ÷ ∂ ∂ ∂ ∂ ∂ ∂ ∂     & (2-43)
  • 22. Spherical Coordinates 2 2 2 2 2 1 1 1 sin sin sin gen T T T T kr k k e c r r r r r t θ ρ θ φ φ θ θ θ  ∂ ∂ ∂ ∂ ∂ ∂ ∂    + + + = ÷ ÷  ÷ ∂ ∂ ∂ ∂ ∂ ∂ ∂     & (2-44)
  • 23. Boundary and Initial Conditions • Specified Temperature Boundary Condition • Specified Heat Flux Boundary Condition • Convection Boundary Condition • Radiation Boundary Condition • Interface Boundary Conditions • Generalized Boundary Conditions
  • 24. Specified Temperature Boundary Condition For one-dimensional heat transfer through a plane wall of thickness L, for example, the specified temperature boundary conditions can be expressed as T(0, t) = T1 T(L, t) = T2 The specified temperatures can be constant, which is the case for steady heat conduction, or may vary with time. (2-46)
  • 25. Specified Heat Flux Boundary Condition dT q k dx = − =& Heat flux in the positive x- direction The sign of the specified heat flux is determined by inspection: positive if the heat flux is in the positive direction of the coordinate axis, and negative if it is in the opposite direction. The heat flux in the positive x- direction anywhere in the medium, including the boundaries, can be expressed by Fourier’s law of heat conduction as (2-47)
  • 26. Two Special Cases Insulated boundary Thermal symmetry (0, ) (0, ) 0 or 0 T t T t k x x ∂ ∂ = = ∂ ∂ ( ), 2 0 LT t x ∂ = ∂ (2-49) (2-50)
  • 27. Convection Boundary Condition [ ]1 1 (0, ) (0, ) T t k h T T t x ∞ ∂ − = − ∂ [ ]2 2 ( , ) ( , ) T L t k h T L t T x ∞ ∂ − = − ∂ Heat conduction at the surface in a selected direction Heat convection at the surface in the same direction = and (2-51a) (2-51b)
  • 28. Radiation Boundary Condition Heat conduction at the surface in a selected direction Radiation exchange at the surface in the same direction = 4 4 1 ,1 (0, ) (0, )surr T t k T T t x ε σ ∂  − = − ∂ 4 4 2 ,2 ( , ) ( , ) surr T L t k T L t T x ε σ ∂  − = − ∂ and (2-52a) (2-52b)
  • 29. Interface Boundary Conditions 0 0( , ) ( , )A B A B T x t T x t k k x x ∂ ∂ − = − ∂ ∂ At the interface the requirements are: (1) two bodies in contact must have the same temperature at the area of contact, (2) an interface (which is a surface) cannot store any energy, and thus the heat flux on the two sides of an interface must be the same. TA(x0, t) = TB(x0, t) and (2-53) (2-54)
  • 30. Generalized Boundary Conditions In general a surface may involve convection, radiation, and specified heat flux simultaneously. The boundary condition in such cases is again obtained from a surface energy balance, expressed as Heat transfer to the surface in all modes Heat transfer from the surface In all modes = Heat Generation in Solids The quantities of major interest in a medium with heat generation are the surface temperature Ts and the maximum temperature Tmax that occurs in the medium in steady operation.
  • 31. The heat transfer rate by convection can also be expressed from Newton’s law of cooling as ( ) (W)s sQ hA T T∞= −& gen s s e V T T hA ∞= + & Rate of heat transfer from the solid Rate of energy generation within the solid = For uniform heat generation within the medium (W)genQ e V=& & - Heat Generation in Solids -The Surface Temperature (2-64) (2-65) (2-66) (2-63)
  • 32. Heat Generation in Solids -The Surface Temperature For a large plane wall of thickness 2L (As=2Awall and V=2LAwall) , gen s plane wall e L T T h ∞= + & For a long solid cylinder of radius r0 (As=2πr0L and V=πr0 2 L) 0 , 2 gen s cylinder e r T T h ∞= + & For a solid sphere of radius r0 (As=4πr0 2 and V=4 /3πr0 3 ) 0 , 3 gen s sphere e r T T h ∞= + & (2-68) (2-69) (2-67)
  • 33. Heat Generation in Solids -The maximum Temperature in a Cylinder (the Centerline) The heat generated within an inner cylinder must be equal to the heat conducted through its outer surface. r gen r dT kA e V dr − = & Substituting these expressions into the above equation and separating the variables, we get ( ) ( )2 2 2 gen gen edT k rL e r L dT rdr dr k π π− = → = − & & Integrating from r =0 where T(0) =T0 to r=ro 2 0 max, 0 4 gen cylinder s e r T T T k ∆ = − = & (2-71) (2-70)
  • 34. Variable Thermal Conductivity, k(T) • The thermal conductivity of a material, in general, varies with temperature. • An average value for the thermal conductivity is commonly used when the variation is mild. • This is also common practice for other temperature- dependent properties such as the density and specific heat.
  • 35. Variable Thermal Conductivity for One-Dimensional Cases 2 1 2 1 ( ) T T ave k T dT k T T = − ∫ When the variation of thermal conductivity with temperature k(T) is known, the average value of the thermal conductivity in the temperature range between T1 and T2 can be determined from The variation in thermal conductivity of a material with can often be approximated as a linear function and expressed as 0( ) (1 )k T k Tβ= + β the temperature coefficient of thermal conductivity. (2-75) (2-79)
  • 36. Variable Thermal Conductivity • For a plane wall the temperature varies linearly during steady one- dimensional heat conduction when the thermal conductivity is constant. • This is no longer the case when the thermal conductivity changes with temperature (even linearly).