Finite Element Analysis of Heat Transfer Problems

 
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FINITE ELEMENT ANALYSIS AND DESIGN
Nam-Ho Kim
 
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Analogy between Stress and Heat Conduction Analysis
 
 
 
 
 
 
 
 
In finite element viewpoint, two problems are identical if a proper
interpretation is given.
More Complex Problems
Coupled structural-thermal problems (thermal strain).
Radiation problem
 
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Goals:
 
 
 
 
 
 
Solve for temperature distribution for a given thermal load.
Boundary Conditions
Essential BC: Specified temperature
Natural BC: Specified heat flux
 
Fourier Heat Conduction Equation:
Heat flow from high temperature to low temperature
 
 
 
 
 
 
Examples of 1D heat conduction problems
 
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Thermal conductivity (
W/m/
C )
 
Heat flux (Watts)
 
 
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Conservation of Energy
Energy In + Energy Generated = Energy Out + Energy Increase
 
 
Two modes of heat transfer through the boundary
Prescribed surface heat flow Qs per unit area
Convective heat transfer
h: convection coefficient (
W/m
2
/
C )
 
 
 
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Conservation of Energy at Steady State
No change in internal energy (
U = 0)
 
 
 
P: perimeter of the cross-section
 
 
Apply Fourier Law
 
 
 
Rate of change of heat flux is equal to the sum of heat generated and
heat transferred
 
 
 
 
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Boundary conditions
Temperature at the boundary is prescribed (essential BC)
Heat flux is prescribed (natural BC)
Example: essential BC at x = 0, and natural BC at x = L:
 
 
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Follow the same procedure with 1D bar element
No need to use differential equation
Element conduction equation
Heat can enter the system only through the nodes
Q
i
: heat enters at node 
i
 (Watts)
Divide the solid into a number of elements
Each element has two nodes and two DOFs (
T
i
 and 
T
j
)
For each element, heat entering the element is positive
 
 
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Fourier law of heat conduction
 
 
From the conservation of energy for the element
 
 
Combine the two equation
 
 
 
Similar to 1D bar element (k = E, T = u, q = f)
 
 
 
 
 
Element conductance matrix
 
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Assembly using heat conservation at nodes
Remember that heat flow into the element is positive
Equilibrium of heat flow:
 
 
 
 
Same assembly procedure with 1D bar elements
Applying BC
Striking-the-rows works, but not striking-the-columns because
prescribed temperatures are not usually zero
 
 
 
 
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Calculate nodal temperatures of four elements
A
 = 1m
2
, 
L
 = 1m, 
k
 = 10
W/m/
C
 
 
 
 
 
Element conduction equation
 
 
 
 
 
 
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Assembly
 
 
 
 
 
Boundary conditions (T
1
 = 200 
o
C, Q1 is unknown)
 
 
 
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Boundary conditions
Strike the first row
 
 
 
 
 
Instead of striking the first column, multiply the first column with
T
1
 = 200 
o
C and move to RHS
 
 
 
 
 
Now, the global matrix is positive-definite and can be solved for nodal
temperatures
 
 
 
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Nodal temperatures
 
 
How much heat input is required to maintain T
1
 = 200
o
C?
Use the deleted first row with known nodal temperatures
 
 
Other example
 
 
 
 
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Direct method is limited for nodal heat input
Need more advanced method for heat generation and
convection heat transfer
Galerkin method in Chapter 3 can be used for this purpose
Consider element (e)
Interpolation
 
 
 
 
Heat flux
 
 
 
 
 
Temperature varies linearly
 
 
Heat flow is constant
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Differential equation with heat generation
Substitute approximate solution
Integrate the residual with N
i
(x) as a weight
Integrate by parts
 
 
 
 
 
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Substitute interpolation relation
 
 
 
Perform integration
 
 
Repeat with N
j
(x) as a weight
 
 
 
 
 
 
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Combine the two equations
 
 
 
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)
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Uniform heat source
 
 
 
Equally divided to the two nodes
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Similar to 1D bar element
 
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Heat chamber
Wall temperature = 200 
C
Uniform heat source inside
the wall Q = 400 W/m
3
.
Thermal conductivity of the
wall is k = 25 W/m

C.
Use four elements through
the thickness (unit area)
Boundary Condition:
T
1
 = 200, q
x=1
 = 0.
 
 
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Element Matrix Equation
All elements are identical
 
 
 
 
Assembly
 
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Boundary Conditions
At node 1, the temperature is given (
T
1
 = 200). Thus, the heat flux at
node 1 (
Q
1
) should be unknown.
At node 5, the insulation condition required that the heat flux (
Q
5
)
should be zero. Thus, the temperature at node 5 should be unknown.
At nodes 2 – 4, the temperature is unknown (
T
2
, 
T
3
, 
T
4
). Thus the heat
flux should be known.
1
2
3
4
5
Q
1
Q
5
 
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Imposing Boundary Conditions
Remove first row because it contains unknown 
Q
1
.
Cannot remove first column because 
T
1
 is not zero.
 
 
 
 
 
 
Instead, move the first column
to the right.
 
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Solution
 
 
 
 
 
 
 
Discussion
In order to maintain 200 degree at node 1, we need to remove heat
 
 
 
Convection Boundary Condition
Happens when a structure is surrounded by fluid
Does not exist in structural problems
BC includes unknown temperature (mixed BC)
 
 
 
 
Heat flow is not prescribed. Rather, it is a function of temperature on
the boundary, which is unknown
1D Finite Element
When both Nodes 1 and 2 are convection boundary
 
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Wall
 
T
 
T
 
q
h
 
T
1
 
T
2
 
 
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)
 
Element
equation
 
 
 
Balance of heat flow
Node 1:
Node 2:
Node 3:
Global matrix equation
 
 
 
 
 
 
 
 
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The above matrix is P.D. because of additional positive terms
in diagonal
How much heat flow through convection boundary?
After solving for nodal temperature, use
 
 
This is convection at the end of an element
 
 
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Firebrick
k
1
=1.2W/m/
o
C
h
i
=12W/m
2
/
o
C
Insulating brick
k
2
=0.2W/m/
o
C
h
o
=2.0W/m
2
/
o
C
 
 
 
 
 
 
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Long rod is submerged into a fluid
Convection occurs across the entire surface
Governing differential equation
 
 
 
 
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DE with approximate temperature
 
 
Minimize the residual with interpolation function 
N
i
(
x
)
 
 
 
Integration by parts
 
 
 
 
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Substitute interpolation scheme and rearrange
 
 
 
 
 
Perform integration and simplify
 
 
 
 
Repeat the same procedure with interpolation function 
N
j
(
x
)
 
 
 
 
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Finite element equation with convection along the rod
 
 
 
 
Equivalent conductance matrix due to convection
 
 
Thermal load vector
 
 
 
 
 
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k
 = 0.2 W/mm/
C, 
h
 = 2
10
4
 W/mm
2
/
C
Element conductance matrix
 
 
Thermal load vector
 
 
Element 1
 
 
 
 
 
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Element conduction equation
Element 1
Element 2
Element 3
Balance of heat flow
Node 1
Node 2
Node 3
Node 4
 
 
 
 
 
 
 
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Assembly
 
 
 
Move T
4
 to LHS and apply known T
1
 = 330
 
 
 
Move the first column to RHS after multiplying with T
1
=330
 
 
 
 
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Solve for temperature
 
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Analogy between stress analysis and heat conduction analysis is discussed. Various thermal problems, including steady-state heat transfer and governing differential equations, are explored. Conservation of energy and boundary conditions are detailed for solving thermal analysis problems.

  • Finite Element Analysis
  • Heat Transfer
  • Thermal Problems
  • Governing Equations
  • Boundary Conditions

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  1. CHAP 5 FINITE ELEMENTS FOR HEAT TRANSFER PROBLEMS FINITE ELEMENT ANALYSIS AND DESIGN Nam-Ho Kim 1

  2. HEAT CONDUCTION ANALYSIS Analogy between Stress and Heat Conduction Analysis Structural problem Displacement Stress/strain Displacement B.C. Surface traction force Body force Heat transfer problem Temperature (scalar) Heat flux (vector) Fixed temperature B.C. Heat flux B.C. Internal heat generation Thermal conductivity Young s modulus In finite element viewpoint, two problems are identical if a proper interpretation is given. More Complex Problems Coupled structural-thermal problems (thermal strain). Radiation problem 2

  3. THERMAL PROBLEM Goals: = [ ]{ } T { } Q K T Thermal load Nodal temperature Conductivity matrix Solve for temperature distribution for a given thermal load. Boundary Conditions Essential BC: Specified temperature Natural BC: Specified heat flux 3

  4. STEADY-STATE HEAT TRANSFER PROBLEM Fourier Heat Conduction Equation: Heat flow from high temperature to low temperature dT = q kAdx x Thermal conductivity (W/m/ C ) Heat flux (Watts) Examples of 1D heat conduction problems Thigh Tlow Thigh qx qx Tlow 4

  5. GOVERNING DIFFERENTIAL EQUATION Conservation of Energy Energy In + Energy Generated = Energy Out + Energy Increase + = + E E E U in generated out Two modes of heat transfer through the boundary Prescribed surface heat flow Qs per unit area Convective heat transfer h: convection coefficient (W/m2/ C ) ( ) = Q h T T h T Qs dq dx x Qg + D q x x q x A dx 5

  6. GOVERNING DIFFERENTIAL EQUATION cont. Conservation of Energy at Steady State No change in internal energy ( U = 0) dq dx ( ) + + + = + q Q P x h T T P x Q A x q x x x s g x E E gen in E out P: perimeter of the cross-section dq Q A dx ( ) = + + hP T T Q P, 0 x L x g s Apply Fourier Law d dT dx + ( ) + + = kA Q A hP T T Q P 0, 0 x L g s dx Rate of change of heat flux is equal to the sum of heat generated and heat transferred 6

  7. GOVERNING DIFFERENTIAL EQUATION cont. Boundary conditions Temperature at the boundary is prescribed (essential BC) Heat flux is prescribed (natural BC) Example: essential BC at x = 0, and natural BC at x = L: T(0) T dT kA q dx = = 0 = L x L 7

  8. DIRECT METHOD Follow the same procedure with 1D bar element No need to use differential equation Element conduction equation Heat can enter the system only through the nodes Qi: heat enters at node i (Watts) Divide the solid into a number of elements Each element has two nodes and two DOFs (Ti and Tj) For each element, heat entering the element is positive N 2 1 Q1 Q2 QN Q3 j i e ( ) e ( ) e jq iq L(e) Tj Ti xi xj 8

  9. ELEMENT EQUATION Fourier law of heat conduction ( ) T T dT dx j L i = = (e) i q kA kA (e) From the conservation of energy for the element (T T) + = (e) i (e) j j L i = + q q 0 (e) j q kA (e) Combine the two equation = T T (e) i (e) j q q 1 1 kA L i Element conductance matrix (e) 1 1 j Similar to 1D bar element (k = E, T = u, q = f) 9

  10. ASSEMBLY Assembly using heat conservation at nodes Remember that heat flow into the element is positive Equilibrium of heat flow: T T Q Q 1 1 N i = (e) i 2 2 Q q = [ ] K i T ( ) e 1 = N N T Q N N Same assembly procedure with 1D bar elements Applying BC Striking-the-rows works, but not striking-the-columns because prescribed temperatures are not usually zero Q2 3 1 (1) (2) 2q 2q Element 2 Element 1 2 10

  11. EXAMPLE Calculate nodal temperatures of four elements A = 1m2, L = 1m, k = 10W/m/ C Q4 = 200W T1 T2 T3 T4 T5 x 200 C 1 2 3 4 Q2 = 500W Q3 = 0 Q5 = 0 Q1 Element conduction equation T 1 1 10 T 1 1 (1) 1 (1) 2 T T q q (2) 2 (2) 3 1 1 q q 1 = 2 = 10 1 1 2 3 T T T T (4) 4 (4) 5 (3) 3 (3) 4 1 1 1 1 q q q q 4 3 = = 10 10 1 1 1 1 5 4 11

  12. EXAMPLE cont. Assembly Q Q Q Q Q T T T T T (1) 1 + + + 1 1 0 0 0 1 2 1 0 0 0 1 2 1 0 0 0 1 2 1 0 0 0 1 1 q 1 1 (1) 2 (2) 3 (3) 4 (2) 2 (3) 3 (4) 4 q q q q q q 2 2 = = 10 3 3 4 4 (4) 5 q 5 5 Boundary conditions (T1 = 200 oC, Q1 is unknown) 200 T T T T 1 1 0 0 0 0 0 0 Q 500 0 200 0 1 1 2 1 2 = 10 0 0 0 1 2 1 3 0 0 1 2 1 4 0 1 1 5 12

  13. EXAMPLE cont. Boundary conditions Strike the first row 200 T T T T 1 2 0 0 0 0 0 1 0 0 0 500 0 200 0 2 1 2 1 = 10 3 1 2 1 4 0 1 1 5 Instead of striking the first column, multiply the first column with T1 = 200 oC and move to RHS T T T T 2 1 0 0 0 500 0 200 0 2000 0 0 0 2 1 2 1 3 = + 10 0 0 1 2 1 4 0 1 1 5 Now, the global matrix is positive-definite and can be solved for nodal temperatures 13

  14. EXAMPLE cont. Nodal temperatures T= { } { } T 200 230 210 190 190 C How much heat input is required to maintain T1 = 200oC? Use the deleted first row with known nodal temperatures = + + + 300W = Q 10T 10T 0T 0T 0T 1 1 2 3 4 5 Other example 100W 3 4 2 4 5 1 2 1 5 3 x 50 C Q = 0 200W Q = 0 14

  15. GALERKIN METHOD FOR HEAT CONDUCTION Direct method is limited for nodal heat input Need more advanced method for heat generation and convection heat transfer Galerkin method in Chapter 3 can be used for this purpose Consider element (e) Interpolation T(x) TN(x) TN (x) = + j i e ( ) e ( ) e iq jq L(e) Tj Ti xi xj i i j j x x x x = = N(x) 1 , N (x) i i i j (e) (e) L L T T i N(x) N (x) = = T(x) { } N T Temperature varies linearly i j j Heat flux dT dx 1 1 = = { } T { } T B Heat flow is constant (e) (e) L L 15

  16. GALERKIN METHOD cont. Differential equation with heat generation d dT dx + = kA Q A 0, 0 x L g dx Substitute approximate solution + d dT dx = kA AQ R(x) Residual g dx Integrate the residual with Ni(x) as a weight + x d dT dx j = kA AQ N(x)dx 0 g i dx x i Integrate by parts x x x j dN dT dx dT dx dx j j = kA N(x) kA dx AQ N(x)dx i i g i x x x i i i 16

  17. GALERKIN METHOD cont. Substitute interpolation relation x x dN dx dN dx dN dx j j j + = + kA T T dx AQ N(x)dx q(x )N(x ) q(x )N(x ) i i i j g i j i j i i i x x i i Perform integration ( i (e) T L x kA j ) = = + (e) i (e) i (e) i T Q q Q AQ N(x)dx j g i x i Repeat with Nj(x) as a weight ( j i (e) T T L x j = kA (e) j Q AQ N (x)dx ) = + (e) j (e) j Q q g j x i 17

  18. GALERKIN METHOD cont. Combine the two equations T T + + (e) i (e) j (e) i (e) j Q Q q q 1 1 kA L = + (e) T (e) (e) [ ]{ } T { } { } k Q q i = (e) 1 1 j Similar to 1D bar element {Q(e)}: thermal load corresponding to the heat source {q(e)}: vector of nodal heat flows across the cross-section Uniform heat source x (e) N(x) N (x) AQ L 1 1 j i g = = (e) { } AQ dx Q g 2 j x i Equally divided to the two nodes Temperature varies linearly in the element, and the heat flux is constant 18

  19. EXAMPLE Insulated No heat flow Heat chamber Wall temperature = 200 C Uniform heat source inside the wall Q = 400 W/m3. Thermal conductivity of the wall is k = 25 W/m C. Use four elements through the thickness (unit area) Boundary Condition: T1 = 200, qx=1 = 0. Wall 200 C x 1 m No heat flow x 200 C T1 T2 T3 T4 T5 1 2 3 4 19

  20. EXAMPLE cont. Element Matrix Equation All elements are identical T T (1) 1 (1) 2 1 1 50 50 q q 1 = + 100 1 1 2 Assembly Q Q Q Q Q T T T T T (1) 1 + + + 1 1 0 0 0 0 0 0 50 100 100 100 50 q 1 1 (1) 2 (2) 3 (3) 4 (2) 2 (3) 3 (4) 4 1 2 1 q q q q q q 2 2 = = 100 0 0 0 1 2 1 3 3 0 0 1 2 1 4 4 (4) 5 0 1 1 q 5 5 20

  21. EXAMPLE cont. Boundary Conditions At node 1, the temperature is given (T1 = 200). Thus, the heat flux at node 1 (Q1) should be unknown. At node 5, the insulation condition required that the heat flux (Q5) should be zero. Thus, the temperature at node 5 should be unknown. At nodes 2 4, the temperature is unknown (T2, T3, T4). Thus the heat flux should be known. 1 2 3 Q1 4 5 Q5 + 200 T T T T 1 1 0 0 0 0 0 0 50 Q 1 1 2 1 100 100 100 50 2 = 100 0 0 0 1 2 1 3 0 0 1 2 1 4 0 1 1 5 21

  22. EXAMPLE cont. Imposing Boundary Conditions Remove first row because it contains unknown Q1. Cannot remove first column because T1 is not zero. 200 T T T T 1 2 1 0 0 0 100 100 100 50 2 0 0 0 1 2 1 = 100 3 0 0 1 2 1 4 0 1 1 5 2 T + = 100( 1 200 100(2 T 1 T ) 100 100 2 3 20000 Instead, move the first column to the right. = + 1 T ) 2 3 T T T T 2 1 0 0 0 100 100 100 50 20000 0 0 0 20100 100 100 50 2 1 2 1 3 = + = 100 0 0 1 2 1 4 0 1 1 5 22

  23. EXAMPLE cont. Solution = 200 C,T = = 206 C,T = = T 203.5 C,T 207.5 C,T 208 C 1 2 3 4 5 208 207 FEM Exact 206 205 204 T 203 202 201 200 x 0 0.2 0.4 0.6 0.8 1 Discussion In order to maintain 200 degree at node 1, we need to remove heat + = = Q 50 100T = 100T 350 1 1 2 Q 400 W 1 23

  24. CONVECTION BC Convection Boundary Condition Happens when a structure is surrounded by fluid Does not exist in structural problems BC includes unknown temperature (mixed BC) Wall qh T T = h q hS(T T) Fluid Temperature Convection Coefficient Heat flow is not prescribed. Rather, it is a function of temperature on the boundary, which is unknown 1D Finite Element When both Nodes 1 and 2 are convection boundary = = q q hAT hAT hAT hAT 1 1 1 2 1 T T 2 2 2 T1 T2 24

  25. EXAMPLE (CONVECTION ON THE BOUNDARY) T1 T2 T3 Element equation T T 1 3 1 2 h3 h1 T T T T (2) 2 (2) 3 (1) 1 (1) 2 1 1 1 1 q q q q kA L kA L 2 1 = = 1 1 1 1 3 2 Balance of heat flow = (1) 1 q h A(T T ) Node 1: 1 1 1 + = (1) 2 (2) 2 h A(T q q 0 Node 2: = (2) 3 q T ) Node 3: Global matrix equation 3 3 3 1 1 0 T T T h A(T T ) 1 1 1 0 1 kA L = 1 2 1 2 0 1 1 h A(T T ) 3 3 3 3 25

  26. EXAMPLE cont. Move unknown nodal temperatures to LHS kA kA h A 0 L L kA 2kA kA L L L kA kA 0 h A L L + 1 T T T h AT 1 1 1 = 0 2 h AT 3 3 3 + 3 The above matrix is P.D. because of additional positive terms in diagonal How much heat flow through convection boundary? After solving for nodal temperature, use = (1) 1 q h A(T T ) 1 1 1 This is convection at the end of an element 26

  27. EXAMPLE: FURNACE WALL Firebrick k1=1.2W/m/oC hi=12W/m2/oC Insulating brick k2=0.2W/m/oC ho=2.0W/m2/oC 16.8 4.8 0 { } {1,411 1,190 = T Insulating brick Firebrick Ta = 20 C Tf = 1,500 C hi x ho 0.12 m 0.25 m 4.8 6.47 1.67 0 T T T 18,000 0 40 1 = 1.67 3.67 2 3 Convection boundary Convection boundary T 552} C No heat flow 1,500 C 20 C x = 1054 W/m = (2) 3 2 q h (T T ) 0 a 3 T1 T2 T3 Tf Ta 1 2 ho hi 27

  28. CONVECTION ALONG A ROD Long rod is submerged into a fluid Convection occurs across the entire surface Governing differential equation d dT kA AQ hP T dx dx + ( ) + = = + T 0, 0 x L P 2(b h) g Convection Fluid T b j h ( ) e jq ( ) e iq i xi Convection xj 28

  29. CONVECTION ALONG A ROD cont. DE with approximate temperature d dT kA AQ dx dx + ( ) + = hP T T R(x) g Minimize the residual with interpolation function Ni(x) x + d dT dx j + = kA AQ hP(T T) N(x)dx 0 g i dx x i Integration by parts x x x x x j dN dT dx dT dx dx j j j j = kA N(x) kA dx hPTNdx AQ N(x)dx hPT Ndx i i i g i i x x x x x i i i i i 29

  30. CONVECTION ALONG A ROD cont. Substitute interpolation scheme and rearrange x x dN dx dN dx dN dx j j j + + + kA T T dx hP(TN TN )N dx i i i j i i j j i x x i i x j = + + (AQ hPT )N dx q(x )N(x ) q(x )N(x ) g i j i j i i i x i Perform integration and simplify ( i j (e) T T hpL L T 6 T 3 kA ) j + + = + (e) (e) i (e) i Q q i x j = + (e) i Q (AQ hPT )N(x)dx g i x i Repeat the same procedure with interpolation function Nj(x) 30

  31. CONVECTION ALONG A ROD cont. Finite element equation with convection along the rod T T + + (e) i (e) j (e) i (e) j Q Q q q 1 1 2 1 2 1 (e) kA L hPL i + = (e) 6 1 1 j T + = + (e) T (e) h (e) (e) [ ] [ ] { } { } k k Q q Equivalent conductance matrix due to convection 2 1 2 1 (e) hPL = (e) h k 6 Thermal load vector + (e) (e) Q Q AQ L hPL T 2 1 1 i g = = (e) { } Q j 31

  32. EXAMPLE: HEAT FLOW IN A COOLING FIN k = 0.2 W/mm/ C, h = 2 10 4 W/mm2/ C Element conductance matrix + = k k 1 1 2 1 2 1 2 10 4 0.2 200 40 320 40 6 + (e) T (e) h [ ] [ ] 1 1 Thermal load vector Convection T = 30 C 1 1 2 10 4 320 40 30 2 = (e) { } Q 160 mm 1.25 mm Element 1 330 C Insulated x 120 mm T1 T2 T3 T4 3 2 1 32

  33. EXAMPLE: HEAT FLOW IN A COOLING FIN cont. Element conduction equation T T (1) 1 (1) 2 1.8533 0.5733 0.5733 1.8533 38.4 38.4 q q 1 = + Element 1 2 T T (2) 2 (2) 3 1.8533 0.5733 0.5733 1.8533 38.4 38.4 q q 2 = + Element 2 3 T T (3) 3 (3) 4 1.8533 0.5733 0.5733 1.8533 38.4 38.4 q q Element 3 3 = + 4 Balance of heat flow = (1) 1 q Q Node 1 1 + = (1) 2 (2) 2 q q 0 Node 2 + = (2) 3 (2) 3 q q 0 Node 3 = (3) 4 q hA(T T ) Node 4 4 33

  34. EXAMPLE: HEAT FLOW IN A COOLING FIN cont. Assembly 1.853 + T T T T 38.4 Q .573 3.706 .573 0 0 0 0 1 1 76.8 76.8 hA(T .573 0 0 .573 3.706 .573 1.853 2 = .573 3 38.4 + T ) 4 4 Move T4 to LHS and apply known T1 = 330 + 330 T T T 1.853 .573 0 0 .573 3.706 .573 0 0 0 0 38.4 Q 1 .573 3.706 .573 1.893 76.8 76.8 39.6 2 = .573 3 4 Move the first column to RHS after multiplying with T1=330 3.706 .573 0 T 265.89 .573 3.706 .573 T 76.8 0 .573 1.893 T 39.6 2 = 3 4 34

  35. EXAMPLE: HEAT FLOW IN A COOLING FIN cont. Solve for temperature T 330 C, T = = = = 77.57 C, T 37.72 C, T 32.34 C 1 2 3 4 350 300 250 200 150 100 50 0 0 40 80 120 35

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