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2.092/2.093 — Finite Element Analysis of Solids  Fluids I Fall ‘09 
Lecture 12 -FEA of Heat Transfer/Incompressible Fluid Flow 
Prof. K. J. Bathe MIT OpenCourseWare 
Reminder: Quiz #1, Oct. 29. Closed book, 4 pages of notes. Reading assigment: Section 7.4.2 
We recall the principle of virtual temperatures. 
θ¯0T kθ0dV = θ¯T q B dV + θ¯T q S dS V VSq 
θ(m) = H(m)θ ; θ¯(m) = H(m)θ ¯ 
θ 0 (m) = B(m)θ ; θ¯0(m) = B(m)θ ¯ 
ΣK(m) θ =Σ QB (m) + QS (m) 
mm 
K(m) = B(m)T k(m)B(m)dV (m) V (m) 
Q(m) = H(m)T q B(m)dV (m) 
B 
V (m) 
Q( Sm) = HS(m) T q S(m)dS(m) (a) 
(m) Sq 
In (a), we may have to integrate over two or more surfaces. 
Example 
H =  
1 4  1 + x 2  (1 + y) 1 4  1 − x 2  (1 + y) 1 4  1 − x 2  (1 − y) B =  h1,x h2,x h3,x h4,x h1,y h2,y h3,y h4,y  HS
(1) = HS
y=+1 =  1 2  1 + x 2  1 2  1 − x 2  0 
1 4  1 + x 2  (1 − y) 0  
 
1

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Mit2 092 f09_lec12

  • 1. Z Z Z Z Z Z 2.092/2.093 — Finite Element Analysis of Solids Fluids I Fall ‘09 Lecture 12 -FEA of Heat Transfer/Incompressible Fluid Flow Prof. K. J. Bathe MIT OpenCourseWare Reminder: Quiz #1, Oct. 29. Closed book, 4 pages of notes. Reading assigment: Section 7.4.2 We recall the principle of virtual temperatures. θ¯0T kθ0dV = θ¯T q B dV + θ¯T q S dS V VSq θ(m) = H(m)θ ; θ¯(m) = H(m)θ ¯ θ 0 (m) = B(m)θ ; θ¯0(m) = B(m)θ ¯ ΣK(m) θ =Σ QB (m) + QS (m) mm K(m) = B(m)T k(m)B(m)dV (m) V (m) Q(m) = H(m)T q B(m)dV (m) B V (m) Q( Sm) = HS(m) T q S(m)dS(m) (a) (m) Sq In (a), we may have to integrate over two or more surfaces. Example H = 1 4 1 + x 2 (1 + y) 1 4 1 − x 2 (1 + y) 1 4 1 − x 2 (1 − y) B = h1,x h2,x h3,x h4,x h1,y h2,y h3,y h4,y HS
  • 2.
  • 4.
  • 5. y=+1 = 1 2 1 + x 2 1 2 1 − x 2 0 1 4 1 + x 2 (1 − y) 0 1
  • 6.
  • 7.
  • 8.
  • 9.
  • 10. Z
  • 11.
  • 12. Z
  • 13.
  • 14.
  • 15. Z Lecture 12 FEA of Heat Transfer/Incompressible Fluid Flow 2.092/2.093, Fall ‘09 HS = H 11 (1 + y)00 (1 − y) 22 = (2) x=+2 For our example, (a) means HS S dS + HS S QS = dSq q (1)(2)(1) (2) S(1) S(2) S θe − θS θe − HS θ = h = h q If θe varies, we can use θe = HS θe . In transient solutions, BB q = q˜− ρcθ˙; θ˙= H(m)θ˙ and ˜qB no longer includes the rate at which heat is stored within the material. Putting this all together, we have: Cθ˙ + Kθ = Q˜ B + QS We also need the initial condition 0θ = θ to solve. t=0 In all cases (linear, nonlinear, transient solutions) we solve the following Qint = Qapplied This is analogous to F = R in stress analysis. We further define: (m)(m) B(m)T Qint =Σ Qint ; Qint = q(m)dV (m) mV (m) (m) = k(m)B(m)θ q By solving these equations, we have Finite element equilibrium • Nodal point equilibrium • For any time t, the following should be satisfied: tQint = tQapplied This equation is generally solved by Newton-Raphson iterations (see previous lecture notes). Incompressible Fluid Flow ρvi,j vj = τij,j + fB i τij = −pδij + 2μeij We define the velocity strain tensor eij as eij = 1 2 (vi,j + vj,i) Continuity in an incompressible fluid requires that (1) (2) (3) The unknowns are vi for i = 1, 2, 3 and p. vi,i = 0 ; r · v = 0 (4) 2
  • 16. Z Z | {z } Z Z Z Lecture 12 FEA of Heat Transfer/Incompressible Fluid Flow 2.092/2.093, Fall ‘09 Principle of Virtual Velocities v¯i (ρvi,j vj ) dV + e¯ij τij dV = v¯ifiB dV + v¯iSf fiSf dS (A) VV F VSf 1 e¯ij = (¯vi,j +¯vj,i) 2 ¯(B) pvi,idV =0 V Next, we interpolate: vi = Hv ; p = Hpp Consider a 2D element: v1 h1 h2 h3 h4 0000 v2 =0000 h1 h2 h3 h4 v where vij means the nodal velocity in the i direction at the node j. For a 4-node element, ⎤⎡ v = ⎢⎢⎢⎢⎢⎢⎢⎢⎢⎢⎢⎢⎢⎢⎢⎢⎣ vvvv vvvv 11 21 31 41 12 22 32 42 ⎥⎥⎥⎥⎥⎥⎥⎥⎥⎥⎥⎥⎥⎥⎥⎥⎦ p(x, y)= Hpp ; x = x1,y = x2 3
  • 17. Lecture 12 FEA of Heat Transfer/Incompressible Fluid Flow 2.092/2.093, Fall ‘09 We need to “wisely” choose the Hp matrix for a given H. Why? Assume the medium is slightly compressible. Then, p = −κ (r· v) where κ is the given bulk modulus, which is very large. If the medium is a solid, then v = displacements. If the medium is a fluid, then we use p˙ and v = velocity. Since v is approximated, error occurs. Even a small error in r· v will get magnified by the bulk modulus κ and will cause large errors in p. The interpolation gives the expression F (v, p)= R which is what we should solve. Thus, in incompressible fluid flow analysis, the same finite element conditions hold as in stress and heat transfer analysis. There are many more interesting and important points: • The coefficient matrix is generally non-symmetric. • High Reynolds number flows need special interpolation schemes. • The number of elements is generally very large (will be discussed in 2.094). 4
  • 18. MIT OpenCourseWare http://ocw.mit.edu 2.092 / 2.093 Finite Element Analysis of Solids and Fluids I Fall 2009 For information about citing these materials or our Terms of Use, visit: http://ocw.mit.edu/terms.