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PBL Jean-Luc Thiffeault Department of Mathematics BULK University - PowerPoint PPT Presentation

heat exchange and exit times PBL Jean-Luc Thiffeault Department of Mathematics BULK University of Wisconsin Madison SZ with Florence Marcotte, William R. Young, Charles R. Doering Workshop Irregular transport: analysis and applications


  1. heat exchange and exit times PBL Jean-Luc Thiffeault Department of Mathematics BULK University of Wisconsin – Madison SZ with Florence Marcotte, William R. Young, Charles R. Doering Workshop Irregular transport: analysis and applications Basel, Switzerland, 26 June 2017 Supported by NSF grant CMMI-1233935 1 / 22

  2. advection–diffusion equation in a bounded region Advection and diffusion of heat in a bounded region Ω, with Dirichlet boundary conditions: ∂ t θ + u · ∇ θ = D ∆ θ, u · ˆ n | ∂ Ω = 0 , θ | ∂ Ω = 0 , with ∇ · u = 0 and θ ( x , t ) ≥ 0. This is the heat exchanger configuration: given an initial distribution of heat, it is fluxed away through the cooled boundaries. This happens through diffusion (conduction) alone, but is greatly aided by stirring. 2 / 22

  3. heat exchangers Our domain will be a 2D cross-section of a traditional coil. 3 / 22

  4. heat flux Write �·� for an integral over Ω. � �·� := · d V Ω The rate of heat loss is equal to the flux through the boundary ∂ Ω: � * ∂ t � θ � = D ∇ θ · ˆ n d S =: − F [ θ ] ≤ 0 . ∂ Ω Goal: find velocity fields u that maximize the heat flux. Note that * is not so good for this, since velocity does not appear. The role of u is to increase gradients near the boundary. What it does internally is not directly relevant. This is in contrast to the traditional Neumann IVP (chaotic mixing, etc). 4 / 22

  5. related problem: mean exit time Take steady velocity u ( x ). The mean exit time τ ( x ) of a Brownian particle initially at x satisfies − u · ∇ τ = D ∆ τ + 1 , τ | ∂ Ω = 0 , This is a steady advection–diffusion equation with velocity − u and source 1. Intuitively, a small integrated mean exit time � τ � = � τ � 1 implies that the velocity is effecient at taking heat out of the system. The mean exit time equation is much nicer than the equation for the concentration: it is steady, and it applies for any initial concentration θ 0 ( x ). 5 / 22

  6. relationship between exit time and mean temperature Recall that �·� is an integral over space, and take � θ 0 � = 1. The quantity � ∞ � θ � d t 0 is a cooling time. Smaller is better for good heat exchange. We have the rigorous bounds � ∞ � ∞ � θ � d t ≤ � τ � ∞ � θ � d t ≤ � τ � 1 � θ 0 � ∞ . 0 0 Thus, decreasing a norm like � τ � 1 or � τ � ∞ will typically decrease the cooling time, as expected. 6 / 22

  7. does stirring always help? [Iyer, G., Novikov, A., Ryzhik, L., & Zlato˘ s, A. (2010). SIAM J. Math. Anal. 42 (6), 2484–2498] Theorem (Iyer et al. 2010) Ω ∈ R n bounded, ∂ Ω ∈ C 1 . Then � τ � L p (Ω) ≤ � τ 0 � L p ( B ) , 1 ≤ p ≤ ∞ , where B ∈ R n is a ball of the same volume as Ω , and τ 0 is the ‘purely diffusive’ solution, 0 = D ∆ τ 0 + 1 on B . That is, measured in any norm, the exit time is maximized for a disk with no stirring. So for a disk stirring always helps, or at least isn’t harmful. They also prove that, surprisingly, if Ω is not a disk, then it’s always possible to make � τ � L ∞ (Ω) increase by stirring. (Related to unmixing flows? [IMA 2010 gang; see review Thiffeault (2012)] ) 7 / 22

  8. optimization problem Let’s formulate an optimization problem to find the best incompressible u . Advection–diffusion operator and its adjoint: L † = − u · ∇ − D ∆ . L := u · ∇ − D ∆ , Minimize � τ � over steady u ( x ) with fixed total kinetic energy E = 1 2 � u � 2 2 . The functional to optimize: F [ τ, u , ϑ, µ, p ] = � τ � − � ϑ ( L † τ − 1) � + 1 2 µ ( � u � 2 2 − 2 E ) − � p ∇ · u � Here ϑ , µ , p are Lagrange multipliers. 8 / 22

  9. Euler–Lagrange equations Introduce streamfunction ψ to satisfy ∇ · u = 0: u x = − ∂ y ψ , u y = ∂ x ψ. The variational problem gives the Euler–Lagrange equations L † τ = 1 , τ | ∂ Ω = 0; L ϑ = 1 , ϑ | ∂ Ω = 0; µ ∆ ψ = J ( τ, ϑ ) , ψ | ∂ Ω = 0; �|∇ ψ | 2 � = 2 E , with the Jacobian J ( τ, ϑ ) := ( ∇ τ × ∇ ϑ ) · ˆ z . 9 / 22

  10. a judicious transformation Transform to new functions η , ξ τ = τ 0 + 1 ϑ = τ 0 + 1 2 ( η + ξ ) , 2 ( η − ξ ) where recall that τ 0 is the solution without flow (purely diffusive). Then by using the Euler–Lagrange equations we can eventually show � τ � = � τ 0 � − 1 4 �|∇ ξ | 2 � − 1 4 �|∇ η | 2 � . Hence, solutions to E–L equations cannot make � τ � increase. So stirring is always better than not stirring. 10 / 22

  11. the nonlinear ansatz For a disk the purely diffusive solution is τ 0 = 1 4 (1 − r 2 ). We then make the ansatz � � ξ = 2 µ B ( r ) cos m θ, η = B ( r ) sin m θ, ψ = ξ/ 2 µ, and look for solutions of that form. Inserting this into the full system gives solutions provided the radial functions B ( r ) satisfy the nonlinear eigenvalue problem r 2 B ′′ + rB ′ + ( r 2 λ − m 2 ) B = 1 2 m 2 B 3 , � λ = m / 2 µ. The left-hand side is Bessel’s equation. Note that it is rather unusual for such a linear-type ansatz to give nonlinear solutions. We also have no guarantee that this is the true optimal solution. 11 / 22

  12. small- E solutions For small energy E , exact solution in terms of Bessel functions J m ( ρ mn r ), where ρ mn are zeros: � τ � / � τ 0 � = 1 − (4 m 2 /πρ 4 mn ) E + O ( E 2 ) . Pick the solution with the smallest � τ � : m = 2 , n = 1 for all E ≪ 1: 8 3 6 2 4 1 2 0 0 -2 -1 -4 -2 -6 -3 -8 u τ − τ 0 × 10 -3 × 10 -4 12 / 22

  13. large E case: numerics Numerical solution with Matlab’s bvp5c , using a continuation method: 10 0 m = 64 m = 2 10 -1 � τ � 10 -2 10 -3 m = { 2 , 10 , 14 , 18 , 24 , 32 , 48 , 64 } 10 -4 10 0 10 2 10 4 10 6 10 8 E Larger m worse at small E , then better, then maybe worse again? 13 / 22

  14. optimal solution for E = 1000, m = 8 PBL Three regions: BULK • Stagnation zone (SZ) SZ • Bulk • Peripheral boundary layer (PBL) 14 / 22

  15. structure of the radial solution B ( r ) for large E 1.5 40 1 0.5 30 0 -0.5 0.01 0.02 0.03 0.04 0.05 20 B 10 0 PBL SZ BULK -10 0 0.2 0.4 0.6 0.8 1 r 15 / 22

  16. large- E asymptotics: outer solution Rescaled variables B = E α ˜ B and λ = E β ˜ λ : r 2 ˜ B ′′ E α + r ˜ B ′ E α + r 2 ˜ BE α + β − m 2 ˜ BE α = 1 2 m 2 ˜ λ ˜ B 3 E 3 α . Outside the boundary layer, the large- E balance must occur between the BE α + β and 1 2 m 2 ˜ terms r 2 ˜ λ ˜ B 3 E 3 α , so β = 2 α . This gives the outer solution � B outer = E α ˜ λ E α r . 2 / m 3 ˜ B = (This does not include the stagnation zone in the center. Neglect for now.) Cannot satisfy B outer (1) = 0: need boundary layer. 16 / 22

  17. large- E asymptotics: inner solution Inner variable r = 1 − ǫρ : (1 − ǫρ ) 2 B ′′ E α + (1 − ǫρ ) B ′ E α + (1 − ǫρ ) 2 ˜ B E 3 α − m 2 ¯ ¯ ¯ λ ¯ B E α ǫ 2 ǫ 2 m 2 ¯ B 3 E 3 α . = 1 Dominant balance: highest derivative with E α = ǫ − 1 : B ′′ + ˜ 2 m 2 ¯ ¯ λ ¯ B = 1 B 3 . This has an exact tanh solution, which after matching with the outer solution as ρ → ∞ gives � λ/ m 2 E α tanh �� � 2˜ B inner = λ/ 2 ρ 17 / 22

  18. large- E asymptotics: energy constraint Finally we apply the energy constraint, which reads � 1 rB ′ 2 + m 2 � � 2 E r B 2 π = d r 0 � 1 − δ � 1 outer + m 2 � � rB ′ 2 r B 2 B ′ 2 inner + m 2 B 2 � � = d r + d r . outer inner 0 1 − δ We skip the details, but dominant balance requires α = 1 / 3, and so β = 2 α = 2 / 3. The optimal integrated exit time thus scales as m − 2 / 3 E − 1 / 3 . 18 / 22

  19. large- E case: asymptotics at fixed m 10 0 m = 64 m = 2 10 -1 � τ � 10 -2 � 1 / 3 m − 2 / 3 E − 1 / 3 π 4 / 6 � 10 -3 m = { 2 , 10 , 14 , 18 , 24 , 32 , 48 , 64 } 10 -4 10 0 10 2 10 4 10 6 10 8 E Fixed- E asymptotic optimal � τ � seems to decrease to zero as m − 2 / 3 . This implies no optimal flow, since arbitrarily efficient at large m . Not so! 19 / 22

  20. large- E , large- m case 10 0 m = 64 m = 2 10 -1 � τ � 10 -2 � 1 / 3 m − 2 / 3 E − 1 / 3 π 4 / 6 � 3 (2 E /π ) − 1 / 2 4 π 10 -3 m = { 2 , 10 , 14 , 18 , 24 , 32 , 48 , 64 } 10 -4 10 0 10 2 10 4 10 6 10 8 E To truly capture the optimal solution, have to let m ∼ E 1 / 4 . This is the dashed line (envelope). 20 / 22

  21. conclusions • Transport in heat exchangers has a very different character than ‘freely-decaying’ problem. • Using the probabilistic mean exit time formulation simplifies the problem. (Idea came from Iyer et al. 2010.) • Optimal solutions for u are reminiscent of Dean flow. • At small energy optimal solution has m = 2, n = 1. • At larger energy there is a boundary layer, which enhances the heat transfer or decreases exit time: � τ � ∼ m − 2 / 3 E − 1 / 3 . • This asymptotic solution breaks down when m gets too large. The stagnation zone becomes larger and penalizes large m . • A distinguished limit in m gives � τ � ∼ E − 1 / 2 . • Generalizations: use different norms, spatial weight. . . 21 / 22

  22. references Iyer, G., Novikov, A., Ryzhik, L., & Zlato˘ s, A. (2010). SIAM J. Math. Anal. 42 (6), 2484–2498. Thiffeault, J.-L. (2012). Nonlinearity, 25 (2), R1–R44. 22 / 22

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