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23 May 2006: a. Fluctuations in the velocities of sedimenting particles – p.3/20. Computer simulations. ... Paradox not entirely resolved. Fluctuations in the velocities of sedimenting particles – p.20/20.

17 Nov 2006: t=0.10.20.30.40.5. c. z. APS2006, Sedimentation fronts – p.2/9. Height of concentration quartiles. ... t=0.50.40.30.20.1. c. (z V t)/δ(t). Universal form. APS2006, Sedimentation fronts – p.9/9.

6 Mar 2006: H α1/103/4(f Ṁ)3/20 µmmpk. 3/8. σ. Cκ. 1/20. Please send comments and corrections to gio10@cam.ac.uk.

23 May 2006: γ2α = ω2µ3a6/ρ2g2σh7]. γ0.30.250.20.150.10.05. κ/(γγ). 5. 4. 3. 2. 1. ... HKM shocks – p.20/25. Structure of the shock. Quasi-steady, with F A(T ) outside, A = π/T.

23 Feb 2006: 5. 0. 5. 10. -10-50510. -20 -10 0 10 20. Isozumi, Nitta, Ohashi and Sakai ‘04.

17 Feb 2006: Penner Lecture, 2006 – p.20/52. B. Flow past a sphere Lagrangian unsteadyNumerical Oldroyd-B. ... a. 1e-05. 0.0001. 0.001. 0.01. 0 5 10 15 20. t.

23 May 2006: 0 5 10 15 20 25(RR0)/R0. 0. 1. 2. 3. 4E S. ... Shallow-water vs SimulationsPSfrag replacements. 4. 3. 2. 1. 00 5 10 15 20.

12 Sep 2006: 5. 10. -10-50510. -20 -10 0 10 20. -10. -5. Figure 3:.

24 Jan 2006: Matrix Anal. Appl. 20 (1998), no. 2, 303–353. [Gab82] D. Gabay, Minimizing a differentiable function over a differential manifold, Journal of Opti-mization Theory and Applications 37 (1982), no. ... Numer. Anal. 20 (1983), 626–637. [TL02] N. T.

20 Oct 2006: of Eq. 20 for the uniform flow was found 11 as1 = u1x , y iv1x , y where. ... 0 5 10 15 20. 0.1. 0.2. 0.3. 0.4. 0.5. 0.6.

7 Sep 2006: complexes. In higher dimensions,domain walls 19 and skyrmions (vortons) 20 have been found. ... 20 -10 0 10 20-20. -10. 0. 10. 20. -20 -10 0 10 20-20.

19 Dec 2006: µ. 0.1. 0.2. 0.3. 0.4. 0.5µ e. 0.425µ0.20. y = x. ... 4.3, we find that k = 0.20 and k =0.17 respectively.

28 Oct 2006: 20. 1.7.9 Examples of Gradients. 21. 1.7.10 Divergence and Curl. 21. ... Equating (1.18) and (1.20) yields. l ψ = ddsψ(r sl). s=0.

26 Jul 2006: 25 30 35 40 45 50. 0.050.10.150.20.250.3. Figure 2: The error scaled by ω7/4 of QL[f] with endpoints for nodes and multiplicities both ... 25 30 35 40 45 50. 0.050.10.150.20.250.30.35. Figure 3: The error scaled by ω13/4 of QL[f] with endpoints for

2 Sep 2006: λ1(x) = eiΦ(x), λ2(x) = eiΦ(x), (2.21). where Φ(x) is given by (2.20). ... p(x) = cos(x) O(x2n2) as x 0,. i.e. Φ(x) = x O(x2n1) in (2.20).

20 Jun 2006: 0.05. 20. 0.1. 0.0. 4 102. 0.025. 1886. 0.075. 0.04. 0.06. ... 20. The method (3.6) cannot be used for approximatingf̂C0 and is less precise for small valuesof n, before the onset of asymptotic behaviour.

22 May 2006: 2 PARTIAL DIFFERENTIAL EQUATIONS 20. • at x = L apply insulating boundary condition: there is no flux of heat to x > L.Then have Θx(L,t) = 0, t 0: Neumann condition;. • ... 0 1 2 3 4 5x. 0. 5. 10. 15. 20.

31 Aug 2006: The. 20 Fast evaluation of 3D polyharmonic splines. per panel accuracy, and its estimation, are described later. ... 2.20(1)64, 000 3.75(4) 5.31(7) 3.66(0) 1.08(1) 9.06(1).

28 Oct 2006: 20. 1.7.9 Examples of Gradients. 21. 1.7.10 Divergence and Curl. 21. ... Equating (1.18) and (1.20) yields. l ψ = ddsψ(r sl). s=0.

22 May 2006: 1. . . =(. 20). . . 6. 4. 1. . ... Similarly, c(bc) =0. 1 LINEAR ALGEBRA 20. 3. Consider. A =. . . a1 a2 a3. b1 b2 b3. c1 c2 c3.