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31 - 40 of 196 search results for TALK:PC53 20 |u:www.damtp.cam.ac.uk where 0 match all words and 196 match some words.

  1. Results that match 1 of 2 words

  2. REDUCED CONSISTENCY SAMPLING IN HILBERT SPACES Ben Adcock1, Anders ...

    www.damtp.cam.ac.uk/research/afha/anders/AdcockHansenSampTA.pdf
    5 Oct 2013: 20 40 60 80 100 120 140. - 10. - 5.

  3. flm1000491a

    www.damtp.cam.ac.uk/user/jneufeld/pubfiles/Vella-2011.pdf
    4 Nov 2013: φ+. x. x=0. φx. x=0. 4. 1 y2=. (23π. )1/2λ̄φ. 1/20. ... 3.20). Substituting the similarity solution for h from (3.16) and (3.15), we find that.

  4. pnasSI201302736 1..6

    www.damtp.cam.ac.uk/user/gold/pdfs/streaming_selforganization_SI.pdf
    27 Aug 2013: Phys Fluids 20(12):123304. 2. Woodhouse FG, Goldstein RE (2012) Spontaneous circulation of confined activesuspensions. ... 1. 2. 3. 4. 5. p. c. 1.000.20. 0.15. 0.10. 0.05.

  5. C2SM27089G 1711..1720

    www.damtp.cam.ac.uk/user/lauga/papers/74.pdf
    26 Jul 2013: g(k) 2[1 cos(k) g log(k) kSi(k) Ci(k)], (20). and with the sine and cosine integrals dened by. ... Roman and J. Bico, J. Phys.: Condens. Matter, 2010, 22,493101. 20 S.

  6. flm1100223a

    www.damtp.cam.ac.uk/user/lauga/papers/54.pdf
    26 Jul 2013: F (ζ ) f (z(ζ )), G(ζ ) g(z(ζ )), (5.20). ... 0.20. 0.25. 0.30. 0.35. Ca. c. c = 8 Ca. Figure 6.

  7. A stability barrier for reconstructions from Fourier samples Ben ...

    www.damtp.cam.ac.uk/research/afha/people/anders/AdcockHansenShadrin.pdf
    5 Oct 2013: See [12, 20]. In a similar spirit, Driscoll & Fornberg introduced Padé-based method in[25]. ... 105. 20 40 60 80 100. 0.1. 0.2. 0.3. 20 40 60 80 100.

  8. Document 1

    www.damtp.cam.ac.uk/user/jneufeld/pubfiles/Daniels-2012.pdf
    4 Nov 2013: to store the energy sector’s emssions at current levels for the next 100 years [19, 20]. ... In this regeneration stage,between 13 and 20% of the power output of the plant can be lost.

  9. flm1100072a

    www.damtp.cam.ac.uk/user/jneufeld/pubfiles/Zimoch-2011-1.pdf
    4 Nov 2013: 0.5, 2, 5, 20.5 and 52. ... t. 1.0. 0.8. 0.6. 0.4. 0.2. 0 10 20 30 40.

  10. Modelling carbon dioxide sequestration in layered strata

    www.damtp.cam.ac.uk/user/jneufeld/pubfiles/Neufeld-2009-1.pdf
    4 Nov 2013: Equation (2.15) is subject to the non-dimensional boundary conditions[HH. X. ]. 0. = αT α1, (2.19). [HH. X. ]. XN. = 0, (2.20). ... short-dashed line), 20(dash–dotted line), 25 (long-dashed line) and 30 (dashed–dotted–dotted line).

  11. The optimal elastic flagellumSaverio E. Spagnoliea� and Eric Laugab�…

    www.damtp.cam.ac.uk/user/lauga/papers/36.pdf
    26 Jul 2013: ESliding t =G. 2. 0. L. 2ds. 20. As with the bending Eq. ... Even though the hydrodynamic efficiencyonly decays 13% from the optimal sawtoothed solution, theswimming speed decreases by approximately 20%.

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