Search

Search Funnelback University

Search powered by Funnelback
1 - 10 of 16 search results for KA :PC53 |u:www.damtp.cam.ac.uk where 0 match all words and 16 match some words.
  1. Results that match 1 of 2 words

  2. 1B Methods 27 . 1B METHODS LECTURE NOTES Richard ...

    www.damtp.cam.ac.uk/user/examples/B8Lb.pdf
    4 Oct 2013: if ψ = 0at r = a then Rnk(a) = Jn(ka) = 0 so for each n, ka = kni with i = 1, 2,.
  3. 1B Methods 62 . 1B METHODS LECTURE NOTES Richard ...

    www.damtp.cam.ac.uk/user/examples/B8Lc.pdf
    4 Oct 2013: Its FT is easy to calculate:. f̃(k) =. aaeikx dx =. aa. cos(kx) dx =2 sin(ka). k. (41). so by the Fourier inversion theorem we get. ... 1. π. eikxsin ka. kdk =. {1 |x| < a,0 |x| > a.
  4. pnas201210548 1187..1192

    www.damtp.cam.ac.uk/user/gold/pdfs/ciliary_contact.pdf
    3 Feb 2013: Phys Rev Lett 105(16):168101. 17. Guasto JS, Johnson KA, Gollub JP (2010) Oscillatory flows induced by microorganismsswimming in two dimensions.
  5. pnas201210548 1..6

    www.damtp.cam.ac.uk/user/gold/pdfs/ciliary_contact_plus_SI_online.pdf
    7 Jan 2013: Phys Rev Lett 105(16):168101. 17. Guasto JS, Johnson KA, Gollub JP (2010) Oscillatory flows induced by microorganismsswimming in two dimensions.
  6. doi:

    www.damtp.cam.ac.uk/user/jneufeld/pubfiles/Hewitt-2013-1.pdf
    28 Nov 2013: J. Fluid Mech. (2013), vol. 737, pp. 205–231. c Cambridge University Press 2013 205doi:10.1017/jfm.2013.559. Stability of columnar convection in a porousmedium. Duncan R. Hewitt1,†, Jerome A. Neufeld1,2,3 and John R. Lister1. 1Institute of
  7. 26 Jul 2013: with similar viscosities (, ) and densities (, ),(b) dimensionless membrane-viscous number, Me U=KA, for two fluids separated by an elastic membrane(thickness t, area modulus KA, density m, bending stiff-ness ... f 2= is an intrinsic viscocapillary
  8. 26 Jul 2013: ¤ and compute a matrix F with components fij = cij =( i ¤j ).The minimal-energy stabilizing feedback controller is then given by u = KÀ , whereK = B ¤ F ¡1.
  9. 26 Jul 2013: FIG. 4. (Color online) Instantaneous velocity and pressure fields (left) and z component of the vorticity (right) for the in-plane beating oftwo flagella, with ka = kb = 0.05, R = 1, ... Bottom: Variation of the ratio of the minimum to themaximum of the
  10. , 20120576, published 2 January 2013469 2013 Proc. R. ...

    www.damtp.cam.ac.uk/user/md327/skyrmion_proc.pdf
    14 Aug 2013: Let K = Ka/xa, a = 0,. , 3 be a vector field generating a one-parameter group oftransformations of M with orbits Γ.
  11. §4 FLOWS WITH A FREE SURFACE Such flows are ...

    www.damtp.cam.ac.uk/user/mem/FLUIDS-IB/waves.pdf
    19 Oct 2013: iσζ̂ kA sinh kh = 0. and from the second (pressure) (). gζ̂ iσA cosh kh = 0. Regarding these as a system of two linear algebraic equations for the two unknown constants ζ̂

Refine your results

Search history

Recently clicked results

Recently clicked results

Your click history is empty.

Recent searches

Recent searches

Your search history is empty.