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  2. www.damtp.cam.ac.uk/user/gold/pdfs/teaching/double_layer_prl.pdf

    www.damtp.cam.ac.uk/user/gold/pdfs/teaching/double_layer_prl.pdf
    10 Apr 2011:
  3. 8 Feb 2011: CC†] = 0 so thatwe may take CC† = 1.The matrix B is defined by BγµB1 = (γ0,γ). ... in question 1 with also C†C = BB = 1.Show that, if X is matrix acting on Dirac spinors,.
  4. nis2.dvi

    www.damtp.cam.ac.uk/user/na/people/Alexei/papers/nis2.pdf
    1 Sep 2011: The general problem is to nd the complete collection G = f(A;B)g of sharpconstants in (1.1) which are dened as(1.2) A A0 := inf(;)2 ; B := ... Bojanov, ed.), SCT Publishing, 1994, pp. 192{204.5. S. B. Stechkin, Best approximation of linear operators,
  5. Multicellularity and the functional interdependenceof motility and…

    www.damtp.cam.ac.uk/user/gold/pdfs/multicellular.pdf
    10 Apr 2011: 1. Enquist, B. J. & Niklas, K. J. (2001) Nature 410, 655– 660.2. ... Schulz, H. N. & Jørgensen, B. B. (2001) Annu. Rev. Microbiol.
  6. Concentration Dependence of the Collective Dynamics of Swimming…

    www.damtp.cam.ac.uk/user/gold/pdfs/sokolov_prl.pdf
    10 Apr 2011: b). Vector fields for velocity V (c) andorientation (d) for the configuration shown in image (b). ... KrZdr0. Z 20d hVr0 Vr r0ihVr0i2:. The correlation length was extracted from Kr by a fit toan exponential, Kr expx=L B, B const.
  7. 10 Apr 2011: F = qE qc. pm. B (B)m. (6)We now introduce into (4) and (5) the following representation for f1,. ... iη. t= 1. 2m. (iη e. cA. )2 e eη. 2mcσ̂ B, (38).
  8. Boundary layer model for vortex fingers in type-II superconductors ...

    www.damtp.cam.ac.uk/user/gold/pdfs/vortex_fingers.pdf
    10 Apr 2011: time in units of th = Cd / h, currents inunits of jc0, and fields as b = B / B1, B1 = 4Jc0Lh / c. ... Blatter, M. V. Feigel’man, V. B. Geshkenbein, A. I. Larkin,and V.
  9. einstein_brownian

    www.damtp.cam.ac.uk/user/gold/pdfs/teaching/einstein_brownian05.pdf
    10 Apr 2011: holds. B B 'But from this and the last equation obtained itfollows that.
  10. 10 Apr 2011: $&' &( ) ,-/.01324/56378/9:;%<=?>A@B CEDFHGJIKLMNPORQTSUSWVYXZ[]%_Aa/bcAdefAggAhiAjkl/mnAop/qrs%tuAuWvw x%yzY{|}JP W WW P ¡¢£¤ ¥«ªHµº º» ¿ÀRÁÂÃÃÅÄÆÇÄ ÈÉËÊÌ?ÍÎ ÏÑÐÅÒÒÓ Ô. ... $#&%' (),-. /0123456798 :<; =?> @&ACB?D EEF
  11. Mathematical Tripos Part III 2007–08Fundamentals of Atmosphere–Ocean…

    www.damtp.cam.ac.uk/user/mem/III-NOTES/mcintyre-fund-atm-oc-dynamics-exs-3.pdf
    15 Jul 2011: 12 f ). Allow fora sloping bottom boundary z = b(x, y), taking care to distinguish between the layer depth h andthe free-surface elevation ζ(x, y, t). ... b = b(y) =. {. ǫa, y > aǫy, |y| < a.

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