Search

Search Funnelback University

Search powered by Funnelback
11 - 30 of 37 search results for `B b cos` |u:www.damtp.cam.ac.uk
  1. Fully-matching results

  2. Optimal feeding is optimal swimming for all Péclet numbers ...

    www.damtp.cam.ac.uk/user/lauga/papers/59.pdf
    26 Jul 2013: mal a or b at given Pe). Starting from a random initial condi-. ... For t 1, the swimming stroke,. b cos t b1 þ sin t bk; (44).
  3. §4 FLOWS WITH A FREE SURFACE Such flows are ...

    www.damtp.cam.ac.uk/user/mem/FLUIDS-IB/waves.pdf
    19 Oct 2013: exponential counterpart, cos(µ) = 12 (e. ... Then φ̂ = φ̂(x, z) exp(kz) cos(kx),equivalent to a single pair of progressive deep-water waves travelling in the x directions.
  4. 26 Jul 2013: 3) leads to 2p = 0. A solutionof the harmonic equation for the pressure is, at the first order inkb, p = p1(r,θ) (A cos s B sin s) with s = ... xi = x0 b cos β sin (s φ) , (34)yi = y0 b sin β sin (s φ).
  5. §3 IRROTATIONAL FLOWS, aka POTENTIAL FLOWS Irrotational flows are ...

    www.damtp.cam.ac.uk/user/mem/FLUIDS-IB/irrot-rot.pdf
    19 Oct 2013: expected. (ii) all A’s, B’s zero except A1:. φ = A1r cos θ = A1z , u = φ = A1ez. ... z. (iii) all A’s, B’s zero except B1:. φ =B1 cos θ.
  6. 1B Methods 62 . 1B METHODS LECTURE NOTES Richard ...

    www.damtp.cam.ac.uk/user/examples/B8Lc.pdf
    4 Oct 2013: B(cos(1 ξ)) A cos ξ = 1. Solving these two equations for A and B gives the Green’s function to be:. ... Then. I. λ=. 0. cos(λx)eαxdx = <(. 0. e(αλi)xdx. ),. = <[e(αλi)x.
  7. PHYSICAL REVIEW E 87, 023015 (2013) Interface pinning of ...

    www.damtp.cam.ac.uk/user/jneufeld/pubfiles/Zhao-2013.pdf
    4 Nov 2013: r1 = [2 cos(φ1)]cos(φ1 θ ). d. 2, (3). r2 = [2. ... 2 cos(φ2)]cos(φ2 θ ). d. 2. (4). In drainage, θ = θr and the drainage capillary entrypressure corresponds to the minimum radius of curvature r1:rdr = minφ1 r1(φ1; θr ).
  8. 26 Jul 2013: uy=y1 = 1 ṠR cos y=y1 , 11a. vy=y1 = ṠR sin y=y1 , 11b. ... uy=y2 = 1 ṠR cos y=y2 U , 11c. vy=y2 = ṠR sin y=y2.
  9. PHYSICS OF FLUIDS 25, 071904 (2013) The wobbling-to-swimming…

    www.damtp.cam.ac.uk/user/lauga/papers/81.pdf
    26 Jul 2013: B]lab = B0[cos(ωt ), si n(ωt ), 0]T. (2). Experimentally this magnetic field provides an external torque to the head of the artificial flagellumbut no external force. ... ξ̄‖ =ξ‖. µ= 2π. ln(2 cos θ/γ ) 1/2,. ξ̄ =ξ.
  10. Inevitability of a magnetic �eld in the Sun'sradiative interiorD. …

    www.damtp.cam.ac.uk/user/mem/oldftp/solar-nature.pdf
    19 Oct 2013: be similar to that of the spherical harmonicP4(cos ), and so we adopt the estimate L 4:5. ... Then equations(1) and (2) imply T=T r2c 2i =gL and juj 2g T=2N2T , where we have takensin cos 21=2.
  11. flm469.dvi

    www.damtp.cam.ac.uk/user/lauga/papers/4.pdf
    26 Jul 2013: a) The no-shear regions are transverse to the flow direction. (b) Theno-shear regions are parallel to the flow direction. ... Thesolution to this problem was derived by conformal mapping in Philip (1972a) and isrecalled in Appendix B.
  12. Bulletin of Mathematical Biology (2010) 72: 973–1005DOI…

    www.damtp.cam.ac.uk/user/lauga/papers/39.pdf
    26 Jul 2013: 23). This equation can be integrated in t as. e(j )i (t, τ) = a(j )i (τ) cos(t) b(j )i (τ) sin(t). ... A(τ) cos(2t) B(τ) sin(2t). C(τ) cos(t) D(τ) sin(t) E(τ), (28).
  13. 26 Jul 2013: 4 m1=1. m2=1. 1. m12 m221 m12. 2m12 m2. 2cos 2 b m1x cos 2 b m2y , 18from which we note that large contributions to Eqs. ... cos m2w W. m1=1. 1m Cm 12m1 12 ln S sdwds , 20b.
  14. Floppy swimming: Viscous locomotion of actuated elastica Eric…

    www.damtp.cam.ac.uk/user/lauga/papers/16.pdf
    26 Jul 2013: x=0, 59. with boundary conditions. y10, t = 0,y1x. 0, t = cos t,2y1x2. ... 1 cos 12 102 Re1010.66. When the swimmer does not have a body, R FU = 0, we obtainthe “elastic scallop,” the flexible version of the two-armswimmer discussed by Purcell
  15. C1SM05503H 8169..8181

    www.damtp.cam.ac.uk/user/lauga/papers/56.pdf
    26 Jul 2013: The scale bar is 10 mm. (b)Speed-frequency characteristics of flexible nanowire motors. ... ment as. x(s, t) b(s)cos[t f(s)], (29). y(s, t) b(s)sin[t f(s)], (30).
  16. The effect of a fissure on storage in a porous medium

    www.damtp.cam.ac.uk/user/jneufeld/pubfiles/Neufeld-2009-2.pdf
    4 Nov 2013: vf (x, t) = kf. μ. ρg(h b). b= φγ kf. ... dp. dx. cos mπ 1cosh mπh/d. (B 2). correcting a factor of 2 from Happel & Brenner (1991).
  17. Propulsion in a viscoelastic fluidEric Laugaa� Department of…

    www.damtp.cam.ac.uk/user/lauga/papers/18.pdf
    26 Jul 2013: 1x, = U1ey , D4a. 1x,0 = b cos x tex a sinx t ey , D4b. ... UN =12 b. 2 2ab cos a2. D17. Allowing tangential motion does therefore reduce the swim-ming speed by the same amount, and the final results of thepapers, Eq.
  18. flm563.dvi

    www.damtp.cam.ac.uk/user/mem/papers/RECOIL/remote-recoil.pdf
    19 Oct 2013: where θ is the polar angle and where the outward normal n̂ now has Cartesiancomponents (cos θ, sin θ). ... Then, noting that the Cartesian components of U atr = b are ( sin θ, cos θ)Γ /(2bπ), we can easily evaluate the integral.
  19. atsc_56_2405.1214_1235

    www.damtp.cam.ac.uk/user/mem/papers/SMINV/inv-mn00.pdf
    19 Oct 2013: Further detailsof the method used can be found in appendix B and inN88. ... 4, and (b) that when judged by comparison withthe reinitialized primitive equation integration, the nor-.
  20. 26 Jul 2013: xm(x, t) =x 'a cos(x Re ω(t)t φ)and ym(x, t) = 'b sin(x Re ω(t)t),. ... xy|y=0 b sinx. 2ψ1. y2|y=0, (3.15). ψ2,x |(x,0) = a cos(x φ)2ψ1.
  21. Beyond consistent reconstructions: optimality and sharp bounds for…

    www.damtp.cam.ac.uk/research/afha/anders/OptimalityFinal.pdf
    5 Oct 2013: As is evident, the quantity cos (θn,n) is exponentially small in n. ... 100. 106. 1010. (a) (b) (c). Figure 1: (a): cos(θn,n) against n.

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.