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26 Jul 2013: Typicalvalues for b range from $%1 for bacteria like E. coli,6 $0for Volvox and artificially created squirmers17,24,27 to $þ1for Chlamydomonas.19.

26 Jul 2013: Received 24 June 2003; accepted 11 February 2004; published online 1 July 2004! ... 24! Here we effectively demonstrate that these ideasalso apply as well to slowly varying flows.

26 Jul 2013: Thesecond mode (n2) defines the local stress applied by theswimmer on the surrounding fluid.8,24. ... cðr; lÞX1m0. CmðrÞLmðlÞ: (26). Substituting Eq. (26) into Eqs. (24) leads after projection on.

26 Jul 2013: We also plot in Fig. 3 the results ofour model for both surface coverage considered in the twoprevious studies: = 0.43 dashed line and = 0.68 solidline.24.

26 Jul 2013: Flexible propeller10L 24 mm. Umax z 94 f 10 HzU z 22 mm s1a. ... The dimensionlessboundary conditions are. N(s 0) 0, (24). M(s 0) 0, (25).

26 Jul 2013: h2. 2 ̄. 3 ̄ ̄̄. 24. III. RELEVANCE TO GASTROPOD CRAWLING:IMPACT OF RHEOLOGY ON LOCOMOTION COST. ... Zool. 24, 231984. 27M. W. Denny, “Invertebrate mucous secretions: Functional alternatives tovertebrate paradigms,” Symp.

26 Jul 2013: F (r ) = C1 Iλ(kr ) C2 Kλ(kr ), (24). ... Applying the condition that p̂ is finite at r = 0 to equation (24)eliminates Kλ as a solution for F.

26 Jul 2013: 24 represents aweak constraint on the validity of neglecting forces from theintermediate region. ... Furthermore, more systematicobservational studies are needed to identify which watersnail species exhibit which modes of “inverted crawling.”

29 May 2013: Although very dif-ferent in size and composition, these systems are oftenjointly termed ‘‘active’’ fluids, for which there is now arange of continuum theories [12,14–24]. ... 2(d)] we observe the linear scaling z Exy=2,with 24 m being roughly

19 Oct 2013: 24. The oldest strain of such non-conformism is Calvinist, Puritan.

24 Apr 2013: models for active systems have beenproposed [2, 17–24], but most of them have yet to be tested against experiments [14, 25]. ... where. M =(. 2 A 00 0. ) (0|k|2 2|k|4 i λ0kxv0)I (24).

17 Jul 2013: second fluid withoutthe membrane [23,24]. ... 174, 381 (1987).[24] K.SugiyamaandM.Sbragaglia,J.Eng.Math.62,35(2008).[25] F. G. Woodhouse and R. E. Goldstein, J.

26 Jul 2013: J. Fluid Mech. (2011), vol. 681, pp. 24–47. c Cambridge University Press 2011doi:10.1017/jfm.2011.223. ... 5.24). where b is some real constant and. I (ζ, Ca) =1.

26 Jul 2013: 24–26 The second type of surface, less stud-ied, is one where the solid is the continuous phase, and theliquid/air contact occurs on isolated domains Fig. ... whose solution is. f xns, f yns =An, Bn. 1 s21/2 1 s 1 , 24.

26 Jul 2013: wall and crash into it. Furthermore, the authors proposed a. Submitted June 24, 2005, and accepted for publication September 28, 2005. ... xx Þ! ; (24). which is very similar to that given by the simple physical.

4 Oct 2013: Xn(x) = Bn sinnπx. Lλn =. n2π2. L2. (24). Note that the first set eq. ... 24) the timeequation gives. Tn(t) = Cn exp(Dn2π2. L2t). The general solution for θ̂ (with odd initial condition θ̂(x, 0)) is thus.

26 Jul 2013: See the article by Howard Berg, PHYSICSTODAY, January 2000, page 24.) The effect is not un-like a corkscrew pulling itself through the cork of awine bottle, except that the flagellum

26 Jul 2013: a). Re 29, onset of local absolute instability at x 1:24 (b) Re 47,onset of linear global instability, (c) Re 100, (d) Re 175, (e)Re 235, (f) Re

26 Jul 2013: minima in the free energy see Ref. 24 for a textbook treat-ment. ... Rev. E 76,. 061914 2007.24 M. Kardar, Statistical Physics of Fields Cambridge University.

19 Oct 2013: Mon.Not. R. ast. Soc., (submitted)24. Nesme-Ribes, E., Sokolo, D., Ribes, J.C. &

26 Jul 2013: 9500 Gilman Drive, La Jolla CA 92093-0411, USA. (Received 11 January 2013; revised 13 March 2013; accepted 24 April 2013).

26 Jul 2013: f2x =. 2π. 0. 〈τ2xy 〉|y=0 dx, (3.24). and only the mean component of the second-order stress, 〈τ2xy 〉, contributes tothe net force.

26 Jul 2013: 2000 Generic aspects of axonemal beating. New J. Phys. 2, 24.

19 Oct 2013: 24. NB: Fluid initially at rest is an important special case.

26 Jul 2013: m=0. (q m)!(α1,0ρ). m m!(q m)! ), (3.24). 12 S. Michelin and E. ... general solution takes the same form, see (3.24). By matching c̃p, C̃p and C̃0 up to O(ε3/2), the values of b̃0, ãp and ap can then bedetermined, and

26 Jul 2013: 4. Experimental Section. Reagents and Solutions: Cupric sulfate pentahydrate, nickel(II) chloride hexahydrate, nickel(II) sulfamate tetrahydrate, gold (Oro-temp 24 RTU RACK) and silver (1025 RTU @ 4.5 Troy/gallon) ... HeLa cells were plated 24 h earlier

4 Oct 2013: u,Av) = (Bu,v) (24). (as you can easily check using the property that (Bu)† = u†B†). ... 36) of the µn values.). 1B Methods 24. 2.5 Parseval’s identity and least square approximations.

5 Oct 2013: R. Driscoll, “Wavelet-encodedMR imaging,” Magn. Reson. Med., vol. 24, pp. 275–287, 1992.

5 Oct 2013: R. Driscoll, “Wavelet-encodedMR imaging,” Magn. Reson. Med., vol. 24, pp. 275–287, 1992.

26 Jul 2013: Following classical modelingapproaches [22–24], the deviatoric stress τ can be splitedinto two components, the viscous solvent stress (τ s ) and thepolymeric stress (τ p); τ s is thus given by. ... 1: Fluid Mechanics 2nd ed. (WileyInterscience, New

19 Oct 2013: variable between about 24 and 36 months — owe their existence and timing to the ir-. ... cycle taking, of course, about 24 to 36 months. The time-altitude contour plot of the.

16 Oct 2013: m=1. α(m)(t)δmn. = α(n)(t) , (1.24). reproducing (1.23) apart from renaming the indices. ... 24. Chapter 2. 2. Groups. This chapter contains the second set of syllabus items, together with a fewitems anticipating the third set:.

26 Jul 2013: 0 aRFU 0 , 24. Text = 0 0 00 0 aRFU0 aRFU 0. ... Optimal III 0.24 3.34 12.6 2.6 7.9 0.336. Optimal IV 0.49 3.20 16.9 2.6 5.4 0.465.

4 Nov 2013: 10 7.37 0.01 401 21.8 1.73 11111 6.63 0.01 401 20.7 1.69 10912 20.35 0.03 401 36.2 2.24 144.

27 Aug 2013: pointed) end to its plus (barbed) end.These cables are bound to the cortically fixed chloroplasts atthe cell periphery (24) in a “barber pole” twist, generating flowspeeds of 50–100 ... Characean algae. Proc Natl Acad Sci USA 73(1):165–167.24.

26 Jul 2013: 2, 0.5) (1.1, 0.4)f (2.2, 0.53) (0.91, 0.29)g (2.3, 0.45) (0.69,1.52) (1.24, 0.52) (1.14,

26 Jul 2013: J. Fluid Mech. (2003), vol. 489, pp. 55–77. c 2003 Cambridge University PressDOI: 10.1017/S0022112003004695 Printed in the United Kingdom. 55. Effective slip in pressure-driven Stokes flow. By ERIC LAUGA AND HOWARD A. STONEDivision of Engineering

26 Jul 2013: Other simple propulsivesystems proposed for locomotion at zero Reynolds numberinclude a deformable two-dimensional loop;18 systems oftwo,19–22 three,21,23,24 or N spheres;25 an oscillating body ... R2. z c. R1, 24. where c = a2 b2, r = x2 y2, r̂ =

12 Aug 2013: Cont. Dynamical Sys. 28, 1345–1367. 24. Figure 3.4: The errors for h(t) for ω = 200π (top row) and ω = 2000π(bottom row): from the left 0, 1 and

5 Oct 2013: xm} is a grid of mequispaced points in [1, 1]. In [24] it was shown that. ... Proc. SPIE, 7535, 2010. [24] D. Coppersmith and T. Rivlin. The growth of polynomials bounded at equally spaced points.

19 Oct 2013: Fluid. Dyn. Res., 24, 375–404.Janssen, P. A. E. M. 1982 Quasilinear approximation for the spectrum of wind-generated.

26 Jul 2013: CA 92093-0411, USA2LadHyX, École Polytechnique-CNRS, 91128 Palaiseau Cedex, France. (Received 28 April 2003 and in revised form 24 March 2004). ... By selecting ξinf = 15.7 andξsup = 24 and defining N = 140 gridpoints via this approach, adequate

4 Nov 2013: Fluids 24, 117102 (2012) Effect of fluctuations on the onset of density-driven convection in porous media Phys. ... Fluids 24, 114102 (2012) Absence of subcritical instabilities and global nonlinear stability for porous ternary diffusive-convective

4 Nov 2013: FC = 24/3λD. (gβ̃. Dν. )1/3(C0 Ci )4/3, (4.3). where λ is a constant. ... 1 9.3 0.1 9 1 10.47 3.73 0.25 unstable230106D 9 1 3.19 0.02 27 0.3 10.47 3.73 0.24 unstable230106E

9 Jan 2013: N 2)(7N 11)ρ (N 1)(7N2 27N 24)ρ2. (N 3)(N 2)(2N 1)ρ3],.

4 Nov 2013: Leakage. † Present address: Department of Mechanical Engineering, MIT, Cambridge MA 02139, USA.‡ Present address: OCCAM, Mathematical Institute, 24-29 St Giles’, Oxford OX1 3LB, UK.

8 Jun 2013: simulations. g, North Atlantic sediment core OCE326-GGC5 231Pa/230Th (ref.24). Temperatures are given as deviations from the early Holocene (11.5–6.5 kyr ago) mean. ... Paleoceanography 18, 1087 (2003). 24. McManus, J. F., Francois, R., Gherardi, J.-M.,

4 Nov 2013: φ̃0(0; λ̄) =. h(0, y)2 dy. (3.24). The solid curve in figure 5 shows the result of substituting the value of φ̃0(0; λ̄)found in this way

26 Jul 2013: Received 24 May 2002; accepted 17 December 2002; published online 30 June 2003.

26 Jul 2013: to the cre-ation of flagella bundles propelling the cells forward as theyswim, as well as the disruption of such bundles when thecells change their swimming direction.22–24. ... U =h̄. 2f x. s. 24. Noting that d / dt = U we therefore get an equation