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13 Jul 2009: Downloaded13Jul2009to131.111.16.20.RedistributionsubjecttoAIPlicenseorcopyright;seehttp://pof.aip.org/pof/copyright.jsp. and depth of the vessel were uniform to within 0.05 cm. ... the Van der Waals force and the drag force was 20 000times the Van der

8 Jul 2009: Experiments were performed in glass-wall vessels of dif-ferent cross sections 20 20 cm2, 10 10 cm2, and4 10 cm2 but filled with the same fluid height of 40 cm. ... The line indicates the best linear fit.The different cross sections presented are 20 20

14 Jul 2009: Hinch. 40. 30. 01. 20. 10. 5 10 15 0 5 10 15. ... 1. o. 0.8. 0.6. D 0.4. 0.2. 0. SL 20. 10.

31 Jul 2009: J. 20, 128. MARUCCI, G. & ACIERNO, D. 1974 J. Polymer Sci. (

18 Jul 2009: 20 (t) 2iS0(t)[C0(t) e. itC0(0)]ψ30 (t) S. 30 (t)ψ. 40 (t)}. ... 20. 0 1 2 30. 1. 2. t. y(t). 0 1 2 30.05.

24 Aug 2009: 31). For r > 20 and < 0-05 respectively, the two sets of values a,gree well. ... With smaller particles, a relatively large number density could be allowed without violating any of our conditions (20), (21), or (22).

13 Jul 2009: 20. lz- 40 -3 3 :g 60. tl E a Q ) 80 78. ... Time, t”. Nicolai et al. Downloaded 13 Jul 2009 to 131.111.16.20.

1 Dec 2009: 0)p1,1 cos 2ωt (2.20). The equation and initial conditions forp2,0 are obtained when analysing theO(ω2)terms. ... The termψ2(t) can be obtained from (2.20) substituting all the data corresponding to thefunctionsh andf in this example.

13 Jun 2009: 20 40 60 80 100! 10! 5. 5. 10. 20 40 60 80 100! ... 20 40 60 80 100! 5. 5. 10. 20 40 60 80 100!5.

10 Jul 2009: 20) except that the pressure gradient 1 p is negligible so that the momentumequation becomes. ... cn µ2(1p)/[p(3p)]s. 0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 20.

8 Jul 2009: z,t0) = 1 ε cos(2πz/20). Let us compare the flow obtained withsmall surface tension, Oh = 3.16 and De = 94.9 and with a. ... 20] J. Étienne, Simulation numérique d’écoulements gravitaires à fortesdifférences de densité, Application aux

21 Apr 2009: sets. For reasons that we makeclear, modified Fourier approximations are best analysed in so-called Sobolev spaces of dominating mixedsmoothness, [20]. ... f(x,y) = esin 6x(y tan2(1 y2). ). 20. 50 100 150 50 100 150.

8 Jul 2009: The forces acting between two col-liding grains are computed from the normal overlap, n, andthe equations of motion displacement and rotation are inte-grated using the Verlet method 20. ... Garcia-Rojo, H. Hermann, and S. McNamaraStuttgart, 2005, p. 853.

10 Jul 2009: 50. 40. 30. 20. 10. 0. 0 0.5 1.0. 0. –1000. ... flow rates and decreases quickly with q towards an almost constantvalue of 20%.

14 Jul 2009: Y. 1.0. 0.5. 0. 0.30. 0.25. 0.20. z 0.15. Shear-induced dispersion in a suspension of spheres. , ... y - yo and z - 20.

6 May 2009: The heavyhorizontal lines mark depths z with nominal values 20.21, 20.9 in the dimensionless units used in V07. ... z 5 20.21, in a plot whose dimensionless length and width are45.5 units.

14 Jul 2009: Rallison and E. J. Hinch. 0.20. 1 2 3 4 5 0 a. ... http://journals.cambridge.org Downloaded: 14 Jul 2009 IP address: 131.111.16.227. 322. 0.20 r.

16 Oct 2009: A long pass interference filterwith a 10 nm transition ramp centered at 620 nm (KnightOptical, UK) was used to avoid any phototactic response[20]. ... 19] D. L. Kirk and M. M. Kirk, Dev. Biol. 96, 493 (1983).[20] O.

23 Jul 2009: o. 0.8. 0.6. 0,. 00. -. 0.4. 0.2. 0. 0 5 10 15 20 25 30 St. ... 5 10 I5 20 St. FIQURE 13. The minimum distance of approach of the deformed surfaces.

23 Jul 2009: 1.3 28.6 0.966 1.20 0.717 0.846 2 13.6 0.693 0.825 0-526 0.583 5 6.58 0.529 0.574 ... 10 4.48 0.468 0.473 0.327 0.335 20 3.30 0.406 0.406 0-285 0.287 30 2.85 0.378 0.376 0.263

31 Jul 2009: The dashed vertical line represents theintrinsic frequency difference observed in cell models (20). ... both cameras with custom Labview (National Instruments, Austin, TX) routines at 20 fps and.

8 Jul 2009: velocities. The study is performed in a 4 m long transparent tubewith an internal diameterd= 20 mm that can be tilted to allangles between vertical and horizontal. ... Experimentally, the frontvelocity Vf is 20% larger than this theoretical value.

13 Jul 2009: 1, January 1994 Kurowski et a/. 115. Downloaded 13 Jul 2009 to 131.111.16.20. ... 1, January 1994 Kurowski et a/. 117. Downloaded 13 Jul 2009 to 131.111.16.20.

10 Jul 2009: top of the tube.The bed was operated in this expanded state for about 20 min to remove any smalltrapped air bubbles or impurities. ... 589 0.5438 E a 2 19 12.0 0.20 3.30 0.02 0.614 0.575 0.544.

31 Jul 2009: 20) where the ro transformation is simply T = T - wt with w = yr/(r2 1).

26 May 2009: to 20 in the horizontal direction, and up to 40 in the verticaldirection. ... 100(a) (b). 50. 20. 10106 107 108 109 1010. Shear-freeRigid. Ra.

10 Nov 2009: Each velocity fieldcontains 160 50 velocity vectors and the field of view is64 20 mm2. ... plane turbulent stress ũw̃ and its dependence with respectto z̃ are similar to those of w̃2, its magnitude being onlyabout 20% that of ũ2.

12 Aug 2009: 5. being settled by 1q(j)n. For example, if n= 5 and m= 20, there are 9 pairs{p(j),q(j)}, generated in the order {1, 2}, {2, 3}, ... 4.23). 19. Moreover, the definitions (2.8) and (4.20) with x0 =xk yield the diagonal elementseTj Aej =. 12‖y. jxk‖4,

13 Jul 2009: Cambridge CB3 9EW, UK. Received 14 November 1996; received in revised form 20 February 1997.

21 Jul 2009: 25. 20. 15. g 10-3. 10. 5. a / '150 0 0.02 0.04 0.06 0.08. ... http://journals.cambridge.org Downloaded: 21 Jul 2009 IP address: 131.111.16.227. 30. 20. 15.

30 Nov 2009: This different rate of decay has. 20 H. Brunner, A. Iserles & S.P.

10 Jul 2009: d/z 0.20 0.15. license or copyright; see http://pof.aip.org/pof/copyright.jsp. ec. mthcta. mowethindtal-. ... Aver-ages are taken over all the particles including those in the sediment andabout 20 realizations.

8 Jul 2009: The heavy horizontallines mark depths z with nominal values 20.21, 20.9 in the dimensionless units used in V07. ... z 5 20.21, in a plot whose dimensionless length and width are45.5 units.

10 Jul 2009: 1.43 mm would therefore require an angular velocity of ω = 20 000π.

8 Jul 2009: Our initial hopes were to find a correctionof 2e to remove the 20% shortfall in the previous predic-tions. ... First, variousquantities were seen to have a second-order behavior whenthe spatial resolution was changed throughny= 10, 15, 20,and 30.

23 Jul 2009: 3.11). dfl = - k2Do f, ik. [(Dt-Do/) -ikf2 (20,- Do /) Vf2 f2D, V v ] eak"n d3r, (3.12). ... provides a check on the manipulations performed here so far. Using the initial condition (3.20) forf, and substituting in (3.16) we obtain (using symmetry).

21 Jul 2009: Vjnkd2r. dt ax. (2.20). (2.21). Combining (2.20) with (2.21), we find. ... From (2.20) it then follows that. [ V 2 n3 - q cos t V3 (n.

3 Sep 2009: 20. Additional vortices can easily be included into Eq. 19 bywriting v = i=1. ... 20 for vortices along = / 2. Different combinations and different circulationsof the single vortex solutions of type I and type II are con-sidered.

24 Aug 2009: Nl(C,7):= N1(C,72n). The integration of equation (20) over r from 0 to 27r thus leads to the integral condition on No. ... Having determined No, the calculation of Nl proceeds as follows. We note, first; of all, that the non-homogeneous part of (20) is

10 Nov 2009: cell having a cross section 10 10 cm2, and C d in the cell having a cross section of 20 20 cm2 with 0 = 0.3%. ... 4 4 cm2 ,10 10 cm2 , and 20 20 cm2 with 0 = 0.3%.

10 Jul 2009: y. 0.1. 00.010. v̂. y. 0.1. 00–20. ω̂. y. 3. 00. ... y. 9. 00.20. v̂. y. 9. 00–1. ω̂–1. (a). (b). (c).

10 Jul 2009: which is for a longer line of 25 particles. Note that 20 particles have a significantrebound velocity, greater than 1% of the initial impact velocity. ... 3. 4. Figure 11. Impact by three particles. The displacements xn as a function of position along

13 Jul 2009: 0 10 20 30 40. cL. Fig. 5. Phase diagram showing the onset of pipe formation as a function of? ... Dotted lines indicates critical strain rate for stretch-coil transition. 0.20. 3 ;ij 0.15 L2.

31 Jul 2009: Hinch. 20.i.,-.----- / O (g). 0 0.2 0.4 0.6 0.8 1.0 0 0.2 0.4 0.6 0.8 1.6.

14 Jul 2009: http://journals.cambridge.org Downloaded: 14 Jul 2009 IP address: 131.111.16.227. J. Fluid Mech. (1996), t d 308, p p. 255-288 Copyright @ 1996 Cambridge University Press. 255. Computer simulations of polymer chain relaxation via Brownian motion. By

10 Jul 2009: Surface tension first appears in φ8 asα0γ. 20 tc22. Key extractions from higher-order terms of h. ... 1198 E. J. Hinch and M. A. Kelmanson. γ 0.30.20.1. /. 5. 4. 3. 2. 10. γκ. 2. Figure 1. Decay rates, κ, obtained from numerical integration of

10 Jul 2009: Received 20 June 2001; accepted 7 December 2001! A linear stability analysis is presented for the Kelvin–Helmholtz instability in a Hele-Shaw cell, ananalysis based on the Navier–Stokes equation

14 Jul 2009: parameters corresponding to rough turbulent regime (with /λ = 0.74, λ/δ = 126,2η0/λ = 0.20).

15 Oct 2009: We will consider the limit e 0 withδ = e1k (20). ... 1.3.4 Stability in the absence of an external field. The stability of the solutions to (23) of the form eiωtfω(x) was first considered in [20, 10] where it

3 Sep 2009: Lett. 77 (1996)5315. [20] S.Stringari,Collectiveexcitationsofatrappedbose-condensedgas,Phys.Rev.Lett. 77 (1996)2360. [21] V.M. Pérez-García, H.Michinel, J.I.