Search

20 Sep 2009: May form part of a larger settlement. • Requires 1,200 hectares or more. ... Norwich 14,100. • Broadland 12,200. • South Norfolk 11,200. • Ipswich 10,000. •

10 Jul 2009: on. July. 10,. 200. 9Pu. blis. hed. on J. anua. ry 1. ... 10,. 200. 9Pu. blis. hed. on J. anua. ry 1. 5, 1.

12 Nov 2009: R = 200 mm,h = 15 & 7 mm,η0 = 1 mm,λ = 50&70 mm,d = 0.5 mm,µ = 0.05 & 1 Pa s. ... L = 2 m, h = 11 & 16 mm, U0/ω 200 mm.

3 Sep 2009: 9. Fluid Dyn. Res. 41 (2009) 051403 N G Berloff. t=0 t=200. ... 12. Fluid Dyn. Res. 41 (2009) 051403 N G Berloff. t=0 t=200.

13 May 2009: This behaviour can be expected, since large values of. 23. 0 5 10 15 200. ... 5. 10. 15. 20. 25. 30. 35. 40. α. β. 0 5 10 15 200.

13 Jul 2009: It is interesting to note that at breakup a jet of a solution of 200 p.p.m. ... 51. They showed that several centimeter long strings of a 200 p.p.m.

8 Jun 2009: We. are therefore confident that the 100 100 grid used in this article is sufficiently accurate, whilecosting 116 th that of the 200 200 grid. ... Diameter (50x50)Diameter (100x100)Diameter (200x200). FIG. 19: Time evolution of droplet diameter using 50

30 Aug 2009: The atmosphere todaycontains about 200 Gton C in excess of the natural 1,750 value. ... time for the uptake would be determined by dividing 200 Gton C by 2 GtonC/year, to yield about 100 years.

8 Jul 2009: The field of view is 600 mm long and its lowerboundary is located at 200 mm above the gate valve thisregion of interest is initially saturated only with the heavytransparent solution. ... R. Soc.London, Ser. A 200, 375 1950. 5E. E. Zukoski, “The

10 Jul 2009: 8 confirm thscaling law in the convective-diffusive regime withC. 200. Eliminatingl between Eqs.9! ... 200–207. 2G. K. Batchelor and J. M. Nitsche, ‘‘Instability of stationary unbound.

31 Jul 2009: http://journals.cambridge.org Downloaded: 31 Jul 2009 IP address: 131.111.16.227. 200 E. J. ... It is only after y / D = 200 that the viscosity as calculated from the exact.

13 Jul 2009: A number of 200 particles was injected for eachexperiment to give good statistics. ... For each experiment withpackets of a given size, a total 200 particles were injectedover several packets.

3 Sep 2009: nismsforcontinuouslyandcoherentlyrefillingtheBECsthesephe-nomena cannot be observed in atomic BECs. Losses are alwayspresent in BECs [200,201,13], and can even be induced throughthe use of focused electron beams [202].

10 Nov 2009: In the present experiments, the recording begins 200 safter the transit of the front and lasts for t = 200 s.

21 Apr 2009: Figure 1: Absolute error |f (x, y) FN [f ](x, y)| for 1 x, y 1 (top row), 0.9 x, y 0.9 (bottom row) andN = 50, 100, 200. ... 200, for (x, y) = ( 34 ,23). (thickest line),(78,3.

10 Jul 2009: F 6. Time-lapse picture of the development of the interface at t 21.20, 21.57, 21.82, 22.00,22.12 and 22.20 with N 200 and γ ... J. Hinch. F 7. Time-lapse picture of the development of the interface at t 21.18, 21.53, 21.77,

24 Aug 2009: He calculated orientation-dependent angle averages for unrestricted aspect ratios, r , and values of y / D ranging from zero t o 200, where y is the shear rate. ... The latter value of 200 essentially represented the limitrs of storage capacity for the

13 Jul 2009: Non-Newtonian Fluid Mech., 44 (1992) 229-265 251. 6 I I I /. 5-. 4- PIPS. 1 ________.__.____________.-.----. No strand. 0 0 200 400 600 800 1000.

6 May 2009: Prandtl’s ratio N/f, whose value at top left is 100 (5 200 km/2 km).

26 May 2009: is even more important to achieve practical inexpensive results. We used stretchedgrids of size up to 200 200, in which the smallest and largest grid spacings differedby a factor of up