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flm1100081a
www.damtp.cam.ac.uk/user/lauga/papers/50.pdf26 Jul 2013: dashed lines) and 3π/4 (dashed-dotted lines), with A = 1 and B = 10. ... A/B) sin zand η2 (A/B) sin(z φ) as might be expected. -
Membrane Viscosity Determined from Shear-Driven Flow in Giant…
www.damtp.cam.ac.uk/user/gold/pdfs/membrane_viscosity.pdf17 Jul 2013: Phys. J. B 12, 589 (1999); K. D. Danov,R. Dimova, and B. ... 99, L44 (2010). [11] A. R. Honerkamp-Smith, B. B. Machta, and S. -
flm801a
www.damtp.cam.ac.uk/user/lauga/papers/30.pdf26 Jul 2013: b c d e. ii. iii. iv. Kn = 0. Kn = 0.2 Kn = 0.4 Kn = 0.5. ... Kn Kn/Knc. 1.00 10.00. (a) (b). CD. 0.2. 0. 0.4. 0.6. -
Adhesion transition of flexible sheets Arthur A. Evans1,* and ...
www.damtp.cam.ac.uk/user/lauga/papers/27.pdf26 Jul 2013: a). (b). (b) (c). (d). (c). (d). 1. 2. FIG. 8. ... New York, 1992.10 B. Chen, P. D. Wu, and H. Gao, Proc. -
A General Allometric and Life-History Model for Cellular…
www.damtp.cam.ac.uk/user/gold/pdfs/amnat.pdf7 Mar 2013: On the other hand, the demand of re-1/2 1/2 1/2 1/2B (B B ) Bsources depends on the number of cells in the colony andthe total cells ... gb Bvif 1, v p 1,dc Cv. g gb B b Bv vif! -
The decay of stabilizability with Reynolds number in a linear model…
www.damtp.cam.ac.uk/user/lauga/papers/3.pdf26 Jul 2013: V2 =¡ (1) (2) ¢ ¢ ¢ (n). ¢;. taking A = ¤ , B = B, Q = I, R = 2I and ¤ cl = ¡ ¤ ¤ , and applying the aboverelationships, it follows that (3.7 ... written in the form _À = ¤ À Bu, where the diagonal matrix ¤ contains theunstable eigenvalues -
On skew-symmetric differentiation matrices Arieh Iserles January 9,…
www.damtp.cam.ac.uk/user/na/NA_papers/NA2013_01.pdf9 Jan 2013: We must instead consider its logarithmic norm(Söderlind 2006) µ[B], namely the largest eigenvalue of the symmetric matrix B̃ =12 (B B. >). ... cussion yet, even if B is skew symmetric, we are not done yet! -
Modelling carbon dioxide sequestration in layered strata
www.damtp.cam.ac.uk/user/jneufeld/pubfiles/Neufeld-2009-1.pdf4 Nov 2013: H = h/SV , L = l/SV , B = b/SV , X = x/SH and T = t/ST ,(2.13a, b, c, d , e). ... 366 J. A. Neufeld and H. E. Huppert. B. B. Injection point. -
Global warming preceded by increasing carbon dioxide concentrations…
www.damtp.cam.ac.uk/user/mem/shakun-co2-temp-lag-nat12.pdf8 Jun 2013: a. b. c. e. f. g. d. HoloceneYDB–AODLGM. Figure 4 | Hemispheric temperatures. ... 33. Stephens, B. B. & Keeling, R. F. The influence of Antarctic sea ice on glacial-interglacial CO2 variations. -
Propulsion in a viscoelastic fluidEric Laugaa� Department of…
www.damtp.cam.ac.uk/user/lauga/papers/18.pdf26 Jul 2013: 2x,0 = a cosx t 1 x x,0 b sinx t 1. ... ̃̇1, D12we obtain, after some algebra,. 4 2 =De1De2 De1. 1 De12 b.
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