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www.damtp.cam.ac.uk/user/lauga/papers/8.pdf26 Jul 2013: also include an induced electrophoreticcomponent,24 proportional to their zeta potential and thestreaming electric field. ... Up(z) ) Uhydro(z) Uelec(z) UkBT (24). Uhydro(z) ) [1 - O(ad)]UPD(z)ex (25). -
htl4.dvi
www.damtp.cam.ac.uk/user/tong/relativity/htl4.pdf27 Feb 2013: Ann travels at a speed given. by β u/c = 24/25 in the x-direction for seven years and then comes back at the. -
Interface_2012
www.damtp.cam.ac.uk/user/lauga/papers/64.pdf26 Jul 2013: we employ insteadthe full non-local SBT [24] to study the hydrodynamics ofthe superhelical swimmers. ... Þ. hþðh. (Þð%Þ. j Uþ(Vj=V. ðj U((Vj=VÞð%. Þ. Aedes. notoscriptus. 0.24. -
On the approximation of spectra of linear operatorson Hilbert ...
www.damtp.cam.ac.uk/research/afha/people/anders/JFA_Final.pdf5 Oct 2013: The second inclusion follows by Theorem VIII.24 ([RS72], p. 290)if we can show that PnAPn A in the strong resolvent sense. ... 11. Proof. Now, (i) follows from the fact that A1,n A strongly (see Theorem VIII.24 in [RS72],p. -
8 Magnetic confinement and the sharp tachopause MICHAEL E. ...
www.damtp.cam.ac.uk/user/mem/papers/SQBO/original-preprint-before-copy-edit-damage.pdf19 Oct 2013: vertical shear u/z with a proportionality coefficient νe, (8.24) be-. low, that is approximately constant like an ordinary viscosity. -
Comparative Hydrodynamics of Bacterial Polymorphism Saverio E.…
www.damtp.cam.ac.uk/user/lauga/papers/48.pdf26 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, -
Optimal feeding is optimal swimming for all Péclet numbers ...
www.damtp.cam.ac.uk/user/lauga/papers/59.pdf26 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. -
Geometric transition in friction for flow over a bubble ...
www.damtp.cam.ac.uk/user/lauga/papers/25.pdf26 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. -
Global warming preceded by increasing carbon dioxide concentrations…
www.damtp.cam.ac.uk/user/mem/shakun-co2-temp-lag-nat12.pdf8 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., -
Spatial and temporal evolution of injected CO2 at the Sleipner Field, …
www.damtp.cam.ac.uk/user/jneufeld/pubfiles/Boait-2012.pdf4 Nov 2013: 8 of 21. [24] Thus, disentangling the effects of varying reflectioncoefficient and signal strength is not straightforward, espe-cially when tuning effects are important.
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