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The effect of particle interactions on dynamic light scattering from…
www.damtp.cam.ac.uk/user/hinch/publications/JFM167_131.pdf23 Jul 2009: 1 ) , ( 2. 2 ) ; and for the case ka 4 1 and a general form of P by Batchelor (1983). ... pO as r / a c o , (3.24). and P-D;Vp = ikD,.P on r = 2a. -
Numerical studies of the influence of the dynamic contact ...
www.damtp.cam.ac.uk/user/hinch/publications/PhysFluids_21_072102.pdf28 Sep 2009: respectively. These parameters ka and krare determined as the best fit parameters to the measurement. ... 24, pp. 273–285. 25J. Li, “Calcul d’interface affine par Morceaux piecewise linear interfacecalculation,” Acad. -
The millennial atmospheric lifetimeof anthropogenic CO2 David Archer…
www.damtp.cam.ac.uk/user/mem/archer-carbon-tail08.pdf30 Aug 2009: 2007) 24–26% 40%(Ridgwell and Hargreaves 2007) 34%(Montenegro et al. 2007) 52%. ... Kvenvolden KA (1988) Methane hydrate—a major reservoir of carbon in the shallow geosphere. -
Raining into shallow water as a description of the collapse of a…
www.damtp.cam.ac.uk/user/hinch/publications/JFM554_259.pdf8 Jul 2009: This should be compared withLube et al.’s (2005) results who found for a > 1.15 a similar dependence with a:h/r0 = ka. ... 2 a1.02r30. In both geometries, the final slope at the front is much lower than the slope thatwould be given by an internal angle
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