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1 - 10 of 12 search results for KaKaoTalk:PC53 24 / |u:www.itg.cam.ac.uk where 0 match all words and 12 match some words.

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  2. On the hydrodynamic interaction between a particle and a ...

    www.itg.cam.ac.uk/people/heh/Paper244.pdf
    30 Jul 2013: 24). The perturbation equations are given, at O(βN), by. 1. η.

  3. The effects of capillary forces on the axisymmetric propagation ...

    www.itg.cam.ac.uk/people/heh/Paper243.pdf
    12 Apr 2013: H = (Q/ub)1/2, (24)and the dimensionless height profile f is solely a function of y, the scaled similarity variable, definedas.

  4. doi:

    www.itg.cam.ac.uk/people/heh/Paper242.pdf
    11 Apr 2013: From the exactsolution we have. W0 =. Z2 1 (π2. 24. ... 4.24). This inner solution indeed satisfies the tip condition w0,in = 0 as Z 0, and asZ it reproduces the source term seen in (4.23).

  5. doi:

    www.itg.cam.ac.uk/people/heh/Paper240.pdf
    14 Feb 2013: 22:. 23:. 24:. 25:. 26:. 27:. 28:. 29:. 30:. 31:. 32:.

  6. PHYSICAL REVIEW E 87, 023015 (2013) Interface pinning of ...

    www.itg.cam.ac.uk/people/heh/Paper239.pdf
    11 Apr 2013: In a related context, the classical modelhas been modified to replace the sharp interface by a capillarytransition zone [24–26]. ... Porous Media 18, 107 (1995).[24] L. W. Lake, Enhanced Oil Recovery (Prentice-Hall, Englewood.

  7. Hogg, Charlie A. R., Clelia L. Marti, Herbert E. Huppert, and…

    www.itg.cam.ac.uk/people/heh/Paper238.pdf
    12 Apr 2013: Parameter Value. Inflow channel width (m) 49Inflow channel depth (m) 1.7Inflow velocity (m s21) 0.48Inflow reduced gravity (m s22) 0.021Inflow temperature (uC) 13.0Lake surface temperature (uC)

  8. Spreading and convective dissolution of carbon dioxide in vertically…

    www.itg.cam.ac.uk/people/heh/Paper237.pdf
    14 Feb 2013: 24] An upscaled model for convective dissolution canthen be incorporated into models such as equation (1) byintroducing a constant loss or sink term [Gasda et al.,2011 ; MacMinn et al., 2011],.

  9. Handbook of Environmental Fluid Dynamics: Overview and Fundamentals

    www.itg.cam.ac.uk/people/heh/Paper236.pdf
    11 Apr 2013: 2 2 2. 24/.467. 35.1 Introduction.

  10. grl50082 307..311

    www.itg.cam.ac.uk/people/grae/105.pdf
    9 Apr 2013: a[1 exp(bt)].[24] This exponential time dependence is explained by our. ... Res. Lett., 24(10), 1251–1254. Worster, M. G. (1992), The dynamics of mushy layers, in InteractiveDynamics of Convection and Solidification, NATO ASI Ser.

  11. Handbook of Environmental Fluid Dynamics: Overview and Fundamentals

    www.itg.cam.ac.uk/people/grae/104.pdf
    9 Apr 2013: 2 2 2. 24/.467. 35.1 Introduction.

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