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1 - 10 of 27 search results for katalk:za31 24 / / / / / |u:www.itg.cam.ac.uk where 0 match all words and 27 match some words.

  1. Results that match 1 of 2 words

  2. Using PHF format

    www.itg.cam.ac.uk/people/heh/Paper150.pdf
    9 Feb 2004: The volume fration of particles in suspension evolves as23,24. df. dt5. ... X5 x/l , 24! T5 t/ v sl /q!1/ a 2 1!, 25!

  3. Tuesday Informal Lunch Seminars

    www.itg.cam.ac.uk/seminars/tue_1.10/lent_2004.html
    10 Feb 2004: 24 February. Steve Roper. (ITG). Magma fracture in tough materials. 2 March.

  4. Theoret. Comput. Fluid Dynamics (1998) 10: 201–212Theoretical and…

    www.itg.cam.ac.uk/people/heh/Paper140.pdf
    9 Feb 2004: r = (F/πV )1/2. (2.24)In contrast to the instantaneous, fixed volume release of the last section, there is not a finite radius at whichthe mass of particulate matter ... Applying these concepts to the relationship for the density of deposit for a single

  5. Solidification of leads: Theory, experiment,and field observations J. …

    www.itg.cam.ac.uk/people/heh/Paper152.pdf
    9 Mar 2004: salinity of the ice) is very small; k #1 0 24 [Gross et al., 1987].

  6. PII: S1359645497004692

    www.itg.cam.ac.uk/people/heh/Paper144.pdf
    12 Mar 2004: requires. P q02pd. : 24. Equation (24) thus links the dendrite tip radius to. ... This solution has a scaled tip radius P = 10.8. and a scaled tip position Z 2:24.

  7. PII: S0997-7546(00)00102-3

    www.itg.cam.ac.uk/people/heh/Paper153.pdf
    9 Feb 2004: 5H1 2(H0U1)′=0, (24)3U1 H ′1 H ′0ϕ1. 1. 2H0ϕ. ′1=0, (25)ϕ1=2720. ... 4y2)], (38). and then subsequent substitution into (24) yields a second-order differential equation forH1(y), namely(1.

  8. PII: S0301-9322(98)00062-7

    www.itg.cam.ac.uk/people/heh/Paper151.pdf
    9 Mar 2004: rNt 0 rN0 24. M. Ungarish, H.E. Huppert / International Journal of Multiphase Flow 25 (1999) 715737 725. ... For this case. the box model yields [rN/rN(0)]max=[8Fr/(3 b)]1/4. (This is by about 24% smaller than for.

  9. PHYSICS OF FLUIDS VOLUME 13, NUMBER 12 DECEMBER 2001 ...

    www.itg.cam.ac.uk/people/heh/Paper167.pdf
    9 Feb 2004: H 0 1!5 2F P12 f P1 1! 4.24! FIG. 2. ... On applicationthe boundary conditions4.23! and 4.24!, we find that. a 5 4.523 102 3, F P15 2 8.42 for Fr5 11.9.

  10. PHYSICS OF FLUIDS VOLUME 10, NUMBER 5 MAY 1998 ...

    www.itg.cam.ac.uk/people/heh/Paper143.pdf
    9 Feb 2004: 870.0 461.1A25 9 3.0 8.0 24.0 500.0 0.432 1.957 939.0 479.8. ... 675.6 0.350 1.776 761.2 428.A13 53 3.0 8.0 24.0 500.0 0.432 1.957 939.0 479.

  11. jb002019 1..16

    www.itg.cam.ac.uk/people/heh/Paper176.pdf
    9 Mar 2004: are captured by Figure 4.[24] The calculations in Figure 4 illustrate that volcanic.

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