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1 - 6 of 6 search results for KA :PC53 |u:www.damtp.cam.ac.uk where 0 match all words and 6 match some words.
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  2. The effect of particle interactions on dynamic light scattering from…

    www.damtp.cam.ac.uk/user/hinch/publications/JFM167_131.pdf
    23 Jul 2009: Third, if ka 9 1 then the relevant scale of number-density fluctuations is small compared with the size of an individual particle. ... 1 ) , ( 2. 2 ) ; and for the case ka 4 1 and a general form of P by Batchelor (1983).
  3. 20 Jan 2009: Ex = ωA sin[ nπy. b. ]. sin(kz ωt),. By = kA sin[ nπy.
  4. Numerical studies of the influence of the dynamic contact ...

    www.damtp.cam.ac.uk/user/hinch/publications/PhysFluids_21_072102.pdf
    28 Sep 2009: respectively. These parameters ka and krare determined as the best fit parameters to the measurement. ... As parameters of the contact angle model, mda= 107, e = 90, mdr = 77, ka = 9.0 10.
  5. Stability of an acid front moving through porous rock

    www.damtp.cam.ac.uk/user/hinch/publications/JFM212_279.pdf
    21 Jul 2009: constants. Far from the front. u1 - kA e-lkxl when lkXl is 0(1), using the matching of u1 a t the leading O ( k ) constant term.
  6. Raining into shallow water as a description of the collapse of a…

    www.damtp.cam.ac.uk/user/hinch/publications/JFM554_259.pdf
    8 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.
  7. The millennial atmospheric lifetimeof anthropogenic CO2 David Archer…

    www.damtp.cam.ac.uk/user/mem/archer-carbon-tail08.pdf
    30 Aug 2009: Kvenvolden KA (1988) Methane hydrate—a major reservoir of carbon in the shallow geosphere.

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