Search

Search Funnelback University

Search powered by Funnelback
51 - 60 of 202 search results for katalk:za31 24 / / / / / |u:www.itg.cam.ac.uk where 0 match all words and 202 match some words.
  1. Results that match 1 of 2 words

  2. Ageostrophic effects in rotating stratified flow

    www.itg.cam.ac.uk/people/heh/Paper17.pdf
    30 May 2006: 24-2. 372 H. E. Huppert and 144. E. Stern. $1. , //,/,////,//////////////,,,/,////// / ///,/I/ // / / / , // , / , / // , / / / / // / /, /' I -. FIGURE 1. An elevation of the channel, bounded by vertical walls at. ... Moh(x/L) e--ikg. (3.24). While in
  3. The Fluid Mechanics of Carbon Dioxide Sequestration

    www.itg.cam.ac.uk/people/heh/Paper246.pdf
    24 Apr 2014: 24/. 14. F. or p. erso. nal u. se o. nly. ... n 04. /24/. 14. F. or p. erso. nal u. se o.
  4. doi:10.1016/j.jcp.2004.11.039

    www.itg.cam.ac.uk/people/grae/62.pdf
    26 Apr 2006: Received 29 March 2004; received in revised form 24 September 2004; accepted 11 November 2004. ... ykumar and Mao [24] again assuming the interface was sharp. The SPH method, as mentioned earlier, does.
  5. PII: 0022-0248(94)90038-8

    www.itg.cam.ac.uk/people/heh/Paper119.pdf
    27 Apr 2006: 2.18), which can be (2.23) and (2.24) more closely.used in (2.22) to show that Segregation is more sensitive to the value of. ... 4.24)mass reduce to and we use this condition together with (4.21)—.
  6. flm1000491a

    www.itg.cam.ac.uk/people/heh/Paper225.pdf
    18 Jan 2011: φ̃0(0; λ̄) =. h(0, y)2 dy. (3.24). The solid curve in figure 5 shows the result of substituting the value of φ̃0(0; λ̄)found in this way
  7. PII: S0022-0248(99)00290-0

    www.itg.cam.ac.uk/people/grae/40.pdf
    26 Apr 2006: 1.0 [24]. The slope of the linethrough data set (h), for silicon carbide particles in a succino-nitrile melt, is! ... Azouni, W. Kalita, M. Yemmou, J. Crystal Growth. 99 (1990) 201.[24] S.
  8. Laminar free convection in confined regions

    www.itg.cam.ac.uk/people/grae/4.pdf
    1 Jun 2006: 1 -. f = 16-21 min. 24.5 25.0 25.5 26.0 26.5 27.0 27.5 28.0 28.5 29.0 T. ... 0 - 1 24.5 25.0 25.5 26.0 26.5 27.0 27.5 28.0 28.5 29.0 29.5 30.0 30.5.
  9. doi:10.1016/j.jcp.2005.12.002

    www.itg.cam.ac.uk/people/grae/74.pdf
    12 Jun 2006: g. [23,24]). The major difficulties then consist in the formulation of accurate internalboundary conditions and in following the evolution of the interfaces through time. ... 104 This study 19.6 16.2 3.53 0.585 2.24[2] 19.51 16.2 3.53 0.586 2.243[3]
  10. 16 Jul 2010: Geophys. Res., 79, 1792-1797, 1974. Gebhart, B., and J. C. Molendorf, A new density relationship for pure and saline water, Deep Sea Res., 24(9), 831-848, 1977. ... Glaciol., 24, 259-271, 1979. Tressler, W. L., and A.M. Ommundsen, Seasonal oceanographic
  11. 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.

Search history

Recently clicked results

Recently clicked results

Your click history is empty.

Recent searches

Recent searches

Your search history is empty.