Search

Search Funnelback University

Search powered by Funnelback
41 - 50 of 202 search results for KaKaoTalk:ZA31 24 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. 23 Dec 2021: seal” configurations observed for inertial impacts of spheres ontoair-water [24] and fluid-fluid [26] interfaces. ... Phys. 3, 180. (2007).[23] D. Lee and H. Kim, Impact of a superhydrophobic sphere onto water, Langmuir 24, 142 (2008).[24] J.
  3. 26 Mar 2023: So, was Ruskin simply blaming air pollution on the devil? Ruskin’s biographer notes the fact that[24].
  4. 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. Nonlinear double-diffusive convection

    www.itg.cam.ac.uk/people/heh/Paper25.pdf
    30 May 2006: J. F u i d Xech. (19761, VOZ. 78, part 4? pp. 821-854 Printed in Great Britain. 82 1. Nonlinear double-diffusive convection By H E R B E R T E. H U P P E R T A N D D A N I E L R. MOORE. Department of Applied Mathematics and Theoretical Physics,
  6. High Reynolds number gravity currents along V-shaped valleys

    www.itg.cam.ac.uk/people/heh/Paper217.pdf
    18 Nov 2009: y1=2ð1 þ yÞ1=2ln. y1=2 þffiffiffiffiffiffiffiffiffiffiffiffi1 þ y. p s þ c1; (24). ... Am.Math. Soc. 46 (1940) 615–683. [24] T.B. Benjamin, Gravity currents and related phenomena, J.
  7. J. Fluid Mech. (2015), vol. 777, pp. 97–121. c© ...

    www.itg.cam.ac.uk/people/heh/Paper252.pdf
    30 Oct 2015: leakage rate predicted by (2.24) is then unphysical because there is no fluidabove the outlet to draw. ... Generally, this assumptionis invalid if the current delivers a smaller flux towards the outlet than is predicted toleak according to (2.24).
  8. 26 Mar 2023: as. th/T = 0.63, (2.24)at which time rN /L = 0.92 and h/L = 0.67. ... Illustrative evaluations of the time scales on which the axisymmetric transition from radial tothin-layer regimes occurs, given by (2.21)–(2.24), for a selection of geological
  9. 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.
  10. 28 Jul 2006: Geology 186 24.6 1.64 220 12.6 1.80. JFM 197 22.5 1.50 265 11.3 1.61.
  11. M411_31c 568..571

    www.itg.cam.ac.uk/people/grae/47.pdf
    27 Apr 2006: 24. Zielinski, G. A. Use of paleo-records in determining variability within the volcanism-climate system.

Search history

Recently clicked results

Recently clicked results

Your click history is empty.

Recent searches

Recent searches

Your search history is empty.