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1 - 16 of 16 search results for KA :PC53 |u:www.itg.cam.ac.uk where 0 match all words and 16 match some words.
  1. Results that match 1 of 2 words

  2. gl037304 1..4

    www.itg.cam.ac.uk/people/grae/90.pdf
    14 Sep 2009: r@z. >@rsat@T. ka @T=@zð Þaþks @T=@zð Þska þ ks. ; ð6Þ. ... involving the conductivity-weighted temperature gradient.If the thermal conductivities ka and ks of air and solid wereequal then condition (6) would be approximately equal to (5):the
  3. 29 Apr 2010: Thermal conductivities of air and thecondensed phase are given by ka and ks, respectively. ... Gm = ksGs0 kaGa0. ks ka (4.2). (cf. the Mullins–Sekerka instability (Mullins & Sekerka 1964)).
  4. doi:10.1016/j.jcp.2005.12.002

    www.itg.cam.ac.uk/people/grae/74.pdf
    12 Jun 2006: Values of these constants ka, b are presented in Fig. 4 as afunction of Tliquidus(Ci) Timp, in comparison with [1]. ... sλ a. ,b. Fig. 4. Dimensionless constants ka, b as a function of the temperature difference between the liquidus temperature at the
  5. Shallow free-surface Stokes flow around a corner

    www.itg.cam.ac.uk/people/heh/Paper272.pdf
    26 Mar 2023: 554, 299–322. (doi:10.1017/S002211200600930X)2. Baxter SJ, Power H, Cliffe KA, Hibberd S.
  6. 30 May 2006: 4.la, b ) G = KA = ( N H / U ) { ( B / H ) 2 - l}, h = e - l ( l - ) = ( ( B / H ) 2 - I}. (
  7. Static and flowing regions in granular collapses down…

    www.itg.cam.ac.uk/people/heh/Paper208.pdf
    13 Nov 2007: Many models adopt a hydrostatic as-sumption such that ka 1, consistent with experimental re-sults of Pouliquen and Forterre.10. ... There are two key parameters, the Earth pressure coeffi-cient ka, which Larrieu et al.
  8. The stability of a large gas bubble rising through liquid

    www.itg.cam.ac.uk/people/heh/Paper81.pdf
    30 May 2006: ka = n, R ) = 50.
  9. 18 May 2017: 2012 Wetting of flexible fibre arrays. Nature 482,510–513. (doi:10.1038/nature10779). 9. Wu X-F, Bedarkar A, Vaynberg KA.
  10. The Crystallization of Lava Lakes

    www.itg.cam.ac.uk/people/heh/Paper118.pdf
    19 Jul 2010: cal g- 1 o C- 1 apr 0.380 cal g- 1 o C- 1 ka 0.008 cal cm -1 s -1 øC-1 k•5 0.008 cal cm -•
  11. flm145.dvi

    www.itg.cam.ac.uk/people/heh/Paper197.pdf
    11 Oct 2006: t. Ka/. P c (0. ). P a/P. c (0. ). 2 4 6 8 10 120. 0.2. 0.4. 0.6. 0.8. 1.0 (a) (b).
  12. 10 Mar 2009: J. Fluid Mech. (2008), vol. 616, pp. 303–326. c 2008 Cambridge University Pressdoi:10.1017/S002211200800400X Printed in the United Kingdom. 303. Energy balances for axisymmetric gravitycurrents in homogeneous and linearly. stratified ambients.
  13. flm661.dvi

    www.itg.cam.ac.uk/people/aa/JFM2.pdf
    9 Mar 2004: J. Fluid Mech. (2003), vol. 497, pp. 167–199. c 2003 Cambridge University PressDOI: 10.1017/S002211200300661X Printed in the United Kingdom. 167. Solidification and compositional convectionof a ternary alloy. By ANDREW F. THOMPSON†, HERBERT E.
  14. flm661.dvi

    www.itg.cam.ac.uk/people/heh/Paper178.pdf
    9 Mar 2004: J. Fluid Mech. (2003), vol. 497, pp. 167–199. c 2003 Cambridge University PressDOI: 10.1017/S002211200300661X Printed in the United Kingdom. 167. Solidification and compositional convectionof a ternary alloy. By ANDREW F. THOMPSON†, HERBERT E.
  15. The fluid mechanics of solidification

    www.itg.cam.ac.uk/people/heh/Paper92.pdf
    16 Jan 2007: Composition, wt % Na,SO,. FIGURE 15. The predicted results a n d experimental d a t a for cooling a n aqueous solution of Ka,SO, from above for t h
  16. flm412.dvi

    www.itg.cam.ac.uk/people/heh/Paper174.pdf
    9 Mar 2004: J. Fluid Mech. (2003), vol. 483, pp. 165–197. c 2003 Cambridge University PressDOI: 10.1017/S0022112003004129 Printed in the United Kingdom. 165. A model for diffusion-controlled solidification ofternary alloys in mushy layers†. By D. M.
  17. The Crystallization of Lava Lakes

    www.itg.cam.ac.uk/people/grae/21.pdf
    29 Jul 2010: cal g- 1 o C- 1 apr 0.380 cal g- 1 o C- 1 ka 0.008 cal cm -1 s -1 øC-1 k•5 0.008 cal cm -•

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