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www.itg.cam.ac.uk/people/grae/90.pdf14 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 -
doi: 10.1098/rspa.2009.0496, 1005-1025 first published online 3…
www.itg.cam.ac.uk/people/grae/91.pdf29 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)). -
doi:10.1016/j.jcp.2005.12.002
www.itg.cam.ac.uk/people/grae/74.pdf12 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 -
Shallow free-surface Stokes flow around a corner
www.itg.cam.ac.uk/people/heh/Paper272.pdf26 Mar 2023: 554, 299–322. (doi:10.1017/S002211200600930X)2. Baxter SJ, Power H, Cliffe KA, Hibberd S. -
Lee waves in a stratified flow Part 3. Semi-elliptical obstacle
www.itg.cam.ac.uk/people/heh/Paper8.pdf30 May 2006: 4.la, b ) G = KA = ( N H / U ) { ( B / H ) 2 - l}, h = e - l ( l - ) = ( ( B / H ) 2 - I}. ( -
Static and flowing regions in granular collapses down…
www.itg.cam.ac.uk/people/heh/Paper208.pdf13 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. -
The stability of a large gas bubble rising through liquid
www.itg.cam.ac.uk/people/heh/Paper81.pdf30 May 2006: ka = n, R ) = 50. -
rspa.royalsocietypublishing.org ResearchCite this article: Cooray H,…
www.itg.cam.ac.uk/people/heh/Paper255.pdf18 May 2017: 2012 Wetting of flexible fibre arrays. Nature 482,510–513. (doi:10.1038/nature10779). 9. Wu X-F, Bedarkar A, Vaynberg KA. -
The Crystallization of Lava Lakes
www.itg.cam.ac.uk/people/heh/Paper118.pdf19 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 -• -
flm145.dvi
www.itg.cam.ac.uk/people/heh/Paper197.pdf11 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). -
Energy balances for axisymmetric gravity currents in homogeneous and…
www.itg.cam.ac.uk/people/heh/Paper213.pdf10 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. -
flm661.dvi
www.itg.cam.ac.uk/people/aa/JFM2.pdf9 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. -
flm661.dvi
www.itg.cam.ac.uk/people/heh/Paper178.pdf9 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. -
The fluid mechanics of solidification
www.itg.cam.ac.uk/people/heh/Paper92.pdf16 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 -
flm412.dvi
www.itg.cam.ac.uk/people/heh/Paper174.pdf9 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. -
The Crystallization of Lava Lakes
www.itg.cam.ac.uk/people/grae/21.pdf29 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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