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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

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)).

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

26 Mar 2023: 554, 299–322. (doi:10.1017/S002211200600930X)2. Baxter SJ, Power H, Cliffe KA, Hibberd S.

30 May 2006: 4.la, b ) G = KA = ( N H / U ) { ( B / H ) 2 - l}, h = e - l ( l - ) = ( ( B / H ) 2 - I}. (

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.

30 May 2006: ka = n, R ) = 50.

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.

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 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).