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17 Jan 2011: 24 February. MR9. Thierry Alboussiere. (ENS Lyon). The 'not so quiet' inner core.

7 Aug 2008: Article history:. Received 8 February 2008. Received in revised form. 24 April 2008. ... When solidifying 24 wt% NH4Cl at the lower temperaturegradient we observed another regime in which chimneys and.

19 Jul 2010: Trans. Geotherm.Res. 24 (1985) 25. Roy. Soc. London A310(1984) 511. [19] H.E.

26 Apr 2006: H inner H s0D D0. 1. 1 : (24). Importantly, we have a value for the apparent cotangent.

9 Apr 2013: a[1 exp(bt)].[24] This exponential time dependence is explained by our. ... Res. Lett., 24(10), 1251–1254. Worster, M. G. (1992), The dynamics of mushy layers, in InteractiveDynamics of Convection and Solidification, NATO ASI Ser.

23 Dec 2021: In addition,power law fits provide α1 = 0.810.07, β1 = 0.310.02, α2 = 2.50.24,and β2 = 0.140.03.

8 May 2007: 2(m2 1). 2u. XY= Mm2h2. (2.24). We posit a solution in the form. ... 4.1) for openchannel flow is replaced by 24/105 = 0.229 for a circular constraining geometry andK/m = 0.137m2/(1 m2) for a V-shaped constrainer.

7 Aug 2008: During the rapid development ofthe initial very thin ice, most of the salt is lost within 24 h.In the slower-growing ice the desalination rate is muchsmaller, and it takes ... 24] Acknowledgments. The field work described in this paperwould not have been

17 Jan 2019: With these scalings, equations(22) and (24) can be written in dimensionless form as. ... 24] A.W. Rempel, M.G. Worster, The interaction between a particle and anadvancing solidification front, J.

30 May 2006: which lead t o the eigenvalue problem? 4" [Jy2(y - c)-2 - $1 $75 = 0) (2.24) = o ( y = T ). ( 2. 2 5 a, b ). There are two infinite families of