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9 Apr 2013: Fluids 24, 091111 (2012); doi: 10.1063/1.4747184 View online: http://dx.doi.org/10.1063/1.4747184 View Table of Contents: ... 091111-2 Sayag, Pegler, and Worster Phys. Fluids 24, 091111 (2012). (b) (c).

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.

14 Feb 2013: 22:. 23:. 24:. 25:. 26:. 27:. 28:. 29:. 30:. 31:. 32:.

11 Apr 2013: In a related context, the classical modelhas been modified to replace the sharp interface by a capillarytransition zone [24–26]. ... Porous Media 18, 107 (1995).[24] L. W. Lake, Enhanced Oil Recovery (Prentice-Hall, Englewood.

12 Apr 2013: Parameter Value. Inflow channel width (m) 49Inflow channel depth (m) 1.7Inflow velocity (m s21) 0.48Inflow reduced gravity (m s22) 0.021Inflow temperature (uC) 13.0Lake surface temperature (uC)

9 Apr 2013: These colloidal concentration gradients, which areneglected in rigid-ice formulations, can trigger a thermody-namic instability that leads to morphological transitions in thepattern of segregated ice.23,24 Recently, these thermodynamicprinciples

9 Apr 2013: 2 2 2. 24/.467. 35.1 Introduction.

11 Apr 2013: 2 2 2. 24/.467. 35.1 Introduction.

14 Feb 2013: 24] An upscaled model for convective dissolution canthen be incorporated into models such as equation (1) byintroducing a constant loss or sink term [Gasda et al.,2011 ; MacMinn et al., 2011],.

30 Jul 2013: 24). The perturbation equations are given, at O(βN), by. 1. η.