Abstract
The dynamics of A+B→C fronts in horizontal solution layers can be influenced by buoyancy-driven convection as soon as the densities of A, B, and C are not all identical. Such convective motions can lead to front propagation even in the case of equal diffusion coefficients and initial concentration of reactants for which reaction-diffusion (RD) scalings predict a nonmoving front. We show theoretically that the dynamics in the presence of convection can in that case be predicted solely on the basis of the knowledge of the one-dimensional RD density profile across the front.
Original language | English |
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Article number | 084503 |
Journal | Physical Review Letters |
Volume | 101 |
Issue number | 8 |
DOIs | |
Publication status | Published - 22 Aug 2008 |