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 |
|---|---|
| Article number | 084503 |
| Journal | Physical Review Letters |
| Volume | 101 |
| Issue number | 8 |
| DOIs | |
| Publication status | Published - 22 Aug 2008 |
Bibliographical note
Copyright ©2008 American Physical SocietyFingerprint
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