Pulsatile chemo-hydrodynamic patterns due to a coupling between an oscillating chemical reaction and buoyancy-driven hydrodynamic flows can develop when two solutions of separate reactants of the Belousov−Zhabotinsky reaction are put in contact in the gravity field and conditions for chemical oscillations are met in the contact zone. In regular oscillatory conditions, localized periodic changes in the concentration of intermediate species induce pulsatile density gradients, which, in turn, generate traveling convective fingers breaking the transverse symmetry. These patterns are the self-organized result of a genuine coupling between chemical and hydrodynamic modes.
SECTION: Liquids; Chemical and Dynamical Processes in SolutionO ut-of-equilibrium, breaking of symmetries and related spatiotemporal patterns have been much studied in hydrodynamic and reaction−diffusion (RD) systems. 1−3 At the intersection between these two fields, chemo-hydrodynamics focuses on analyzing patterns and instabilities that result from a nonlinear coupling of hydrodynamic and RD processes. 4 Related problems range from fingering instabilities of reactive interfaces 5,6 or traveling chemical fronts 4 to the spatiotemporal dynamics of chemicals advected in complex flow fields. 7,8 The reaction−diffusion−convection (RDC) interplay impacts numerous applications areas as diverse as combustion, 9 polymer processing, 10 extraction techniques 5,11 and CO 2 sequestration. 12 When chemicals are passively slaved to the flow, the convective motions develop independently of the presence of reactive processes. On the other hand, in presence of active chemistry, the reactions modify a physical property of the fluid like its density, viscosity, or surface tension for instance. Concentration gradients in RD processes can then trigger unfavorable mobility gradients, which in turn can yield convection. As an example, even when starting from an initially stable density stratification of a less dense reactive solution on top of a denser one in the gravity field, chemical processes can trigger buoyancy-driven convection. This occurs when the reaction produces either a denser product locally or when differential diffusion phenomena implying the various chemicals 6,13−16 or heat and mass 17 come into play. The hydrodynamic patterns are then typically convective fingers growing vertically. Simple A+B→ C reactions have been shown to be able to break the up−down symmetry of such convective fingers. 13 More complex reactions prone to produce spatiotemporal RD structures can induce other synergetic combinations of chemical and hydrodynamic modes. Typical examples of such intrinsic chemo-hydrodynamic scenarios include reaction-driven convection around a traveling chemical front stably stratified from both solutal and thermal perspectives 4,17,18 and buoyancy or Marangoni-induced convective cells following chemical waves in excitable and oscillatory systems. 19−23 In such cases, the chemical kinetics drives the source of the convective flows, and the velo...