Combining the CO2(aq)+H2O ↔ H+ HCO3– equilibrium and a slow removal of CO2 from the solution with an oscillatory H2O2–HSO3––[Fe(CN)6]4– system gives rise to chaotic temporal pH changes in a continuous-flow stirred tank reactor.
G. Rábai, A. Kaminaga and I. Hanazaki, Chem. Commun., 1996, 2181 DOI: 10.1039/CC9960002181
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