Abstract
A traveling wave of in the chlorite-thiourea reaction has shown concentric precipitation patterns upon being triggered by the autocatalyst HOCl. The precipitation patterns show circular rings of alternate null and full precipitation regions. This self-organization appears to be the result of the formation of a convective torus. The formation of the convective torus can be described as a Bénard-Marangoni instability with lateral heating.
- Received 20 January 1997
DOI:https://doi.org/10.1103/PhysRevE.55.7299
©1997 American Physical Society