“…Various organic radical cations can be generated spontaneously by inclusion of their precursors into zeolites. , The rigid microporous solids stabilize the otherwise highly reactive radical cations due to the combined effects of (a) the intense electrostatic fields inside zeolites, (b) topological restrictions that prevent the access of external reagents, and (c) the limiting dimensions of the zeolite channels, which may restrict the shape of the enclosed intermediates. , Typically, radical cations generated in zeolites have extended lifetimes and can, therefore, be studied by conventional spectroscopic techniques. On the other hand, some radical cations sequestered in zeolites undergo rapid conversions, which are without precedent in cryogenic matrices or in solution . For example, p -propylanisole gave rise to p -propenylanisole radical cation;8a 2-phenyl-1,3-dithiane formed 1,2-dithiolane radical cation;8b trans -1,2-diphenylcyclopropane was converted to exo , exo -1,3-diphenylallyl radical;8c and p -cyclopropylanisole gave rise to p -propenylanisole radical cation 8d…”