The visible light-induced reaction between 2,3-dimethyl-2-butene and O 2 in zeolite NaY at -100°C was recorded on the millisecond time scale by rapid scan FT-infrared spectroscopy. The experiment revealed the growth of the sole product, 2,3-dimethyl-3-hydroperoxy-1-butene, during a 150 ms photolysis pulse. Since this duration is short compared to the time scale estimated for cage-to-cage diffusion of the product, it allowed us to determine the number of cages participating in the reaction induced by the pulse. On the basis of this measurement and a comparison of product yields in pulsed and continuous irradiation experiments, we estimate that at a minimum 1% of all NaY supercages participate in the photoreaction. This is 1-3 orders of magnitude larger than the concentration of any defect sites (Lewis acid, radical sites) that might be present in NaY zeolite. This confirms that the sole physical property of the zeolite cage, namely the high electrostatic field in the vicinity of the alkali ions, is responsible for the visible light-induced olefin oxidation.
I. IntroductionIn recent photochemical work on hydrocarbon oxidation by O 2 in zeolites, we have found that small alkenes, alkanes, or alkylbenzenes can be partially oxidized under visible light with very high selectivity. 1 The primary photoproduct detected by in situ FT-infrared spectroscopy is the corresponding allyl, alkyl, or benzyl hydroperoxide. Final oxidation products of these reactions, which were conducted on mixtures of hydrocarbon and O 2 gas loaded into alkali or alkaline-earth zeolite Y or L, are the corresponding aldehyde or ketone. Exceptions are systems such as 2,3-dimethyl-2-butene or isobutane whose hydroperoxide product does not feature an H at the R carbon, preventing spontaneous dehydration to form a carbonyl compound. 1b,e Products of these partial oxidations are of commercial importance, and the high selectivity is a unique aspect of the method. To expand such visible light-induced reactions in zeolites to new synthesis, a firm understanding of the mechanism is essential. This motivated us to employ timeresolved FT-infrared spectroscopy as a tool for gaining mechanistic insight not accessible in our previous studies using static FT-IR spectroscopy.UV-visible spectroscopy of alkali and alkaline-earth zeolite Y loaded with alkane (alkene, arene) and O 2 revealed a visible absorption tail attributed to the hydrocarbon‚O 2 contact chargetransfer transition. 2,3 This assignment is based on the observed increase of the absorption threshold with the ionization potential of the hydrocarbon. UV charge-transfer bands of alkane, alkene, or arene‚O 2 contact complexes are well-known from studies in the high-pressure O 2 gas phase and O 2 -saturated solution. 4-6 Further strong evidence for the charge-transfer assignment is the dependence of the absorption onset on the magnitude of the electrostatic field in the vicinity of exchangeable cations in the zeolite cage. 2 These fields lie at the origin of the mild oxidation method. In the case of NaY or ...