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Fourier-transform infrared spectroscopy electron transfer

In 1993, Blatter and Frei [34] extended the Aronovitch and Mazur [28] photo-oxidation into zeolitic media, which resulted in several distinctive advantages as described below. Irradiation in the visible region (633 nm) of zeolite NaY loaded with 2,3-dimethyl-2-butene, 16, and oxygen resulted in formation of allylic hydroperoxide, 17, and a small amount of acetone. The reaction was followed by in situ Fourier-transform infrared (FTlR) spectroscopy and the products were identified by comparison to authentic samples. The allylic hydroperoxide was stable at - 50°C but decomposed when the zeolite sample was warmed to 20°C [35]. In order to rationalize these observations, it was suggested that absorption of light by an alkene/Oi charge-transfer complex resulted in electron transfer to give an alkene radical cation-superoxide ion pair which collapses... [Pg.291]


See other pages where Fourier-transform infrared spectroscopy electron transfer is mentioned: [Pg.349]    [Pg.6473]    [Pg.1623]    [Pg.6472]    [Pg.429]    [Pg.161]    [Pg.189]    [Pg.931]    [Pg.375]    [Pg.99]    [Pg.456]    [Pg.693]    [Pg.221]    [Pg.2299]    [Pg.6387]    [Pg.6574]    [Pg.20]    [Pg.6386]    [Pg.6573]    [Pg.104]    [Pg.87]    [Pg.101]    [Pg.2373]    [Pg.173]   
See also in sourсe #XX -- [ Pg.522 ]




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