The formation of H adducts during radiolysis of zeolites containing olefinic and aromatic hydrocarbon guests
was demonstrated to occur by H atom transfer from the zeolite to the adsorbed molecules. The H adducts and
other paramagnetic radiolysis products (radical cations and H-loss radicals) were detected by EPR spectroscopy.
The mechanism of H adduct formation was confirmed by, inter alia, H/D isotopic labeling and comparison
of results in HZSM5 and H−Mordenite to results in their Na+-exchanged counterparts. The effects of charge
transfer among radiolysis products and zeolite−adsorbate interactions on the relative yields of trapped species
is discussed. It is proposed that molecules smaller that a critical size adsorb inhomogeneously in ZSM5,
forming aggregates in which ion−molecule reactions occur. Interpretation of the experimental results was
aided by quantum chemical calculations of the molecular properties of the intermediates and their reaction
energetics. This included evaluation of electron-transfer exothermicities, activation energies for H addition,
and the relative acidities of the radical cations.