After coadsorption of electron-donor
(p-terphenyl,
PTP) and electron-acceptor (1,4-dicyanobenzene, DCB) molecules within
the channels of silicalite-1 and MZSM-5 (M = Na+, H+) zeolites, photoinduced or spontaneous electron transfers
were investigated. In aluminum-free silicalite-1, the reaction mechanisms
after PTP ionization are similar
in the presence and in the absence of the acceptor molecule. Photoionization
leads to a PTP•+ radical cation, which recombines
directly. In NaZSM-5, p-terphenyl photoexcitation
induces PTP•+ formation evolving to an electron–hole
pair through capture of another electron of zeolite. This behavior
is observed with and without DCB. However, when DCB is coadsorbed
with PTP, recombination decays for PTP•+ and for
the electron–hole pair are significantly slower. Pulsed EPR
experiments show strong electron density close to DCB, through a coupling
of unpaired electrons with 14N nuclei. Nevertheless, the
electron transfer remains insufficient to allow DCB•– radical anion formation. High confinement within ZSM-5 and intrinsic
strength of zeolite acceptor sites might be put forward to explain
the nonformation of the anion. The acceptor properties of DCB and
of the zeolite might then be competitive. The zeolite electron acceptor
character is even more marked when PTP is coadsorbed with DCB in acidic
HZSM-5. Ionization occurs spontaneously, and transient species are
stabilized for months. No electronic coupling with nitrogen atoms
of DCB could be observed, indicating no partial transfer to the acceptor
molecule and electron trapping in acidic zeolite.