Abstract
Photoinduced electron transfer from Fe2+ loaded in zeolite Y to the singlet excited state of 10-methylacridinium ion in the zeolite occurs to give the acridinyl radical which reduces 7,7,8,8-tetracyanoquinodimethane in acetonitrile solution to yield the radical anion; the back electron transfer from the radical anion to Fe3+ across the zeolite-solution interface is shown to be negligibly slow.
Original language | English |
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Pages (from-to) | 213-214 |
Number of pages | 2 |
Journal | Chemical Communications |
Issue number | 2 |
DOIs | |
State | Published - 1996 |