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 |
|---|---|
| Pages (from-to) | 213-214 |
| Number of pages | 2 |
| Journal | Chemical Communications |
| Issue number | 2 |
| DOIs | |
| State | Published - 1996 |
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