INTRAZEOLITE COMPLEXATION OF TRANSITION-METAL IONS BY TRIAZACYCLONONANE-TYPE LIGANDS - CONTROL OF CLUSTER NUCLEARITY AND OXYGEN-BINDING IN CONFINED REACTION SPACES

Authors
Citation
D. Devos et T. Bein, INTRAZEOLITE COMPLEXATION OF TRANSITION-METAL IONS BY TRIAZACYCLONONANE-TYPE LIGANDS - CONTROL OF CLUSTER NUCLEARITY AND OXYGEN-BINDING IN CONFINED REACTION SPACES, Journal of the American Chemical Society, 119(40), 1997, pp. 9460-9465
Citations number
49
Categorie Soggetti
Chemistry
ISSN journal
00027863
Volume
119
Issue
40
Year of publication
1997
Pages
9460 - 9465
Database
ISI
SICI code
0002-7863(1997)119:40<9460:ICOTIB>2.0.ZU;2-M
Abstract
1,4,7-Triazacyclononane (L) and its methylated analog (L') form comple xes with zeolite-exchanged Mn2+ Co2+, or Cu2+. Through comparison with diluted solutions of the complexes, the effect of the zeolite environ ment on the complex formation was evaluated. In the case of Mn2+ the c omplexation was monitored by observing the zero-field splitting in the X-and Q-band ESR spectra of the Mn2+ ion, Adsorption oft into metal Y zeolites yields bis L complexes; the L' mono complexes are formed. Th e latter complexes are not coordinated by the zeolite surface, as dedu ced from the spectral parameters of the [Mn(L')](2+) and [Cu(L')](2+) complexes. Mono [Co(L')](2+) in the zeolite is a reversible dioxygen b inder, a property not previously documented for these complexes in sol ution. Exposure of [Mn(L)(2)](2+) or [Mn(L')](2+) containing Y zeolite s to H2O2 results in intraporous formation of oxidized Mn dimers. The constrained zeolite environment seems to stabilize the oxidized dimers of Mn and L by preventing further cluster expansion.