DEACTIVATION OF METHYLRHENIUM TRIOXIDE-PEROXIDE CATALYSTS BY DIVERSE AND COMPETING PATHWAYS

Citation
Mm. Abuomar et al., DEACTIVATION OF METHYLRHENIUM TRIOXIDE-PEROXIDE CATALYSTS BY DIVERSE AND COMPETING PATHWAYS, Journal of the American Chemical Society, 118(21), 1996, pp. 4966-4974
Citations number
28
Categorie Soggetti
Chemistry
ISSN journal
00027863
Volume
118
Issue
21
Year of publication
1996
Pages
4966 - 4974
Database
ISI
SICI code
0002-7863(1996)118:21<4966:DOMTCB>2.0.ZU;2-4
Abstract
The peroxides from methylrhenium trioxide (MTO) and hydrogen peroxide, CH3ReO2(eta(2)-O-2), A, and CH3Re(O)(eta(2)-O-2)(2)(H2O), B, have bee n fully characterized in both organic and aqueous media by spectroscop ic means (NMR and UV-vis). In aqueous solution, the equilibrium consta nts for their formation are K-1 = 16.1 +/- 0.2 L mol(-1) and K-2 = 132 +/- 2 L mol(-1) at pH 0, mu = 2.0 M, and 25 degrees C. In the presenc e of hydrogen peroxide the catalyst decomposes to methanol and perrhen ate ions with a rate that is dependent on [H2O2] and [H3O+]. The compl ex peroxide and pH dependences could be explained by one of two possib le pathways: attack of either hydroxide on A or HO2- on MTO. The respe ctive second-order rate constants for these reactions which were deduc ed from comprehensive kinetic treatments are k(A) = (6.2 +/- 0.3) x 10 (9) and k(MTo) = (4.1 +/- 0.2) x 10(8) L mol(-1) s(-1) at mu = 0.01 M and 25 degrees C. The plot of log ky: versus pH for the decomposition reaction is linear with a unit slope in the pH range 1.77-6.50. The di peroxide B decomposes much more slowly to yield O-2 and CH3ReO3. This is a minor pathway, however, amounting to <1% of the methanol and perr henate ions produced from the irreversible deactivation at any given p H. Within the limited precision for this rate constant, it appears to vary linearly with [OH-] with k = 3 x 10(-4) s(-1) at pH 3.21, mu = 0. 10 M, and 25 degrees C. Without peroxide, CH3ReO3 is stable below pH 7 , but decomposes in alkaline aqueous solution to yield CH4 and ReO4-. As a consequence, the decomposition rate rises sharply with [H2O2], pe aking at the concentration at which [A] is a maximum, and then falling to a much smaller value. Variable-temperature H-1 NMR experiments rev ealed the presence of a labile coordinated water in B, but supported t he anhydride form for A.