Isomorphously substituted Fe-ZSM-5 zeolites as catalysts causes of catalyst ageing as revealed by X-band EPR, Mossbauer and 29Si MAS NMR spectra

被引:42
作者
Fejes, P
Lázár, K
Marsi, I
Rockenbauer, A
Korecz, L
Nagy, JB
Perathoner, S
Centi, G
机构
[1] Univ Szeged, Dept Appl & Environm Chem, H-6720 Szeged, Hungary
[2] CRC, Inst Isotope & Surface Chem, H-1525 Budapest, Hungary
[3] Univ Szeged, Juhasz Gyula Teachers Training Coll, Inst Chem, H-6720 Szeged, Hungary
[4] Tech Univ Budapest, Inst Expt Phys, Budapest, Hungary
[5] FUNDP, Dept Chim, Lab RMN, Namur, Belgium
[6] Univ Messina, Dept Ind Chem & Engn Mat, Messina, Italy
关键词
Fe-ZSM-5; zeolites; EPR spectrum deconvolution; experimental determination of the transition probability; r; of Fe(III) in the oxide as a means to study catalyst action and fouling;
D O I
10.1016/S0926-860X(03)00385-5
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
An unconstrained curve fitting/parameter estimation program adapted to PC was applied for the deconvolution. of X-band EPR spectra of Fe(III) in ZSM-5 (MFI) zeolites. The sub-spectra of framework (FW) and extra-framework (EFW) Fe(III) ions sited in environments of different (ligand) symmetry could be identified. The EPR transition probability, r, of Fe(III) in the little oxide clusters (diads, triads) was 13.75 times larger than that incorporated into the lattice. Increase of the cluster size and ordering of the random structure led to reduction of r. When the co-ordination of Fe(III) ions in the oxide clusters approached the cubic symmetry of Fe(III) in the lattice, r converged to 1.0. The state: r = 1.0 is equivalent to the development of a crystalline phase. The experimental determination of r revealed important details of catalyst action. The initial activity in the direct oxidation of benzene to phenol (oxidant: N2O) is due to oxide clusters of random structure (known as "ferrihydrite"). Partial and eventually (almost) complete loss of activity occurs when the clusters get ordered to hematite (or in reducing atmosphere to magnetite, as well). Contrary to fully inactive hematite, magnetite retains about 50% of the original activity because it exposes [Fe(III)](Th)-O-[FeIII)](Oh) linkages supposed to be responsible for oxidation activity. (C) 2003 Elsevier B.V. All rights reserved.
引用
收藏
页码:75 / 90
页数:16
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