Synergy between alpha-Sb2O4 and Fe-2(MaO(4))(3) during the first hours of the catalytic oxidation of isobutene to methacrolein

Citation
Yl. Xiong et al., Synergy between alpha-Sb2O4 and Fe-2(MaO(4))(3) during the first hours of the catalytic oxidation of isobutene to methacrolein, J MOL CAT A, 155(1-2), 2000, pp. 59-71
Citations number
33
Categorie Soggetti
Physical Chemistry/Chemical Physics
Journal title
JOURNAL OF MOLECULAR CATALYSIS A-CHEMICAL
ISSN journal
13811169 → ACNP
Volume
155
Issue
1-2
Year of publication
2000
Pages
59 - 71
Database
ISI
SICI code
1381-1169(20000420)155:1-2<59:SBAAFD>2.0.ZU;2-5
Abstract
The physico-chemical properties and the catalytic behaviour of mixtures of iron molybdate and antimony oxide in the selective oxidation of isobutene t o methacrolein were studied with special consideration of the possibility o f changes of these oxides during the catalytic reaction. The catalysts were separately prepared Fe-2(MoO4)(3) and alpha-Sb2O4 and mixtures thereof. Th ey were characterized by BET surface area measurements, X-ray diffraction ( XRD), Conventional Transmission Electron Microscopy (CTEM), Electron Probe Micro Analysis (EPMA), X-ray Photoelectron Spectroscopy (XPS), Ion Scatteri ng Spectroscopy (ISS) and Mossbauer spectroscopy before and after the catal ytic reaction. Under the reaction conditions used, no mutual contamination was detectable neither before nor after test. Pure alpha-Sb2O4 is inactive. Fe-2(MoO4)(3) is active but poorly selective. The alpha-Sb2O4-Fe,(MoO4)(3) mixtures exhibit a synergetic effect, corresponding to an increase both in the methacrolein yield and in the selectivity to methacrolein. The donor p roperties of alpha-Sb2O4 and the acceptor properties of the Fe-2(MoO4)(3) o xide can explain this synergism in the frame of the Remote Control theory: oxygen spillover would be emitted by alpha-Sb2O4, and migrate to Fe-2(MoO4) (3) creating or regenerating selective sites on this last phase. The benefi cial effect of spillover oxygen seems to reside in its ability to keep iron in a higher oxidation state, close to Fe+3. (C) 2000 Elsevier Science B.V. All rights reserved.