Abstract
The aluminum introduction into the zinc ferrite ZnFe2-(x)Al(x)O4 in the range 0.0 ≤ χ ≤ 1.0 was studied. These ferrites were calcined at two temperatures, 550°C and 750°C. X-ray diffraction (XRD) patterns showed that they have a spinel structure with Al3+ replacing Fe3+ in octahedral sites. The crystallite size decreased as the aluminum introduction increased. At high calcination temperature, sintering and segregation processes occur. Linear correlations were found between XRD and Mossbauer parameters. Mossbauer spectra showed that the symmetry of the electron distribution decreased around the nucleus of Fe3+, as the aluminum content increased. Such asymmetrical distribution of the electron density may be associated to the spatial accommodation of aluminum in the neighboring octahedral sites. Oxygen atoms turn out to be more basic due to the charge transfer from Fe3+ to O2- in the Fe-O bond. Hence the acid-base type dissociation of the C-H bond for the n-butenes activation is favored. The highest yield of butadiene was obtained for the samples treated at 750°C whereas for the samples calcined at 550°C, double bond isomerization of 1-butene occurs in competition with the oxidative dehydrogenation.
Original language | English |
---|---|
Pages (from-to) | 53-62 |
Number of pages | 10 |
Journal | Journal of Molecular Catalysis A: Chemical |
Volume | 125 |
Issue number | 1 |
DOIs | |
State | Published - 31 Oct 1997 |
Externally published | Yes |
Keywords
- 1-butene oxidative dehydrogenation
- Aluminum zinc ferrite
- Ferrites
- Metal oxides
- Mossbauer spectroscopy
- Spinels
- X-ray diffraction