“…From the comparison of this behavior with the results of Topsøe et al, 26 Lund et al 21 and Gao et al 27 in their studies on magnetite-supported lead, silica-supported magnetite and titania-supported magnetite, it is suggested that the iron cations in octahedral sites in the first reduction stage of the In-Fe 2 O 3 /HZSM-5(I) catalyst were substituted by indium cations, resulting in the decrease in S. After the sample was treated at 630 C, the spectrum showed a doublet with parameters typical of high-spin Fe 2+ in tetrahedral vacancies, 16,28,29 a typical sextuplet of a-Fe and a singlet which possibly resulted from the small particles of metallic iron. 30,31 Since pure wustite is thermodynamically unstable at room temperature, 22,32 and the interaction between indium oxide and iron oxide was weak in the In-Fe 2 O 3 /HZSM-5(I) catalyst, the existence of stable ferric cations was apparently caused by the interaction between the iron oxide and the HZSM-5 support. From Table 3 it can be seen that, at the end of the TPR process, 51.5% Fe 0 was found, implying that 48.5% Fe 2+ could not be reduced due to the strong interaction between Fe 2+ and the HZSM-5 support.…”