alpha-Fe3O3-supported molybdenum catalysts were prepared by heating a
mixture of MoO3 and alpha-Fe2O3. XRD, XPS, LRS, FT-IR, and Mossbauer s
pectroscopy were used to study the interactions between MoO3 and alpha
-F2O3. At the temperature of 693 K, the dispersion capacity of MoO3 on
alpha-Fe2O3 determined by XRD and XPS is 0.80 mmol MoO3/100 m(2) alph
a-Fe2O3, i.e., 4.8 Mo6+/nm(2). LRS and FT-IR results show that at low
MoO3 loading (1.8 Mo6+/nm(2)), Mo6+ cations are located in the tetrahe
dral sites of the alpha-Fe2O3 surface. The occcupation of octahedral s
urface vacant sites increases with the MoO3 loading. Considering the f
act that each Mo6+ is accompanied by 3O(2-) anions and that alpha-Fe2O
3 has a hexagonal structure, almost all the incorporated Mo6+ on the s
urface are in octahedral coordination environment. Based on the assump
tions that the (001) plane of alpha-Fe2O3 is preferentially exposed on
the surface and that all the usable surface vacant sites have been oc
cupied, the formation of a close-packed layer on the alpha-Fe2O3 surfa
ce by the O2- anions linked with the incorporated Mo6+ can be expected
, which is in good agreement with the result predicted by the incorpor
ation model proposed previously. A relationship between the residual b
ulk MoO3 and the calcination time shows that Mo6+ ions occupy the surf
ace vacant sites of alpha-Fe2O3 in two stages. The first stage may cor
respond to the migration of Mo6+ cations from the bulk MoO3 to the tet
rahedral surface vacant sites on the surface. The second stage may cor
respond to the migration of Mo6+ from the bulk MoO3 into the octahedra
l unoccupied vacant sites. Mossbauer spectroscopy and XRD results indi
cate that a new phase, Fe-2(MoO4)(3), is formed when the sample contai
ning 10.0Mo(6+)/nm(2) alpha-Fe2O3 was calcined at 743 K, suggesting th
at the calcination temperature is important to the interaction extent
between MoO3 and alpha-F2O3. (C) 1997 Academic Press.