The evolution of the dispersed surface molybdate phase on
high-surface-area magnesium oxide is studied
as a function of weight loading of MoO3 and calcination
temperature using in situ Mo L3-edge X-ray
absorption near edge spectroscopy, in situ laser Raman spectroscopy,
and thermogravimetry−mass
spectroscopy. Under ambient, hydrated conditions, the magnesium
support is present as magnesium
hydroxide, rather than MgO, and the molybdate species is present on the
surface as an isolated tetrahedral
species for weight loadings of 5−20 wt % MoO3.
Under these hydrated conditions the form of the
molybdate
species is controlled by the net surface pH at the point of zero charge
and is the same as that observed
in aqueous solution. As the catalyst is calcined in air, the
molybdate species transforms from a tetrahedral
species, MoO4, to an octahedral one, MoO6.
This transformation occurs at the same temperature,
∼450
°C, as that at which the support changes from hydroxide to oxide.
This transformation temperature is
independent of the MoO3 loading. It is suggested that
it is this support-induced structural change that
drives the change in the form of the surface molybdate species and not
the desorption of adsorbed water.