Iron silicalite samples with a different degree of crystallinity have
been synthesized and characterized. Reduced samples were then tested a
s catalysts for carbon dioxide hydrogenation. It is observed that when
ever the zeolitic phase is present, reduction of the iron species is s
trongly encumbered. As a consequence, over such catalysts the reverse
water-gas shift reaction occurs specifically while formation of hydroc
arbons does not occur. This is attributed to the lack of formation of
surface carbidic species which appear to be responsible for the hydroc
arbon formation.