Ferrisilicalite and FAPO-5 were synthesized hydrothermally with iron c
ontents from 0.1 to 1% on a molar basis and investigated by X-ray diff
raction and electron spin resonance (e.s.r.) in the as-synthesized, ox
idized, and reduced forms. The amount of Fe in the solid, the degree o
f crystallinity, and the Fe3+ e.s.r, signal intensity all increase wit
h synthesis time in the same manner, indicating a gradual incorporatio
n of Fe3+. At the same Fe content, different spectral behaviors of Fe3
+ in Fe-silicalite and in FAPO-5 are attributed to the differences in
the degree of isomorphous substitution, in the amount of Fe3+ in defec
t sites, and in the form of oxidic clusters.