Fully oxygenated perovskites with
the same chemical composition
crystallize in different polymorphs, o-LaCa2Fe3O9 with A-site triple-layer order and d-(LaCa2)Fe3O9 with A-site disorder. Both compounds
contain unusually high valence Fe3.67+ and, when they are
heated, release oxygen to reduce such an unusual valence state. Thermogravimetry
analysis revealed that the ordered/disordered arrangements of the
A-site cations in the perovskite structures strongly influence the
stability of unusually high valence Fe ions at the B-site. The A-site-ordered
o-LaCa2Fe3O9 releases its oxygen
topotactically and selectively from the FeO6 octahedra
between the Ca layers above 400 °C, and the released oxygen is
not incorporated back on cooling in air, Ar, or O2 atmospheres.
On the other hand, oxygen in d-(LaCa2)Fe3O9 is released from and incorporated into the rigid octahedra
reversibly when the compound is heated in air or O2. More
importantly, the oxygen-deficient d-(LaCa2)Fe3O8 obtained by heating d-(LaCa2)Fe3O9 in Ar incorporates extra oxygen to increase the valence
state of Fe in an unusually high value even under ambient conditions.
Once the A-site cation disorder structure framework is established,
unusually high valence states, which usually require extreme conditions,
can be stabilized by incorporating extra oxygen into the structure
even under ambient conditions.