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Bibliografía
Reaction of the anion-deficient,
cation-ordered perovskite phase
Ba<sub>2</sub>YFeO<sub>5</sub> with 80 atm of oxygen pressure at 410
°C results in the formation of the Fe<sup>4+</sup> phase Ba<sub>2</sub>YFeO<sub>5.5</sub>. The topochemical insertion of oxide ions
lifts the inversion symmetry of the centrosymmetric host phase, Ba<sub>2</sub>YFeO<sub>5</sub> (space group <i>P</i>2<sub>1</sub>/<i>n</i>), to yield a noncentrosymmetric (NCS) phase Ba<sub>2</sub>YFeO<sub>5.5</sub> (space group <i>Pb</i>2<sub>1</sub><i>m</i> (No. 26), <i>a</i> = 12.1320(2) Å, <i>b</i> = 6.0606(1) Å, <i>c</i> = 8.0956(1) Å, <i>V</i> = 595.257(2) Å<sup>3</sup>) confirmed by the observation
of second-harmonic generation. Dielectric and PUND ferroelectric measurements,
however, show no evidence for a switchable ferroelectric polarization,
limiting the material to pyroelectric behavior. Magnetization and
low-temperature neutron diffraction data indicate that Ba<sub>2</sub>YFeO<sub>5.5</sub> undergoes a magnetic transition at 20 K to adopt
a state which exhibits a combination of ferromagnetic and antiferromagnetic
order. The symmetry breaking from centrosymmetric to polar noncentrosymmetric,
which occurs during the topochemical oxidation process is discussed
on the basis of induced lattice strain and an electronic instability
and represents a new strategy for the preparation of NCS materials
that readily incorporate paramagnetic transition metal centers