Inorganic Chemistry · 2018 · 16 citations · 16 references
High-resolution synchrotron X-ray and neutron powder diffraction data demonstrate that, in contrast to recent reports, Sr<sub>2</sub>FeIrO<sub>6</sub> adopts an I1̅ symmetry double perovskite structure with an a<sup>-</sup>b<sup>-</sup>c<sup>-</sup> tilting distortion. This distorted structure does not tolerate cation substitution, with low levels of A-site (Ca, Ba, La) or Fe-site (Ga) substitution leading to separation into two phases: a stoichiometric I1̅ phase and a cation-substituted, P2<sub>1</sub>/ n symmetry, a<sup>-</sup>a<sup>-</sup>c<sup>+</sup> distorted double perovskite phase. Magnetization, neutron diffraction, and <sup>57</sup>Fe Mössbauer data show that, in common with Sr<sub>2</sub>FeIrO<sub>6</sub>, the cation substituted Sr<sub>2- x</sub>A <sub>x</sub>Fe<sub>1- y</sub>Ga <sub>y</sub>IrO<sub>6</sub> phases undergo transitions to type-II antiferromagnetically ordered states at T<sub>N</sub> ∼ 120 K. However, in contrast to stoichiometric Sr<sub>2</sub>FeIrO<sub>6</sub>, cation substituted samples exhibit a further magnetic transition at T<sub>A</sub> ∼ 220 K, which corresponds to the ordering of J<sub>eff</sub> ≠ 0 Ir<sup>5+</sup> centers in the cation-substituted, P2<sub>1</sub>/ n symmetry, double perovskite phases.
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B-cation arrangements in double perovskites
Michael W. Anderson, Kevin B. Greenwood, George Taylor et al. · Progress in Solid State Chemistry · 1993 · 1.1K citations