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Jahn-Teller distortions, cation ordering and octahedral tilting in perovskites

机译:钙钛矿中的Jahn-Teller变形,阳离子有序化和八面体倾斜

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In transition metal oxides, preferential occupation of specific d orbitals on the transition metal ion can lead to the development of a long-range ordered pattern of occupied orbitals. This phenomenon, referred to as orbital ordering, is usually observed indirectly from the cooperative Jahn-Teller distortions (CJTDs) that result as a consequence of the orbital ordering. This paper examines the interplay between orbital ordering, octahedral tilting and cation ordering in perovskites. Both ternary AMX(3) perovskites containing an active Jahn-Teller (J-T) ion on the octahedral site and quaternary A(2)MM'X-6 perovskites containing a J-T ion on one-half of the octahedral sites have been examined. In AMX3 perovskites, the tendency is for the occupied 3d(3x2-r2) and 3d(3z2-r2) orbitals to order in the ac plane, as exemplified by the crystal structures of LaMnO3 and KCuF3. This arrangement maintains a favorable coordination environment for the anion sites. In AMX3 perovskites, octahedral tilting tends to enhance the magnitude of the J-T distortions. In A(2)MM'X-6 perovskites, the tendency is for the occupied 3d(3z2-r2) orbitals to align parallel to the c axis. This pattern maintains a favorable coordination environment about the symmetric M'-cation site. The orbital ordering found in rock-salt ordered A(2)MM'X-6 perovskites is compatible with octahedral rotations about the c axis ( Glazer tilt system a 0 a 0 c.) but appears to be incompatible with GdFeO3-type octahedral tilting (tilt system (-)b(+)a.). [References: 48]
机译:在过渡金属氧化物中,过渡金属离子上特定d轨道的优先占据会导致占据轨道的长程有序模式的发展。通常,这种现象称为轨道排序,通常是由于轨道排序导致的协同Jahn-Teller失真(CJTD)间接观察到的。本文研究了钙钛矿中轨道有序,八面体倾斜和阳离子有序之间的相互作用。八面体位点上均含有活性Jahn-Teller(J-T)离子的三元AMX(3)钙钛矿和八面体位点的一半中均含J-T离子的四元A(2)MM'X-6钙钛矿都已被研究过。在AMX3钙钛矿中,被占据的3d(3x2-r2)和3d(3z2-r2)轨道趋向于在ac平面上有序排列,例如LaMnO3和KCuF3的晶体结构。这种安排为阴离子部位保持了良好的配合环境。在AMX3钙钛矿中,八面体倾斜会增强J-T变形的幅度。在A(2)MM'X-6钙钛矿中,趋势是被占据的3d(3z2-r2)轨道平行于c轴对齐。这种模式在对称的M'阳离子位点上保持了良好的配位环境。在岩石盐有序A(2)MM'X-6钙钛矿中发现的轨道有序与绕c轴的八面体旋转兼容(Glazer倾斜系统a 0 a 0 c。),但似乎与GdFeO3型八面体倾斜不兼容。 (倾斜系统(-)b(+)a。)。 [参考:48]

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