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Chemically-induced structural deformation of layered perovskite oxides

机译:层状钙钛矿氧化物的化学诱导结构变形

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In order to understand the behavior of the crystal lattice deformation induced by the interstitial oxygen formation in La2(Ni0.9M0.1)O4+δ (M = Fe, Co, Cu), thermogravimetry, coulometric titration, and high temperature X-ray diffraction measurements were carried out in the temperature range between 873 to 1173 K and the P(O2) range between 10-24 to 1 bar. Oxygen content variation under wide range of P(O2) could be successfully evaluated by combining thermogravimetry and coulometric titration techniques. Compared with non-doped La2NiO4+δ, La2(Ni0.9Fe0.1)O4+δ and La2(Ni0.9Co0.1)O4+δ have more interstitial oxygen while La2(Ni0.9Cu0.1)O4+δ have less. Crystal structure at high temperatures was analyzed assuming the tetragonal symmetry, I4/mmm, for all compositions. With increasing interstitial oxygen concentration, the lattice parameter perpendicular to the perovskite layer increased and that parallel to the perovskite layer decreased. Consequently, the change of the cell volume by the interstitial oxygen formation was small, meaning macroscopic chemical expansion is small.
机译:为了了解由La2(Ni0.9M0.1)O4 +δ(M = Fe,Co,Cu),热重法,库仑滴定法和高温X射线中的间隙氧形成引起的晶格变形行为衍射测量是在873至1173 K的温度范围和P(O2)在10至24至1 bar的温度范围内进行的。结合热重法和库仑滴定技术可以成功地评估P(O2)在宽范围内的氧含量变化。与未掺杂的La2NiO4 +δ相比,La2(Ni0.9Fe0.1)O4 +δ和La2(Ni0.9Co0.1)O4 +δ的间隙氧更多,而La2(Ni0.9Cu0.1)O4 +δ的间隙氧更少。 。假设所有组成均为四方对称,则分析高温下的晶体结构。随着间隙氧浓度的增加,垂直于钙钛矿层的晶格参数增加,而平行于钙钛矿层的晶格参数减小。因此,由间隙氧形成引起的细胞体积变化小,意味着宏观化学膨胀小。

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