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Unusual properties and features of oxygen nonstoichiometry of La-Sr manganites with manganese replacement by a combination of nickel and germanium

机译:镍和锗组合置换锰的La-Sr锰氧化物氧非化学计量的异常性质和特征

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When studying manganites of the system La_(1-c)Sr_cMn_(1-x)(Ni~((2+)_(0.5))Ge~((4+)_(0.5)))_xO_(3+γ) (x = 0.05; 0.10; 0.15; 0.15 ≤ c ≤ 0.35), it was experimentally established that after reductive annealing, which leads the oxygen content to the stoichiometric one, unit cell volume (v) of the samples decreases and at c ≥ 0.19 it is less than after annealing in oxygen. Based on the analysis of various charge compensation mechanisms using derived dependences of v on the oxygen content and taking into account the changes in magnetic and electrical parameters, it is established that experimental data can be explained only with the allowance for formation of singly charged oxygen ions. The relationships between magnetic parameters of the manganites and their composition, structural characteristics and deviations from oxygen stoichiometry are explained. The possibility of local ferromagnetic ordering of uncompensated spins of Ni~(2+) ions due to their interaction with singly charged O~- anions is considered.
机译:在研究La_(1-c)Sr_cMn_1-x(Ni~((2+)(0.5))Ge~((4+)(0.5))xO_3+γ(x=0.05;0.10;0.15;0.15)系锰氧化物时≤ C≤ 0.35),实验证明,在还原退火后,使氧含量达到化学计量比,样品的单位电池体积(v)减小,在c≥ 0.19小于在氧气中退火后的值。基于对各种电荷补偿机制的分析,利用导出的v对氧含量的依赖关系,并考虑到磁性和电学参数的变化,可以确定,实验数据只能在允许形成单电荷氧离子的情况下进行解释。解释了锰氧化物的磁性参数与其组成、结构特征和氧化学计量偏差之间的关系。考虑了Ni~(2+)离子与单电荷O~-阴离子相互作用产生的非补偿自旋局部铁磁有序化的可能性。

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