铁掺杂镧锶锰矿中氧交换的特征

IF 0.2 Q4 FORESTRY Lesnoy Zhurnal-Forestry Journal Pub Date : 2023-04-14 DOI:10.17073/1609-3577-2023-1-5-16
A. Gurskii, N. Kalanda, M. Yarmolich, A. Petrov, P. N. Kireev
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引用次数: 0

摘要

根据热重分析数据,计算了固相反应法制备的La0.7Sr0.3Mn0.9Fe0.1O3-δ组成的锰矿石的氧指数(3 -δ)。氧吸附-解吸曲线分析表明,在pO2 = 10 Pa和pO2 = 400 Pa时,氧的释放和吸收过程是不可逆的。氧萃取速率最大值对应的导数dδ/dt = f(T)的最小值反映了锰矿氧脱附速率变化的复杂特征。当加热和冷却速率从6.6 K/min降低到2.6 K/min时,磁体结构中负离子迁移率的变化∆δ显著,表明负离子迁移率与磁体结构中氧浓度的关系。结果表明,在La0.7Sr0.3Mn0.9Fe0.1O3-δ锰矿中,氧的解吸动力学与Cramers模型的指数依赖关系很好地描述了,这意味着解吸氧没有返回到样品中。该模型表明了样品中氧解吸过程中通过屏障的扩散通量的非平稳性。用Merzhanov法计算了不同氧分压下的氧解吸活化能,结果表明,在La0.7Sr0.3Mn0.9Fe0.1O3-δ抽氧初期,氧解吸活化能有一个最小值(Еа = 103.7 kJ/mol, δ = 0.005),随着氧空位浓度的增加,氧解吸活化能逐渐升高,达到饱和(Еа = 134.3 kJ/mol, δ = 0.06)。假设随着氧空位浓度的增加,它们之间发生相互作用,随后是它们的排序过程和缔合物的形成。
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Characteristic features of oxygen exchange in lanthanum-strontium manganites doped with iron
Based on the data of thermogravimetric analysis the values of the oxygen index (3–δ) in the manganite of the La0.7Sr0.3Mn0.9Fe0.1O3-δ composition, obtained by solid-phase reaction technique, have been calculated. The analysis of oxygen sorption-desorption curves showed that the processes of oxygen release and absorption at pO2 = 10 Pa and pO2 = 400 Pa are not reversible. The minima of the derivative dδ/dt = f(T) corresponding to the maxima of the oxygen extraction rate indicate the complex character of changes in the oxygen desorption rate from manganite. The decrease in the heating and cooling rate from 6.6 to 2.6 K/min resulted in a significant change in the value ∆δ, indicating the dependence of anion mobility on the oxygen concentration in the magnet structure. It has been revealed that in the La0.7Sr0.3Mn0.9Fe0.1O3-δ manganite the oxygen desorption kinetics is well described by the exponential dependence on the Cramers model, which implies no return of desorbed oxygen to the sample. This model indicates the non-stationarity of the diffusion flux through the barrier during desorption of oxygen from samples. The calculation of the activation energy of oxygen desorption by the Merzhanov method at various partial pressures of oxygen has shown that at the initial stage of oxygen extraction from La0.7Sr0.3Mn0.9Fe0.1O3-δ, the activation energy of oxygen desorption has a minimum value (Еа = 103.7 kJ/mol at δ = 0.005) and as the concentration of oxygen vacancies increases, it rises reaching saturation (Еа = 134.3 kJ/mol at δ = 0.06). It is assumed that with an increase in the concentration of oxygen vacancies, an interaction occurs between them, followed by the processes of their ordering with the formation of associates.
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