掺杂锰酸盐La0.7Sr0.3Mn0.95Fe0.05O3-δ的氧非化学计量学和磁性能

N. Kalanda, M. Yarmolich, A. Gurskii, A. Petrov, A. Zhaludkevich, O. Ignatenko, M. Serdechnova
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引用次数: 2

摘要

本文采用固相反应技术制备了不同氧含量的La0.7Sr0.3Mn0.95Fe0.05O3-δ固溶体。通过对样品在加热过程中氧指数(3 - δ)变化的动力学研究,确定了退火后晶粒中形成应力态。这导致了Mn4+ + e -→Mn3+还原阳离子过程中氧空位迁移率的降低,并解释了随着δ的增加和样品升温速率的增加,氧释放量减少的原因。对所得样品的磁性能进行研究,发现磁化强度与温度的关系符合居里-魏斯定律,固溶体的居里温度随着氧缺乏度的增加而降低。在“零场模式”的М (Т)依赖的低温区域(Т: ТВ)测量时,发现这些粒子处于冻结的铁磁状态。在Т ТВ处存在铁磁性,导致磁性有序状态,在这种状态下,磁性粒子的磁矩受到热波动的影响。在考虑镧锶锰矿样品磁化的温度值时,发现随着低温区温度的升高,磁振子的激发使磁有序受到干扰,磁振子的数量与波矢量能量呈二次依赖关系,且磁振子的数量与T3/2成比例增加。这导致了锰矿磁化强度的降低。考虑到磁振子光谱的二次和非二次色散规律,对在“场冷却模式”下测量到的磁化强度的温度依赖性进行了近似。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Oxygen nonstoichiometry and magnetic properties of doped manganites La0.7Sr0.3Mn0.95Fe0.05O3-δ
In this work, solid solutions of La0.7Sr0.3Mn0.95Fe0.05O3-δ with different oxygen content were obtained by the solid-phase reactions technique. Based on the investigation of the dynamics of changes in the oxygen index (3 – δ) during heating of the samples, the formation of a stressed state in their grains as a result of annealing was established. This results in a decrease in the mobility of oxygen vacancies during the reduction of cations according to the Mn4+ + e– → Mn3+ scheme and explains the decrease of released oxygen amount with an increase of δ as well as the heating rate of the samples. When studying the magnetic properties of the obtained samples, it was found that the temperature dependence of the magnetization obeys the Curie–Weiss law and as the oxygen defficiency increases, the Curie temperature for solid solutions decreases. It was found that the particles are in a frozen ferromagnetic state when measured in the low-temperature region of the М (Т) dependence in “zero-field mode” at Т ˂ ТВ. The presence of ferromagnetism at Т ˃ ТВ leads to a magnetically ordered state, in which the resulting magnetic moment of the magnetic particle is influenced by thermal fluctuations. When considering the temperature values of the magnetization of lanthanum-strontium manganite samples, it was found that with an increase of temperature in the low-temperature region, magnetic ordering is disturbed due to the excitation of magnons with a quadratic dependence of the energy from the wave vector, the number of which increases in proportion to T3/2. This results in a decrease in the manganite magnetization. The observed temperature dependence of the magnetization measured in the “field-cooling mode” was approximated taking into account the quadratic and non-quadratic dispersion laws of the magnon spectrum.
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