Studies of manganites by magnetic resonance spectroscopy methods

V. Dyakonov, A. Prohorov, V. Shapovalov, V. Pashchenko, P. Aleshkevych, S. Piechota, H. Szymczak
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Abstract

In this work, we present the studies of manganites with superfluous manganese content performed by the magnetic resonance spectroscopy methods. The ferromagnetic resonance (FMR) has been measured on the films. The symmetrical FMR line in paramagnetic phase has the Dysonian-like shape below Tc. The FMR linewidth increases abruptly near the transition temperature. By comparing resonance fields oriented parallel and perpendicular to the film plane, the easy axis of magnetization was determined to be perpendicular to the film plane. In the perpendicular magnetic field, the spin-wave resonance (SWR) spectrum consisting of seventeenth of spin-wave modes has been observed in the (formula available in paper) film. Two of them observed on the high-field side of SWR spectrum are connected to a surface modes. The others are the bulk nonuniform spin-wave modes. Based on a study of temperature and angular dependencies of SWR and FMR spectra, the spin- wave stiffness, g-factor and exchange constant were established. An analysis of the (formula available in paper)has shown that a wide asymmetrical line can be uniquely expanded into four components with different resonance frequencies. There are manganese ions, which ionization states are close to (3+) and (4+) as well as the Mn ions with intermediate valence resulted from the high-frequency electron exchange.
磁共振波谱法研究锰矿石
在这项工作中,我们提出了用磁共振波谱法对锰含量过剩的锰矿石进行研究。对薄膜进行了铁磁共振(FMR)测量。顺磁相对称FMR线在Tc以下呈戴森氏状。FMR线宽在转变温度附近急剧增大。通过对比平行于膜面和垂直于膜面的共振场,确定了垂直于膜面的易磁化轴。在垂直磁场中,在薄膜中观察到由17个自旋波模式组成的自旋波共振谱。其中在SWR谱高场侧观测到的两个与表面模式相连。其他是体非均匀自旋波模式。通过对SWR和FMR光谱的温度依赖性和角依赖性的研究,建立了自旋波刚度、g因子和交换常数。对(论文中提供的公式)的分析表明,宽的不对称线可以唯一地扩展成具有不同谐振频率的四个分量。其中有电离态接近(3+)和(4+)的锰离子,也有高频电子交换产生的中间价态锰离子。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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