Predictions and Magnetic Characterization of M-type Hexaferrites Doped with Two Cations in the Fe3+ Site

Pedro Antonio Mariño-Castellanos, Valery Alexevich Lapshinsky, C. Pupo, A. Vega-García, E. Fernandez-cruz, Braddy Ivan Jimenez-Morales
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引用次数: 1

Abstract

A theoretical and experimental study of magnetic properties of M-type barium hexaferrites, doped with two cations in the Fe3+ sites: (Co3+, Al3+), (Co2+, Ti4+) and (Co2+, Sn4+) is reported. The theoretical predictions were made using the generalization of a model on the distribution of dopants in the crystallographic sites under study. This approach allows a better interpretation of the kinetics of obtaining the samples from the structural and magnetic characterization. In the reported model, the maximum limit refers to theoretical optimum parameters. With these concepts, were established quantitative relationships between dopant amount per crystallographic site and magnetic properties predicted of these systems. The comparison between the experimental values and the predicted magnitudes showed that, in general, the samples were obtained with parameters obtained close to the theoretical ones for traditional ceramic methods. Such an approach is rarely taken into account in the reported bibliography.
在Fe3+位置掺杂两种阳离子的m型六铁体的预测和磁性表征
本文报道了在Fe3+位置掺杂两种阳离子(Co3+, Al3+)、(Co2+, Ti4+)和(Co2+, Sn4+)的m型钡六铁体的磁性能的理论和实验研究。理论预测是利用对所研究的晶体位置中掺杂物分布的模型进行推广。这种方法可以更好地解释从结构和磁性表征中获得样品的动力学。在所报道的模型中,最大极限是指理论最优参数。利用这些概念,建立了每个晶位掺杂量与预测体系磁性能之间的定量关系。实验值与预测震级的比较表明,总体而言,得到的样品参数接近传统陶瓷方法的理论参数。在报告的参考书目中很少考虑到这种方法。
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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