首页> 外文期刊>Solid State Communications >Evidence for the Griffiths phase in pure and Y-, Ca- and Cr-doped LaSr2Mn2O7 manganites
【24h】

Evidence for the Griffiths phase in pure and Y-, Ca- and Cr-doped LaSr2Mn2O7 manganites

机译:纯和Y,Ca和Cr掺杂LaSr2Mn2O7锰矿中格里菲斯相的证据

获取原文
获取原文并翻译 | 示例
           

摘要

The paramagnetic susceptibility measured on La1-xYxSr2-yCay Mn2O7 (x,x or z=0, 0.03 and 0.1) manganites does not obey the Curie-Weiss law. The Curie constant exceeds the expected values by more than order of magnitude. Based on strong disorder we have compared the experimental data with predictions based on Griffith's singularity model. We find that this model allows for consistent interpretation of the data in contrary to a model assumes that magnetic polarons make contribution akin to cluster to susceptibility. In particular the values of Curie constant agree excellently with those theoretically expected, whereas the magnetic polarons model is less satisfactory. (c) 2005 Elsevier Ltd. All rights reserved.
机译:在La1-xYxSr2-yCay Mn2O7(x,x或z = 0,0.03和0.1)锰矿上测得的顺磁化率不服从居里-魏斯定律。居里常数超出期望值的数量级以上。基于强无序性,我们将实验数据与基于格里菲斯奇点模型的预测进行了比较。我们发现,该模型允许对数据进行一致的解释,这与模型假设磁极化子做出类似于磁化率簇的贡献相反。特别是居里常数的值与理论上期望的值非常吻合,而磁极化子模型则不太令人满意。 (c)2005 Elsevier Ltd.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号