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arXiv 1002.1635cond-mat.str-el
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磁电和多铁辉石LiFeSi2O6和NaFeSi2O6的μ子自旋弛豫和heat capacity测量

Muon-spin relaxation and heat capacity measurements on the magnetoelectric and multiferroic pyroxenes LiFeSi2O6 and NaFeSi2O6

P. J. Baker, H. J. Lewtas, S. J. Blundell, T. Lancaster, I. Franke, W. Hayes, F. L. Pratt, L. Bohaty, P. Becker

摘要:

两个辉石化合物LiFeSi2O6和NaFeSi2O6的μ子自旋弛豫和热容测量的结果表明,尽管其潜在的结构相似的磁有序是相当不同的。在LiFeSi2O6中,在TN以下观察到单个μ子旋进频率,这与热容量和相称的磁结构中TN处的单峰一致。在外加磁场中,热容峰一分为二。相比之下,对于天然NaFeSi2O6,在零磁场下观察到多铁性,观察到快速的高斯去极化,表明磁性结构更复杂。合成NaFeSi2O6显示出单一的μ子旋进频率,但具有比锂化合物大得多的阻尼率。热容量测量再现以前从其他技术得到的相图,并表明磁熵主要与准一维Fe 3+链中的相关性的建立有关。

英文摘要:

The results of muon-spin relaxation and heat capacity measurements on two pyroxene compounds LiFeSi2O6 and NaFeSi2O6 demonstrate that despite their underlying structural similarity the magnetic ordering is considerably different. In LiFeSi2O6 a single muon precession frequency is observed below TN, consistent with a single peak at TN in the heat capacity and a commensurate magnetic structure. In applied magnetic fields the heat capacity peak splits in two. In contrast, for natural NaFeSi2O6, where multiferroicity has been observed in zero-magnetic-field, a rapid Gaussian depolarization is observed showing that the magnetic structure is more complex. Synthetic NaFeSi2O6 shows a single muon precession frequency but with a far larger damping rate than in the lithium compound. Heat capacity measurements reproduce the phase diagrams previously derived from other techniques and demonstrate that the magnetic entropy is mostly associated with the build up of correlations in the quasi-one-dimensional Fe3+ chains.

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