arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 1305.4497cond-mat.str-elcond-mat.mtrl-sci
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双钙钛矿结构Sr $_{2}$ FeMoO $_{6}$中硬磁晶界的观察

Observation of magnetically hard grain boundaries in double-perovskite Sr$_{2}$FeMoO$_{6}$

Y. Takahashi, V. K. Verma, G. Shibata, T. Harano, K. Ishigami, K. Yoshimatsu, T. Kadono, A. Fujimori, A. Tanaka, F. -H. Chang, H. -J. Lin, D. J. Huang, C. T. Ch… 展开作者

Y. Takahashi, V. K. Verma, G. Shibata, T. Harano, K. Ishigami, K. Yoshimatsu, T. Kadono, A. Fujimori, A. Tanaka, F. -H. Chang, H. -J. Lin, D. J. Huang, C. T. Chen, B. Pal, D. D. Sarma

摘要:

铁磁Sr $_{2}$ FeMoO $_{6}$多晶的异常低温磁电阻(MR)归因于作为自旋阀的硬磁晶界。利用X射线吸收光谱(XAS)和X射线磁性圆二色性(XMCD)的不同探测模式探测到了多晶Sr $_{2}$ FeMoO $_{6}$晶粒和晶界的不同磁滞曲线,即:总电子产额(TEY)模式(探测深度$\sim$ 5 nm)和总荧光产额(TFY)模式(探测深度$\sim$ 100 nm)。在20 K时,在TEY模式($H_{\rm c,TEY}$)中检测到的磁性是在TFY模式($H_{\rm c,TFY}$)中检测到的磁性的数倍,表明晶界的铁磁性比晶粒的铁磁性更强。在室温下,晶界磁性变软,$H_{\rm c,TEY}$和$H_{\rm c,TFY}$几乎相同。从XAS和XMCD谱的线形分析,我们发现,在晶界区域的铁磁成分主要由Fe $^{2+}$或良好的屏蔽信号,而非磁性成分主要由Fe $^{3+}$或不良的屏蔽信号。

英文摘要:

Unusual low temperature magneto-resistance (MR) of ferromagnetic Sr$_{2}$FeMoO$_{6}$ polycrystals has been attributed to magnetically hard grain boundaries which act as spin valves. We detected the different magnetic hysteresis curves for the grains and the grain boundaries of polycrystalline Sr$_{2}$FeMoO$_{6}$ by utilizing the different probing depths of the different detection modes of x-ray absorption spectroscopy (XAS) and x-ray magnetic circular dichroism (XMCD), namely, the total electron yield (TEY) mode (probing depth $\sim$5 nm) and the total fluorescence yield (TFY) mode (probing depth $\sim$100 nm). At 20 K, the magnetic coercivity detected in the TEY mode ($H_{\rm c,TEY}$) was several times larger than that in the TFY mode ($H_{\rm c,TFY}$), indicating harder ferromagnetism of the grain boundaries than that of the grains. At room temperature, the grain boundary magnetism became soft and $H_{\rm c,TEY}$ and $H_{\rm c,TFY}$ were nearly the same. From line-shape analysis of the XAS and XMCD spectra, we found that in the grain boundary region the ferromagnetic component is dominated by Fe$^{2+}$ or well-screened signals while the non-magnetic component is dominated by Fe$^{3+}$ or poorly-screened signals.

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