2013/05/20 by Y. Takahashi, V. K. Verma, G. Shibata +14
Materials Science · Physics and Astronomy · #Chemical and Physical Properties of Materials #Coercivity #Ferromagnetism #Grain boundary #Grain size #Magnetic and transport properties of perovskites and related materials #Magnetic circular dichroism #Magnetism #Multiferroics and related materials #cond-mat.mtrl-sci #cond-mat.str-el
paper · pdf · doi:10.1209/0295-5075/108/27003
published as Europhys. Lett. 108, 27003 (2014) · 4 pages, 3 figures
arxiv created 2013/05/20 · openalex publication_date 2014/10/01 · arxiv updated 2014/10/21 · openalex created_date 2016/06/24 · openalex updated_date 2026/08/05
Unusual low temperature magneto-resistance (MR) of ferromagnetic Sr2FeMoO6 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 Sr2FeMoO6 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 ∼5 nm) and the total fluorescence yield (TFY) mode (probing depth ∼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 Fe2+ or well-screened signals while the non-magnetic component is dominated by Fe3+ or poorly-screened signals.