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低掺杂锰氧化物轨道域中的选择性取代:基于格里菲斯现象和玻璃态特征改性的研究

Selective substitution in orbital domains of a low doped manganite: an investigation from Griffiths phenomenon and modification of glassy features.

作者信息

Mukherjee K, Banerjee A

机构信息

UGC-DAE Consortium for Scientific Research, University Campus, Khandwa Road, Indore 452017, MP, India.

出版信息

J Phys Condens Matter. 2009 Mar 11;21(10):106001. doi: 10.1088/0953-8984/21/10/106001. Epub 2009 Feb 13.

DOI:10.1088/0953-8984/21/10/106001
PMID:21817440
Abstract

An effort is made to study the contrast in magnetic behavior resulting from minimal disorder introduced by substitution of 2.5% Ga or Al in Mn site of La(0.9)Sr(0.1)MnO(3). It is considered that Ga or Al selectively create disorder within the orbital domains or on its walls, causing enhancement of Griffiths phase (GP) singularity for the former and disappearance of it in the latter case. It is shown that Ga replaces Mn(3+), which is considered to be concentrated within the domains, whereas Al replaces Mn(4+), which is segregated on the hole-rich walls, without causing any significant effect on structure or ferromagnetic transition temperatures. Thus, it is presumed that the effect of disorder created by Ga extends across the bulk of the domain having correlation over a similar length scale, resulting in enhancement of the GP phenomenon. In contrast, the effect of disorder created by Al remains restricted to the walls, resulting in the modification of the dynamics arising from the domain walls and suppresses the GP. Moreover, contrasting features are observed in the low temperature region of the compounds; a re-entrant spin-glass-like behavior is observed in the Ga-doped sample, while the observed characteristics for the Al-doped sample are ascribed only to modified domain wall dynamics with the absence of any glassy phase. Distinctive features in third-order susceptibility measurements reveal that the magnetic ground state of the entire series comprises of orbital domain states. These observations bring out the role of the nature of disorder on the GP phenomenon and also reconfirms the character of self-organization in low doped manganites.

摘要

人们致力于研究在La(0.9)Sr(0.1)MnO(3)的Mn位点上用2.5%的Ga或Al进行替代所引入的最小无序导致的磁行为差异。据认为,Ga或Al会在轨道畴内或其壁上选择性地产生无序,前者会导致格里菲斯相(GP)奇点增强,而在后者情况下则会使其消失。结果表明,Ga取代了被认为集中在畴内的Mn(3+),而Al取代了在富空穴壁上偏析的Mn(4+),且对结构或铁磁转变温度没有产生任何显著影响。因此,可以推测由Ga产生的无序效应会扩展到具有相似长度尺度相关性的整个畴体,从而导致GP现象增强。相比之下,由Al产生的无序效应仅限于壁,导致畴壁动力学发生改变并抑制了GP。此外,在这些化合物的低温区域观察到了对比特征;在Ga掺杂样品中观察到了类似再入自旋玻璃的行为,而Al掺杂样品观察到的特征仅归因于畴壁动力学的改变,且不存在任何玻璃相。三阶磁化率测量中的独特特征表明,整个系列的磁基态由轨道畴态组成。这些观察结果揭示了无序性质对GP现象的作用,也再次证实了低掺杂锰酸盐中自组织的特性。

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