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在斯格明子气泡状无限层LaSrMnO锰钙钛矿中存在类3D伊辛铁磁性。

3D-Ising like ferromagnetism in skyrmionic-bubbles host infinite-layer LaSrMnO manganite perovskite.

作者信息

Kumar Tiwari Jeetendra, Chandr Chauhan Harish, Kumar Birendra, Ghosh Subhasis

机构信息

School of Physical Sciences, Jawaharlal Nehru University, New Delhi 110067, India.

出版信息

J Phys Condens Matter. 2020 May 8;32(19):195803. doi: 10.1088/1361-648X/ab6d14.

Abstract

The critical behavior of infinite-layer LaSrMnO of Ruddlesden-Popper series manganite has been studied around the transition temperature ([Formula: see text]). To reveal the universality class that explains the critical behavior in LaSrMnO several methods, such as modified Arrott plots, Kouvel-Fisher, entropy and critical isotherm analysis have been employed. The critical exponent [Formula: see text] for infinite-layer is obtained independently from critical magnetization isotherm and found to satisfy the Widom scaling relation [Formula: see text]. The universality class of the critical phenomenon in infinite-layer LaSrMnO manganite can be explained with the help of renormalization group theory approach for three dimensional (3D) systems. We have shown that a short-range 3D-Ising type interaction is responsible for ferromagnetic and second-order phase transition to paramagnetic phase.

摘要

已围绕转变温度([公式:见正文])对Ruddlesden-Popper系列锰氧化物的无限层LaSrMnO的临界行为进行了研究。为了揭示解释LaSrMnO中临界行为的普适类,采用了多种方法,如修正的阿罗特图、库维尔-费舍尔法、熵和临界等温线分析。无限层的临界指数[公式:见正文]是从临界磁化等温线独立获得的,并发现满足维登标度关系[公式:见正文]。无限层LaSrMnO锰氧化物中临界现象的普适类可以借助三维(3D)系统的重整化群理论方法来解释。我们已经表明,短程3D伊辛型相互作用是铁磁和向顺磁相的二级相变的原因。

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