Successive ferroelectric orders and magnetoelectric coupling without long-range magnetic order in highly frustrated pyrochlore compounds: Sm$_2$Ti$_{2-x}$V$_x$O$_7$

S. Mukherjee, O. Ivashko, S. Majumdar, A. Kumar, S. Giri
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Abstract

Sm$_2$Ti$_2$O$_7$, a member of rare-earth titanate pyrochlores, exhibits dipolar-octupolar antiferromagnetism below $T_N$ = 0.35 K. We observed two ferroelectric transitions at 182 ($T_{FE1}$) and 52 K ($T_{FE2}$), significantly higher than $T_N$ for Sm$_2$Ti$_{2-x}$V$_x$O$_7$ ($x$ = 0, 0.1). Although the ferroelectric transition temperatures remain unchanged, the polarization value decreases considerably with V doping. A structural transition to a polar $R3m$ rhombohedral phase from the cubic $Fd\bar{3}m$ structure occurs at $T_{FE1}$, involving a distortion in the pyochlore lattice. Remarkably, significant linear magnetoelectric coupling is observed in both compounds, with further enhancement of magnetoelectric coupling due to magnetic V doping. The existence of magnetoelectric coupling without long-range magnetic order in a frustrated pyrochlore system could enable the tailoring of magnetoelectric coupling properties, which can be further fine-tuned through V doping. The emergence of ferroelectricity in a frustrated magnetic system introduces an intriguing aspect to these compounds and paves the way for developing ferroelectric order driven by the alleviation of magnetic frustration in pyrochlore systems.
高沮度火成化合物中无长程磁序的连续铁电阶和磁电耦合:Sm$_2$Ti$_{2-x}$V$_x$O$_7$
Sm$_2$Ti$_2$O$_7$ 是稀土钛酸盐火成岩的一种,在 $T_N$ = 0.35 K 以下表现出两极-八极反铁磁性。我们观察到 Sm$_2$Ti$_{2-x}$V$_x$O$_7$ ($x$=0,0.1) 在 182 ($T_{FE1}$) 和 52 K ($T_{FE2}$) 发生了两个铁电转换,明显高于 $T_N$。在 $T_{FE1}$ 时,结构从立方的 $Fd\bar{3}m$ 结构转变为极性的 $R3m$ 菱形相,这涉及到菱形晶格的畸变。值得注意的是,在这两种化合物中都观察到了显著的线性磁电耦合,而磁性 V 掺杂又进一步增强了磁电耦合。掺杂磁性 V 可进一步增强磁电耦合。在受挫火绿宝石体系中存在无长程磁序的磁电耦合,这使得磁电耦合特性的定制成为可能,并可通过掺杂 V 对其进行进一步微调。在沮喪磁性體系中出現的鐵電性為這些化合物帶來了有趣的一面,並為在火成體系中緩解磁沮喪驅動鐵電秩序的發展鋪平了道路。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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