arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 2105.12331cond-mat.str-elcond-mat.mtrl-sci
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双钙钛矿$R_2$ NiMnO $_6$的稀土调谐磁性和磁热效应

Rare-earth tuned magnetism and magnetocaloric effects in double perovskites $R_2$NiMnO$_6$

Anzar Ali, Kanika Pasrija, Gyaneshwar Sharma, Sanjeev Kumar, Yogesh Singh

摘要:

对双钙钛矿材料$R_2$ NiMnO $_6$与$R =$ Pr,Nd,Sm,Gd,Tb,Dy的磁化强度和磁热效应进行了全面的实验研究。虽然顺磁性到铁磁性的转变,T $_{\rm C}$在$\sim 100 - 200~$ K范围内,是一个共同的特点,可以归因于Mn $^{4+}$和Ni $^{2+}$磁矩的排序,定性不同的行为取决于$R$的选择,在低温下观察到。磁化强度的这些低温异常也表现在磁熵的变化中,$-ΔS_{M}$,其符号取决于$R$的选择。为了理解这些结果,我们提出了基于平均场近似和Monte Carlo模拟的最小自旋模型的理论分析。该模型正确地捕捉了实验观察的关键特征。

英文摘要:

We present a comprehensive experimental study of magnetization and magnetocaloric effect (MCE) in double perovskite (DP) materials $R_2$NiMnO$_6$ with $R =$ Pr, Nd, Sm, Gd, Tb, and Dy. While a paramagnetic to ferromagnetic transition, with T$_{\rm C}$ in the range $\sim 100 - 200~$K, is a common feature that can be attributed to the ordering of Mn$^{4+}$ and Ni$^{2+}$ magnetic moments, qualitatively distinct behavior depending on the choice of $R$ is observed at low temperatures. These low-temperature anomalies in magnetization are also manifest in the change in magnetic entropy, $-ΔS_{M}$, whose sign depends on the choice of $R$. In order to understand these results, we present theoretical analysis based on mean-field approximation and Monte Carlo simulations on a minimal spin model. The model correctly captures the key features of the experimental observations.

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