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首页> 外文期刊>RSC Advances >Critical phenomena and estimation of the spontaneous magnetization from a mean field analysis of the magnetic entropy change in La0.7Ca0.1Pb0.2Mn0.95Al0.025Sn0.025O3
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Critical phenomena and estimation of the spontaneous magnetization from a mean field analysis of the magnetic entropy change in La0.7Ca0.1Pb0.2Mn0.95Al0.025Sn0.025O3

机译:从La 0.7 Ca 0.1 Pb 0.2 Mn 的磁熵变的平均场分析确定临界现象和自发磁化0.95 Al 0.025 Sn 0.025 O 3

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摘要

In the present work, we have studied the universal critical behavior in the perovskite-manganite compound La0.7Ca0.1Pb0.2Mn0.95Al0.025Sn0.025O3. Experimental results revealed that all samples exhibit a second-order magnetic phase transition. To study the critical behavior of the paramagnetic–ferromagnetic transition, various techniques such as modified Arrott plots, the Kouvel–Fisher method and critical isotherm analysis were used to determine the values of the Curie temperature TC, as well as the critical exponents β (corresponding to the spontaneous magnetization), γ (corresponding to the initial susceptibility) and δ (corresponding to the critical magnetization isotherm). The critical exponent values for our sample are consistent with the prediction of the mean field model (β = 0.46, γ = 1.0, and δ = 2.94 at an average TC = 302.12 K), indicating that the magnetic interactions are long-range. The reliability of the critical exponent values was confirmed by the Widom scaling relation (WSR) and the universal scaling hypothesis. Moreover, to estimate the spontaneous magnetization of La0.7Ca0.1Pb0.2Mn0.95Al0.025Sn0.025O3 perovskite, we used the magnetic entropy change (ΔSM), obtained from isothermal magnetization. The results obtained through this approach are compared to those obtained from classical analysis using Arrott curves. An excellent agreement is found between this approach and the one obtained from the extrapolation of the Arrott curves.
机译:在目前的工作中,我们研究了钙钛矿-锰矿化合物La 0.7 Ca 0.1 的普遍临界行为。铅 0.2 Mn 0.95 Al 0.025 Sn < small> 0.025 O 3 。实验结果表明,所有样品均表现出二阶磁性相变。为了研究顺磁-铁磁转变的临界行为,使用了各种技术,例如修改后的Arrott图,Kouvel-Fisher方法和临界等温线分析来确定居里温度 T 的值。 C 以及临界指数β(对应于自发磁化强度),γ(对应于初始磁化率)和δ(与临界磁化等温线相对应)。我们样本的临界指数值与平均场模型的预测一致(β = 0.46,γ = 1.0和δ =在平均 T C = 302.12 K时为2.94),表明磁性相互作用是长距离的。关键指数值的可靠性通过Widom比例关系(WSR)和通用比例假设得到了证实。此外,估计La 0.7 Ca 0.1 Pb 0.2 的自发磁化强度 Mn 0.95 Al 0.025 Sn 0.025 O 3 钙钛矿,我们使用了磁熵变(Δ S M < / small>),由等温磁化获得。将通过此方法获得的结果与使用Arrott曲线从经典分析获得的结果进行比较。在此方法与从Arrott曲线外推获得的方法之间找到了一个极好的协议。

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