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arXiv 1806.03098cond-mat.mtrl-scicond-mat.stat-mech
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内外微扰对锰氧化物铁磁相变的作用:三临界点的存在

Role of external and internal perturbations on ferromagnetic phase transitions in manganites: Existence of tricritical points

Prabir K Mukherjee, Prosenjit Sarkar, Amit K Chattopadhyay

摘要:

提出了一个唯象的平均场论来描述外磁场、压力和化学替代对锰氧化物铁磁-顺磁相变性质的作用。外场(或压力)的应用转移的过渡,导致场(或压力)依赖的相边界,沿该三临界点被证明存在的一阶FM-PM转变成为二阶。我们表明,FM过渡上的化学取代的效果是类似的外部扰动(磁场和压力),这包括存在一个三临界点,在该过渡的顺序变化。我们的理论预测令人满意地解释了FM-PM过渡的性质,在几个系统中观察到的。从我们的实验数据,如Sm $_{0.52}$ Sr $_{0.48}$ MnO $_3$的大范围的巨磁阻锰氧化物单晶的建模假设已得到严格验证。理论模型预测的一个三临界点已在本实验中得到验证,这提供了一个主要的分歧的强度的模型提出。

英文摘要:

A phenomenological mean-field theory is presented to describe the role of external magnetic field, pressure and chemical substitution on the nature of ferromagnetic (FM) to paramagnetic (PM) phase transition in manganites. The application of external field (or pressure) shifts the transition, leading to a field (or pressure) dependent phase boundary along which a tricritical point is shown to exist where a first-order FM-PM transition becomes second-order. We show that the effect of chemical substitution on the FM transition is analogous to that of external perturbations (magnetic field and pressure); this includes the existence of a tricritical point at which the order of transition changes. Our theoretical predictions satisfactorily explain the nature of FM-PM transition, observed in several systems. The modeling hypothesis has been critically verified from our experimental data from a wide range of colossal magnetoresistive manganite single crystals like Sm$_{0.52}$Sr$_{0.48}$MnO$_3$. The theoretical model prediction of a tricritical point has been validated in this experiment which provides a major ramification of the strength of the model proposed.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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