Magnon and spin transition contribution in heat capacity of ferromagnetic Cr-doped MnTe: Experimental evidence for a paramagnetic spin-caloritronic effect

M. H. Polash, M. Rasoulianboroujeni, D. Vashaee
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引用次数: 12

Abstract

We present experimental evidence for the simultaneous existence of the magnons and spin-state transition contributions to the heat capacity in ferromagnetic (FM) Cr-doped MnTe (Tc~280K), where the magnon heat capacity is attributed to the observed magnon-bipolar carrier-drag thermopower. The pristine antiferromagnetic (AFM) MnTe shows only a magnon-induced peak in the heat capacity near the Neel temperature, TN~307K. However, Cr-doped MnTe shows a magnon-contributed heat capacity peak at ~293K with an additional peak in the deep paramagnetic domain near 780K. Temperature-dependent magnetic susceptibility reveals that Cr-doping initially creates low-spin (LS) states Mn2+ ions into MnTe near and below TN due to a higher crystal field induced by Cr ions. Above 400K, LS Mn2+ ions start converting into high-spin (HS) Mn2+ ions. The LS-to-HS transition of Mn2+ leads to an excess entropy and hence excess heat capacity contribution in the system. Temperature-dependent X-ray diffraction (XRD) and magnetic field-dependent susceptibility (M-H) confirmed no presence of any structural changes and magnetic polaron, respectively. Both XRD and M-H ensure that the peak of the heat capacity in the paramagnetic domain is originated solely by the spin-state transition. The heat capacity versus temperature was calculated to explain the contribution of each component, including the ones due to the phonons, magnons, spin-transition, Schottky anomaly, and lattice dilation. With the recent advances in spin-caloritronics extending the spin-based effects from magnetic to paramagnetic materials, the data from the heat capacity can play a crucial role to probe the presence of different phenomena such as paramagnon-carrier-drag and spin-entropy thermopowers.
磁振子和自旋跃迁对铁磁cr掺杂MnTe热容量的贡献:顺磁自旋热电子效应的实验证据
我们提供了同时存在的磁振子和自旋态跃迁对铁磁(FM) cr掺杂MnTe (Tc~280K)热容的贡献的实验证据,其中磁振子热容归因于观察到的磁非双极载流子拖热功率。原始反铁磁(AFM) MnTe在Neel温度(TN~307K)附近的热容只有一个磁振子感应峰。然而,cr掺杂的MnTe在~293K处表现出一个磁振子贡献的热容峰值,在780K附近的深顺磁区有一个额外的峰值。温度相关磁化率表明,Cr离子掺杂首先在靠近TN和低于TN的MnTe中产生低自旋(LS)态的Mn2+离子,这是由于Cr离子诱导的更高的晶体场。在400K以上,LS Mn2+离子开始转变为高自旋(HS) Mn2+离子。Mn2+从ls到hs的转变导致了系统中熵的过剩和热容的过剩。温度相关的x射线衍射(XRD)和磁场相关的磁化率(M-H)分别证实没有任何结构变化和磁极化子的存在。XRD和M-H均证实了顺磁畴的热容峰值完全由自旋态跃迁引起。计算了热容与温度的关系来解释每个组分的贡献,包括声子、磁振子、自旋跃迁、肖特基异常和晶格膨胀。随着自旋热电子学的最新进展,将自旋效应从磁性材料扩展到顺磁性材料,热容数据可以在探索顺磁非载流子阻力和自旋熵热能等不同现象的存在方面发挥关键作用。
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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