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首页> 外文期刊>Journal of Physics. Condensed Matter >Weak ferromagnetism and time-stable remanence in hematite: effect of shape, size and morphology
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Weak ferromagnetism and time-stable remanence in hematite: effect of shape, size and morphology

机译:赤铁矿弱铁磁性和时间稳定的剩余:形状,大小和形态的影响

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A number of Dzyaloshinskii-Moriya interaction (DMI) driven canted antiferromagnets or weak ferromagnets (WFM) including hematite exhibit two distinct time scales in magnetization relaxation measurements, one of which is ultra-slow. This leads to the observation of a part of remanence that is time-stable in character. In this work, our endeavor is to optimize the magnitude of this time-stable remanence for the hematite, a room temperature WFM, as a function of shape size and morphology. A substantial enhancement in the magnitude of this unique remanence is observed in porous hematite, consisting of ultra-small nano particles, as compared to crystallites grown in regular morphology, such as cuboids or hexagonal plates. This time-stable remanence exhibits a peak-like pattern with magnetic field, which is significantly sharper in porous sample. Experimental data suggest that the extent and the magnitude of the spin canting associated with the WFM phase can be best gauged by the presence of this remanence and its unusual magnetic field dependence. Temperature variation of lattice parameters bring out correlations between strain effects that alter the bond length and bond angle associated with primary super exchange paths, which in-turn systematically alter the magnitude of the time-stable remanence. This study provides insights regarding a long standing problems of anomalies in the magnitude of magnetization on repeated cooling in case of hematite. Our data caps on these anomalies, which we argue, arise due to spontaneous spin canting associated with WFM phase. Our results also elucidate on why thermal cycling protocols during bulk magnetization measurements are even more crucial for hematite which exhibits both canted as well as pure antiferromgnetic phase.
机译:许多Dzyaloshinskii-Moriya相互作用的(DMI)驱动倾斜反铁磁体或弱铁磁体(WFM),包括赤铁矿显示出两个不同的时间尺度中磁化弛豫的测量,其中之一是超慢。这导致剩磁的一部分,这是时间稳定在人物的观察。在这项工作中,我们的努力是优化该时间稳定剩磁为赤铁矿,室温WFM的大小,作为形状的大小和形态的函数。在这种独特的剩磁的大小的大幅度提高该多孔赤铁矿中观察到,其由超小纳米颗粒的,相比于常规的形态生长晶体,诸如长方体或六角形板。该时间稳定剩磁表现出峰状与磁场,其是多孔的样品中显著更清晰的图案。实验数据表明,程度和与WFM相关联的自旋斜的大小可以通过本剩磁的存在和它的不寻常的磁场依存性被最好地衡量。晶格参数带出该改变键长和与伯超级交换路径,这在转系统改变时稳定剩磁的大小相关联的键角应变效应之间的相关性的温度变化。这项研究提供了关于长在赤铁矿的情况下反复冷却站在异常的问题在磁化大小的见解。由于自发自旋这些异常我们的数据上限,我们认为,出现伪善与WFM阶段有关。我们的研究结果还阐明为什么在批量磁化,测量热循环协议是更关键的赤铁矿其表现出这两种倾斜以及纯antiferromgnetic相。

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