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Domain structure evolution in the ferromagnetic Kagome-lattice Weyl semimetal Co3Sn2S2

机译:域结构演变在铁磁性kagome-rateice weyl semimetal co3sn2s2中

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摘要

Co3Sn2S2, a Weyl semimetal that consists of layers of Kagome lattices, undergoes a transition from a high temperature paramagnetic phase to a low temperature ferromagnetic phase below 177 K. The phase transition occurs through an intermediate non-trivial magnetic phase, the so called 'A'-phase just below the Curie temperature. The 'A'-phase was earlier linked with a competing anti-ferromagnetic phase, a spin-glass phase and certain indirect measurements indicated the possibility of magnetic Skyrmions in this phase. We have imaged the magnetic domain structure in a single crystal of Co3Sn2S2 at different temperatures, magnetic fields and field-angles by magnetic force microscopy. At low temperatures, we observed stripe domains indicating presence of uniaxial anisotropy. Above 130 K, the domain walls become mobile and they tend to align relatively easily when the magnetic field is increased along the c-axis than in the a-b plane. Our detailed study of field-dependent domain evolution reveal that the anomalous phase below T-c through which the transition happens is most probably governed by domain wall motion.
机译:Co3Sn2S2是一种由Kagome晶格层组成的Weyl半金属,在177 K以下经历了从高温顺磁相到低温铁磁相的转变。相变发生在居里温度以下的中间非平凡磁相,即所谓的“a”相。“A”相早先与竞争性反铁磁相、自旋玻璃相联系,某些间接测量表明,在该相中可能存在磁Skyrmion。我们用磁力显微镜对Co3Sn2S2单晶在不同温度、磁场和场角下的磁畴结构进行了成像。在低温下,我们观察到条纹畴,表明存在单轴各向异性。在130 K以上,磁畴壁变得可移动,并且当磁场沿c轴增加时,磁畴壁倾向于相对容易地对齐,而不是在a-b平面中。我们对场相关畴演化的详细研究表明,在T-c以下发生跃迁的反常相很可能受畴壁运动的控制。

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