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arXiv 1808.03362cond-mat.mtrl-sci
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FeTi2S4和Fe2TiS4中铁磁矩的阻塞和自旋密度波

Blocking of iron magnetic moments and Spin density wave in FeTi2S4 and Fe2TiS4

B. P. Embaid, O. M. Barrios, M. V. Bello

摘要:

用粉末X射线衍射Rietveld精修法和57 Fe穆斯堡尔谱变温研究了铁钛硫化物FeTi_2S_4和Fe_2 Ti_2S_4的结构和磁性。这两种硫化物具有相同的晶体相,基于单斜Cr 3S 4型结构,并且原子坐标不同; FeTi 2S 4保留了为Cr 3S 4相提出的理想原子位置,而在Fe 2 TiS 4中,金属从理想位置的位移是明显的。穆斯堡尔谱揭示了不同的磁行为;在FeTi_2S_4中,在Tc = 145 K时存在从顺磁有序到磁有序的转变,如果与先前报道的铁的磁矩值相比,基于由源自3d Ti原子的自旋密度波(SDW)阻挡Fe局域磁矩来解释该行为。在Fe_2 TiS_4中,在Tc = 290 K时发生顺磁性向(SDW)的转变,SDW在Fe和Ti金属中均通过[101]晶面扩展,并在TIC = 255 K时发生一级转变,即从无公度SDW(ISWD)向公度SDW(CSDW)转变。两种硫化物的磁行为与晶胞中原子的位置有关。

英文摘要:

Iron-titanium sulfides FeTi2S4 and Fe2TiS4 have been structurally and magnetically characterized using powder X Ray Diffraction with Rietveld refinement method and 57Fe Mössbauer spectroscopy at variable temperature. Both sulfides have the same crystallographic phase, based on the monoclinic Cr3S4 type structure and vary in atomic coordinates; FeTi2S4 retains the ideal atomic positions proposed for the Cr3S4 phase, while in Fe2TiS4 the metal displacements from ideal sites are noticeable. Mössbauer spectra reveal different magnetic behaviors; in FeTi2S4 there is a transition from paramagnetic to magnetic ordering at temperature Tc = 145 K, giving rise to unusually low hyperfine magnetic field of 2.5 T (at 77 K) if compared with values of iron magnetic moments reported previously, this behavior is explained on the basis of blocking Fe localized magnetic moments by the Spin density wave (SDW) originated from 3d Ti atoms. In Fe2TiS4 a transition from paramagnetic to (SDW) arises at Tc = 290 K, the SDW is spread in both Fe and Ti metals through [101] crystallographic plane and undergoes a transition of first order from Incommensurate SDW (ISWD) to Commensurate SDW (CSDW) at TIC = 255 K. The atomic positions in the unit cell are correlated to the magnetic behavior in both sulfides.

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