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arXiv 0811.3084cond-mat.str-el
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高分辨同步辐射X射线和中子粉末衍射研究ZnCr $_2$ Se $_4$和ZnCr $_2$ S $_4$自旋驱动相变

Spin-driven Phase Transitions in ZnCr$_2$Se$_4$ and ZnCr$_2$S$_4$ Probed by High Resolution Synchrotron X-ray and Neutron Powder Diffraction

F. Yokaichiya, A. Krimmel, V. Tsurkan, I. Margiolaki, P. Thompson, H. N. Bordallo, A. Buchsteiner, N. Stüßer, D. N. Argyriou, A. Loidl

摘要:

用高分辨粉末同步辐射和中子衍射研究了尖晶石型化合物ZnCr $_2$ S $_4$和ZnCr $_2$ Se $_4$的晶体结构和磁性。ZnCr $_2$ Se $_4$在$T_N=21$ K处表现出一级相变,转变为无公度螺旋磁结构。$T_N$以上的磁波动耦合到晶格,表现为负热膨胀。复杂的磁结构和异常的结构行为都可能与磁挫挫有关。外加磁场的应用使有序化温度和负热膨胀状态向低温方向移动。因此,自旋排序变为锥形结构。ZnCr $_2$ S $_4$在$T_{N1}=15$ K和$T_{N2}=8$ K处表现出两个伴随着结构相变的磁转变。晶体结构在高温顺磁状态下从立方尖晶石型(空间群$Fd$ \={3} $m$)转变为$T_{N2} < T < T_{N1}$的四方畸变中间相(空间群$I4_1$ / $amd$),转变为$T < T_{N2}$的低温正交相(空间群$I m m a$)。硫离子通过交换伸缩的协同置换是这些结构相变的起源。ZnCr $_2$ S $_4$的低温结构与Verwey转变以下的磁铁矿的正交结构相同。当施加5 T的磁场时,该系统显示出在ZnCr $_2$ Se $_4$中观察到的中间磁相中的诱导负热膨胀。

英文摘要:

The crystal and magnetic structures of the spinel compounds ZnCr$_2$S$_4$ and ZnCr$_2$Se$_4$ were investigated by high resolution powder synchrotron and neutron diffraction. ZnCr$_2$Se$_4$ exhibits a first order phase transition at $T_N=21$ K into an incommensurate helical magnetic structure. Magnetic fluctuations above $T_N$ are coupled to the crystal lattice as manifested by negative thermal expansion. Both, the complex magnetic structure and the anomalous structural behavior can be related to magnetic frustration. Application of an external magnetic field shifts the ordering temperature and the regime of negative thermal expansion towards lower temperatures. Thereby, the spin ordering changes into a conical structure. ZnCr$_2$S$_4$ shows two magnetic transitions at $T_{N1}=15$ K and $T_{N2}=8$ K that are accompanied by structural phase transitions. The crystal structure transforms from the cubic spinel-type (space group $Fd$\={3}$m$) at high temperatures in the paramagnetic state, via a tetragonally distorted intermediate phase (space group $I4_1$ / $amd$) for $T_{N2} < T < T_{N1}$ into a low temperature orthorhombic phase (space group $I m m a$) for $T < T_{N2}$. The cooperative displacement of sulfur ions by exchange striction is the origin of these structural phase transitions. The low temperature structure of ZnCr$_2$S$_4$ is identical to the orthorhombic structure of magnetite below the Verwey transition. When applying a magnetic field of 5 T the system shows an induced negative thermal expansion in the intermediate magnetic phase as observed in ZnCr$_2$Se$_4$.

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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