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三元HoNiSi和HoNiGe化合物的晶体结构与磁结构:以ZrNiP原型结晶的金属间化合物实例

Crystal and Magnetic Structures of the Ternary HoNiSi and HoNiGe Compounds: An Example of Intermetallics Crystallizing with the ZrNiP Prototype.

作者信息

Provino Alessia, Ritter Clemens, Smetana Volodymyr, Mudring Anja-Verena, Pani Marcella, Pecharsky Vitalij K, Manfrinetti Pietro

机构信息

Department of Chemistry, University of Genova, 16146 Genova, Italy.

The Ames Laboratory, U.S. Department of Energy, Iowa State University, Ames, Iowa 50011-3020, United States.

出版信息

Inorg Chem. 2021 Nov 1;60(21):16397-16408. doi: 10.1021/acs.inorgchem.1c02211. Epub 2021 Oct 15.

Abstract

We report two new rare-earth (R) ternary intermetallic compounds-HoNiT with T = Si and Ge-that correspond to the RNiT phase earlier reported to form in Dy-Ni-T and Ho-Ni-T ternary systems. The compounds crystallize in a filled version of the orthorhombic ZrNiP-type structure with = 0.52; their stoichiometry, determined from both single-crystal and powder X-ray diffraction data, is centered on HoNiT with a narrow solid solubility range for the silicide, while the germanide appears to be a line phase. In addition to R = Dy and Ho, RNiT compounds also form for R = Y and Tb, representing the first examples of rare-earth-based compounds adopting the ZrNiP structural prototype. Bulk magnetization data reveal the main transitions of the ferrimagnetic or ferromagnetic type at = 38 K for HoNiSi and = 37 K for HoNiGe, which are followed by subsequent magnetic reordering at lower temperatures. Neutron diffraction shows complex magnetic structures below with both ferromagnetic and antiferromagnetic components and magnetic propagation vector κ = [0, 0, 0]. Below ≅ 24 K (22 K) for the silicide (germanide), an additional antiferromagnetic coupling following an incommensurate magnetic propagation vector κ = [κ, 0, 0] appears to coexist with the first magnetic structure.

摘要

我们报道了两种新的稀土(R)三元金属间化合物——HoNiT(其中T = Si和Ge),它们与之前报道在Dy-Ni-T和Ho-Ni-T三元体系中形成的RNiT相相对应。这些化合物结晶为正交ZrNiP型结构的填充版本,其占有率 = 0.52;根据单晶和粉末X射线衍射数据确定,它们的化学计量以HoNiT为中心,硅化物的固溶度范围较窄,而锗化物似乎是一个线性相。除了R = Dy和Ho之外,R = Y和Tb时也会形成RNiT化合物,这是采用ZrNiP结构原型的稀土基化合物的首个实例。体磁化数据显示,HoNiSi在 = 38 K时以及HoNiGe在 = 37 K时发生亚铁磁性或铁磁性类型的主要转变,随后在较低温度下发生后续磁重排。中子衍射表明,低于 时存在复杂的磁性结构,同时包含铁磁和反铁磁分量,磁传播矢量κ = [0,

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/af99/8564752/84a0c404ff3d/ic1c02211_0001.jpg

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