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Ag-In- 稀土 1/1 准晶的磁性。

Magnetic properties of the Ag-In-rare-earth 1/1 approximants.

机构信息

Institute of Solid State Physics, University of Tokyo, 106-1 Shirakata, Tokai, Ibaraki 319-1106, Japan.

出版信息

J Phys Condens Matter. 2011 Feb 9;23(5):056001. doi: 10.1088/0953-8984/23/5/056001. Epub 2011 Jan 13.

Abstract

We have performed magnetic susceptibility and neutron scattering measurements on polycrystalline Ag-In-RE (RE, rare-earth) 1/1 approximants. In the magnetic susceptibility measurements, for most of the RE elements, inverse susceptibility shows linear behaviour in a wide temperature range, confirming well localized isotropic moments for the RE(3 + ) ions. Exceptionally for the light RE elements, such as Ce and Pr, nonlinear behaviour was observed, possibly due to significant crystalline field splitting or valence fluctuation. For RE = Tb, the susceptibility measurement clearly shows a bifurcation of the field-cooled and zero-field-cooled susceptibility at T(f) = 3.7 K, suggesting a spin-glass-like freezing. On the other hand, neutron scattering measurements detect significant development of short-range antiferromagnetic spin correlations in the elastic channel, which is accompanied by a broad peak at [Formula: see text] meV in the inelastic scattering spectrum. These features have striking similarity to those in the Zn-Mg-Tb quasicrystals, suggesting that the short-range spin freezing behaviour is due to local high-symmetry clusters commonly seen in both systems.

摘要

我们对多晶 Ag-In-RE(RE,稀土元素)1/1 近晶相进行了磁化率和中子散射测量。在磁化率测量中,对于大多数 RE 元素,在很宽的温度范围内,反磁化率呈线性行为,这证实了 RE(3+) 离子的局域各向同性磁矩。对于轻稀土元素,如 Ce 和 Pr,观察到了异常的非线性行为,这可能是由于晶场劈裂或价态波动较大。对于 RE=Tb,磁化率测量清楚地表明在 T(f)=3.7 K 时,磁场冷却和零场冷却磁化率发生分叉,表明存在自旋玻璃状冻结。另一方面,中子散射测量在弹性通道中探测到短程反铁磁自旋关联的显著发展,这伴随着在非弹性散射谱中在 [Formula: see text] meV 处出现宽峰。这些特征与 Zn-Mg-Tb 准晶中的特征非常相似,表明短程自旋冻结行为是由于在这两个系统中都常见的局部高对称簇引起的。

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