Chemistry and Physics of Materials Unit and International Centre for Materials Science, Jawaharlal Nehru Centre for Advanced Scientific Research, Jakkur PO, Bangalore, India.
J Phys Condens Matter. 2011 Nov 2;23(43):436001. doi: 10.1088/0953-8984/23/43/436001. Epub 2011 Oct 13.
The first-order spin-reorientation transition in the Mn-substituted yttrium orthoferrites, YFe(1-x)Mn(x)O(3) (x = 0.1, 0.15 and 0.2), has been investigated using (57)Fe Mössbauer spectroscopy. Owing to its large anisotropy, substitution of Mn(3+) ions in YFeO(3) induces a spin-reorientation transition from the low-temperature antiferromagnetic state to a high-temperature weak ferromagnetic state. With increasing x, the spin-reorientation transition temperature (T(SR)) increases whereas the Néel temperature (T(N)) decreases. Analysis of the Mössbauer spectra unambiguously confirms the occurrence of spin reorientation relative to crystal axes. At a given temperature, the mean hyperfine field decreases with the increasing Mn concentration. The variation of canting angle with temperature for YFe(0.85)Mn(0.15)O(3) has been estimated.
使用 (57)Fe Mössbauer 光谱研究了 Mn 取代的钇正铁氧体 YFe(1-x)Mn(x)O(3)(x = 0.1、0.15 和 0.2)中的一级自旋重定向转变。由于其各向异性较大,Mn(3+) 离子在 YFeO(3)中的取代导致低温反铁磁态向高温弱铁磁态的自旋重定向转变。随着 x 的增加,自旋重定向转变温度 (T(SR)) 增加,而奈尔温度 (T(N)) 降低。Mössbauer 光谱的分析明确证实了相对于晶体轴的自旋重定向的发生。在给定温度下,平均超精细场随 Mn 浓度的增加而减小。已估计 YFe(0.85)Mn(0.15)O(3)的倾斜角随温度的变化。