Interplay of Fe and Tm moments through the spin-reorientation transition in TmFeO3

被引:16
|
作者
Staub, U. [1 ]
Rettig, L. [1 ,5 ]
Bothschafter, E. M. [1 ]
Windsor, Y. W. [1 ,5 ]
Ramakrishnan, M. [1 ]
Avula, S. R. V. [1 ]
Dreiser, J. [1 ]
Piamonteze, C. [1 ]
Scagnoli, V. [2 ,3 ]
Mukherjee, S. [4 ]
Niedermayer, C. [4 ]
Medarde, M. [3 ]
Pomjakushina, E. [3 ]
机构
[1] Paul Scherrer Inst, Swiss Light Source, CH-5232 Villigen, Switzerland
[2] ETH, Dept Mat, Lab Mesoscop Syst, CH-8093 Zurich, Switzerland
[3] Paul Scherrer Inst, Lab Multiscale Mat Expt, CH-5232 Villigen, Switzerland
[4] Paul Scherrer Inst, Lab Neutron Scattering & Imaging, CH-5232 Villigen, Switzerland
[5] Fritz Haber Inst Max Planck Soc, Dept Phys Chem, Faradayweg 4-6, D-14915 Berlin, Germany
基金
瑞士国家科学基金会;
关键词
DIFFRACTION; DICHROISM;
D O I
10.1103/PhysRevB.96.174408
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
X-ray magnetic circular dichroism (XMCD) and x-ray magnetic linear dichroism (XMLD) have been used to investigate the Fe magnetic response during the spin-reorientation transition (SRT) in TmFeO3. Comparing the Fe XMLD results with neutron-diffraction and magnetization measurements on the same sample indicates that the SRT has an enhanced temperature range in the near surface region of approximately 82 to 120 K compared to approximately 82 to 92 K in bulk. This view is supported by complementary resonant soft x-ray-diffraction experiments at the Tm M-5 edge. These measurements find an induced magnetic moment on the Tm sites, which is well described by a dipolar mean-field model originating from the Fe moments. Even though such a model can describe the 4f response in the experiments, it is insufficient to describe the SRT even when considering a change in the 4f anisotropy. Moreover, the results of the Fe XMCD show a different temperature evolution through the SRT, the interpretation of which is hampered by additional spectral shape changes of the XCMD signal.
引用
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页数:11
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