Giant spontaneous exchange bias obtained by tuning magnetic compensation in samarium ferrite single crystals

2018 ◽  
Vol 20 (5) ◽  
pp. 3687-3693 ◽  
Author(s):  
Xiao-xiong Wang ◽  
Shang Gao ◽  
Xu Yan ◽  
Qiang Li ◽  
Jun-cheng Zhang ◽  
...  

A giant spontaneous exchange bias of 1 T of samarium ferrite single crystals was obtained by tuning magnetic compensation by temperature.

2021 ◽  
Vol 104 (1) ◽  
Author(s):  
Bimalesh Giri ◽  
Bhawna Sahni ◽  
C. Salazar Mejía ◽  
S. Chattopadhyay ◽  
Uli Zeitler ◽  
...  

2019 ◽  
Vol 9 (1) ◽  
Author(s):  
D. C. Joshi ◽  
P. Nordblad ◽  
R. Mathieu

AbstractThe anisotropic antiferromagnet FeF2 has been extensively used as an antiferromagnetic layer to induce exchange bias effects in ferromagnetic/antiferromagnetic bilayers and heterostructures. In this work, an apparent exchange bias occurring in the low temperature hysteresis loops of FeF2 single crystals is investigated. A detailed investigation of the hysteresis and remnant magnetization indicates that the observation of an apparent exchange bias in FeF2 stems from an intrinsic excess moment associated with a distortion of the antiferromagnetic structure of piezomagnetic origin.


2009 ◽  
Vol 86 (4) ◽  
pp. 47003 ◽  
Author(s):  
P. D. Kulkarni ◽  
A. Thamizhavel ◽  
V. C. Rakhecha ◽  
A. K. Nigam ◽  
P. L. Paulose ◽  
...  

2021 ◽  
Vol 9 (1) ◽  
pp. 181-188
Author(s):  
Tyler Del Rose ◽  
Arjun K. Pathak ◽  
Yaroslav Mudryk ◽  
Vitalij K. Pecharsky

Inter-lanthanide interactions in a distinctly layered lattice lead to magnetic compensation, exchange bias, and magnetic memory effects.


2017 ◽  
Vol 111 (18) ◽  
pp. 182403 ◽  
Author(s):  
Chandan De ◽  
Ajaya K. Nayak ◽  
Michael Nicklas ◽  
A. Sundaresan

2020 ◽  
Vol 137 (3) ◽  
pp. 368-373
Author(s):  
Jing-Jing Wang ◽  
Wei Tang ◽  
Hai-Peng Xie ◽  
Ke Wang ◽  
Guang-Hua Guo

Author(s):  
Lucien F. Trueb

A new type of synthetic industrial diamond formed by an explosive shock process has been recently developed by the Du Pont Company. This material consists of a mixture of two basically different forms, as shown in Figure 1: relatively flat and compact aggregates of acicular crystallites, and single crystals in the form of irregular polyhedra with straight edges.Figure 2 is a high magnification micrograph typical for the fibrous aggregates; it shows that they are composed of bundles of crystallites 0.05-0.3 μ long and 0.02 μ. wide. The selected area diffraction diagram (insert in Figure 2) consists of a weak polycrystalline ring pattern and a strong texture pattern with arc reflections. The latter results from crystals having preferred orientation, which shows that in a given particle most fibrils have a similar orientation.


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