Magneto-crystalline anisotropy of NdFe0.9Mn0.1O3 single crystal

2018 ◽  
Vol 536 ◽  
pp. 89-92 ◽  
Author(s):  
Marián Mihalik ◽  
Matúš Mihalik ◽  
Mária Zentková ◽  
Klára Uhlířová ◽  
Marie Kratochvílová ◽  
...  
1960 ◽  
Vol 13 (2) ◽  
pp. 196 ◽  
Author(s):  
FD Stacey

It is well known that in most rocks the ferromagnetic fraction occurs as small grains dispersed in a solid, magnetically inert matrix. Recently the magnetic anisotropy of rocks and of chondritic meteorites has been subjected to detailed study by the torque-meter method, and, in an attempt to obtain a physical understanding of the shape and crystal alignments of grains which cause magnetic anisotropy in these natural bodies, a number of artificial specimens have been prepared. Iron, nickel, and magnetite powders were mixed into solidifying media and allowed to set in a cylindrical mould in a 10 kilo-oersted field. The torque curves of the resulting specimens reveal a surprising result. It appears that single crystal magnetic grains tend to string together along lines of forc~, thus producing strongly anisotropic specimens, only when the first magneto crystalline anisotropy constant of the ferromagnetic material is positive.


1985 ◽  
Vol 52 (1-4) ◽  
pp. 434-436 ◽  
Author(s):  
Y. Isikawa ◽  
K. Mori ◽  
K. Ueno ◽  
K. Sato ◽  
K. Maezawa

2013 ◽  
Vol 818 ◽  
pp. 72-76 ◽  
Author(s):  
Gang Su

The crystalline electric field parameters Anmfor HoFe11Ti under different pressures were evaluated by fitting calculations to the magnetization curves measured on the single crystals at several temperatures. It was found that magneto-crystalline anisotropy has been changed by high pressure and the Anmfor HoFe11Ti under high pressures are strikingly different from Anmfor the corresponding HoFe11Ti H with interstitial hydrogen atom.


Physica B+C ◽  
1977 ◽  
Vol 86-88 ◽  
pp. 299-300
Author(s):  
O. Yamada ◽  
F. Ono ◽  
K. Mitsuoka

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