DocumentCode :
1047804
Title :
Anisotropy, magnetostriction, and In3+ion distribution in nickel ferrite indate crystals
Author :
Krishnan, Ramanathan ; Cagan, Vladimir
Author_Institution :
Centre National de la Recherche Scientifique, Bellevue, France
Volume :
7
Issue :
3
fYear :
1971
fDate :
9/1/1971 12:00:00 AM
Firstpage :
613
Lastpage :
616
Abstract :
Single crystals of the spinel system NiFe2-x Inx O4 have been prepared with 
and studied by ferrimagnetic resonance techniques in the 
band and in the temperature range 4.2 to 323°K. Magnetic moment variation with indicates that for 
, In3+enter the 
sites but for higher values of 
enter the 
sites. At 0°K, K1 variation with can be explained in terms of single ion energy only if the cubic field splitting parameter aB Fe3+in the site is supposed to increase with In3+. This has been attributed to the contraction of a site due to accommodating a large In3+in the site. The decrease in site Fe3+concentration is seen to increase both |λ 100| and |λ 111| at lower temperatures.
and studied by ferrimagnetic resonance techniques in the band and in the temperature range 4.2 to 323°K. Magnetic moment variation with indicates that for , In3+enter the sites but for higher values of enter the sites. At 0°K, K can be explained in terms of single ion energy only if the cubic field splitting parameter a site is supposed to increase with In3+. This has been attributed to the contraction of a site due to accommodating a large In3+in the site. The decrease in site Fe3+concentration is seen to increase both |λ 100| and |λ 111| at lower temperatures.Keywords :
Magnetic anisotropy; Magnetostriction; Nickel ferrite indate crystals; Anisotropic magnetoresistance; Crystals; Ferrimagnetic materials; Ferrites; Magnetic moments; Magnetic properties; Magnetic resonance; Magnetostriction; Nickel; Temperature distribution;
fLanguage :
English
Journal_Title :
Magnetics, IEEE Transactions on
Publisher :
ieee
ISSN :
0018-9464
Type :
jour
DOI :
10.1109/TMAG.1971.1067201
Filename :
1067201
Link To Document :
