MAGNETOCRYSTALLINE ANISOTROPY OF NON-UNIAXIAL R-T MAGNETIC-MATERIALS STUDIED BY THE SINGULAR POINT DETECTION TECHNIQUE - AN APPLICATION TO R(2)FE(17-X)GA(X) COMPOUNDS (R=Y OR GD AND X=0 OR 1)
Xc. Kou et al., MAGNETOCRYSTALLINE ANISOTROPY OF NON-UNIAXIAL R-T MAGNETIC-MATERIALS STUDIED BY THE SINGULAR POINT DETECTION TECHNIQUE - AN APPLICATION TO R(2)FE(17-X)GA(X) COMPOUNDS (R=Y OR GD AND X=0 OR 1), Journal of physics. Condensed matter, 8(10), 1996, pp. 1557-1565
The easy magnetization direction of R(2)Fe(17-x)Ga(x) lies within the
basal plane over all magnetic ordering temperatures. A spinning-sample
magnetic alignment technique was used to align the basal planes of fi
ne single crystallites of R(2)Fe(17-x)Ga(x) (R = Y or Gd and x = 0 or
1) to be parallel to each other. The degree of magnetic alignment was
checked by x-ray diffraction. The magnetocrystalline anisotropy field
of R(2)Fe(17-x)Ga(x) has been determined by a singularity appearing in
the curve of d(2)M/dt(2) versus H measured on a magnetically aligned
sample when an external field is applied perpendicular to aligned basa
l planes. The temperature dependence of the anisotropy fields was meas
ured from 4.2 K up to the corresponding Curie temperatures. It was fou
nd that the Curie temperatures of R(2)Fe(17) compounds with R = Y or G
d were enhanced upon partial substitution of Fe by Ga. However, the ma
gnetic anisotropy fields of Ga-containing compounds are smaller than t
hose of the corresponding pure R(2)Fe(17) compounds at low temperature
s.