A study of the magnetic anisotropy of single-crystal YFe11Ti and of it
s hydride is reported. The measurements were performed on a vibrating-
sample and a torsion magnetometer on field-oriented single-crystal and
powder samples. The temperature dependence of the magnetic anisotropy
constants K-1 and K-2 was determined by a mathematical treatment of e
xperimental torque curves and by applying the Sucksmith-Thompson techn
ique to magnetization data. It is shown that the temperature dependenc
e of the magnetic anisotropy constants of YFe11Ti and of its hydride d
oes not follow the prediction of the single-ion exchange model. It is
found that hydrogenenation results in a growth of the magnetic anisotr
opy constant, which can be explained by an electron-density redistribu
tion near the lattice positions occupied by iron atoms. (C) 1998 Ameri
can Institute of Physics.