Abstract
Paramagnetic susceptibilities, χi(i=a,b,c) of single crystals of rare-earth orthoferrites RFeO3 (R=Nd, Sm, Gd, Dy, Er, Yb and Y) were measured along the a, b and c axes at room temperature and 77 K. The main parts of the effective magnetic moments μeff,i’s were found to originate from rare-earth ions. All rare-earth ions except Dy3+ and Er3+ showed rather isotropic effective magnetic moments, which are nearly equal to those of the free ions. Er3+ and especially Dy3+ ions showed large anisotropy and the anisotropy increases with decreasing temperature. For Dy3+ μeff,b>μeff,a>μeff,c and for Er3+ μeff,c>μeff,a>μeff,b. The values of μeff,i for Dy3+ and Er3+ were obtained by using reported g-factors derived from optical experiments and the observed large anisotropy was found to result from the anisotropy of g-factor of the ground state.