Abstract:
The resonant properties of gadolinium ferroborate GdFe$_3$(BO$_3$)$_4$ single crystals of varying quality are compared: nominally pure and those containing Bi$^{3+}$ ion impurities. The EDS method determined that the actual bismuth impurity content is close to the previously estimated 6% based on magnetic studies. The resonance properties confirm that both crystals form similar magnetic phase diagrams with an orientational transition between easy-axis and easy-plane antiferromagnetic ordering, which occurs either as a spontaneous transition at temperature $T_{SR}$ or as a transition to a magnetic field-induced easy-plane state at $T<T_{SR}$. Temperature dependencies of the effective magnetic anisotropy fields and the magnetoanisotropic contributions of the iron and gadolinium subsystems are calculated from the resonance data. It is concluded that the Bi$^{3+}$ ion impurity not only suppresses the contribution of the gadolinium subsystem, which these ions partially replace, but also causes a reduction in the contribution of the iron subsystem. As a result, the total change in the effective anisotropy field of the crystal is rather weak.
Keywords:magnetic anisotropy, resonance properties, magnetic phase diagrams, rare-earth ferroborates.