Publikationsrepositorium - Helmholtz-Zentrum Dresden-Rossendorf

Magnetization of a Ho₂Fe₁₄Si₃ single crystal was measured in a steady magnetic field of up to 9 T and in pulsed fields of up to 60 T applied along the principal axes. Ho₂Fe₁₄Si₃ is a ferrimagnet below T_C = 480 K, has a spontaneous magnetic moment of about 8 µ_B/f.u. (at T = 4.2 K) and exhibits a large easy-plane magnetic anisotropy. There is also a certain anisotropy within the basal plane, the b axis [120] being the easy-magnetization direction. In fields applied along the a and b axes field-induced first-order phase transitions are observed at 29 T and at 22 T, respectively. Along the easy axis b we observe also an S-shaped anomaly at about 47 T, which does not correspond to a phase transition. A simple model predicts that the two observed first-order transitions are the only ones taking place in Ho₂Fe₁₄Si₃; the magnetization should subsequently grow continuously and arrive at saturation at ~100 T. This is in stark contrast to the behavior of the parent compound Ho₂Fe₁₇, where as many as three sequential first-order transitions are expected for H‖b. The reason for the disparity is that the basal-plane anisotropy constant K_Ho is at least one order of magnitude smaller in Ho₂Fe₁₄Si₃ than it is in Ho₂Fe₁₇.