Half-doped Pr 1-x Sr x CoO 3 (x=0.5) displays anomalous magnetism most notably manifest in the field-cooled magnetization versus temperature curves under different applied cooling fields.Recently, an explanation was advanced that a magnetocrystalline anisotropy transition driven by a structural transition at 120 K is the origin of this behavior. In this paper, we further elucidate the nature of the magnetic anisotropy across the low temperature phase transition in this material by means of transverse susceptibility (TS) measurements performed using a self-resonant tunnel diode oscillator. TS probes magnetic materials by means of a small radio frequency oriented transverse to a DC field which sweeps from positive to negative saturation. TS scans as a function of field clearly reveal peaks associated with the anisotropy (H K ) and switching fields (H S ). When peak position is examined as a function of temperature, around 120 K the signature of a ferromagnetic to ferromagnetic (FM-FM) phase transition is evident as a sharp feature in H K and a corresponding cusp in H S . A third TS peak (not previously observed in other classes of magnetic oxides such as manganites and spinel ferrites) is found to be correlated with the crossover field (H cr ) in the unconventional magnetization versus temperature (M(T)) behavior.
2We observe a strong temperature dependence of H cr around 120 K using this technique, which suggests the magnetic field-influenced magnetocrystalline anisotropy transition. We show the switching between the high-field magnetization state and the low-field magnetization state associated with the magnetocrystalline anisotropy transition is irreversible when the magnetic field is re-cycled. Finally, we demonstrate that the TS peak magnitude indicates easy axis switching associated with this phase transition, even in these polycrystalline samples. Our results further confirm that TS provides new insights into the magnetic behavior of complex oxides. 75.30.Gw, 75.47.Lx, 75.30.Cr
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