Abstract
The magnetization curve of the ferrimagnetic alternating spin chain with the single-ion anisotropy is investigated with the numerical exact diagonalization of finite clusters and size-scaling analyses. The system has a plateau at 1/3 of the saturation moment, which corresponds to the spontaneous magnetization for D=0. Varying in the 1/3-magnetized ground state under the external field along the axis of , a quantum phase transition is revealed to occur at the critical value where the plateau vanishes. Except for the critical point, the plateau is always opening, but the mechanism is different between and . The change of mechanisms is an evidence to clarify that the plateau originates from the quantization of magnetization.
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