These changes can be explained in terms of the decrease in average diameter of rare-earth ions and the model of spin clusters.
这些变化可以用稀土离子平均直径的减小和自旋团簇模型来解释。
Therefore, it is concluded that the phase-separated state in cobaltites consist of FM clusters and non-FM matrix, and spin glass-like regions.
因此体系自发地相分离为铁磁团簇、非磁基底和自旋玻璃相。
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