The dependence of magnetotransport behaviors on A-site disorder induced by A-site cational size mismatch in ferromagnetic manganites is investigated by characterizing a series of samples with the same A-site cational mean radius ⟨rA⟩=1.200.3em0ex but different A-site ionic radii variance σ²=∑ᵢxᵢrᵢ²-⟨rA⟩², where xᵢ and rᵢ are the atomic fraction and ionic radii of i-type ions at A-site, respectively. It is revealed that the ground state transits from ferromagnetic metal to cluster-glass insulator upon increasing the variance σ² from 0.0003 for La0.55Ca0.45MnO₃ to 0.015 for Sm0.55(Ca0.6Ba0.4)0.45MnO₃, while the crystallographic structure and lattice constants of these manganites remain unchanged. Nevertheless, the increasing A-site disorder is believed to enhance the random local radial distortion of MnO₆ octahedra and suppress the ferromagnetic long-range order. In the manganites of high A-site disorder, the long-range ferromagnetic ordering is completely melted into the short-range magnetically ordered clusters and then the stepwise magnetization. With decreasing temperature, the short-range ordered clusters become frustrated at the frustrating point, below which a cluster-glass transition occurs due to the weak intercluster interaction.
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Wang et al. (2006) studied this question.
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