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首页> 外文期刊>Journal of the Physical Society of Japan >Unusual Ferromagnetic-to-Antiferromagnetic-to-Ferromagnetic Transitions in Cu2+ (S=1/2) Cubic Spin Lattice of A-Site Ordered Perovskites
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Unusual Ferromagnetic-to-Antiferromagnetic-to-Ferromagnetic Transitions in Cu2+ (S=1/2) Cubic Spin Lattice of A-Site Ordered Perovskites

机译:A站点有序钙钛矿的Cu2 +(S = 1/2)立方自旋晶格中异常的铁磁到反铁磁到铁磁跃迁

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摘要

Very unusual transitions from ferromagnetic CaCu3Ge4O12 to antiferromagnetic CaCu3Ti4O12 to ferromagnetic CaCu3Sn4O12 are observed in solid solutions of the A-site ordered perovskites. The effective magnetic interaction between Cu2+ spins changes gradually and systematically from ferromagnetic to antiferromagnetic to ferromagnetic in the solid solution. At intermediate compositions the perfect balance of the competing interactions causes unusual instability. The ferromagnetic-to-antiferromagnetic switching is different from the known change by the bond angles mechanism of the superexchange interaction and has not been observed previously in any ferromagnetic-antiferromagnetic compounds. The present solid solutions provide a unique system where either ferromagnetism or antiferromagnetim arises within the simple A-site cubic S = 1/2 spin sublattice.
机译:在A-位有序钙钛矿的固溶体中观察到从铁磁性CaCu3Ge4O12到反铁磁性CaCu3Ti4O12到铁磁性CaCu3Sn4O12的非常不寻常的过渡。在固溶体中,Cu2 +自旋之间的有效磁相互作用从铁磁性逐渐反系统地改变为铁磁性。在中间成分中,竞争相互作用的完美平衡会导致异常的不稳定。通过超交换相互作用的键角机制,铁磁到反铁磁的切换不同于已知的变化,并且以前在任何铁磁-反铁磁化合物中都没有观察到。本发明的固体解决方案提供了独特的系统,其中在简单的A位置立方S = 1/2自旋亚晶格内产生铁磁性或反铁磁。

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