首页> 外文期刊>The European physical journal, B. Condensed matter physics >Pressure induced antiferromagnet-ferromagnet transition in La_(0.5)Ba_(0.5)CoO_(2.8) cobaltite
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Pressure induced antiferromagnet-ferromagnet transition in La_(0.5)Ba_(0.5)CoO_(2.8) cobaltite

机译:La_(0.5)Ba_(0.5)CoO_(2.8)钴矿中压力诱导的反铁磁体-铁磁体转变

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摘要

The anion deficient cobaltite La_(0.5)Ba_(0.5)CoO_(2.8) with the formal cobalt valence state close to 3+ has been studied as function of pressure up to 6.5 GPa at different temperatures by neutron powder diffraction. At ambient pressure the crystal structure of this compound has cubic symmetry (space group Pm3m) and is found to become antiferromagnetic with TN close to 250 K. Applied pressure induces a gradual transition from the antiferromagnetic into a ferromagnetic state through a mixed magnetic state. The transition is not accompanied by obvious changes in the macroscopic crystal symmetry. It is suggested that the magnetic ground state strongly depends on the unit cell volume and that the transition is associated with a spin state crossover of the cobalt ions whereas the formal Co~(3+)/Co~(4+) ratio is less important than expected following the double exchange scenario for the appearance of ferromagnetism.
机译:通过中子粉末衍射研究了在不同温度下高达6.5 GPa的压力下,具有贫钴形式的价态接近3+的贫阴离子钴La_(0.5)Ba_(0.5)CoO_(2.8)。在环境压力下,该化合物的晶体结构具有立方对称性(空间群Pm3m),并且在TN接近250 K时会变成反铁磁性。施加的压力会导致其从反铁磁性逐渐过渡为混合磁性,从而转变为铁磁性。该转变不伴随宏观晶体对称性的明显变化。建议磁基态强烈依赖于晶胞体积,过渡与钴离子的自旋态交叉相关,而正式的Co〜(3 +)/ Co〜(4+)比不那么重要在出现铁磁性双重交换情况之后,超出了预期。

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