首页> 外文期刊>Journal of Applied Crystallography >Neutron Laue diffraction study of the complex low-temperature magnetic behaviour of brownmillerite-type Ca2Fe2O5
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Neutron Laue diffraction study of the complex low-temperature magnetic behaviour of brownmillerite-type Ca2Fe2O5

机译:中性Laue衍射研究褐铁矿型Ca2Fe2O5的复杂低温磁行为

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摘要

The atomic and magnetic structure of brownmillerite Ca2Fe2O5 has been refined against single-crystal neutron Laue diffraction data collected at 300, 100 and 10K under zero-field and low-magnetic field (35 Oe = 35 x 10(3)/4Am(-1)) conditions. Ca2Fe2O5 is a canted G-type antiferromagnet with Pcmn symmetry, the magnetic moments on Fe being directed approximately along the crystallographic c axis at room temperature. The refinement results show clearly that this magnetic structure persists down to T = 10K, despite a previous suggestion that an anomalous magnetic susceptibility enhancement observed in Ca2Fe2O5 single crystals between 40 and 140K might signify a reorientation of the antiferromagnetic easy axis from c to a below 40K. Alternative explanations for this susceptibility anomaly are considered in terms of the evidence for partial or short-range loss of order in the anomalous regime, possibly due to the presence of multiple competing sublattice interactions.
机译:针对零场和低磁场(35 Oe = 35 x 10(3)/ 4Am(-1)下在300、100和10K收集的单晶中子Laue衍射数据,已经细化了棕褐色Ca2Fe2O5的原子和磁性结构。 )) 条件。 Ca2Fe2O5是具有Pcmn对称性的倾斜G型反铁磁体,在室温下,Fe上的磁矩大致沿晶体c轴定向。精炼结果清楚地表明,尽管先前曾暗示在40至140K之间的Ca2Fe2O5单晶体中观察到异常的磁化率增强可能表明反铁磁易轴从c重新定向到了低于40K,但这种磁性结构一直持续到T = 10K。 。对于这种敏感性异常的替代解释,是根据异常情况下部分或短期失序的证据来考虑的,这可能是由于存在多个竞争性亚晶格相互作用所致。

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