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Neutron Laue diffraction study of the complex low-temperature magnetic behaviour of brownmillerite-type Ca2Fe2O5.

机译:中子Laue衍射研究褐铁矿型Ca2Fe2O5的复杂低温磁行为。

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 10 K under zero-field and low-magnetic field (35 Oe = 35 × 103/4[pi] A m-1) conditions. Ca2Fe2O5 is a canted G-type antiferromagnet with Pcm'n' 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 = 10 K, despite a previous suggestion that an anomalous magnetic susceptibility enhancement observed in Ca2Fe2O5 single crystals between 40 and 140 K might signify a reorientation of the antiferromagnetic easy axis from c to a below 40 K. 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. © International Union of Crystallography
机译:相对于在零场和低磁场(35 Oe = 35×103 /4πA m)下在300、100和10 K下收集的单晶中子Laue衍射数据,已经细化了棕褐色Ca2Fe2O5的原子和磁性结构。 -1)条件。 Ca2Fe2O5是具有Pcm'n'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 K和140 K之间的Ca2Fe2O5单晶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a,但该磁性结构一直持续到T = 10K。低于40K。针对此磁化率异常的替代解释是根据异常体制中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。 ©国际晶体学联盟

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