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通过中子对分布函数识别LaBaMnO和BaYFeO中的局部结构单元。

Identifying the local structural units in LaBaMnO and BaYFeO through the neutron pair distribution function.

作者信息

King Graham, Thompson Corey M, Luo Kun, Greedan John E, Hayward Michael A

机构信息

Materials Science and Technology Division, Los Alamos National Laboratory, Los Alamos, NM 87545, USA.

Department of Chemistry, Purdue University, 560 Oval Drive, West Lafayette, IN 47907, USA and Department of Chemistry and Brockhouse Institute of Materials Research, McMaster University, Hamilton, ON L8S 4M1, Canada.

出版信息

Dalton Trans. 2017 Jan 24;46(4):1145-1152. doi: 10.1039/c6dt04291k.

Abstract

Neutron pair distribution function data are used to investigate the local structures of two oxygen deficient perovskites with simple cubic crystal structures. LaBaMnO is found to have alternating layers of MnO octahedra and MnO tetrahedra, making it similar to other members of the LaBaMnO series with smaller x values which have brownmillerite crystal structures. Our fitting results suggest that LaBaMnO is not locally similar to any one brownmillerite structure type but instead has a variety of intra-layer and inter-layer relationships. We propose that this could be due to short range segregation of the much differently sized La and Ba cations, which creates significantly different inter-layer distances. BaYFeO is found not to have a brownmillerite-type local structure but rather seems to consist of structural units which are similar to BaYFeO, an earlier member of the BaYFeO series. The PDF analysis shows that there are never neighboring Y atoms and that the O vacancies lie exclusively between Fe atoms, such that Y is always octahedrally coordinated. The PDF also suggests that there are more tetrahedral Fe than expected, which could be due to the presence of terminal O atoms in Fe centered dimeric units, similar to what is found in BaYFeO.

摘要

中子对分布函数数据用于研究两种具有简单立方晶体结构的缺氧钙钛矿的局部结构。发现LaBaMnO具有MnO八面体和MnO四面体的交替层,这使其与具有较小x值且具有褐锰矿晶体结构的LaBaMnO系列的其他成员相似。我们的拟合结果表明,LaBaMnO在局部上与任何一种褐锰矿结构类型都不相似,而是具有多种层内和层间关系。我们认为这可能是由于尺寸差异很大的La和Ba阳离子的短程偏析,这产生了明显不同的层间距离。发现BaYFeO没有褐锰矿型局部结构,而是似乎由与BaYFeO系列的早期成员BaYFeO相似的结构单元组成。PDF分析表明,从未有相邻的Y原子,且O空位仅位于Fe原子之间,则Y始终为八面体配位。PDF还表明,四面体Fe比预期的更多,这可能是由于以Fe为中心的二聚体单元中存在末端O原子,类似于在BaYFeO中发现的情况。

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