Ginga Kitahara, A. Yoshiasa, M. Tokuda, T. Tobase, K. Sugiyama
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In Ce – and Nb – perovskites, the total charges at the A – and B – sites achieved near – ideal divalent and tetravalent states such as Ca 2+ Ti 4+ O 3 , respectively, due to complex elemental substitutions. Local distortions around Ti in the perovskite solid solutions were greater, and the pre – edge features of the Ti atoms in Ce – and Nb – perovskites were di ff erent from those in pure CaTiO 3 . The valence states and local structures of Fe in Ce – and Nb – perovskites were signi fi cantly di ff erent. The existence of divalent Fe 2+ at the B – site in Ce – perovskite was con fi rmed. It is presumed that the displacement ellipsoids of all atoms and local irregularities in Ce – perovskite increase owing to the radiative decay of the actinoid element Th. We recon fi rmed that the composition and three – dimensional structure of perovskite – type structures were fl exible and caused various electrical, structural changes.","PeriodicalId":51093,"journal":{"name":"Journal of Mineralogical and Petrological Sciences","volume":"1 1","pages":""},"PeriodicalIF":0.9000,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"XANES analyses on minor elements and X–ray single crystal structure analyses of Ce– and Nb–perovskite\",\"authors\":\"Ginga Kitahara, A. Yoshiasa, M. Tokuda, T. Tobase, K. Sugiyama\",\"doi\":\"10.2465/JMPS.200424\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Structural analysis of Ce – and Nb – perovskites containing Fe, Zr, Nb, and rare earth elements (REEs) in CaTiO 3 perovskite was performed using single – crystal X – ray di ff raction and X – ray absorption near – edge structure (XANES) analyses. Based on chemical analysis results, XANES measurements and the site – occupation of elements at A – and B – sites showed the chemical formula: (Ca 2+0.817 REE 3+0.087 Na +0.081 Sr 2+0.005 Th 4+0.003 ) 1.998+0.993 (Ti 4+0.941 Nb 5+0.017 Fe 3+0.013 V 5+0.010 Fe 2+0.007 Sc 3+0.006 Zn 2+0.005 Al 3+0.002 Ge 4+0.001 W 6+0.001 ) 3.996+1.003 O 3 for Ce – perovskite and (Ca 2+0.937 Ce 3+0.021 Na +0.020 La 3+0.015 Sr 2+0.003 ) 2.008+0.996 (Ti 4+0.730 Nb 5+0.122 Fe 3+0.108 Al 3+0.020 Zr 4+0.009 V 5+0.008 ) 3.990+0.997 O 3 for Nb – perovskite. In Ce – and Nb – perovskites, the total charges at the A – and B – sites achieved near – ideal divalent and tetravalent states such as Ca 2+ Ti 4+ O 3 , respectively, due to complex elemental substitutions. Local distortions around Ti in the perovskite solid solutions were greater, and the pre – edge features of the Ti atoms in Ce – and Nb – perovskites were di ff erent from those in pure CaTiO 3 . The valence states and local structures of Fe in Ce – and Nb – perovskites were signi fi cantly di ff erent. The existence of divalent Fe 2+ at the B – site in Ce – perovskite was con fi rmed. It is presumed that the displacement ellipsoids of all atoms and local irregularities in Ce – perovskite increase owing to the radiative decay of the actinoid element Th. 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引用次数: 1
摘要
采用单晶X射线衍射和X射线吸收近边结构(XANES)分析方法对ctio3钙钛矿中含有Fe、Zr、Nb和稀土元素(REEs)的Ce和Nb钙钛矿进行了结构分析。根据化学分析结果,XANES测量和元素在A -和B -位点的位置占用显示了化学式:(Ca 2+0.817 REE 3+0.087 Na +0.081 Sr 2+0.005 Th 4+0.003) 1.998+0.993 (Ti 4+0.941 Nb 5+0.017 Fe 3+0.013 V 5+0.010 Fe 2+0.007 Sc 3+0.006 Zn 2+0.005 Al 3+0.002 Ge 4+0.001 W 6+0.001) 3.996+1.003 O 3 (Ca 2+0.937 Ce 3+0.021 Na +0.020 La 3+0.015 Sr 2+0.003) 2.008+0.996 (Ti 4+0.730 Nb 5+0.122 Fe 3+0.108 Al 3+0.020 Zr 4+0.009 V 5+0.008) 3.990+0.997 O 3 (Nb -钙钛矿)在Ce -和Nb -钙钛矿中,由于复杂的元素取代,A位和B位的总电荷分别达到接近理想的二价和四价状态,如ca2 + ti4 + o3。钙钛矿固溶体中Ti周围的局部畸变较大,且Ce -和Nb -钙钛矿中Ti原子的前边缘特征与纯catio3中Ti原子的前边缘特征不同。Fe在Ce -和Nb -钙钛矿中的价态和局部结构有显著差异。证实了钙钛矿中B位存在二价fe2 +。推测Ce -钙钛矿中所有原子的位移椭球体和局部不规则性的增加是由于锕系元素Th的辐射衰变。我们发现钙钛矿型结构的组成和三维结构是柔性的,可以引起各种电学和结构的变化。
XANES analyses on minor elements and X–ray single crystal structure analyses of Ce– and Nb–perovskite
Structural analysis of Ce – and Nb – perovskites containing Fe, Zr, Nb, and rare earth elements (REEs) in CaTiO 3 perovskite was performed using single – crystal X – ray di ff raction and X – ray absorption near – edge structure (XANES) analyses. Based on chemical analysis results, XANES measurements and the site – occupation of elements at A – and B – sites showed the chemical formula: (Ca 2+0.817 REE 3+0.087 Na +0.081 Sr 2+0.005 Th 4+0.003 ) 1.998+0.993 (Ti 4+0.941 Nb 5+0.017 Fe 3+0.013 V 5+0.010 Fe 2+0.007 Sc 3+0.006 Zn 2+0.005 Al 3+0.002 Ge 4+0.001 W 6+0.001 ) 3.996+1.003 O 3 for Ce – perovskite and (Ca 2+0.937 Ce 3+0.021 Na +0.020 La 3+0.015 Sr 2+0.003 ) 2.008+0.996 (Ti 4+0.730 Nb 5+0.122 Fe 3+0.108 Al 3+0.020 Zr 4+0.009 V 5+0.008 ) 3.990+0.997 O 3 for Nb – perovskite. In Ce – and Nb – perovskites, the total charges at the A – and B – sites achieved near – ideal divalent and tetravalent states such as Ca 2+ Ti 4+ O 3 , respectively, due to complex elemental substitutions. Local distortions around Ti in the perovskite solid solutions were greater, and the pre – edge features of the Ti atoms in Ce – and Nb – perovskites were di ff erent from those in pure CaTiO 3 . The valence states and local structures of Fe in Ce – and Nb – perovskites were signi fi cantly di ff erent. The existence of divalent Fe 2+ at the B – site in Ce – perovskite was con fi rmed. It is presumed that the displacement ellipsoids of all atoms and local irregularities in Ce – perovskite increase owing to the radiative decay of the actinoid element Th. We recon fi rmed that the composition and three – dimensional structure of perovskite – type structures were fl exible and caused various electrical, structural changes.
期刊介绍:
The Journal of Mineralogical and Petrological Sciences (JMPS) publishes original articles, reviews and letters in the fields of mineralogy, petrology, economic geology, geochemistry, planetary materials science, and related scientific fields. As an international journal, we aim to provide worldwide diffusion for the results of research in Japan, as well as to serve as a medium with high impact factor for the global scientific communication
Given the remarkable rate at which publications have been expanding to include several fields, including planetary and earth sciences, materials science, and instrumental analysis technology, the journal aims to encourage and develop a variety of such new interdisciplinary scientific fields, to encourage the wide scope of such new fields to bloom in the future, and to contribute to the rapidly growing international scientific community.
To cope with this emerging scientific environment, in April 2000 the journal''s two parent societies, MSJ* (The Mineralogical Society of Japan) and JAMPEG* (The Japanese Association of Mineralogists, Petrologists and Economic Geologists), combined their respective journals (the Mineralogical Journal and the Journal of Mineralogy, Petrology and Economic Geology). The result of this merger was the Journal of Mineralogical and Petrological Sciences, which has a greatly expanded and enriched scope compared to its predecessors.