中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Mossbauer studies of baotite and bafertisite

文献类型:期刊论文

作者Shinno, I; Li, Z
刊名HYPERFINE INTERACTIONS
出版日期1998
卷号116期号:1-4页码:189-196
ISSN号0304-3843
文献子类Article
英文摘要The Mossbauer effect was used to study silicate minerals of baotite and bafertisite at 298 K and 95 K. Each spectrum of baotite at 298 K and 95 K consists of two doublets, and they are contributed from Fe2+ and Fe3+ in the octahedral Ti-sites, respectively. Each spectrum of bafertisite at 298 K and 95 K is composed of two doublets, and they are mainly caused by Fe2+ in the octahedral Fe(I)- and Fe(II)-sites, respectively. The average effective ionic radii of the Ti sites in baotite and the Fe(I)- and Fe(II)-sites in bafertisite were estimated based on the correlation of the isomer shifts with the average effective ionic radii in silicates, and they are 0.56 Angstrom, 0.73 Angstrom and 0.73 Angstrom, respectively.
WOS研究方向Physics
语种英语
WOS记录号WOS:000077312800018
出版者BALTZER SCI PUBL BV
源URL[http://ir.iggcas.ac.cn/handle/132A11/75120]  
专题中国科学院地质与地球物理研究所
通讯作者Shinno, I
作者单位1.Kyushu Univ, Grad Sch Social & Cultural Studies, Fukuoka 810, Japan
2.Chinese Acad Sci, Inst Geol, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Shinno, I,Li, Z. Mossbauer studies of baotite and bafertisite[J]. HYPERFINE INTERACTIONS,1998,116(1-4):189-196.
APA Shinno, I,&Li, Z.(1998).Mossbauer studies of baotite and bafertisite.HYPERFINE INTERACTIONS,116(1-4),189-196.
MLA Shinno, I,et al."Mossbauer studies of baotite and bafertisite".HYPERFINE INTERACTIONS 116.1-4(1998):189-196.

入库方式: OAI收割

来源:地质与地球物理研究所

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