A Mossbauer effect study of Fe3+ bearing γ-Fe2SiO4

被引:5
作者
Li, Z [1 ]
Shinno, I
Ye, DN
Fu, PQ
Zhang, YM
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
[2] Grad Sch Social & Cultural Studies, Fukuoka 810, Japan
[3] Acad Sinica, Inst Geochem, Guiyang 550002, Peoples R China
来源
SCIENCE IN CHINA SERIES D-EARTH SCIENCES | 2001年 / 44卷 / 01期
基金
日本学术振兴会; 中国国家自然科学基金;
关键词
Fe3+ bearing iron silicate spinel; Mossbauer effect; bond lengths; cell parameters; oxygen parameters; next nearest neighbor effects;
D O I
10.1007/BF02906883
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Three synthetic Fe3+ bearing gamma -Fe2SiO4 were analyzed using electron probe method, and the Mossbauer spectra of the samples at 298 K, 150 K, and 95 K were measured. Each spectrum at three temperatures is composed of two doublets. These two doublets are assigned to Fe2+ in the octahedral sites and Fe3+ in the tetrahedral sites, respectively. Site occupancies were determined. The results show that Fe3+ and a small amount of Si4+ are in the tetrahedral and octahedral sites, respectively. The average bond lengths of the octahedral and tetrahedral sites were calculated according to the equations primarily given by Hill et al., O'Neill and Navrotsky and modified by the authors. Furthermore, the octahedral and tetrahedral bond lengths were used to calculate cell parameters and oxygen parameters. In addition, Fe3+ line broadening in the Mossbauer spectra of Fe3+ bearing gamma -Fe2SiO4 were interpreted by using the next nearest neighbor effects.
引用
收藏
页码:34 / 46
页数:13
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