氧烷
氧化态
三角双锥分子几何
谱线
结晶学
协调数
化学
K-边
材料科学
晶体结构
金属
物理
离子
天文
有机化学
作者
Max Wilke,François Farges,P. Petit,Gordon E. Brown,François Martin
出处
期刊:American Mineralogist
[Mineralogical Society of America]
日期:2001-05-01
卷期号:86 (5-6): 714-730
被引量:976
标识
DOI:10.2138/am-2001-5-612
摘要
High-resolution Fe K-edge XANES spectra of a series of crystalline Fe2+- and Fe3+-bearing model compounds were measured in an effort to correlate characteristics of the pre-edge feature with oxidation state and local coordination environment of Fe atoms. The model compounds comprise 30 natural minerals and synthetic compounds, with Fe coordination environments ranging from 4 to 12 O atoms for Fe2+, including 5-coordinated trigonal bipyramidal Fe2+, and from 4 to 6 O atoms for Fe3+. Most pre-edge spectra show two components (due to crystal-field splitting) that are located just above the Fermi level.
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