尖晶石
离子半径
八面体
化学计量学
结晶学
热膨胀
粘结长度
晶体结构
单晶
四面体
离子键合
衍射
公式单位
材料科学
分析化学(期刊)
化学
离子
物理化学
物理
冶金
光学
有机化学
色谱法
作者
Giovanni B. Andreozzi,Francesco Princivalle,Henrik Skogby,A. Della Giusta
出处
期刊:American Mineralogist
[Mineralogical Society of America]
日期:2000-09-01
卷期号:85 (9): 1164-1171
被引量:159
标识
DOI:10.2138/am-2000-8-907
摘要
The equilibrium distribution of Mg and Al between the tetrahedral and octahedral sites of a flux grown, stoichiometric MgAl2O4 spinel was investigated between 600 and 1100 °C by single-crystal X-ray diffraction of quenched samples. The cation distribution for both ordering and disordering runs was obtained by minimizing accurate crystallographic parameters and effective ionic radii. Along with the variation of the degree of inversion from 0.18 to 0.29 between 600 and 1100 °C, both unit cell and oxygen positional parameter decreased linearly. Multiple non-linear least-squares fit of our data with the thermodynamic model of O’Neill and Navrotsky (1983) gave α = 23 ± 2 KJ/mol and β = 13 ± 4 KJ/mol. The influence of both cation inversion and thermal expansion on T-O and MO bond length variation was determined by comparison of our data with previous in situ studies. In the thermal interval investigated, the inversion accounts for change of -0.014 Å for T-O and +0.007 Å for M-O. Mean linear polyhedral thermal expansion coefficients of 6.5 × 10-6 °C-1 and 8.9 × 10-6 °C-1 were calculated for T and M sites, respectively.
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