Crystal chemistry of cation order-disorder in pseudobrookite-type MgTi2O5

被引:41
|
作者
Yang, HX
Hazen, RM
机构
[1] Carnegie Inst Washington, Geophys Lab, Washington, DC 20015 USA
[2] Carnegie Inst Washington, Ctr High Pressure Res, Washington, DC 20015 USA
基金
美国国家科学基金会;
关键词
D O I
10.1006/jssc.1998.7775
中图分类号
O61 [无机化学];
学科分类号
070301 ; 081704 ;
摘要
Effects of caticon order-disorder on the pseudobrookite-type MgTi2O5 structure have been studied with single-crystal X-ray diffraction on five synthetic crystals (labeled P600, P700, P800, P1000, and P1400) ananealed a; 600, 700, 800, 1000, and 1400 degrees C, respectively. The disorder parameters (X = Ti ins the M1 site) determined for five samples range from 0.070(5) to 0.485(5). Unit-cell dimensions a and c increase with X, whereas b decreases. The decrease in b with increasing cation disorder results primarily from the marked reduction in the O3-O3 distance within the M1 octahedron, whereas the variation of n and c is controlled by the size of the M2 octahedron. From P600 to P1400, the mean M1-O length shortens by 2.35%; in contrast, the mean M2-O distance lengthens by 1.16%. as a consequence, the M1 and M2 sites have a nearly identical octahedral volume in P1400. With increasing cation disorder, the degree of distortion of the M1 octahedron is reduced significantly, while that of M2 remains essentially unchanged, Cation disorder is also accompanied by straightening of the bands consisting of the M1 and M2 octahedra. There is a close correlation between atomic isotropic displacement factors (B-iso) and cation order-disorder: B-iso factors of all atoms in more disordered samples are larger than those in less disordered ones, (C) 1998 Academic Press.
引用
收藏
页码:238 / 244
页数:7
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