Crystal structures of the α and β forms of K2ZnGeO4

被引:8
作者
Colbeau-Justin, C
Wallez, G
Elfakir, A
Quarton, M
机构
[1] Univ Paris 06, Lab Cristallochim Solide, CNRS, URA 1388, F-75252 Paris 05, France
[2] Inst Max Von Laue Paul Langevin, F-38042 Grenoble, France
关键词
D O I
10.1006/jssc.1997.7536
中图分类号
O61 [无机化学];
学科分类号
070301 ; 081704 ;
摘要
The crystal structures of two phases of K2ZnGeO4 have been refined by the Rietveld method using neutron powder diffraction data, at 298 K (alpha form) and 1153 K (beta form), to R-B = 4.8 and 7.3%, respectively. alpha-K2ZnGeO4 is orthorhombic, a = 11.1131(4) Angstrom, b = 5.5369(2) Angstrom, c = 15.8629(5) Angstrom, space group Pca2(1), and Z = 8, beta-K2ZnGeO4 is cubic, a = 8.0254(5) Angstrom, space group F (4) over bar 3m, and Z = 4, Phase transition between alpha and beta forms occurs at 1049 K, Both phases are stuffed cristobalites and correspond to a distortion of the ideal cristobalite structure, Neutron diffraction data show an ordered and alternating arrangement of ZnO4 and GeO4 tetrahedra in alpha-K2ZnGeO4. The beta phase shows a static or dynamic superposition of short-range ordered clusters analogous to SiO2 cristobalite, (C) 1997 Academic Press.
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页码:59 / 66
页数:8
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