RIETVELD REFINEMENT OF THE KAOLINITE STRUCTURE AT 1.5-K

被引:523
作者
BISH, DL
机构
[1] Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos
关键词
CRYSTAL STRUCTURE; H-POSITIONS; KAOLINITE; LOW TEMPERATURE; NEUTRON POWDER DIFFRACTION; RIETVELD REFINEMENT;
D O I
10.1346/CCMN.1993.0410613
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 [物理化学]; 081704 [应用化学];
摘要
The crystal structure of Keokuk kaolinite, including all H atoms, was refined in space group C1 using low-temperature (1.5 K) neutron powder diffraction data (lambda = 1.9102 angstrom) and Rietveld refinement/difference-Fourier methods to R(wp) = 1.78%, reduced chi2 = 3.32. Unit-cell parameters are: a = 5.1535(3) angstrom, b = 8.9419(5) angstrom, c = 7.3906(4) angstrom, alpha = 91.926(2)-degrees, beta = 105.046(2)-degrees, gamma = 89.797(2)-degrees, and V = 328.70(5) angstrom3. Unit-cell parameters show that most of the thermal contraction occurred along the [001] direction, apparently due to a decrease in the interlayer distance. The non-H structure is very similar to published Cl structures, considering the low temperature of data collection, but the H atom positions are distinct. The inner OH group is essentially in the plane of the layers, and the inner-surface OH groups make angles of 60-degrees-73-degrees with the (00 1) plane. Difference-Fourier maps show minor anisotropy of the inner-OH group in the [001] direction, but the inner-surface OH groups appear to have their largest vibrational (or positional disorder) component parallel to the layers. Although no data indicate a split position of any of the H sites in kaolinite,there is support for limited random positional disorder of the H atoms. However, these data provided no support for a space group symmetry lower than Cl.
引用
收藏
页码:738 / 744
页数:7
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