White Claire E, Provis John L, Riley Daniel P, Kearley Gordon J, van Deventer Jannie S J
Department of Chemical & Biomolecular Engineering, University of Melbourne, Victoria 3010, Australia.
J Phys Chem B. 2009 May 14;113(19):6756-65. doi: 10.1021/jp810448t.
Density functional modeling of the crystalline layered aluminosilicate mineral kaolinite is conducted, first to reconcile discrepancies in the literature regarding the exact geometry of the inner and inner surface hydroxyl groups, and second to investigate the performance of selected exchange-correlation functionals in providing accurate structural information. A detailed evaluation of published experimental and computational structures is given, highlighting disagreements in space groups, hydroxyl bond lengths, and bond angles. A major aim of this paper is to resolve these discrepancies through computations. Computed structures are compared via total energy calculations and validated against experimental structures by comparing computed neutron diffractograms, and a final assessment is performed using vibrational spectra from inelastic neutron scattering. The density functional modeling is carried out at a sufficiently high level of theory to provide accurate structure predictions while keeping computational requirements low enough to enable the use of the structures in large-scale calculations. It is found that the best functional to use for efficient density functional modeling of kaolinite using the DMol3 software package is the BLYP functional. The computed structure for kaolinite at 0 K has C1 symmetry, with the inner hydroxyl group angled slightly above the a,b plane and the inner surface hydroxyls aligned close to perpendicular to that plane.
对结晶层状铝硅酸盐矿物高岭石进行了密度泛函建模,一是为了协调文献中关于内表面和内表面羟基确切几何结构的差异,二是为了研究选定的交换相关泛函在提供准确结构信息方面的性能。对已发表的实验和计算结构进行了详细评估,突出了空间群、羟基键长和键角方面的分歧。本文的一个主要目标是通过计算解决这些差异。通过总能量计算比较计算结构,并通过比较计算的中子衍射图与实验结构进行验证,最后使用非弹性中子散射的振动光谱进行评估。密度泛函建模在足够高的理论水平上进行,以提供准确的结构预测,同时保持计算要求足够低,以便能够在大规模计算中使用这些结构。结果发现,使用DMol3软件包对高岭石进行高效密度泛函建模时,最佳的泛函是BLYP泛函。计算得到的0K时高岭石结构具有C1对称性,内表面羟基在a、b平面上方略有倾斜,内表面羟基几乎垂直于该平面排列。