Department of Chemical & Biomolecular Engineering, University of Melbourne, Victoria 3010, Australia.
J Phys Chem A. 2010 Apr 15;114(14):4988-96. doi: 10.1021/jp911108d.
Understanding the atomic-level changes that occur as kaolinite is converted (thermally dehydroxylated) to metakaolin is critical to the optimization of this large-scale industrial process. Metakaolin is X-ray amorphous; therefore, conventional crystallographic techniques do not reveal the changes in local structure during its formation. Local structure-based experimental techniques are useful in understanding the atomic structure but do not provide the thermodynamic information which is necessary to ensure plausibility of refined structures. Here, kaolinite dehydroxylation is modeled using density functional theory, and a stepwise methodology, where several water molecules are removed from the structure, geometry optimization is carried out, and then the process is repeated. Hence, the structure remains in an energetically and thermodynamically feasible state while transitioning from kaolinite to metakaolin. The structures generated during the dehydroxylation process are validated by comparison with X-ray and neutron pair distribution function data. Thus, this study illustrates one possible route by which dehydroxylation of kaolinite can take place, revealing a chemically, energetically, and experimentally plausible structure of metakaolin. This methodology of density functional modeling of the stepwise changes in a material is not limited in application to kaolinite or other aluminosilicates and provides an accurate representation of the local structural changes occurring in materials used in industrially important processes.
理解高岭石在转化(热脱羟)为偏高岭土的过程中发生的原子级变化对于优化这一大规模工业过程至关重要。偏高岭土是无定形的 X 射线,因此常规晶体学技术无法揭示其形成过程中局部结构的变化。基于局部结构的实验技术有助于理解原子结构,但无法提供确保细化结构合理性所需的热力学信息。在这里,使用密度泛函理论对高岭石脱羟进行建模,并采用逐步方法,从结构中去除几个水分子,进行几何优化,然后重复该过程。因此,在从高岭石向偏高岭土转变的过程中,结构保持在能量和热力学上可行的状态。通过与 X 射线和中子对分布函数数据的比较,验证了脱羟过程中生成的结构。因此,本研究说明了高岭石脱羟可能发生的一种途径,揭示了偏高岭土的化学、能量和实验上合理的结构。这种逐步改变材料的密度泛函建模方法不仅限于高岭石或其他铝硅酸盐的应用,并且可以准确地表示工业重要过程中使用的材料中发生的局部结构变化。