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高岭土晶体结构与热机械性能之间的关系:超越标准密度泛函理论

Relationship between crystal structure and thermo-mechanical properties of kaolinite clay: beyond standard density functional theory.

作者信息

Weck Philippe F, Kim Eunja, Jové-Colón Carlos F

机构信息

Sandia National Laboratories, Albuquerque, NM 87185, USA.

出版信息

Dalton Trans. 2015 Jul 28;44(28):12550-60. doi: 10.1039/c5dt00590f.

Abstract

The structural, mechanical and thermodynamic properties of 1 : 1 layered dioctahedral kaolinite clay, with ideal Al2Si2O5(OH)4 stoichiometry, were investigated using density functional theory corrected for dispersion interactions (DFT-D2). The bulk moduli of 56.2 and 56.0 GPa predicted at 298 K using the Vinet and Birch-Murnaghan equations of state, respectively, are in good agreement with the recent experimental value of 59.7 GPa reported for well-crystallized samples. The isobaric heat capacity computed for uniaxial deformation of kaolinite along the stacking direction reproduces calorimetric data within 0.7-3.0% from room temperature up to its thermal stability limit.

摘要

利用考虑色散相互作用校正的密度泛函理论(DFT-D2)研究了化学计量比为理想的Al2Si2O5(OH)4的1:1层状二八面体高岭土粘土的结构、力学和热力学性质。使用维内特(Vinet)状态方程和伯奇-莫纳汉(Birch-Murnaghan)状态方程分别预测的在298K时的体模量为56.2 GPa和56.0 GPa,与最近报道的结晶良好样品的实验值59.7 GPa吻合良好。计算得到的高岭土沿堆积方向单轴变形的等压热容在从室温到其热稳定性极限的范围内,与量热数据的偏差在0.7%-3.0%以内。

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