Ab Initio Simulation of Changes in Geometry, Electronic Structure, and Gibbs Free Energy Caused by Dehydration of Hydrotalcites Containing Cl- and CO32- Counteranions

被引:56
作者
Costa, Deyse G. [1 ]
Rocha, Alexandre B. [2 ]
Souza, Wladmir F. [3 ]
Chiaro, Sandra Shirley X. [3 ]
Leitao, Alexandre A. [1 ]
机构
[1] Univ Fed Juiz de Fora, Dept Qum, BR-36036330 Juiz De Fora, MG, Brazil
[2] Univ Fed Rio de Janeiro, Inst Qum, Dept Fsicoqum, BR-21941909 Rio De Janeiro, Brazil
[3] Ilha Fundao, PETROBRAS CENPES, BR-21941915 Rio De Janeiro, Brazil
关键词
LAYERED-DOUBLE-HYDROXIDES; NATURAL HYDROTALCITES; POWDER DIFFRACTION; X-RAY; INTERLAYER STRUCTURE; DFT CALCULATIONS; ANIONIC CLAYS; DYNAMICS; ZN; SPECTROSCOPY;
D O I
10.1021/jp110668s
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 ; 081704 ;
摘要
This ab initio study was performed to better understand the correlation between intercalated water molecules and layered double hydroxides (LDH), as well as the changes that occur by the dehydration process of Zn-Al hydrotalcite-like compounds containing Cl- and CO32- counterions. We have verified that the strong interaction among intercalated water molecules, cointercalated anions, and OH groups from hydroxyl layers is reflected in the thermal stability of these compounds. The Zn2/3Al1/3(OH)(2)Cl-1/3 center dot 2/3H(2)O hydrotalcite loses all the intercalated water molecules around 125 degrees C, while the Zn2/3Al1/3(OH)(2)(CO3)(1/6)center dot 4/6H(2)O compound dehydrates at about 175 degrees C. These values are in good agreement with experimental data. The interlayer interactions were discussed on the basis of electron density difference analyses. Our calculation shows that the electron density in the interlayer region decreases during the dehydration process, inducing the migration of the Cl anion and the displacement of the hydroxyl layer from adjacent layers. Changes in these compound structures occur to recover part of the hydrogen bonds broken due to the removal of water molecules. It was observed that the chloride ion had initially a lower Lowdin charge (Cl-0.43), which has increased its absolute value (Cl-0.58) after the water molecules removal, while the charges on carbonate ions remain invariant, leading to the conclusion that the Cl anion can be more influenced by the amount of water molecules in the interlayer space than the CO32- anion in hydrotalcite-like compounds.
引用
收藏
页码:3531 / 3537
页数:7
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