Temperature dependence of interfacial structures and acidity of clay edge surfaces

被引:25
作者
Liu, Xiandong [1 ]
Lu, Xiancai [1 ]
Cheng, Jun [2 ,3 ]
Sprik, Michiel [2 ]
Wang, Rucheng [1 ]
机构
[1] Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210093, Jiangsu, Peoples R China
[2] Univ Cambridge, Dept Chem, Cambridge CB2 1EW, England
[3] Univ Aberdeen, Dept Chem, Aberdeen AB24 3UE, Scotland
基金
美国国家科学基金会;
关键词
INITIO MOLECULAR-DYNAMICS; ATOMIC-SCALE STRUCTURES; AB-INITIO; NA-MONTMORILLONITE; WATER INTERFACE; SORPTION; ENERGY; KAOLINITE; CHEMISTRY; MINERALS;
D O I
10.1016/j.gca.2015.04.005
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
In the pursuit of a microscopic understanding of the effects of temperature on the surface reactivity of clay minerals, we conducted first principles molecular dynamics (FPMD) simulations to study the interfacial structures and acidity of clay edge surfaces at elevated temperatures. The common edge surfaces ((010) and (110) types) of phyllosilicates were investigated at 348 K and 423 K, and the results were compared with those previously derived at ambient conditions. We found that the stable surface sites are the same as at ambient conditions, including equivalent to Al(OH2)(2) (6-fold Al), equivalent to Al(OH2) (5-fold Al) and, equivalent to Si(OH) on the (010) facet, and equivalent to Al(OH2)Al(OH)Si equivalent to and equivalent to Si(OH) on the (110) surface. The FPMD-based vertical energy gap technique was applied to compute the acidity constants of edge sites and the resulting pKa values show a decreasing trend with temperature. The results demonstrate that although changes in the point of zero charge of the entire material are insignificant up to 348 K, the decrease in surface pKa can be 3 pKa units, while it can be as large as 6 pKa units up to 423 K. The derived interface structures and pKa values can be used in future experimental and modeling research, e.g., in interpreting experiments and predicting the surface complexation of metal cations and organics. This study therefore provides a physical basis for investigating the interfacial processes of clay minerals in environments that experience elevated P-T conditions, such as sedimentary basins and geological nuclear waste repositories. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:91 / 99
页数:9
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