Interlayer Structures and Dynamics of Arsenate and Arsenite Intercalated Layered Double Hydroxides: A First Principles Study

被引:7
|
作者
Zhang, Yingchun [1 ]
Liu, Xiandong [1 ]
Zhang, Chi [1 ]
He, Mengjia [1 ]
Lu, Xiancai [1 ]
机构
[1] Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210046, Jiangsu, Peoples R China
基金
美国国家科学基金会;
关键词
arsenic; layered double hydroxides; first principles; adsorption; interlayer structure; mobility; DENSITY-FUNCTIONAL CALCULATIONS; AQUEOUS-SOLUTION; CLAY-MINERALS; SURFACE COMPLEXATION; ANION-EXCHANGE; XANES EVIDENCE; ADSORPTION; REMOVAL; SIMULATION; PHOSPHATE;
D O I
10.3390/min7040053
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 this study, by using first principles simulation techniques, we explored the basal spacings, interlayer structures, and dynamics of arsenite and arsenate intercalated Layered double hydroxides (LDHs). Our results confirm that the basal spacings of NO3--LDHs increase with layer charge densities. It is found that Arsenic (As) species can enter the gallery spaces of LDHs with a Mg/Al ratio of 2: 1 but they cannot enter those with lower charge densities. Interlayer species show layering distributions. All anions form a single layer distribution while water molecules form a single layer distribution at low layer charge density and a double layer distribution at high layer charge densities. H2AsO4- has two orientations in the interlayer regions (i.e., one with its three folds axis normal to the layer sheets and another with its two folds axis normal to the layer sheets), and only the latter is observed for HAsO42-. H2AsO3- orientates in a tilt-lying way. The mobility of water and NO3- increases with the layer charge densities while As species have very low mobility. Our simulations provide microscopic information of As intercalated LDHs, which can be used for further understanding of the structures of oxy-anion intercalated LDHs.
引用
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页数:15
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