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Influences of Cation Ratio, Anion Type, and Water Content on Polytypism of Layered Double Hydroxides.
Chen, Meng; Zhu, Runliang; Lu, Xiancai; Zhu, Jianxi; He, Hongping.
Afiliação
  • Chen M; CAS Key Laboratory of Mineralogy and Metallogeny/Guangdong Provincial Key Laboratory of Mineral Physics and Materials, Guangzhou Institute of Geochemistry , Chinese Academy of Sciences (CAS) , Guangzhou 510640 , China.
  • Zhu R; University of Chinese Academy of Sciences , 19 Yuquan Road , Beijing 100049 , China.
  • Lu X; CAS Key Laboratory of Mineralogy and Metallogeny/Guangdong Provincial Key Laboratory of Mineral Physics and Materials, Guangzhou Institute of Geochemistry , Chinese Academy of Sciences (CAS) , Guangzhou 510640 , China.
  • Zhu J; University of Chinese Academy of Sciences , 19 Yuquan Road , Beijing 100049 , China.
  • He H; State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering , Nanjing University , Nanjing 210093 , China.
Inorg Chem ; 57(12): 7299-7313, 2018 Jun 18.
Article em En | MEDLINE | ID: mdl-29863856
ABSTRACT
Layered double hydroxides (LDHs) are a significant sink of anions (CO32-, SO42-, NO3-, Cl-, etc.) and divalent transition-metal cations in soil. The anion exchange capacity gives rise to functional materials. The stability of LDHs is determined by the interaction between cation-bearing layers and intercalated water and anions, which is correlated with polytypism and coordination structure. A systematic investigation is performed to show the influence of cation ratio, anion type, and water content on polytypism, swelling behavior, and interlayer structure of Mg-Al-LDHs using molecular dynamics simulations. LDHs intercalated with NO3- ions exhibit a polytype transition from 3 R1 (three-layer rhombohedral polytype) to 1 T (one-layer trigonal polytype) with increasing water content. NO3- ions exhibit a D3 h point group symmetry at low water contents. The polytype transition coincides with the complete transformation into tilted NO3- ion with a C2 v point group symmetry. The transition appears at a lower water content when the Mg/Al ratio is lower. LDHs with SO42- ions exhibit a three-stage polytypism. The first and last stages are 3 R1. The intermediate stage could be 1 T or a mixture of different O(octahedra)-type interlayers, which depends on the cation ratio. The relative popularity of SO42- ions with a C s point group symmetry is characteristic for the intermediate stage, while mostly SO42- ions exhibit a C3 v symmetry. There is no clear relevance between cation ratio and water content at which a polytype transition happens. The configurational adjustments of NO3- and SO42- ions facilitate the swelling behavior of LDHs. LDHs with CO32- or Cl- ions always maintain a 3 R1 polytype irrespective of water content and hardly swell. The configurations of anions and water reflect local coordination structure due to hydrogen bonds. The layer-stacking way influences long-ranged Coulombic interactions. Hydrogen-bonding structure and long-ranged Coulombic interactions collectively determine polytypism and stability of LDHs.

Texto completo: 1 Base de dados: MEDLINE Idioma: En Revista: Inorg Chem Ano de publicação: 2018 Tipo de documento: Article País de afiliação: China

Texto completo: 1 Base de dados: MEDLINE Idioma: En Revista: Inorg Chem Ano de publicação: 2018 Tipo de documento: Article País de afiliação: China