2018Inorganic ChemistryRequires access

Influences of Cation Ratio, Anion Type, and Water Content on Polytypism of Layered Double Hydroxides

Meng Chen, Runliang Zhu, Xiancai Lu, Jianxi Zhu, Hongping He

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Abstract

Layered double hydroxides (LDHs) are a significant sink of anions (CO 3 2–, SO 4 2–, NO 3 –, 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 NO 3 – ions exhibit a polytype transition from 3 R 1 (three-layer rhombohedral polytype) to 1 T (one-layer trigonal polytype) with increasing water content. NO 3 – ions exhibit a D 3 h point group symmetry at low water contents. The polytype transition coincides with the complete transformation into tilted NO 3 – ion with a C 2 v point group symmetry. The transition appears at a lower water content when the Mg/Al ratio is lower. LDHs with SO 4 2– ions exhibit a three-stage polytypism. The first and last stages are 3 R 1 . 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 SO 4 2– ions with a C s point group symmetry is characteristic for the intermediate stage, while mostly SO 4 2– ions exhibit a C 3 v symmetry. There is no clear relevance between cation ratio and water content at which a polytype transition happens. The configurational adjustments of NO 3 – and SO 4 2– ions facilitate the swelling behavior of LDHs. LDHs with CO 3 2– or Cl – ions always maintain a 3 R 1 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.

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What this paper is about

Layered double hydroxides (LDHs) are a significant sink of anions (CO 3 2–, SO 4 2–, NO 3 –, 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 NO 3 – ions exhibit a polytype transition from 3 R 1 (three-layer rhombohedral polytype) to 1 T (one-layer trigonal polytype) with increasing water content. NO 3 – ions exhibit a D 3 h point group symmetry at low water contents. The polytype transition coincides with the complete transformation into tilted NO 3 – ion with a C 2 v point group symmetry. The transition appears at a lower water content when the Mg/Al ratio is lower. LDHs with SO 4 2– ions exhibit a three-stage polytypism. The first and last stages are 3 R 1 . 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 SO 4 2– ions with a C s point group symmetry is characteristic for the intermediate stage, while mostly SO 4 2– ions exhibit a C 3 v symmetry. There is no clear relevance between cation ratio and water content at which a polytype transition happens. The configurational adjustments of NO 3 – and SO 4 2– ions facilitate the swelling behavior of LDHs. LDHs with CO 3 2– or Cl – ions always maintain a 3 R 1 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.

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Available abstract

Layered double hydroxides (LDHs) are a significant sink of anions (CO 3 2–, SO 4 2–, NO 3 –, 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 NO 3 – ions exhibit a polytype transition from 3 R 1 (three-layer rhombohedral polytype) to 1 T (one-layer trigonal polytype) with increasing water content. NO 3 – ions exhibit a D 3 h point group symmetry at low water contents. The polytype transition coincides with the complete transformation into tilted NO 3 – ion with a C 2 v point group symmetry. The transition appears at a lower water content when the Mg/Al ratio is lower. LDHs with SO 4 2– ions exhibit a three-stage polytypism. The first and last stages are 3 R 1 . 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 SO 4 2– ions with a C s point group symmetry is characteristic for the intermediate stage, while mostly SO 4 2– ions exhibit a C 3 v symmetry. There is no clear relevance between cation ratio and water content at which a polytype transition happens. The configurational adjustments of NO 3 – and SO 4 2– ions facilitate the swelling behavior of LDHs. LDHs with CO 3 2– or Cl – ions always maintain a 3 R 1 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.

Key concepts: Chemistry, Ion, Divalent, Octahedron, Inorganic chemistry, Layered double hydroxides, Ion exchange, Crystallography

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Influences of Cation Ratio, Anion Type, and Water Content on Polytypism of Layered Double Hydroxides — Research Paper | ScholarLens