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
Abstract
Meng Chen, Runliang Zhu, Xiancai Lu, Jianxi Zhu, Hongping He
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.
OpenAlex reports 37 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
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