A molecular dynamics study of swelling, structural and dynamic properties of 2:1 Cis-vacant Cs saturated smectite
Source abstract
Abstract
Smectite, a family of phyllosilicates, exhibits discrete hydration/swelling states and high cation exchange capacity based on interlayer water and ion activities, rendering it a crucial material in engineering and environmental fields. Both cis-vacant ( cv) and trans-vacant ( tv) structures are observed in natural smectites. Previous molecular-level studies have predominantly assumed a tv configuration, potentially leading to incorrect predictions of smectite`s thermodynamic and microscopic properties. Here, three representative cis-vacant smectites (i.e., Wyoming-type, Ari-type, and beidellite) with Cs interlayer cations were employed as a model framework to explore the thermodynamic and microscopic properties of smectite using classical molecular dynamic simulations. The swelling behaviors of smectite with different interlayer water content, Cs binding structures, distributions and mobility of interlayer water and Cs species, and cation exchange between Cs/Na saturated smectites were investigated. The results suggested that the monolayer hydrate is the most stable hydration state of Cs saturated smectites. The diffusion of interlayer water was relatively slower compared to the corresponding bulk case, while Cs cations can be effectively fixed at low water content. Furthermore, Cs cations showed higher mobility in the direction parallel to the basal plane of smectite rather than in the perpendicular direction. Cs cations form a stable inner-sphere complexation structure within the interlayer, primarily binding at the hexagonal sites (H-sites) and triangular sites (T-sites). In addition, the calculated cationic selectivity coefficients between Cs/Na ions were found to be significantly high (Log K c = 1.69), indicating effective retention of Cs cations and comparable to the reported experiments. Moreover, all the results obtained from the cv smectite are further compared to those derived from the tv smectite. The comparison results showed that both smectites have highly similar thermodynamic and microscopic properties. This study provides an extended understanding to facilitate fundamental research of smectite in geochemistry and environmental material science.
Source: expertdata · Quality: candidate unverified · Source record ↗
Research context
OpenAlex topics: Clay minerals and soil interactions · Soil and Unsaturated Flow · Iron oxide chemistry and applications
SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.
References (66)
Show source-provided references
1. Geo’chemical research: a key building block for nuclear waste disposal safety cases10.1016/j.jconhyd.2008.09.012 ↗
2. Mechanism of Adsorption and Desorption of Water Vapor by Homoionic Montmorillonites: 2. The Li+, Na+, K+, Rb+ and Cs+-Exchanged Forms10.1346/CCMN.1995.0430307 ↗
3. The Missing Term in Effective Pair Potentialst10.1021/j100308a038 ↗
4. Monte Carlo Molecular Modeling Studies of Hydrated Li-, Na-, and K-Smectites: Understanding the Role of Potassium as a Clay Swelling Inhibitor10.1021/ja00155a025 ↗
5. Connecting the Molecular Scale to the Continuum Scale for Diffusion Processes in Smectite-Rich Porous Media10.1021/es903645a ↗
6. Molecular dynamics simulations of the electrical double layer on smectite surfaces contacting concentrated mixed electrolyte (NaCl–CaCl2) solutions10.1016/j.jcis.2011.04.063 ↗
7. Stable and radioactive cesium: a review about distribution in the environment, uptake and translocation in plants, plant reactions and plants’ potential for bioremediation10.1016/j.scitotenv.2017.09.298 ↗
8. Hydratation de la montmorillonite et diffusion des cations compensateurs. I. Saturation par des cations monovalents
9. Effect of exchangeable cation on the swelling property of 2:1 dioctahedral smectite-a periodic first principle study10.1063/1.1640333 ↗
10. Swelling characteristics of montmorillonite mineral particles in Gaomiaozi bentonite10.1016/j.conbuildmat.2024.137335 ↗
11. Mobility of Na and Cs on Montmorillonite Surface under Partially Saturated Conditions10.1021/es401530n ↗
12. Clay minerals in the meuse-haute Marne underground laboratory (France): possible influence of organic matter on clay mineral evolution10.1346/CCMN.2004.0520501 ↗
13. Molecular Models of Hydroxide, Oxyhydroxide, and Clay Phases and the Development of a General Force Field10.1021/jp0363287 ↗
14. Advances in Clayff Molecular simulation of Layered and Nanoporous Materials and their Aqueous Interfaces10.1021/acs.jpcc.1c04600 ↗
15. A comparative study of DFT and XPS with reference to the adsorption of caesium ions in smectites10.1016/S0927-0256(98)00116-5 ↗
16. Clay profiling: the classification of montmorillonites10.1346/CCMN.2009.0570110 ↗
17. HTO and selenate diffusion through compacted Na-, Na–Ca-, and Ca-montmorillonite10.1016/j.apgeochem.2024.106090 ↗
18. Acid–Base Properties of Cis-Vacant Montmorillonite Edge Surfaces: A Combined First-Principles Molecular Dynamics and Surface Complexation Modeling Approach10.1021/acs.est.2c07171 ↗
19. Influence of Fe(II), Fe(III) and Al(III) Isomorphic Substitutions on Acid-Base Properties of Edge Surfaces of Cis-Vacant Montmorillonite: Insights from First-Principles Molecular Dynamics Simulations and Surface Complexation Modeling10.2138/am-2023-9057 ↗
20. Mechanistic understanding of dehydroxylation reaction of smectites: Insights from reactive force field (ReaxFF) molecular dynamics simulation
21. Molecular Simulation of Structure and Diffusion at Smectite–Water Interfaces: Using Expanded Clay Interlayers as Model Nanopores10.1021/acs.jpcc.5b03314 ↗
22. Characterization of Adsorbed Alkali Metal Ions in 2:1 Type Clay Minerals from First-Principles Metadynamics10.1021/acs.jpca.5b05934 ↗
23. Estimation of Effective Diffusivity in Compacted Ben Tonite10.1557/PROC-353-277 ↗
24. Molecular simulation of cesium adsorption at the basal surface of phyllosilicate minerals10.1346/CCMN.2016.0640405 ↗
25. Diffusion of Na and Cs in montmorillonite10.1346/CCMN.2008.0560205 ↗
26. Lithium partition and isotopic fractionation for cation exchange in clay: Insights from molecular simulations10.1016/j.gca.2023.07.024 ↗
27. A cation exchange model to describe Cs+ sorption at high ionic strength in subsurface sediments at Hanford site, USA10.1016/S0169-7722(03)00143-8 ↗
28. Effects of layer-charge distribution on the thermodynamic and microscopic properties of Cs-smectite10.1016/j.gca.2008.01.028 ↗
29. Molecular-level understanding of metal ion retention in clay-rich materials10.1038/s43017-022-00301-z ↗
30. Quantifying the Mechanisms of Site-specific Ion Exchange at an Inhomogeneously Charged Surface: Case of Cs+/K+ on Hydrated Muscovite Mica10.1021/acs.jpcc.6b13108 ↗
31. A modified version of Archie’s law to estimate effective diffusion coefficients of radionuclides in argillaceous rocks and its application in safety analysis studies10.1016/j.apgeochem.2015.04.002 ↗
32. Microscopic Simulations of Interlayer Structure and Dynamics in Bihydrated Heteroionic Montmorillonites10.1021/jp022084z ↗
33. Microscopic simulation of Structure and Dynamics of Water and Counterions in a Monohydrated Montmorillonite10.1063/1.1493186 ↗
34. Radionuclide Interaction with Clays in Dilute and Heavily Compacted Systems: a critical Review10.1021/es203025q ↗
35. Modeling cesium retention onto Na-, K- and Ca-smectite: Effects of ionic strength, exchange and competing cations on the determination of selectivity coefficients10.1016/j.gca.2013.10.007 ↗
36. Adsorption of Water Vapor by Montmorillonite. II. Effect of Exchangeable Ions and Lattice Swelling as measured by X-Ray Diffraction10.1021/ja01126a002 ↗
37. In situ x-ray diffraction study of the swelling of montmorillonite as affected by exchangeable cations and temperature10.1346/CCMN.2011.0590205 ↗
38. Structural arrangements of Isomorphic Substitutions in Smectites: Molecular simulation of the Swelling Properties, Interlayer Structure, and Dynamics of Hydrated Cs–Montmorillonite Revisited with New Clay Models10.1021/jp500538z ↗
39. Structure and dynamics of hydrated ions10.1021/cr00019a014 ↗
40. Radiocesium interaction with clay minerals: Theory and simulation advances Post–Fukushima10.1016/j.jenvrad.2018.03.011 ↗
41. Competitive adsorption processes at clay mineral surfaces: a coupled experimental and modeling approach10.1021/acsearthspacechem.1c00323 ↗
42. Selective adsorption and irreversible fixation behavior of cesium onto 2:1 layered clay mineral: a mini review10.1016/j.jhazmat.2019.02.061 ↗
43. Direct Exchange Mechanism for Interlayer Ions in Non-Swelling Clays10.1021/acs.est.6b04747 ↗
44. Application of Double-Layer Theories to the Extensive Crystalline Swelling of Li-Montmorillonite10.1021/la970484l ↗
45. Diffusion of Cs, Np, Am and Co in compacted sand-bentonite mixtures: evidence for surface diffusion of Cs cations10.1180/claymin.2013.048.2.19 ↗
46. Molecular Computer Simulations of the Swelling Properties and Interlayer Structure of Cesium Montmorillonite10.1021/la980015z ↗
47. Thermodynamics of ion exchange coupled with swelling reactions in hydrated clay minerals10.1016/j.jcis.2021.09.106 ↗
48. Structural implications of interfacial hydrogen bonding in hydrated Wyoming-montmorillonite clay10.1021/acs.jpcc.9b11339 ↗
49. Molecular simulation of Interlayer Structure and Dynamics in 12.4 Å Cs-Smectite Hydrates10.1006/jcis.2000.7416 ↗
50. A Molecular Mechanism of Hysteresis in Clay Swelling10.1002/anie.200353612 ↗
51. Molecular simulations of swelling clay minerals10.1021/jp049799h ↗
52. Swelling properties of montmorillonite and beidellite clay minerals from molecular simulation: comparison of temperature, interlayer cation, and charge location effects10.1021/acs.jpcc.5b03253 ↗
53. LAMMPS - a flexible simulation tool for particle-based materials modeling at the atomic, meso, and continuum scales10.1016/j.cpc.2021.108171 ↗
54. Cation Exchange Selectivity Coefficient Values on Smectite and Mixed-Layer Illite/Smectite Minerals10.2136/sssaj2008.0285 ↗
55. Resolving experimental biases in the interpretation of diffusion experiments with a user-friendly numerical reactive transport approach10.1038/s41598-023-42260-5 ↗
56. Preface of the special issue of Applied Clay Science “8th International Conference on Clays in Natural and Engineered Barriers for Radioactive Waste Confinement”10.1016/j.clay.2024.107331 ↗
57. The distribution of octahedral cations in the 2:1 layers of dioctahedral smectites studied by oblique-texture electron diffraction10.1180/claymin.1984.019.2.05 ↗
58. Nanoscale chemomechanical variations of montmorillonite induced by the specificity of counterions-an in situ XRD and AFM study10.1016/j.clay.2022.106760 ↗
59. A comprehensive characterization of dioctahedral smectites10.1346/CCMN.2009.0570111 ↗
60. Atomistic simulations of cation hydration in sodium and calcium montmorillonite nanopores10.1063/1.4992001 ↗
61. Simulations of clay mineral swelling and hydration: dependence upon interlayer ion size and charge10.1021/jp000146k ↗
62. Sorption of Cs+ to micaceous subsurface sediments from the Hanford site, USA10.1016/S0016-7037(01)00759-1 ↗
63. Molecular dynamics simulations of exchange behavior of radionuclides into montmorillonite: Unraveling the dynamic processes and microscopic structures10.1016/j.clay.2022.106579 ↗
64. Molecular dynamics study of the exchange processes of heavy metals into montmorillonite: Characterization of hydrated edge surfaces and dynamic exchange mechanism10.1016/j.apgeochem.2023.105587 ↗
65. Coupling between clay swelling/collapse and cationic partition10.1016/j.gca.2020.07.007 ↗
66. Molecular simulation on Cs, Rb retention in Na/K-montmorillonite interlayer coupling clay swelling/collapse10.1016/j.apgeochem.2024.106249 ↗