A molecular dynamics study of swelling, structural and dynamic properties of 2:1 Cis-vacant Cs saturated smectite

IF 5.3 2区 地球科学 Q2 CHEMISTRY, PHYSICAL
Pengyuan Gao , Yingchun Zhang , Xiandong Liu , Xiancai Lu
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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 Kc = 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.
关于 2:1 顺式-空隙 Cs 饱和闪长岩溶胀、结构和动态特性的分子动力学研究
蒙脱石是层状硅酸盐的一种,具有离散的水化/膨胀状态和基于层间水和离子活性的高阳离子交换能力,是工程和环境领域的重要材料。顺式空(cv)和反式空(tv)结构在天然蒙脱石中都可以观察到。先前的分子水平研究主要假设了tv结构,这可能导致对蒙脱石热力学和微观性质的错误预测。本文以三种具有代表性的具有Cs层间阳离子的顺式空蒙脱石(即wyoming型、arii型和beidellite)为模型框架,利用经典分子动力学模拟方法探讨了蒙脱石的热力学和微观性质。研究了不同层间含水量的蒙脱石的膨胀行为、Cs结合结构、层间水和Cs的分布和迁移率以及Cs/Na饱和蒙脱石之间的阳离子交换。结果表明,单层水化是Cs饱和蒙脱石最稳定的水化状态。层间水的扩散速度相对较慢,而Cs阳离子在低含水量条件下可以有效固定。此外,Cs阳离子在与蒙脱石基面平行方向上的迁移率高于垂直方向。Cs阳离子在中间层内形成稳定的内球络合结构,主要结合在六边形位点(h位点)和三角形位点(t位点)。此外,计算出的Cs/Na离子之间的阳离子选择性系数非常高(Log Kc = 1.69),表明Cs阳离子有效保留,与报道的实验相当。此外,还进一步将cv蒙脱石所得结果与tv蒙脱石所得结果进行了比较。对比结果表明,两种蒙脱石具有高度相似的热力学和微观性能。本研究为蒙脱石在地球化学和环境材料科学中的基础研究提供了一个拓展的认识。
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来源期刊
Applied Clay Science
Applied Clay Science 地学-矿物学
CiteScore
10.30
自引率
10.70%
发文量
289
审稿时长
39 days
期刊介绍: Applied Clay Science aims to be an international journal attracting high quality scientific papers on clays and clay minerals, including research papers, reviews, and technical notes. The journal covers typical subjects of Fundamental and Applied Clay Science such as: • Synthesis and purification • Structural, crystallographic and mineralogical properties of clays and clay minerals • Thermal properties of clays and clay minerals • Physico-chemical properties including i) surface and interface properties; ii) thermodynamic properties; iii) mechanical properties • Interaction with water, with polar and apolar molecules • Colloidal properties and rheology • Adsorption, Intercalation, Ionic exchange • Genesis and deposits of clay minerals • Geology and geochemistry of clays • Modification of clays and clay minerals properties by thermal and physical treatments • Modification by chemical treatments with organic and inorganic molecules(organoclays, pillared clays) • Modification by biological microorganisms. etc...
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