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Study on the differences of Na- and Ca-montmorillonites in crystalline swelling regime through molecular dynamics simulation

机译:通过分子动力学模拟研究Na-和Ca-蒙脱石在晶体溶胀中的差异

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The swelling of Na- and Ca-montmorillonites (MMTs) has been studied through energy optimization and molecular dynamics simulations with the Universal Force Field (UFF) in this work. It was performed to reveal the interlayer spacing and water density in the interlayer as the function of water molecules increasing from 0 to 96, and the structural and diffusive properties of interlayer species when formed one-, two-, three-layer hydrates in interlayer. The results presented the swelling pattern of the MMTs, and the process of that water molecules formed layers in MMT interlayers. It has been found that Ca-MMT had a stronger hydration swelling than Na-MMT in the crystalline swelling regime, which might be due to that Ca2+ had a larger hydrated radius than Na+. Water molecules in the interlayers of Na-MMT had a larger self-diffusion coefficient than those of Ca-MMT at the same water content. Moreover, Na+ had a higher self-diffusion coefficient than Ca2+. It was demonstrated that the difference at the swelling of the two MMTs was attributed to that Ca2+ had a stronger hydration than Na+ in the MMT interlayers. (C) 2016 The Society of Powder Technology Japan. Published by Elsevier B.V. and The Society of Powder Technology Japan. All rights reserved.
机译:在这项工作中,已经通过能量优化和分子动力学模拟和万能力场(UFF)研究了钠和钙蒙脱石(MMT)的溶胀。进行了研究,揭示了随着水分子从0增加到96的功能,夹层中的夹层间距和水密度,以及当在夹层中形成一,二,三层水合物时夹层物种的结构和扩散特性。结果显示了MMT的膨胀模式,以及水分子在MMT中间层中形成层的过程。已经发现,在结晶溶胀状态下,Ca-MMT的水合溶胀比Na-MMT强,这可能是由于Ca2 +的水合半径大于Na +。在相同的含水量下,Na-MMT中间层中的水分子具有比Ca-MMT更大的自扩散系数。此外,Na +具有比Ca2 +高的自扩散系数。结果表明,两种MMT溶胀的差异是由于MMT中间层中Ca2 +的水合性比Na +强。 (C)2016日本粉末技术学会。由Elsevier B.V.和日本粉末技术学会出版。版权所有。

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