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Sugar-influenced water diffusion, interaction, and retention in clay interlayer nanopores probed by theoretical simulations and experimental spectroscopies

机译:通过理论模拟和实验光谱学研究了糖影响的水在粘土夹层纳米孔中的扩散,相互作用和保留

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摘要

Understanding the hydrodynamics in clay nanopores is important for gaining insights into the trapping of water, nutrients, and contaminants in natural and engineered soils. Previous investigations have focused on the interlayer organization and molecular diffusion coefficients (D) of cations and water molecules in cation-saturated interlayer nanopores of smectite clays. Little is known, however, about how these interlayer dynamic properties are influenced by the ubiquitous presence of small organic compounds such as sugars in the soil environment. Here we probed the effects of glucose molecules on montmorillonite interlayer properties. Molecular dynamics simulations revealed re-structuring of the interlayer organization of the adsorptive species. Water-water interactions were disrupted by glucose-water H-bonding interactions. "Dehydration" of the glucose-populated nanopore led to depletion in the Na solvation shell, which resulted in the accumulation of both Na ions (as inner-sphere complexes) and remaining hydrated water molecules at the mineral surface. This accumulation led to a decrease in both D-Na and D-water. In addition, the reduction in D-glucose as a function of increasing glucose content can be explained by the aggregation of glucose molecules into organic clusters H-bonded to the mineral surface on both walls of the nanopore. Experimental nuclear magnetic resonance and X-ray diffraction data were consistent with the theoretical predictions. Compared to clay interlayers devoid of glucose, increased intensities and new peaks in the Na-23 nuclear magnetic resonance spectra confirmed increasing immobilization of Na as a function of increasing glucose content. And, the X-ray diffraction data indicated a reduced collapse of glucose-populated interlayers exposed to decreasing moisture conditions, which led to the maintenance of hydrated clay nanopores. The coupling of theoretical and experimental findings sheds light on the molecular to nanoscale mechanisms that control the enhanced trapping of water molecules and solutes within sugar-enriched clay nanopores. (C) 2017 Elsevier Ltd. All rights reserved.
机译:了解粘土纳米孔中的流体动力学对于深入了解自然和工程土壤中的水,养分和污染物的捕集至关重要。先前的研究集中在蒙脱石粘土的阳离子饱和的层间纳米孔中的阳离子和水分子的层间组织和分子扩散系数(D)。但是,对于土壤环境中普遍存在的小有机化合物(如糖)如何影响这些层间动力学特性知之甚少。在这里,我们探讨了葡萄糖分子对蒙脱土层间性能的影响。分子动力学模拟揭示了吸附物种的层间组织的重构。葡萄糖-水的氢键相互作用破坏了水-水的相互作用。葡萄糖填充的纳米孔的“脱水”导致Na溶剂化壳的耗竭,这导致Na离子(作为内球络合物)和残留的水化水分子在矿物质表面积累。这种积累导致D-Na和D-水减少。另外,D-葡萄糖的减少是葡萄糖含量增加的函数,这可以通过将葡萄糖分子聚集成H-键合到纳米孔两壁的矿物表面上的有机簇来解释。实验核磁共振和X射线衍射数据与理论预测一致。与不含葡萄糖的粘土夹层相比,Na-23核磁共振波谱的强度增加和出现了新的峰,这证实了Na的固定化随葡萄糖含量的增加而增加。并且,X射线衍射数据表明暴露于降低的水分条件下的葡萄糖填充的中间层的塌缩减少,这导致水合粘土纳米孔的维持。理论和实验结果的结合揭示了分子到纳米尺度的机制,该机制控制了水分子和溶质在富含糖的粘土纳米孔中的增强捕集。 (C)2017 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Advances in Water Resources》 |2017年第8期|24-38|共15页
  • 作者单位

    Cornell Univ, Coll Agr & Life Sci, Dept Biol & Environm Engn, Ithaca, NY 14853 USA|Cornell Univ, Coll Agr & Life Sci, Sch Integrat Plant Sci, Soil & Crop Sci Sect, Ithaca, NY 14853 USA;

    Cornell Univ, Coll Agr & Life Sci, Dept Biol & Environm Engn, Ithaca, NY 14853 USA;

    Cornell Univ, Coll Agr & Life Sci, Sch Integrat Plant Sci, Soil & Crop Sci Sect, Ithaca, NY 14853 USA;

    Cornell Univ, Coll Agr & Life Sci, Dept Biol & Environm Engn, Ithaca, NY 14853 USA;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Soil nanopore; Water diffusion; Smectite clays; Mineral interlayers;

    机译:土壤纳米孔;水扩散;蒙脱土;矿物夹层;

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