含水饱和度对HDTMA-、HDTMP-和hdpy改性蒙脱土有机粘土层间性质的影响

IF 5.3 2区 地球科学 Q2 CHEMISTRY, PHYSICAL
Molly S. Costanza-Robinson , Emory M. Payne , Elaine Dellinger , Kae Fink , Richard C. Bunt , Malcolm Littlefield , Barbara A. Mejaes , Rachael K. Morris , Lauren N. Pincus , Emma H. Wilcox
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引用次数: 0

摘要

表面活性剂改性的粘土矿物,有机粘土,已经得到了很好的研究,并在商业上用于去除水中的污染物。然而,干有机粘土特性通常用于理解和预测污染物吸附。在这项工作中,研究了水饱和度对污染物吸附的两个重要性质的影响:有机粘土层间空间和表面活性剂烷基尾部构象有序。使用三种表面活性剂:十六烷基三甲铵(HDTMA)、十六烷基吡啶鎓(HDPy)和十六烷基三甲鏻(HDTMP)将蒙脱石改性为0.25–3.0 CEC。在低表面活性剂负载量(<;1CEC和<;15%fOC)下,水饱和度使最大有机粘土夹层膨胀了4–8Å,这取决于表面活性剂及其负载量,但对表面活性剂尾部构象有序性几乎没有影响。在低表面活性剂负载量下,由于夹层的物理约束的放松,相对于基于干燥有机粘土性质的预期,水饱和度可能促进污染物吸附,特别是对于较大的污染物。在较高的表面活性剂负载量下,HDTMA和HDTMP有机粘土表现出相对较小的水饱和度影响,但HDPy有机粘土的影响显著。在20.7%fOC下,HDPy有机粘土的最大层间空间在水合时膨胀了3倍(+22.3Å),这归因于吡啶鎓头基的显著重排。所有具有fOC>;20%的烷基在水合时经历了烷基尾部构象有序性的显著增加,变得完全固体状,即使在最高负载下发生的层间膨胀可以忽略不计。在高HDPy负载下,由于在更像固体的层间相中形成空穴的能量屏障,相对于基于干燥特性的预期,水饱和度可能会限制污染物的吸附。这项工作从三种类型的有机粘土中提供了证据,证明水饱和有机粘土的性质与干燥有机粘土的特性有很大不同。在与污染物吸附相关的水饱和条件下对有机粘土进行表征将有助于我们理解和提高有机粘土的性能。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Influence of water saturation on interlayer properties of HDTMA-, HDTMP-, and HDPy-modified montmorillonite organoclays

Influence of water saturation on interlayer properties of HDTMA-, HDTMP-, and HDPy-modified montmorillonite organoclays

Surfactant-modified clay minerals, organoclays, are well-studied and used commercially for removing contaminants from water. Nevertheless, dry organoclay properties are typically used to understand and predict contaminant sorption. In this work, the effects of water saturation on two properties important to contaminant sorption were examined: organoclay interlayer space and surfactant alkyl tail conformational ordering. Montmorillonite was modified to 0.25–3.0 CEC using three surfactants: hexadecyltrimethylammonium (HDTMA), hexadecylpyridinium (HDPy), and hexadecyltrimethylphosphonium (HDTMP). At low surfactant-loadings (< 1 CEC and < 15% fOC), water saturation expanded the maximum organoclay interlayer by 4–8 Å, depending on the surfactant and its loading but had little effect on surfactant tail conformational ordering. At low surfactant loadings, water saturation likely promotes contaminant sorption relative to expectations based on dry organoclay properties, particularly for larger contaminants, due to a relaxation of the physical constraints of the interlayer. At higher surfactant loadings, HDTMA and HDTMP organoclays showed relatively small effects of water saturation, but effects were significant for HDPy organoclays. The maximum interlayer space of the HDPy organoclay at 20.7% fOC expanded 3-fold (+22.3 Å) upon hydration, which is attributed to a substantial rearrangement of the pyridinium headgroup. All HDPy organoclays with fOC > 20% experienced a notable increase in the alkyl tail conformational ordering upon hydration, becoming fully solid-like, even as negligible interlayer expansion occurred at the highest loadings. At high HDPy-loading water saturation would likely restrict sorption of contaminants relative to what might be expected based on dry properties, due to the energetic barrier of cavity formation in the more solid-like interlayer phase. This work provides evidence from three types of organoclays that water-saturated organoclay properties can differ substantially from those of dry organoclays. Characterization of organoclays under water-saturated conditions that are relevant to contaminant sorption will facilitate our understanding and improvement of organoclay performance.

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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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