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首页> 外文期刊>Colloids and Surfaces, A. Physicochemical and Engineering Aspects >Structural evolution of salt-free aqueous Laponite dispersions: A study based on low-field NMR relaxometry and rheological investigations
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Structural evolution of salt-free aqueous Laponite dispersions: A study based on low-field NMR relaxometry and rheological investigations

机译:无盐水溶液分散体的结构演变:基于低场NMR弛豫和流变研究的研究

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摘要

The combination of Low-Field NMR relaxometry (LF-NMR) and rheological analyses was used to investigate the kinetics of aging and structural evolution of salt-free aqueous Laponite dispersions with concentrations ranging from 0.33 to 2.00 wt%. The examination of LF-NMR results reveals that the rate of nanoclay delamination increases with increasing Laponite concentration while its degree decreases. Furthermore, the LF-NMR results were interpreted together with rheological results to assess the kinetics of processes occurring on different length scales reflecting on the time evolution of the three-dimensional structure. The structural evolution is described by the definition and comparison of three different characteristic times. The LF-NMR decay time (t(r)) designates the time required for Laponite delamination. The induction time (t(i)) indicates when interparticle edge-face interactions become effective enough for incipient networking. The gelation time (t(g)) corresponds to sufficiently high degree of interparticle connectivity for the development of a macroscopic gel behavior. The comparison of t(i) and t(g), on one hand, and t(r), on the other hand, allows to conclude that for low concentration Laponite dispersions nanoclay delamination is a prerequisite for the formation of the new dispersion structure with a macroscopic gel behavior. Interestingly, the development of the new structure, based on orientation of clay disks into edge-to-face pattern and mutual interparticle attractive interactions, starts when the delamination process is still running.
机译:低场NMR弛豫谱(LF-NMR)和流变分析的组合用于探讨含有无盐水溶液分散体的衰老和结构演化的动力学,其浓度为0.33-2.00wt%。对LF-NMR结果的检查表明,纳米粘土分层的速率随着Laponite浓度的增加而增加,而其程度降低。此外,将LF-NMR结果与流变结果一起解释,以评估在不同长度尺度上发生的过程的动力学,反映在三维结构的时间展现中。结构演变由三种不同特征时间的定义和比较描述。 LF-NMR衰减时间(T(R))指定Laponite分层所需的时间。诱导时间(T(i))表示何时颗粒边缘面部交互对于初始网络足够有效。凝胶化时间(T(g))对应于宏观凝胶行为的开发的足够高度的颗粒连接性。另一方面,T(I)和T(g)的比较允许得出结论,对于低浓度的Laponite分散体,纳米粘土分层是形成新的分散结构的先决条件具有宏观凝胶行为。有趣的是,新结构的发展,基于粘土磁盘的方向进入边缘面对面的模式和相互夹层的互动,当分层过程仍在运行时开始。

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