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水悬浮液中 Laponite 的相行为:微观证据的新见解。

Phase Behavior of Aqueous Suspension of Laponite: New Insights with Microscopic Evidence.

机构信息

Department of Chemical Engineering, Indian Institute of Technology , Kanpur 208016, India.

出版信息

Langmuir. 2017 Mar 7;33(9):2370-2377. doi: 10.1021/acs.langmuir.7b00151. Epub 2017 Feb 24.

Abstract

Investigating microstructure of suspensions with particles having anisotropic shape that share complex interactions is a challenging task leading to competing claims. This work investigates phase behavior of one such system: aqueous Laponite suspension, which is highly contested in the literature, using rheological and microscopic tools. Remarkably, we observe that over a broad range of Laponite (1.4 to 4 wt %) and salt concentrations (0 to 7 mM), the system overwhelmingly demonstrates all the rheological characteristics of the sol-gel transition leading to a percolated network. Analysis of the rheological response leads to fractal dimension that primarily depends on the Laponite concentration. We also obtain the activation energy for gelation, which is observed to decrease with increase in Laponite as well as salt concentration. Significantly, the cryo-TEM images of the postgel state clearly show the presence of a percolated network formed by interparticle bonds. The present work therefore conclusively establishes the system to be in an attractive gel state resolving a long-standing debate in the literature.

摘要

研究具有各向异性形状且具有复杂相互作用的颗粒悬浮液的微观结构是一项具有挑战性的任务,这导致了相互竞争的说法。本工作使用流变学和显微镜工具研究了这样一个系统的相行为:水滑石悬浮液,该系统在文献中存在很大争议。值得注意的是,我们观察到,在广泛的水滑石(1.4 至 4 重量%)和盐浓度(0 至 7mM)范围内,该系统压倒性地表现出导致渗透网络的溶胶-凝胶转变的所有流变特性。对流变响应的分析导致分形维数主要取决于水滑石的浓度。我们还获得了凝胶化的活化能,观察到随着水滑石和盐浓度的增加而降低。重要的是,后凝胶状态的 cryo-TEM 图像清楚地显示了由颗粒间键形成的渗透网络的存在。因此,本工作明确地确立了该系统处于有吸引力的凝胶状态,解决了文献中长期存在的争议。

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