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蒙脱土中絮凝体和原纤形成的本质:pH 的作用。

Nature of flocculation and tactoid formation in montmorillonite: the role of pH.

机构信息

Advanced Light Source, Lawrence Berkeley National Laboratory, Berkeley, California 94720, USA.

出版信息

Phys Chem Chem Phys. 2015 Nov 28;17(44):29608-15. doi: 10.1039/c5cp04007h. Epub 2015 Oct 19.

Abstract

The dissolution and swelling properties of montmorillonite at different pH have been studied, using small angle X-ray scattering (SAXS), imaging and osmotic stress methods combined with Monte Carlo simulations. The acidity of montmorillonite dispersions has been varied as well as the counterions to the net negatively charged platelets. At low pH, Na montmorillonite dissolves and among other species Al(3+) is released, hydrated, polymerized and then it replaces the counterions in the clay. This dramatically changes the microstructure of Na montmorillonite, which instead of having fully exfoliated platelets, turns into a structure of aggregated platelets, so-called tactoids. Montmorillonite dispersion still has a significant extra-lamellar swelling among the tactoids due to the presence of very small nanoplatelets.

摘要

已使用小角 X 射线散射 (SAXS)、成像和渗透压方法结合蒙特卡罗模拟研究了不同 pH 值下蒙脱石的溶解和溶胀特性。改变了蒙脱石分散体的酸度以及带净负电荷薄片的抗衡离子。在低 pH 值下,钠蒙脱石溶解,除其他物质外,还释放出 Al(3+),然后它被水合、聚合,然后取代粘土中的抗衡离子。这极大地改变了钠蒙脱石的微观结构,使原本完全剥离的薄片变成了所谓的“片层结构体”的聚集薄片。由于存在非常小的纳米薄片,片层结构体之间的蒙脱石分散体仍然具有显著的额外层间溶胀。

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