Experimental methods to study clay minerals and perspective applications of Fluorohectorite

P. H. Michels-Brito, L. Michels, K. Hunvik, É. C. dos Santos, B. Pacakova, L. Cavalcanti, K. Knudsen, H. Bordallo, O. Fossum
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Abstract

Fluorohectorite is a synthetic 2:1 layer smectite clay where the presence of exchangeable cations located between water molecules in the interlayer space allows for expansion of the crystal lattice. This swelling property is extremely relevant to many applications including water treatment, bioactive molecules intercalation (drug delivery), soil remediation, CO2capture as well as extra-terrestrial environment studies. In the present chapter, the aim is to discuss why Fluorohectorite can be in particular advantageous for many applications where retention of big volumes is an issue. We will also discuss on the main experimental techniques used to study these materials.
粘土矿物的实验研究方法及氟辉石的前景应用
氟立方石是一种合成的2:1层蒙脱石粘土,其中层间空间中位于水分子之间的可交换阳离子的存在允许晶格膨胀。这种膨胀特性与许多应用非常相关,包括水处理、生物活性分子嵌入(药物输送)、土壤修复、二氧化碳捕获以及地外环境研究。在本章中,目的是讨论为什么氟hectorite可以在许多应用中特别有利,其中保留大体积是一个问题。我们还将讨论用于研究这些材料的主要实验技术。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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