Frost RL, Kristof J, Horvath E, Kloprogge JT
Centre for Instrumental and Developmental Chemistry, Queensland University of Technology, 2 George Street, Brisbane, QLD 4001, Australia
J Colloid Interface Sci. 1999 Jun 1;214(1):109-117. doi: 10.1006/jcis.1999.6177.
The modification of kaolinite hydroxyl surfaces of both ordered and disordered kaolinites has been studied under a range of conditions and intercalating agents. This has been achieved by the study of the kaolinite hydroxyl deformation vibrations by the application of diffuse reflectance Fourier transform infrared (DRIFT) spectroscopy. Kaolinites showed resolved bands at 940 and 915 cm-1 with an additional band at 923 cm-1. The bands at 940 and 923 cm-1 are assigned to the hydroxyl deformation modes of the inner surface hydroxyl groups, and the 915 cm-1 band is assigned to that of the inner hydroxyl group. When the kaolinite is intercalated with potassium acetate additional bands were found at 909 and 897 cm-1 for the ordered kaolinites. An additional band at 877 cm-1 is observed for the disordered kaolinite and is attributed to the hydroxyl deformation mode of non-hydrogen-bonded hydroxyl groups. The bands at 909 and 897 cm-1 range are attributed to inner surface hydroxyl groups hydrogen bonded to water or acetate groups. The intensity of these bands reflects the degree of disorder introduced into the kaolinite through intercalation. The intensities of the kaolinite hydroxyl deformation modes are a function of the starting kaolinite order and the method of preparation. Copyright 1999 Academic Press.
在一系列条件和插层剂作用下,对有序和无序高岭土的高岭石羟基表面改性进行了研究。这是通过应用漫反射傅里叶变换红外(DRIFT)光谱研究高岭石羟基变形振动来实现的。高岭土在940和915 cm-1处显示出分辨的谱带,在923 cm-1处还有一条附加谱带。940和923 cm-1处的谱带归属于内表面羟基的羟基变形模式,915 cm-1处的谱带归属于内羟基的变形模式。当高岭土用醋酸钾插层时,有序高岭土在909和897 cm-1处发现了附加谱带。无序高岭土在877 cm-1处观察到一条附加谱带,归因于非氢键合羟基的羟基变形模式。909和897 cm-1范围内的谱带归因于与水或醋酸根基团形成氢键的内表面羟基。这些谱带的强度反映了通过插层引入高岭土的无序程度。高岭石羟基变形模式的强度是起始高岭土有序度和制备方法的函数。版权所有1999年学术出版社。