Department of Metallurgical Engineering, College of Mines and Earth Sciences, University of Utah, 135 South 1460 East, Room 412, Salt Lake City, UT 84112, USA.
J Colloid Interface Sci. 2010 Dec 1;352(1):75-80. doi: 10.1016/j.jcis.2010.08.002. Epub 2010 Aug 9.
The crystal lattice images of the two faces of kaolinite (the silica face and the alumina face) have been obtained using contact-mode atomic force microscopy (AFM) under ambient conditions. Lattice resolution images reveal the hexagonal surface lattice of these two faces of kaolinite. Analysis of the silica face of kaolinite showed that the hexagonal surface lattice ring of oxygen atoms had a periodicity of 0.50±0.04nm between neighboring oxygen atoms, which is in good agreement with the surface lattice structure of the mica basal plane. The center of the hexagonal ring of oxygen atoms is vacant. Analysis of the alumina face of kaolinite showed that the hexagonal surface lattice ring of hydroxyls surround a hydroxyl in the center of the ring. The atomic spacing between neighboring hydroxyls was determined as 0.36±0.04nm. Ordering of the kaolinite particles for examination of the silica and alumina surfaces was accomplished using different substrates, a procedure previously established. Crystal lattice imaging supports previous results and independently confirms that the two faces of kaolinite have been properly identified.
使用环境条件下的接触模式原子力显微镜(AFM)获得了高岭石(硅面和铝面)两面的晶格图像。晶格分辨率图像揭示了这两种高岭石表面的六边形晶格。对高岭石硅面的分析表明,相邻氧原子之间的氧原子六边形表面晶格环的周期性为 0.50±0.04nm,与云母基面的表面晶格结构非常吻合。氧原子六边形环的中心是空位。对高岭石铝面的分析表明,羟基的六边形表面晶格环围绕着环中心的一个羟基。相邻羟基之间的原子间距确定为 0.36±0.04nm。为了检查硅面和铝面,使用了不同的基底来对高岭石颗粒进行有序排列,这是之前已经建立的程序。晶格成像支持了先前的结果,并独立证实了高岭石两面已经被正确识别。