School of Geoscience and Surveying Engineering, China University of Mining & Technology, Beijing 100083, China.
J Colloid Interface Sci. 2010 Aug 15;348(2):355-9. doi: 10.1016/j.jcis.2010.05.006. Epub 2010 May 6.
Structural changes in intercalated kaolinite after wet ball-milling were examined by scanning electron microscopy (SEM), X-ray diffraction (XRD), specific surface area (SSA) and Fourier transform infrared spectroscopy (FT-IR). The X-ray diffraction pattern at room temperature indicated that the intercalation of potassium acetate into kaolinite caused an increase of the basal spacing from 0.718 to 1.42 nm, and with the particle size reduction. The surface area increased sharply with the intercalation and delamination by ball-milling. The wet ball-milling kaolinite after intercalation did not change the structural order, and the particulates have high aspect ratio according SEM images.
采用扫描电子显微镜(SEM)、X 射线衍射(XRD)、比表面积(SSA)和傅里叶变换红外光谱(FT-IR)研究了插层高岭石经湿磨后的结构变化。室温下的 X 射线衍射图谱表明,乙酸钾插层进入高岭石后,层间距从 0.718nm 增加到 1.42nm,同时颗粒粒径减小。通过球磨的插层和剥离作用,比表面积急剧增加。插层后的湿磨高岭石并未改变其结构有序性,SEM 图像显示颗粒具有高纵横比。