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Delamination of kaolinite-potassium acetate intercalates by ball-milling

机译:高岭石-醋酸钾插层球磨脱层

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摘要

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.
机译:通过扫描电子显微镜(SEM),X射线衍射(XRD),比表面积(SSA)和傅里叶变换红外光谱(FT-IR)检查了湿式球磨后插层高岭石的结构变化。室温下的X射线衍射图表明,乙酸钾插入高岭石中导致基础间距从0.718增加到1.42。纳米,并且随着粒度减小。随着球磨机的插入和分层,表面积急剧增加。插入后的湿式球磨高岭石未改变结构顺序,并且根据SEM图像,颗粒具有高的长宽比。

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