莫来石
结晶度
高岭石
成核
材料科学
等温过程
衍射
矿物学
化学工程
结晶学
复合材料
化学
冶金
热力学
光学
物理
有机化学
陶瓷
工程类
作者
F. J. Serrano,J. Bastida,José M. Amigó,A. Sanz
标识
DOI:10.1002/crat.2170310818
摘要
Abstract An X‐ray diffraction microstructural study on 110, 220, 001 and 111 peaks has been performed on mullite in the temperature range of primary mullite formation in order to monitor nucleation and growth process. Considering the crystallinity of the starting kaolinites, a greater disorder of the kaolinite has been found to enhance the mullite formation. Isothermal growth is related to a decrease in the Al 2 O 3 content of mullite.
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