The ultra-structure of kaolin
Kaolin samples obtained from a wide range of sources and origins in eastern Australia (ie, Pittong, Lal Lal, Meredith, Vic.; Woodside, SA; Swan Bay, Bexhill, NSW; Weipa, Tarong, Cooyar, Nanango, Pierce's Creek, Mt Morgan, Qld.) were examined using Xray diffraction (XRD), infrared (IR), scanning electron microscopic (SEM) and transmission electron microscopic (TEM) techniques. Kaolinite as the dominant kaolin mineral occurs in most samples of weathered, hydrothermal and secondary...[Show more]
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