NANOMORPHOLOGY OF KAOLINITES - COMPARATIVE SEM AND AFM STUDIES

Nanomorphological structure of well-crystallized Georgia and poorly cr ystallized North Queensland kaolinite particles have been compared usi ng field emission scanning electron microscopy (SEM) and atomic force microscopy (AFM). In general, there is good agreement in information f rom the 2 very different imaging techniques. AFM gives more detailed i nformation on step and ledge dimensions, microvalleys and crystallogra phic orientation of irregularities on basal planes and edges of the cr ystallites. There are major differences in nanomorphology and surface structure between the 2 kaolin samples with the Georgia kaolin showing 200-500-nm, relatively flat basal planes with some cascade-like step growth 50-100 nm wide. The edges, apparently flat and right angled in SEM images, appear beveled in AFM images due to artifacts from the asp ect ratio of the AFM tip. The North Queensland kaolinite has much more complex surface structure with anhedral crystallites attached to larg er particles, high density of steps and nm-scale irregularities (often crystallographically directed).The additional step edge site contribu tion from the attached crystallites is estimated as a minimum of 6%, g iving a total edge contribution above 30% of the kaolinite total surfa ce area. These structures will generate a substantial pH-dependent cha rge across the surfaces of the North Queensland kaolinite platelets. A n idealized, uniform, pH-independent, negatively charged basal plane c annot be assumed from these structures. There is also some evidence, f rom both SEM and AFM images, of curvature in the thinner, poorly order ed structures of the North Queensland kaolinite particles.