Dickite, Al2Si2O5(OH)4, is a kaolin polymorph and, as such, is a 1:1 aluminous dioctahedral phyllosilicate (clay) mineral. It exhibits mica-like layers with silicate sheets of 6-membered rings bonded to aluminum oxide/hydroxcide layers. The crystal structure displayed to the left is based on a Rietveld refinement derived from powder time-of-flight neutron diffraction data.
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As part of the kaolinite clay family, dickite is used in ceramics, as paint filler, rubber, plastics and glossy paper.
Bish, D.L., and C.T. Johnston, 1993. Rietveld Refinement and Fourier-Transform Infrared Spectroscopic Study of the Dickite Structure at Low Temperature. Clays and Clay Minerals. 41:297-304.