Abstract
Porous silica was prepared by selective leaching of chlorite and the influence on the porous properties of the product of the acid type and acid concentration, solution temperature and leaching time were investigated. After leaching, only SiO 2 remained, the other components being selectively leached from the sample in the order MgO < Fe 2O 3 < Al 2O 3. The specific surface area of the product obtained by H 2SO 4-leaching was greater than with HNO 3- and HCl-leaching. The highest specific surface area (394 m 2/g) was obtained by leaching the chlorite with 5 N H 2SO 4 at 90 °C for 1.5 h. The pore size distribution of the products showed a maximum at about 5 nm with a pore size much larger than would be expected for selective leaching of the octahedral chlorite sheets. The 29Si MAS NMR spectra of the products showed a stronger Q 4 peak (related to a framework structure unit) than the Q 3 peak (from a layer structure unit), suggesting the presence of a framework structure similar to silica gel rather than the original layered structure. The resultant structure of the silica product results in a lower specific surface area than found in leached vermiculite and phlogopite.
Published Version
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