Mullite is the unique intermediate compound thermodynamically stable in the binary system Al2O3 - SiO2, in the weight range from 70.5 to 74.0% of Al2O3. However mullite metastable in the range from 74 to 83.6% of Al2O3 can be obtained. Due to its excellent physical and mechanical properties at high temperatures such as high melting point, low thermal expansion, good resistance to fracture and to thermal shock, high creep resistance, thermal stability, low density and low dielectric constant, it has become widely used in ceramic bodies. However, the mineral mullite is rare and almost nonexistent in the nature. To better assist to a growing market, synthetic mullites are produced, by mixtures of powders of Al2O3 and SiO2 in molecular scale, by using sol-gel technique, or by the calcination of minerals that contains silica and alumina in their structures, so called alumino silicates. Usually these minerals contain impurities, and as consequence, they produce mullite accompanied by a glassy phase. In this work showed that the topaz is another alternative to obtaining a pure and cheap mullite through the calcination of the topaz Al2SiO4 [Fx(OH)1-x]2 . Colorless topaz and imperial topaz were used for the mullite production. The colorless topaz doesn't have commercial or gemological value, it is quite abundant. For the imperial topaz it was used drosses of its extraction. The yield in the calcination was high, around 80%, and it was obtained at a temperature not very high, around 1300ºC, producing a very pure mullite without glassy phase. The microstructure of the obtained mullite was of needle type (mulitte whiskers) and high porosity. These two features are intrinsic properties that are associated to the topaz decomposition. This study showed that the topaz may be an inexpensive source for obtaining mullite of high quality.
topaz; mullite
