Mullite contained in a silicoaluminous fly ash (originating from power plan
t of La Mere, near Metz in the east of France) issue from bituminous coal c
ombustion has been studied by X-ray diffraction, nuclear magnetic resonance
of Si-29 spinning at magic angle, and transmission electron microscopy lin
ked with energy-dispersive spectroscopy. By using results from X-ray diffra
ction [1] and nuclear magnetic resonance spectroscopy [2], an average value
of 0.35 for x, the oxygen holes rate in mullite Al4+2xSi2-2xO10-x, could b
e determined. Thus, Al2O3 content is only slightly higher than those corres
ponding to the classical formula (Al2O3)(3).(SiO2)(2). It is shown also tha
t the composition is heterogeneous and depends on the crystallites; Ti and
Fe are impurities substituting for Al in the structure. The average chemica
l formula of the mullite determined here is Al4.61Fe0.05Ti0.02O9.65. (C) 20
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