Abstract
Mullite solid-solution can be represented by the formula Al4+2xSi2-2xO10-x, Z = 1 where x is the number of oxygen atoms missing per unit cell. The presence of a miscibility gap between sillimanite (x < 0.04) and siliceous mullite (x = 0.17) suggests that their different ordering schemes, deduced from SAED studies, may be the underlying cause, and that the true end-member is aluminum-rich. Supporting evidence lies in the lengthening of the modulation wavelength, interpreted as a systematic coarsening of mullite antiphase domains, with increasing Al content. The concomitant trend toward greater sharpness and complexity of the superstructure reflections defining domain size may be a consequence simply of chemical fluctuations near domain boundaries, but is also very likely to result from the long-range ordering of oxygen vacancies. Mullite cell dimensions vary almost linearly with composition, and when extrapolated beyond those for the most aluminous one found in this study (76 mole percent Al2O3; x = 0.59), fall very close to those of a metastable polymorph of alumina, t-Al2O3. A structure for this mullite end-member is postulated, and a hypothetical phase diagram given for the system Al2SiO5-Al2O3 in the absence of corundum.