I. Jaymes et al., SI-29 AND AL-27 NMR-STUDY IN THE MULLITE SOLID-SOLUTION AL-2(AL2-2X)O-10-X(2XSI2), Journal de chimie physique et de physico-chimie biologique, 92(10), 1995, pp. 1851-1854
The Si-29 MAS NMR study has shown the existence of four different site
s for Si whatever the composition of mullite. Their population evolve
linearly with the composition in the solid solution. The major site, n
ot reported in precedent studies due to its broad distribution of chem
ical shifts, increases as 2x, x being the number of oxygen vacancies.
It is assigned to all the tetrahedra near an oxygen vacancy. By extrap
olation it is not present in sillimanite (x = 0). Two other sites are
modified silimanite-type sites and decrease as 1x. The (27)AlMAS NMR s
tudy has been carried out at two different magnetic fields (7 and 11.7
T). The spectra have been simulated with quadrupolar bands and show t
hat the Al(IV)/Al(VI) ratio decreases abnormally for alumina-rich mull
ites. The Al-27 NMR is not quantitative. Particularly the most distort
ed tetrahedra, more present in alunina-richer mullites, are only parti
ally seen by NMR.