H. Bjorklund et Lkl. Falk, BETA-SI3N4 GRAIN-GROWTH .2. INTERGRANULAR GLASS CHEMISTRY, Journal of the European Ceramic Society, 17(11), 1997, pp. 1301-1308
The intergranular chemistry and the substitution level of the beta'-gr
ains in a Si3N4 ceramic fabricated with 9.5 mol% Al2O3 and Y2O3 have b
een characterised by high resolution analytical transmission electron
microscopy. The Y2O3/Al2O3 molar ratio of the starting powder mixture
corresponded to that of the Y,Al-garnet (5Al(2)O(3) . 3Y(2)O(3)). Al a
nd O were incorporated into the Si3N4 structure during densification a
nd a dilute beta'-Si3N4 formed. Al concentration gradients were not ob
served in the beta'-grains, although the Al substitution level varied
within and between beta'-grains (0.16 less than or equal to less than
or equal to less than or equal to 0.24). The consequently reduced Al c
ontent of the oxynitride liquid phase sintering medium resulted in a l
imited formation of N-alpha-wollastonite (Y2SiAlO5N) during cooling fr
om the densification temperature. Y and Al were not homogenously distr
ibuted in the residual glass pockets; an enrichment close to the beta-
Si3N4 grains could be observed. Both Y and Al were observed also in th
e glassy films between adjacent beta'-grains. Growth ledges on {10 (1)
over bar 0} facets of beta'-grains facing curved grain boundaries res
ulted in a variation of the intergranular film thickness. These featur
es are consistent with grain growth by coalescence. (C) 1997 Elsevier
Science Limited.