An amorphous intergranular layer, 0.4 nm thick, is found by high-resolution
transmission electron microscopy of beta-SiC ceramics fabricated by the HI
P glass-encapsulation technique without the use of additives. The intergran
ular layer is found to contain oxygen, which may also be present in the SIC
grains near the grain boundary. The mean composition of the intergranular
layer is determined to be SiO0.10 (+/-) C-0.01(0.93) (+/- 0.04), whose C/O
ratio is close to a hypothetical Si-oxycarbide stoichiometry. Electron ener
gy loss spectroscopy shows that both the Si-L-23 and O-K edges from the int
ergranular layer are distinctive compared to those of SiC and/or SiO2. This
provides direct evidence of the presence of oxygen in a chemical environme
nt different to that in glassy SiO2, that can also be found in the intergra
nular layer. First principle calculations by the DV-X alpha method using an
interface model cluster, satisfactorily reproduce the chemical shifts of t
he energy loss near edge structure (ELNES) for both the Si-L-23 and O-K edg
es. (C) 1999 Acta Metallurgica Inc. Published by Elsevier Science Ltd. All
rights reserved.