A study of the exposure of SiC at 1200 degrees C and high water-vapor press
ures (1.5 atm) has shown SiC recession rates that exceed what is predicted
based on parabolic oxidation at water-vapor pressures of less than or equal
to similar to 1 atm. After exposure to these conditions, distinct silica-s
cale structures are observed; thick, porous, nonprotective cristobalite sca
les form above a thin, dense silica layer. The porous cristobalite thickens
with exposure time, while the thickness of the underlying dense layer rema
ins constant. These observations suggest a moving-boundary phenomenon that
is controlled by the rapid conversion of dense vitreous silica to a porous,
nonprotective crystalline SiO2.