A. Seidl et al., EXPERIMENTAL-OBSERVATION AND NUMERICAL-SIMULATION OF WAVE PATTERNS INA CZOCHRALSKI SILICON MELT, Journal of crystal growth, 137(3-4), 1994, pp. 326-334
Azimuthal m-folded (m = 2, 3, 4,...) wave patterns have been observed
in a Czochralski silicon melt by analysis of temperature measurements.
Three-dimensional time dependent simulations of the unsteady melt flo
w in the down-scaled Czochralski configuration were executed and quali
tatively compared with the experimental data. Both experimental and nu
merical results show processing wave patterns. The wave drift directio
n relative to the crucible rotation reveals a transition from co-rotat
ion to counter-rotation with increasing crucible rotation rate. The hi
gher the crucible rotation rate the faster is the phase velocity of th
e wave drift. Slow co-rotating and fast counter-rotating modes were al
so reported by Goldstein et al. [Journal of Fluid Mechanics, 248 (1993
) 583], when investigating rotational Rayleigh-Benard convection in fl
uids of relatively high Prandtl numbers by means of an analytical appr
oach. Moreover, experimental investigations of baroclinic waves in low
-Prandtl number fluids [Fein and Pfeffer, Journal of Fluid Mechanics 7
5 (1976) 81] definitely showed counter-rotation for smaller and co-rot
ation for higher annulus rotation rates. Hence it is suggested that th
e m-folded waves may be due to the mechanism of Kuppers-Lortz instabil
ities, which mainly occur in flow configurations with a dominant verti
cal temperature gradient.