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Astron. Astrophys. 363, 629-639 (2000) 9. ConclusionsThe ISO/SWS observation of the silicate carbon star V778 Cyg
revealed that there has been little change in the spectral profile of
the silicate features in the last 14 years, since the IRAS/LRS
observation. H2O and CO2 molecules marginally
detected in emission, are probably located in the circumstellar
environment. The near-infrared spectrum indicates that the present-day
mass-loss rate is small. The silicate features can only be fitted by
optically thin emission from small (sub-micron size) dust grains. We
propose that the features arise from the continuous dust outflow from
a companion disk, as dust grains spill out from the gravitational
restriction and are blown away by the radiation pressure from the
central star. We discussed formation of a disk in a binary system
under the strong radiation field from the central star. It turned out
that the orbital separation is a key parameter which determines the
fate of the system. A heavy circum-binary disk is formed when the
system is a close-binary, while a disk around the companion star
results for the wide separation system. V778 Cyg is of the latter
case. Objects such as the Red Rectangle and IRAS 09425-6040
are probably formed by the former mechanism. The primary of
V778 Cyg is likely in the AGB phase. We assume that the
oxygen-rich material was stored during the previous AGB mass-loss
phase, but the conclusion does not change even if the material was
provided in the earlier phase, during RGB or at the He-core flash. The
dust mass in the disk of V778 Cyg is of the order of
© European Southern Observatory (ESO) 2000 Online publication: December 11, 2000 ![]() |