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A&A 460, L9-L12 (2006)
DOI: 10.1051/0004-6361:20066322
Letter
Too little radiation pressure on dust in the winds of oxygen-rich AGB stars
P. WoitkeLeiden University, PO Box 9513, 2300 RA Leiden, The Netherlands
e-mail: woitke@strw.leidenuniv.nl
(Received 30 August 2006 / Accepted 6 October 2006)
Abstract
Aims.It is commonly assumed that the massive winds of AGB stars are
dust-driven and pulsation-enhanced. However, detailed
frequency-dependent dynamical models that can explain the observed
magnitudes of mass loss rates and outflow velocities have been
published so far only for C-stars. This letter reports on first
results of similar models for oxygen-rich AGB stars. The aim is to
provide a better understanding of the wind driving mechanism, the
dust condensation sequence, and the role of pulsations.
Methods.New dynamical models for dust-driven winds of oxygen-rich AGB
stars are presented which include frequency-dependent Monte Carlo
radiative transfer by means of a sparse opacity distribution
technique and a time-dependent treatment of the nucleation, growth
and evaporation of inhomogeneous dust grains composed of a mixture
of Mg2SiO4, SiO2, Al2O3, TiO2, and solid Fe.
Results.The frequency-dependent treatment of radiative transfer reveals
that the gas is cold close to the star (
K at
) which facilitates the nucleation process. The
dust temperatures are strongly material-dependent, with differences
as large as 1000 K for different pure materials, which has an
important influence on the dust formation sequence. Two dust layers
are formed in the dynamical models: almost pure glassy Al2O3
close to the star (
) and the more opaque
Fe-poor Mg-Fe-silicates further out. Solid Fe and Fe-rich silicates
are found to be the only condensates that can efficiently absorb
the stellar light in the near IR. Consequently, they play a
key role in the wind driving mechanism and act as a
thermostat. Only small amounts of Fe can be incorporated into the
grains, because otherwise the grains become too hot. Thus, the
models reveal almost no mass loss, and no dust shells.
Conclusions.The observed dust sequence Al2O3
Fe-poor Mg-Fe-silicates for
oxygen-rich AGB stars having low
high mass loss rates is in
agreement with the presented model and can be understood as
follows: Al2O3 is present in the extended atmosphere of the
star below the wind acceleration region, also without mass loss.
The Mg-Fe-silicates form further out and, therefore, their amount
depends on the mass loss rate. The driving mechanism of oxygen-rich
AGB stars is still an unsolved puzzle.
Key words: hydrodynamics -- radiative transfer -- stars: winds, outflows -- stars: mass-loss -- stars: AGB and post-AGB
© ESO 2006
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