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Astron. Astrophys. 321, 485-491 (1997)
4. Results
Fig. 2 shows the results for ,
. At a time we assume
number fractions C/He=N/He/=O/He=Ne/He= for all
heavy elements. The lower boundary condition is such that the
compositition remains constant there, so that for long times the
abundance distribution should converge to the stationary case, for
which we predicted an atmosphere dominated by heavy elements with
traces of helium only (see Fig. 4a in Paper I). After 10000 y the
atmosphere is still far from a stationarity as can be seen from
Fig. 2a. This time is comparable to the time scales of stellar
evolution of post-AGB stars in the corresponding region of the HRD
(according the evolutionary track in Fig. 1d of Wood &
Faulkner, 1986, for ). Thus it becomes clear
immediately that the transformation of a helium-rich into a metal-rich
atmosphere is not possible in times which are short in comparison to
the time scales of stellar evolution. The number fraction of carbon is
still below everywhere in the atmosphere.
However, the number fraction of oxygen in the outer regions near
is 0.05, which is only slightly lower than the
typical oxygen abundance of PG 1159 stars. Although the influence of
stellar evolution cannot be neglected for longer times, for this
example we proceed with the calculations until the atmosphere is
transformed into a metal-rich one. After 50000 y maximal number
fractions of oxygen and neon of 0.2 and 0.3, respectively, are
obtained in a region with (Fig. 2a). After
200000 y (Fig. 2c) neon becomes more abundant than helium near
. The carbon number fraction has a maximum value
of 0.23 at (the temperature there is 380000 K).
Only in this part of the atmosphere where the state of ionization
changes from to a carbon
enrichment by radiative forces is possible. It takes longer than
200000 y until a carbon abundance typical for PG 1159 stars is
possible. After this time, however, the star should already have
cooled down to effective temperatures below 100000 K. Therefore it
seems to be impossible to explain the observed number ratios of carbon
by diffusion, at least if we start from approximately solar number
fractions. After 800000 y (Fig. 2c) we expect a thin metal-rich
region of about floating ontop of the
helium-rich mantle. A comparison with Fig. 4a of Paper I shows
that stationary conditions are still not possible. Only in the outer
regions with the number fractions of carbon,
oxygen and neon are close to their stationary value. The nitrogen
abundance has a sharp minimum near . The rapidly
increasing radiative forces lead to an increasing diffusion flow of
nitrogen in outward direction, which in turn leads to a depletion of
the region between the two abundance maxima. At
nitrogen diffuses still outwards with a high diffusion velocity of
m/s. The diffusion velocities of the elements
C, O and Ne are lower by about four orders of magnitude. The number
fraction of helium is still much larger than predicted for the
stationary cases. It still diffuses inwards with a diffusion velocity
of about m/s.
![[FIGURE]](img75.gif) |
Fig. 2a-d. Number fractions of the elements He (full drawn line), C (- - - -), N (- - -), O (- - - -), Ne (- - -) as a function of the gas pressure for , after various times. The number fractions are on a logarithmic scale and are defined as the ratio of all particles of an element to all heavy particles. The gas pressure is in SI-units! The three tick marks in the upper part of each figure show where the Rosseland mean optical depth is , respectively.
|
Fig. 3 shows the results for ,
, again with C/He=N/He=O/He=Ne/He=
at time . After 100 y
(Fig. 3a) the atmosphere is still helium-rich. After 500 y
(Fig. 3b) carbon and neon are more abundant than helium near
and smaller optical depths. According to the
evolutionary track of a 0.89 post-AGB remnant
of Wood & Faulkner (1986) this time is in the same order of
magnitude similar as the time scales of stellar evolution. So we see
that a transformation from a helium-rich into a metal-rich atmosphere
is indeed possible in this case, at least if there is no mass-loss.
After 1000 y (Fig. 3b) the helium number fraction in the
photosphere has dropped below 0.1 and carbon and neon are the most
abundant elements. A comparison with Fig. 7a of Paper I shows
that the atmosphere is still far away from a diffusive equilibrium
state. Here again time-independent calculations are inadequate.
In Figs. 4 and 5 we take number ratios typical for PG 1159 stars at
time : C/He=0.5 and O/He=0.1. Furthermore is
assumed N/He= and Ne/He=
. Two cases are considered, both with gravities
: (Fig. 4) and
(Fig. 5). In Paper I surface abundances of
carbon and oxygen were predicted which are clearly lower than the
observed ones. Therefore it is an interesting question if these
discrepancies are simply due to long diffusion time scales or not. A
look at Figs. 4 and 5 reveals that in both cases carbon as well as
oxygen should sink in time scales which are clearly short compared to
these of stellar evolution.
For , carbon is significantly depleted already
after 100 y in the outermost regions near . Its
number fraction has decreased by about a factor of three. After 1000 y
(Fig. 4b) carbon is a trace element in regions with
. At all number fractions
are already very close to the values which have been predicted in
Paper I for the stationary case. The calculations have been continued
until (Fig. 4c). It is remakable that the
depletion of carbon goes on only slowly. This is due to the radiative
forces acting in regions where carbon is mainly
. In depths with almost
the original abundance is maintained. The carbon-depleted region
comprises a surface layer mass of not more than
. The number fraction of oxygen has a maximum
value of 0.10 near (the temperature there is
). Therefore in this region it has slightly
increased in time (original number fraction at t =0: 0.062),
which is also due to the effective radiative forces in regions where
oxygen has hydrogen-like configuration.
For the depletion of carbon and oxygen
proceeds still more quickly. After 100 y (Fig. 5a), all number
fractions in the photosphere near are below
, after 1000 y (Fig. 5b) they have reached
their value which has been predicted for the stationary case. The
dramatic decrease of the neon abundance in the outermost regions is
not realistic. This is because we have entirely neglected the
radiative forces for and states of lower
ionization. In Paper I the contribution of the bound-bound transitions
of has been taken into account, therefore the
predictions there are more accurate for this case. After
a strong depletion of heavy elements is
predicted in the outer region, which comprises a surface layer mass of
about (at ). For
comparison, Dreizler et al. (1994) obtain from the model atmosphere
analysis of HS 0704+6153 number ratios C/He = 0.2, O/He
0.05. Also in the inner regions carbon and
oxygen tend to sink. Only near the oxygen
abundance is still the original one (more exactly: it has increased by
). The temperature in this depth is
.
© European Southern Observatory (ESO) 1997
Online publication: June 30, 1998
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