The WD models on which the present results are based have been calculated by means of a detailed evolutionary code developed by us at La Plata Observatory. The code has been employed in previous studies on WD evolution (Althaus et al. 2001a,b) and it has recently been modified to study the evolutionary stages prior to the WD formation (see Althaus et al. 2001c). The constitutive physics include: up-to-date OPAL radiative opacities for different metallicities, conductive opacities, neutrino emission rates, a detailed equation of state and a complete network of thermonuclear reaction rates for hydrogen and helium burning (see Althaus et al. 2001c). For a proper treatment of the diffusively evolving chemical stratification, gravitational settling and the thermal and chemical diffusion of nuclear species have been considered.
The evolutionary stages prior to the WD formation have been fully
taken into account. Specifically, we started our calculations from a 3
star at the zero-age main sequence and we follow its further
evolution all the way from the stage of hydrogen and helium burning in
the core up to the tip of the asymptotic giant branch where helium
thermal pulses occur. After experiencing 11 thermal pulses, the model
is forced to evolve towards its WD configuration by invoking strong
mass loss episodes. As a result, a WD remnant of 0.563
is obtained. The evolution of this remnant is pursued through the
stage of planetary nebulae nucleus to the domain of the ZZ Ceti stars
on the WD cooling branch. An important aspect of these calculations
is related to the evolution of the chemical abundance during the WD
cooling. In particular, the shape of the composition transition zones
is of the utmost importance regarding the pulsational properties of
the ZZ Ceti models. In this respect, diffusion processes cause near
discontinuities in the abundance distribution at the start of the
cooling branch to be considerably smoothed out by the time the ZZ Ceti
domain is reached. This can be appreciated in Fig. 1, which also
illustrates the profile of the hydrogen-helium interface resulting
from the predictions of diffusive equilibrium in the trace element
approximation (thin dotted line). The shape of the innermost carbon
and oxygen distribution emerges from the chemical rehomogenization
process due to the Rayleigh-Taylor instability occurring at early
stages of the WD evolution (see Althaus et al. 2001c and also Salaris
et al. 1997)
. Surrounding the carbon-oxygen interior there is
a shell rich in both carbon (
35%) and helium (
60%), and a overlying layer consisting of nearly pure helium of mass
0.003
.
The presence of carbon in the helium-rich region below
the helium buffer stems from the short-lived convective mixing episode
that has driven the carbon-rich zone upwards during the peak of the
last helium pulse on the asymptotic giant branch. We want to mention
that the total helium content within the star once helium shell
burning is eventually extinguished amounts to 0.014
and that
the mass of hydrogen that is left at the start of the cooling branch
is about
,
which is reduced to
due to the interplay of residual nuclear burning and
element diffusion by the time the ZZ Ceti domain is reached.
Copyright ESO 2001