A&A 466, 1043-1051 (2007)
DOI: 10.1051/0004-6361:20067023
P. G. Prada Moroni1,2 - O. Straniero3
1 - Dipartimento di Fisica "E. Fermi'', University of Pisa,
largo B. Pontecorvo 3, 56127 Pisa, Italy
2 -
INFN, largo B. Pontecorvo 3, 56127 Pisa, Italy
3 -
INAF - Osservatorio Astronomico di Collurania, via Maggini, 64100 Teramo, Italy
Received 23 December 2006 / Accepted 29 January 2007
Abstract
Context. Given the importance of white dwarfs (WDs) in many fields of modern astrophysics, the precise knowledge of the actual degree of accuracy of the associated theoretical predictions is a primary task. In the first paper of a series dedicated to the modeling of WD structure and evolution we discussed the limits of the available theoretical studies of cooling sequences.
Aims. In the present work we extend this analysis to isochrones and luminosity functions of WDs belonging to old stellar systems, like globular or old disk clusters. The discussion is focused on the most common DA, those with a CO core and an H-rich envelope.
Methods. We discuss, in particular, the variation of the age derived from the observed WD sequence caused by different assumptions about the conductive opacity as well as that induced by changing the carbon abundance in the core.
Results. The former causes a global uncertainty of the order of 10% and the latter of about 5%. We discuss different choices of the initial-to-final mass relation, which induces an uncertainty of 8% on the GC age estimate.
Key words: stars: white dwarfs - stars: luminosity function, mass function - stars: evolution
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Figure 1:
WD isochrones for ages in the interval 8-14 Gyr in the
theoretical plane, i.e.
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Here we are interested in the use of WDs as cosmic chronometers (Schmidt 1959)
and standard candles (Fusi Pecci & Renzini 1979).
Due to the intrinsic faintness of WD sequences in stellar clusters,
only very recently have these tools become useful.
Their application to the nearest globular clusters (GCs)
provides age and distance estimates that are independent of those
obtained by means of the
classical methods (those based on the main sequence and horizontal branch stars),
thus allowing us to further constrain the lower
limit of the Universe's age (Hansen et al. 2002;
De Marchi et al. 2004).
One should, however, check the reliability of the
theoretical cooling time predictions before adopting WDs as cosmic clocks.
Notwithstanding the significant advances in the computation of
the WD structure and evolution, there is still a
sizeable uncertainty in the prediction of the cooling times
of the old WDs (Montgomery et al. 1999; Salaris et al. 2000;
Fontaine et al. 2001; Paper I).
At low luminosity (
)
the differences among the most recent models available in the literature
reach about 4 Gyr (see e.g. Fig. 1 in Paper I).
In Paper I we analyzed some of the main
sources of uncertainty in the evolution of a 0.6
C-O WD. In particular,
we discussed uncertainties due to both the WD progenitor history and the
adopted input physics.
The evolution of a WD can be roughly described as a cooling process where the luminosity is supplied by the heat content of the internal matter; thermonuclear energy generation is negligible, except during the very early phase. Thus, the evolution results from the balance between the thermal energy stored in the C-O ions constituting the core (about 98% of the WD mass) and the energy transport through the He-rich mantel and the H-rich envelope, the most opaque region of the star.
In Paper I, we showed that the factors that most severely limit the accuracy
of theoretical predictions are the assumed conductive opacity in the partially
degenerate regime, a condition that is usually fulfilled in the outer layer of the
core and in the He-rich mantel, and the amount of carbon and oxygen in the core.
At
,
these two sources produce a
total uncertainty on the predicted cooling age of about 27%.
However, the analysis reported in Paper I gives only a rough idea
of the uncertainty in dating GCs
with WDs, while a more precise estimate of this uncertainty
should be based on WD luminosity functions instead of tracks of given mass,
since this is the best WD chronometer.
For this work we have calculated several grids of models of C-O WDs with a
hydrogen rich atmosphere, with mass in the range 0.5-0.9
,
under
different assumptions of the conductive opacity and the C-O profile.
The related isochrones and luminosity functions
(LFs) are compared to reveal the main uncertainty factors.
For old stellar systems, such as GCs, the best chronometer relying
on WD evolution is their luminosity function
instead of the related isochrones.
Figure 1 shows WD isochrones for ages in the interval 8-14 Gyr
in the theoretical plane (
vs.
,
panel a)
and in three CM diagrams for different HST/ACS pass-bands, F336W (broad U),
F439W (broad B), F606W (broad V) and F814W (broad I).
In the theoretical plane (panel a), there is a clear and unambiguous
age dependent feature: the blue-turn of the WD isochrone, which plays
the same role of clock pointer as the turn-off point in the main sequence
phase. The luminosity of the blue-turn depends only on the evolutionary
time scales, both of the WDs and of their progenitors.
On the other hand, on the observational CM diagram, the situation is less
clear, in fact the morphology of the old (>10 Gyr) WD isochrones
significantly depends on the adopted pass-bands, particularly the luminosity
of the blue-turn. In the V(606) vs. V(606)-I(814) diagram,
commonly used in observations of cool WDs, the blue-turn is almost
insensitive to the age for isochrones older than about 10 Gyr.
This behavior is a consequence of the strong depletion of the IR flux
in the emerging spectrum of cool (
K) DA WDs due to the
collision induced absorption (CIA) of H2-H2
(see e.g. Bergeron et al. 1995).
Since the latter blue shift is
an atmospheric effect that reflects the departure of
the emergent spectrum from the black body appearance, its extension
depends sensitively on the wavelength of the transmission curves of the
filter adopted in the observations. The blue shift will be much larger
in the V-I color than in the B-V, because the CIA is the main opacity
source in the IR region of the spectrum. Such an occurrence explains why
in the V vs. V-I plane the blue-hook luminosity of old WD
isochrones is essentially insensitive to the age and the blue-tail of the 14 Gyr
WD isochrone is brighter than the 12 Gyr one.
The degeneracy of the position of the blue-turn with age and the
necessity to accurately model the CIA opacity sources in the
WD model atmospheres severely reduce the effectiveness of the WD isochrones
in dating old stellar systems such as galactic GCs.
A much firmer estimate relies on star counts, i.e. luminosity functions,
which directly reflect the evolutionary time scales.
Figure 2 shows the WD LFs for 12, 13, 14 Gyr. These and the following WD LFs have been computed with Monte Carlo simulations that distribute 50 000 WDs along the related isochrones. This figure clearly illustrates the potential of WD LFs in dating old stellar systems. Note that the peak of the luminosity function shifts by about 0.3 mag per Gyr in the V band, while the main sequence turn-off luminosity, the clock classically used to date stellar clusters, shifts only by about 0.1 mag. This implies that the WD age estimate is significantly less affected by the uncertainty on the distance modulus, which represents the main source of error in dating GCs with the method based on the turn off luminosity. Let us briefly recall the main WD evolutionary phases in order to explain the principal features in the WD isochrones and LFs. The evolution of WDs is initially characterized by a rapid drop of the luminosity and of the central temperature. The main energy loss characterizing this initial phase is the emission of neutrinos. The corresponding zone of the isochrone closely follows the track of a WD of fixed mass. Then, as a WD cools, the Coulomb interaction between ions becomes progressively greater and leads to the crystallization of carbon and eventually oxygen (Abrikosov 1960; Kirzhnits 1960; Salpeter 1961). Due to the latent heat released by the liquid-solid transition, the cooling rate slows temporarily (D'Antona & Mazzitelli 1990; Fontaine et al. 2001). At the same time, the external convective zone penetrates the region where thermal conduction by degenerate electrons is very efficient. Such an occurrence (known as convective coupling), initially produces a further slowing down of the cooling timescale (see e.g. Chabrier et al. 2000; Fontaine et al. 2001). The steep increase in the WD luminosity function is the effect of such a decrease in the cooling rate. Finally, the WD enters the Debye regime, where the heat capacity decreases as T3, thus depleting the WD of its main energy reservoir. As a consequence its luminosity quickly drops.
The morphology of the luminosity function reflects the variations of the cooling timescale: the LF is generally sparse at the brightest magnitudes and presents a steep rise, followed by a sharp cutoff, in the faintest part (see e.g. Fontaine et al. 2001).
The best way to date stellar systems through WDs is the analysis of their LF.
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Figure 2:
Theoretical LFs for 12 (solid line),
13 (dashed line) and 14 Gyr
(long-dashed line). Each magnitude bin is
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The present WD theoretical tracks have been computed with the FRANEC (Chieffi & Straniero 1989), a full evolutionary code that adopts the Henyey method and that is able to model the whole evolution of stars from the hydrostatic pre-main sequence phase up to the WD stage.
To provide the starting model for the WD evolution, we started from the ZAHB (Zero Age Horizontal Branch) model. The first model consists of a helium core (99% of the total mass) and a thin hydrogen rich envelope (Y=0.24 Z=10-4). Then, we followed the evolution at constant mass, through the core He-burning. Due to the reduced envelope, at the central helium exhaustion the model rapidly moves towards the blue region of the HR diagram. During this transition the He- and the H-burning shells are eventually active. As discussed in Paper I, the model settles on the cooling sequence when the masses of both the He-rich and the H-rich layers are reduced to certain critical values and the thermonuclear burning dies down.
We are aware that in the real world a
DA C-O WD of a given mass can be formed through several different evolutionary paths,
depending on the mass loss rate and on the initial chemical
composition. This was
one of the main points discussed in Paper I, where we studied three extreme cases,
and we showed that the internal structure of the resulting WD
is poorly affected by the different evolutionary histories
(see e.g. Figs. 2 and 3 of Paper I). Moreover, the computation of the
evolution through the thermally pulsing asymptotic giant branch (TP-AGB),
although more realistic, is very time consuming.
Thus, the method we have adopted represents a useful way to provide realistic
WD starting models consistent with the evolution of the progenitors.
In particular the chemical abundance profiles of carbon and oxygen in the core
is largely independent of the evolutionary history.
Obviously, the computation through the TP-AGB evolution should be
preferred if the initial, hot phase of WD evolution is analyzed. In
such an early phase of the cooling the outer layers still bear the
record of the complex chemical abundance profile left by TP-AGB evolution,
which is subsequently modified by diffusion.
The metallicity of the progenitors determines the maximum value of the
envelope mass, but this quantity does not significantly affect the cooling timescale
(see Paper I).
The only important quantity
is the relation between the progenitor mass and the WD mass (initial-to-final mass relation)
which is needed to correctly evaluate the time spent before the cooling sequence and,
in turn, correctly locate a WD with a certain mass
on the HR diagram (see Sect. 2.3).
We stop the progenitor evolution when the newly formed WD reaches
log
0. At this point, the helium and
hydrogen in the envelope are fully sorted, in order
to reproduce the observed chemical stratification
of the atmospheres of DA WDs. Several studies have indeed shown
that in such a compact stars, where the surface gravity g is of the order of
108-109 cm s-2, the gravitational settling is efficient
enough to account for the monoelemental feature of
WD spectra (Fontaine & Michaud 1979; Muchmore 1984;
Paquette et al. 1986).
The model obtained with this method is our starting point for the computation of the
cooling sequence.
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Figure 3: Initial-to-final mass relationship for the four labeled metallicities from our stellar models. See text for details. |
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Let us recall the major features of the present models; for a detailed description see Paper I. We put considerable effort into updating the main input physics, namely the equation of state (EOS) for a high-density plasma, the radiative and conductive opacity and the model atmospheres. We updated and extended the EOS for a fully ionized plasma originally described by Straniero (1988). In particular, we have adopted the most recent results for the electrostatic corrections both in the liquid and in the solid phase (see Paper I for references). Concerning the Rosseland radiative opacity, we adopted the OPAL (Iglesias & Rogers 1996) for high temperature (log T [K] > 4.0) and the Alexander & Ferguson (1994) molecular opacities for the low temperatures (log T [K] < 4.0).
As we have shown in Paper I, for the cooling evolution of old WDs, the treatment of electron conduction in the partially degenerate regimes typical of the outer layers is complex. We have computed sets of theoretical cooling sequences and the related isochrones adopting the conductive opacity by Hubbard & Lampe (1969, hereafter HL69), by Itoh and coworkers (Itoh et al. 1983; Mitake et al. 1984; and Itoh et al. 1993, hereafter I93), Potekhin (1999, hereafter P99; see also Potekhin et al. 1999), and combinations. The description of the different assumptions and the related effects on the cooling sequences of WDs is given in Sect. 5.
The computations of reliable cooling models rely on the choice of
appropriate boundary conditions, namely the pressure at the base
of the photosphere. As shown by Fontaine et al. (1974)
and then confirmed by successive studies
(see e.g. Tassoul et al. 1990; Hansen 1999)
it is important to use a detailed model atmosphere
to fix the surface boundary conditions.
It is well known that one of the most important events in the
evolution of old WDs, the coupling between the outer convective envelope
and the isothermal degenerate core (see e.g.Chabrier et al. 2000;
Fontaine et al. 2001) is quite sensitive to the details of
atmosphere stratification, in particular a gray approximation overestimate
the inward penetration of the convection. The quoted coupling initially produces
a sizeable slow down in the cooling evolution followed by a rapid drop in the
luminosity. Since the occurrence of the convective coupling, the core,
which is essentially the energy reservoir of the star, and the atmosphere, where
the energy is radiated in space, are directly coupled.
The pressure at the outer boundary, namely the layer where the optical
depth
,
has
been obtained by interpolating on a grid of model atmospheres (Bergeron 2001)
which cover a range of surface gravities between
107.5-109 cm/s2 and effective temperatures between 1500-100 000 K.
A detailed
treatment of the atmospheric structure is fundamental also for the prediction
of the observable properties, the emergent spectrum and the photometric colors.
As shown by Bergeron et al. (1995),
when a WD with a pure hydrogen atmosphere cools down to
K and
the molecular recombination begins, the collisionally induced absorption
(CIA) of H2-H2 progressively becomes the most important opacity source
for the out-flowing infrared photons, so that the emergent spectrum departs from the blackbody
appearance and the colors are blue shifted (see e.g. also Hansen 1999).
The present models take into account the liquid-solid phase transition and the related energy release (see e.g. Paper I) but neglect the effect of the phase separation during the crystallization of the core, i.e. the chemical redistribution of carbon and oxygen due to the shape of the phase diagram for this binary mixture (Stevenson 1980). We are interested in an evaluation of the relative effects on WD evolution of different physical aspects rather than to provide a reference standard model. Since the effect on WD evolution of chemical fragmentation has been already discussed several times in literature (see e.g. Segretain et al. 1994; Salaris et al. 1997; Montgomery et al. 1999; Isern et al. 1997, 2000) we do not further investigate this issue.
In order to compute isochrones, the age of the progenitor at the entrance of the cooling sequence must be added to the cooling time. This quantity depends on the mass and the chemical composition of the progenitor. The relationship between the main sequence mass and the final WD mass is still uncertain; it is sensitive to many poorly known phenomena, like the extention of the H-burning convective core, which affects the stellar lifetime, and the efficiency of the mass loss mechanism, particularly during the TP-AGB phase when the star loses the greatest fraction of its mass, which affects the final mass.
Semiempirical initial-to-final mass relations are only available for the
chemical composition of the solar neighborhood and for the Magellanic Clouds
(see e.g. Weidemann & Koester 1983; Weidemann 1987,
2000; Herwig 1997).
For the typical composition of the halo, the long distance and the large age
limits a direct determination of the initial-to-final mass relation.
Thus, in spite of the great uncertainty, we are forced to use theoretical
relations.
Figure 3 shows the initial-to-final mass relationship
from the homogeneous set of stellar models of low and intermediate mass stars
computed by Straniero et al. (1997) and Dominguez et al. (1999),
with the same stellar evolutionary code used to provide the present
set of WD models. The mass loss during the AGB phase has been obtained by
best fitting the period-mass loss diagrams obtained by Whitelock et al. (2003).
In stars with initial mass lower than 3
,
an additional pre-AGB mass loss
has been considered based on the Reimers formula with the parameter
.
Table 1 reports the initial-to-final mass relations
shown in Fig. 3.
Table 1:
Initial-to-final mass relationship for the four labeled
metallicities from our stellar models. See text for
details. Masses are in
.
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Figure 4: Theoretical LFs for 12 (thin lines) and 14 Gyr (thick lines) for WDs with low (solid lines) and high (dashed lines) C abundance. |
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The chemical abundance profiles in the core of a C-O WD are the result of
the helium burning that occurred in the core and in the shell of the
progenitor star.
As is well known, initially the 3
reaction produces carbon and
afterwards the 12C
O synthesizes oxygen.
The final chemical stratification in the core of a WD
depends on the relative efficiency
of these two reactions. In particular, the reaction rate of the
12C
O at an energy relevant for the stellar He-burning
(about 300 KeV) is only known within a factor of 2 (see e.g. Buchman
1996; Kunz et al. 2002). The treatment of the convective
mixing during the core He-burning phase also affects the predicted C/O ratio
(see Imbriani et al. 2001; Straniero et al. 2003).
In Paper I we analyzed the changes of the cooling timescale
of a 0.6
CO WD caused by the variation of
the 12C
O reaction rate, within the present
error bars, and by different prescriptions for the core convection.
In this section we extend that analysis to masses from 0.5 to 0.9
and calculate the corresponding isochrones and LFs.
Then, two sets of WD cooling tracks were obtained
for two different C-O chemical
stratifications in the core, the low carbon abundance model with a central carbon mass
fraction of about 0.2 and the high ones with 0.50, a range that
roughly represents the present
uncertainty in the theoretical prediction. The
former value appears in better agreement with the abundance derived from the
power spectra of variable WDs (Metcalfe et al. 2001),
although the feasibility of this kind of measurement has been questioned
(Fontaine & Brassard 2002).
Figure 4 shows the 12 (thin lines) and 14 Gyr (thick lines) LFs for WDs with low (solid lines) and high (dashed lines) C abundance. As expected, due to the lower heat capacity of the carbon-poor material, the cooling time is shorter in these models than the cooling time of the carbon-rich models. As a consequence, the WD LF peak occurs at lower luminosity. The effect of the present uncertainty on the chemical profile in the core is sizeable.
Taking into account that the position of
the WD LF peak is a very sensitive function of the age (
Age
0.3 mag/Gyr for GCs ages), the poor determination of the C abundance
in the core translates directly into an uncertainty of about 0.6 Gyr in the inferred
GC age.
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Figure 5:
Theoretical LFs for 12 (thin lines) and 14 Gyr (thick
lines) for WD models computed adopting the conductive opacity
of Itoh and coworkers (I93) in the fully degenerate regime (
|
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The electrons in the core of a WD are fully degenerate. In these conditions the energy transfer is largely dominated by electron conduction whose efficiency is high enough to keep the core almost isothermal. On the contrary, in the mantel (He-rich) and in the envelope (H-rich) the electrons are only partially or not degenerate, so that thermal conduction is less efficient. In bright WDs, the thin envelope is the most opaque region of the WD, a kind of insulating layer which regulates the temperature decrease of the core. The progressive development of the external convection penetrating the partially degenerate region in cool WDs causes the already mentioned convective coupling. Therefore, it is of primary importance for the description of the cooling process to understand the detailed treatment of the energy transport through the external layers (see e.g. D'Antona & Mazzitelli 1990; Fontaine et al. 2001).
In our knowledge, there are only two published conductive opacities suitable
for partially degenerate regimes, the pioneering study by Hubbard & Lampe
(1969, hereafter HL69) and Potekhin (1999,
hereafter P99; see also Potekhin et al. 1999)
.
Regarding the fully degenerate regime, in addition to the just mentioned works,
there are also the fundamental contributions by Itoh and coworkers (Itoh et al.
1983; Mitake et al. 1984; and Itoh et al. 1993,
hereafter I93).
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Figure 6:
Theoretical LFs for 12 (thin lines) and 14 Gyr
(thick lines) for WD models computed adopting the conductive opacity
of Potekhin (P99) and HL69 in the regions where, respectively,
|
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As discussed in detail in Paper I, the HL69,
although nominally valid, should not be adopted in regions with a high Coulomb
coupling parameter (
,
where
and a is the interionic distance) due to an outdated treatment of the
liquid-solid transition. On the other hand, the I93 computations are
strictly valid only in the completely
degenerate regimes (
,
where
is the electronic Fermi
temperature), in fact they underestimate the
contribution of the electron-electron interactions which is not negligible
in the partially degenerate regimes. The only conductive opacity computations
suitable for the whole WD structure and evolution are those by P99.
In Paper I we showed the dramatic effect on the evolution of a 0.6
WD
of different assumptions for the conductive opacity in the thin envelope.
At log
the adoption of the I93 in the whole WD structure
leads to an age 17% younger than that obtained by using HL69 in the
partially degenerate regime.
In this section we extended
that analysis to evaluate the effect on the WD isochrones and
LFs of different assumptions on the conductive opacity.
We have computed five sets of cooling tracks with masses in the range 0.5-0.9
and the related set of isochrones and LFs.
Figure 5 shows the theoretical LFs for 12 (thin lines)
and 14 Gyr (thick lines) for WD models computed adopting the conductive opacity
of Itoh and coworkers (I93) in the fully degenerate regime (
)
and
Hubbard & Lampe (HL69) in the partially degenerate one (
)
(I93+HL69, solid lines) and I93 in the whole structure (I93, dashed lines).
Notwithstanding that the two pairs of sets differ only in the conductive efficiency
adopted in the partially degenerate regime, roughly corresponding to
the thin external layer, whose mass is less than 1% of the WD mass,
the effect is very large causing a shift in the position of the LF peak
of about 0.3 mag for 12 Gyr and 0.5 mag for 14 Gyr, which means roughly a difference
in age of 1 Gyr and 1.6 Gyr, respectively.
Itoh suggested to use a different match between the I93 and the HL69
conductive opacity (private communication). Thus, we have calculated an additional
set of cooling sequences, here referred to as I93+HL69 smooth, where
I93 is used for
,
HL69 for
and a linear interpolation
is used between the two for
.
The variation of the WD LF peak is less than 0.1 mag.
In addition, we have computed cooling models adopting the conductive
opacity of Potekhin (P99) and HL69 in the regions where, respectively,
and
,
and a linear
interpolation in the transition zone (here referred as P99+HL69 smooth).
To compute the conductive opacity of Potekhin
we use Fortran codes provided by Potekhin.
The differences are small, as expected from a previous analysis presented in Paper I,
because the P99 predictions are in good agreement with the I93 ones where this
latter is nominally valid.
Figure 6 shows the LFs for 12 (thin lines) and 14 Gyr
(thick lines) for the just presented "P99+HL69 smooth'' WD models (solid lines)
and the ones computed adopting the P99 conductive opacity in the whole structure
(dashed lines). The discrepancy between the two sets of models is quite large,
for the presented ages the shift of the WD LF peak is about 0.4 mag, roughly
corresponding to 1.3 Gyr. As in the case shown in Fig. 5,
this result proves again the extreme sensitivity of the computed cooling
times and thus of the theoretical WD LFs to the treatment of
conductive opacity in the very thin (
)
envelope, where electrons
are only partially degenerate.
To our knowledge, Potekhin
provides the only homogeneous conductive opacity computations suitable
for the description of the whole WD structure available in the literature.
On the other hand, these results for nondegenerate plasmas, as stated by
Potekhin himself, "are based on a
continuation from the degenerate domain (using Fermi-Dirac averaging) and can
be considered as order-of-magnitude estimates.'' (see e.g. description at
http://www.ioffe.rssi.ru/astro/conduct/conduct.html).
To provide firmer predictions of WD cooling times we need
more precise treatments of electron conduction for partially degenerate regimes.
At present the choice of the prescription adopted for the conductive opacity affects the age estimate of GCs at the level of 10%.
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Figure 7: Theoretical LFs of 14 Gyr for the four labeled metallicities. |
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The larger the metallicity, the thinner the external H-layer, because the H burning efficiency increases with a larger amount of CNO. Due to the compact nature of these stellar remnants the gravitational settling is so efficient as to produce an envelope constituted by two layers of almost pure elements, i.e. a buffer of He surrounded by a very thin H surface envelope.
On the contrary, the WD isochrones and LFs are considerably affected by metallicity variations because, as is well known, the pre-WD evolutionary time scale is a sensitive function of the original chemical abundance. In addition, the initial-to-final mass relation changes with metallicity.
In order to estimate the effect of the assumed chemical abundance, we computed four sets of isochrones and the related LFs for metallicities covering a range suitable for population I and II stars, i.e. Z=0.0001, 0.001, 0.006 and 0.02. As already mentioned, we adopted the pre-WD evolutionary times and the initial-to-final mass relationship (see e.g. Fig. 3) from the homogeneous set of stellar models of low and intermediate mass stars by Dominguez et al. (1999) and Straniero et al. (1997).
Figure 7 shows the theoretical
WD LFs for an age of 14 Gyr and the four labeled metallicities.
The position of the peak of the WD LF is a sensitive function
of the metal content of the progenitor stars. Between Z=0.0001 and Z=0.001,
there is a difference in the visual magnitude of the peak of about 0.4 mag,
the same between Z=0.001 and Z=0.006. Thus, in order to use WDs to date GCs,
one should compute theoretical isochrones and LFs with
the cluster metallicity. For galactic GCs the typical error on [Fe/H] is of the
order of 0.1 dex.
This means that the typical uncertainty on the metallicity measurements only
slightly affects the estimates of the GC ages based on the WD cooling sequences,
provided that WD isochrones
and LFs have been computed with the nominal value of the cluster metal abundance.
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Figure 8: Initial-to-final mass relations for the solar chemical composition from: Weidemann (2000, filled circles); Girardi et al. (2000, dashed line); our relation (solid line); Hurley et al. (2000, short dashed line). |
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![]() |
Figure 9: Theoretical WD LFs for 12 Gyr and different initial-to-final mass relations for the solar chemical composition from: Weidemann (2000, filled circles); Girardi et al. (2000, dashed line); our relation (solid line); Hurley et al. (2000, short dashed line). |
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Girardi et al. (2000) rely on synthetic AGB models.
This means that the evolution of the AGB stellar properties
(the core mass, the total mass, the luminosity or the effective
temperature) is obtained by semiempirical prescriptions,
instead of solving the stellar structure equations
(see e.g. Groenewegen & de Jong 1993; Bertelli et al. 1994;
Marigo et al. 1996, 1998; Girardi & Bertelli 1998).
The Hurley et al. (2000) relation has been computed with the
SSE package, kindly provided by Hurley, which uses
analytic formulae derived by fitting the stellar models
computed by Pols et al. (1995).
Our prescription for the initial-to-final mass relation is based
on full stellar evolution computations, from the pre-MS up to the AGB tip
(Straniero et al. 1997; Dominguez et al. 1999;
Straniero et al. 2005). The pre-AGB mass loss is based on the
Reimers' formula (
), and an empirical calibration of the mass
loss-period relation is used for the AGB evolution (see Straniero et al.
2005, for details). Thus, the three curves reported in
Fig. 8 are representative of the different methods commonly
used to derive the initial-to-final mass relation.
Figure 9 shows the WD LFs related to the initial-to-final
mass relations described in Fig. 8.
In all cases we have adopted the same set of cooling evolutionary models and
the same slope of the IMF. We derived the pre-WD ages
from the homogeneous set of stellar models of low and intermediate mass stars
by Straniero et al. (1997) and Dominguez et
al. (1999), except for the Girardi et al. (2000)
and the Hurley et al. (2000) relations, for which we used the
life times provided by their own stellar models.
The substitution of our relation by the Weidemann (2000) one
produces a shift of the peak of about 0.1 mag,
roughly corresponding to 0.3 Gyr. The same shift, but in the opposite
direction, is produced by substituting our relation with the
Hurley et al. (2000) one. A larger effect is determined by
changing our relation with the Girardi et al. (2000) one;
in this case the peak shifts by about 0.3 mag, which translates into an age
error of 1 Gyr.
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Figure 10:
Theoretical WD LFs for 12 Gyr and solar metallicity.
Three different slopes of the IMF ( |
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WD cosmochronology is becoming a feasible tool for dating stellar clusters. In this paper we have analyzed the accuracy of the available calibration of the WDs age, by computing various sets of WD isochrones and LFs under different prescriptions for the theoretical ingredients. We discussed the effect on the WD LFs, and thus on the globular cluster age derived with these compact objects, of the assumed conductive opacity, C-O abundance in the core, and initial-to-final mass relation and IMF.
The main effect is caused by the adopted conductive opacity, in particular in the partially degenerate regime characteristic of the thin outer layer. For the range of ages typical of galactic GCs the conductive opacity affects the dating by the order of 10%.
Concerning the C-O amount in the core, the uncertainty in the age
is less than 5%. Moreover, this contribution
will further decrease in the near future thanks to
experiments to
measure the
reaction rate
at the energy of interest.
The IMF does not affect the position of the peak and consequently the estimated ages. At variance, the initial-to-final mass relation plays an important role in dating globular clusters because it significantly affects the shape of the WD LF, in particular the position of the peak. The uncertainty on the age can reach 8%.
Finally, given the sensitive dependence of the evolution of the WD progenitors on the metal content, in order to use WDs to date GCs, one has to compute WD isochrones and LFs for the metallicity of the cluster. In fact, between Z=0.0001 and 0.001 and between Z=0.001 and 0.006, the difference in the inferred age is, for the range of interest, of the order of 10%.
Acknowledgements
We thank P. Bergeron for kindly providing us the model atmosphere and N. Itoh and S. Shore for the many helpful comments. We are grateful to J. R. Hurley for kindly providing us the SSE package.