![]() | ![]() |
Astron. Astrophys. 317, 90-98 (1997) 6. Discussion and conclusionsAs very recently stated in the paper by Baraffe et al. (1995), till recent times the theoretical framework for VLM stars appeared far from being satisfactory, "all the existing theoretical models failing to reproduce the observed magnitude-color diagram for the faintest objects, predicting temperature that are too large for a given luminosity". As a matter of fact, the history of VLM models is the history of the continuous decrease of model effective temperatures driven by the continuous improvement in the evaluation of the input physics (see, e.g. Dorman et al. 1989). In this context, solar metallicity models appear as the most difficult objects to be theoretically reproduced, just because of the difficult task of taking into the right account the proper influence of metals on both opacity and EOS.
Numerical experiments (Ciacio 1994) as well as inspection of the
results already appeared in the literature, show that the treatment of
the atmosphere or the improved physical inputs mainly affect the
stellar temperature, with only a minor influence on the model
luminosity. As a consequence, it could be suggested that theoretical
mass-luminosity relations should have reached a reasonable degree of
reliability. However, recently Chabrier et al. (1996) have emphasized
the need to use accurate boundary conditions (nongray model
atmospheres) between the atmosphere and the interior structure to
derive more reliable mass - luminosity relationship. Nevertheless, one
has to notice that not negligible differences still exist between
different sets of model atmospheres (Bessel 1995, Chabrier et al.
1996) due mainly to the different methods adopted in the opacity
calculations (straight-mean approximation
versus opacity-sampling technique). In Fig. 10, we compare
theoretical predictions from the present paper, by Baraffe et al.
(1995) and by Chabrier et al. (1996) with observational data by Henry
& McCarthy (1993). It is worth noting that our models are in good
agreement with the observations and also with the theoretical
mass-luminosity relation by Chabrier et al. (1996) obtained adopting
the most accurate model atmospheres (Allard et al. 1996, Brett 1995)
presently available. This evidence reinforces the suggestion, given in
the previous sections, that the use of a
© European Southern Observatory (ESO) 1997 |