We computed a large number of solar models using the GARching SOlar Model (GARSOM) code which has been described in its latest version in Schlattl (2001). Our standard model has been compared with other contemporary solar models by Turck-Chièze et al. (1998), who found a good agreement between various programs.
The solar photospheric radius and luminosity have been assumed to be
(Brown & Christensen-Dalsgaard 1998) and
,
respectively. The surface
metal ratio
has been taken from Grevesse & Noels (1993), thus
Z/X=0.0245.
The mixing length parameter (Böhm-Vitense 1958), initial helium and metal
content have been adjusted in all models to reproduce these values
with an accuracy better than 10-4.
In the actual calculations the latest OPAL-opacities (Iglesias & Rogers 1996) completed in the low-temperature regime by tables of Alexander & Fergusson (1994) have been implemented. The outer boundary condition was determined assuming an Eddington grey atmosphere. Microscopic diffusion of hydrogen, helium and all major metals is taken into account. For the EOS we used either the OPAL- (Rogers et al. 1996) or the MHD-tables (Hummer & Mihalas 1988; Mihalas et al. 1988; Däppen et al. 1988). The original OPAL EOS (OPAL96) has been updated by treating electrons relativistically and by improving the activity expansion method for repulsive interactions (Rogers 2001), denoted OPAL01 in the following.
In the case of MHD EOS the relativistic corrections are not directly
included in the tables. We have therefore corrected the adiabatic index
employing the expression of Elliott & Kosovichev (1998),
The nuclear reaction rates are taken either from Bahcall et al. (1995) or
from Adelberger et al. (1998) with
being
in the first and
in the latter case. Other differences in the reaction rates are not
very significant in determining the evolutionary stage of the solar core.
Copyright ESO 2002