Element | Initial abundance |
H | 0.76996750 |
3He | 0.00002438 |
4He | 0.22999812 |
12C | 7.5500e-7 |
13C | 0.1000e-7 |
14N | 2.3358e-7 |
15N | 0.0092e-7 |
16O | 67.100e-7 |
17O | 0.0300e-7 |
18O | 0.1500e-7 |
20Ne | 7.8368e-7 |
22Ne | 0.6306e-7 |
24Mg | 3.2474e-7 |
25Mg | 0.4268e-7 |
26Mg | 0.4897e-7 |
The initial composition is given in Table 1.
The composition
is enhanced in -elements.
As in Paper VII, the opacities are
from Iglesias & Rogers (1996), complemented at low
temperatures with the molecular opacities of Alexander
(http://web.physics.twsu.edu/alex/wwwdra.htm). The nuclear
reaction rates are also the same as in Paper VII and are
based on the new NACRE data basis (Angulo et al. 1999).
The physics of the present models at Z=10-5 is the same
as for models at Z=0.004 (Maeder & Meynet 2001).
For rotation, the hydrostatic effects and the surface distortion
are included (Meynet & Maeder 1997), so that the
given here corresponds to an average orientation angle. The
diffusion by shears,
which is the main effect for the mixing of chemical elements,
is included (Maeder 1997), with
account of the effects of the horizontal turbulence,
which reduces the shear effects in regions of steep
-gradients and reinforces it in regions of low
-gradients (Maeder & Meynet 2001).
Meridional circulation is the main effect for the
internal transport of angular momentum. We use here the
expression by Maeder & Zahn (1998) for
the vertical component U(r) of the meridional circulation.
It is interesting to represent graphically this circulation.
Figure 1 illustrates the patterns of the
meridional circulation in a 20
star at Z=0.020and initial rotation velocity
km s-1on the ZAMS.
The figure is symmetrical with respect
to the rotation axis, as well with respect to the equatorial plane.
The small inner sphere is the edge of the central convective core.
The inner tube, in the upper hemisphere,
represents an interior cell of the meridional circulation.
There is an ensemble of such concentric
tubes with different meridional velocities.
The motions occur in a meridian plane (i.e. turning around
the tube).
In the upper hemisphere and around the inner tube,
the fluid elements go upward
on the inner side of the tube and descend toward the equator on the
outer side of the tube (U(r) is positive).
The external tube represents an outer circulation cell,
due to the Gratton-Opik term, which is important in the outer stellar
layers.
This term leads to a negative U(r), which means
that, in the upper hemisphere, the fluid goes up on the outer side
of the tube and down along the inner side.
There also, this tube is one among an ensemble of stream lines turning
in the meridian plane.
The mass loss rates are based on the same references as in the paper for
the Z=0.004 models (Maeder & Meynet 2001) and in particular
on the data by Kudritzki & Puls (2000) for the OB stars.
Of course, the
strong reduction of the mass loss rates with
metallicity for stars below 60
makes the mass
loss rather unimportant for the metallicity Z=10-5 considered here, as illustrated by Table 1
which shows the values of the final masses.
We account for
the effects of rotation on the mass loss rates, according to
the standard stellar wind theory applied to a rotating star
(Maeder & Meynet 2000). The net result is
that the very massive stars with initial
may still experience significant mass loss as shown in Table 1,
if they rotate very fast.
Star models with initial masses superior or equal to 9
were computed
up to the end of the carbon-burning phase. Star models with masses between 2 and 7
were evolved beyond
the end of the He-burning phase through a few thermal pulses during the AGB phase.
Copyright ESO 2002