The method of calculating spectroscopic gravities using the standard
technique of making
abundances of
both neutral and ionized iron lines agree was not used here due to the
scarcity of usable Fe II lines in the observed
wavelength range. Alternatively, surface gravities were derived for those
stars with accurate parallaxes in the HIPPARCOS catalogue
following a method similar to that described in Nissen et al. (1997). In short,
the method relies on the basic relations
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(1) |
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(2) |
The mass of the stars were calculated from its position in the
-log
diagram by interpolating in the isochrones given in
Claret (1995). The mass so calculated was used as input value in
the
log
-
diagram to obtain the surface gravity. A chemical
composition X = 0.70, Z = 0.02 (solar abundance) was adopted. This is based on the fact that
the main contribution to the overall metallicity is due to
C, N, O (solar abundant in
Bootis stars). Furthermore, there are strong indications that the
Bootis phenomenon is restricted to the stellar surface (Holweger &
Rentzsch-Holm 1995). The mixing length and core
overshooting parameters were fixed to 1.52 and 2.0 respectively. Surfaces
gravities are given in Table 2. Parallaxes, bolometric corrections,
magnitudes,
luminosities, masses and ages are displayed in Table 3. Age estimations for the sample
stars indicate that they cover an area slightly above the Main Sequence. Surface gravities calculated
using HIPPARCOS are only slightly higher
than those derived using Moon & Dworetsky (1985) (
). A conservative
value of
= 0.15 dex has been estimated based on errors in the
bolometric correction and in the calculated mass.
Copyright ESO 2001