Astron. Astrophys. 318, 171-178 (1997)
3. Thermal imbalance of observed contact binaries
3.1. Observational properties
From the observational data a few global parameters can be
determined. The period is exactly known. The mass ratio and a lower
limit for the total mass can be found from
radial velocities. The temperature difference
and the mean effective temperature can be
approximately determined from the colours and spectral types of the
components.
If the spectroscopic mass ratio is known, additional properties
(e.g. mass M, light ratio , degree of
contact F) can be determined in a light curve analysis, but the
results are often uncertain. For this reason the light curve will be
used directly (i.e. without interpretation in a light curve analysis)
as an observational property.
3.2. The temperature difference
In many observed systems the secondary is hotter than the primary.
In theoretical configurations with typical mass ratios however the
primary is slightly hotter than the secondary, i.e.
is positive. For systems in good thermal
contact this follows from the equal entropy condition (5) and Lucy's
(1967) discussion (in hydrostatic equilibrium the mean effective
gravity is slightly larger in the primary than in the secondary). If
the thermal contact is poor, the entropy difference
is positive and the temperature difference is
even larger.
If these theoretical results are reliable, observed systems with a
negative temperature difference are far from hydrostatic equilibrium
and thus not in thermal equilibrium.
The theoretical temperature difference is however only an
approximation. A mixing-length formalism is used to calculate the
temperature gradient, and the mixing-length
is assumed to be the same in both components.
On account of these approximations the argument against thermal
equilibrium is not conclusive.
Summarizing, a negative observed temperature difference (and the
resulting properties of the light curve) cannot be explained in the
present theoretical treatment since in hydrostatic equilibrium the
theoretical difference is always positive. Both differences are
however small and can be neglected in an approximate discussion.
3.3. Test of thermal imbalance
Consider an observed system with reliable spectroscopic values for
q and . We shall ask whether the system
can be in thermal equilibrium.
For this purpose we have to check all theoretical equilibrium
configurations with the given (observed) values of period and mass
ratio. As shown in Sect. 2.3 they can be approximately described by
two parameters. For some choice of these parameters, the properties of
the theoretical configuration must be compatible with the
observations, the contact condition (7) must be satisfied, and the
configuration must be thermally stable. Otherwise thermal equilibrium
can be excluded within the framework of our approximations.
Taking into account the observable properties as collected in the
preceding subsections, the result can be summarized as follows. If an
observed system is in thermal equilibrium, there exists a theoretical
equilibrium configuration with the observed values of period and mass
ratio having the following properties: (I) The mean effective
temperature is compatible with the
observations. (II) The theoretical light curve is compatible with the
observed light curve, with the possible exception of differences
between the two minima. Note that the inclination of a theoretical
configuration is known from the mass M and the observed value
of . The theoretical light curve is therefore
also known. (III) The contact condition (7) is satisfied. (IV) The
configuration is thermally stable.
For given period and mass ratio, a theoretical equilibrium
configuration has two degrees of freedom. They can usually be adjusted
to satisfy the conditions (I) and (II). (An exception concerns systems
with a very high inclination. Since the mass is approximately known
from the observed value of , there is no freedom
to satisfy two conditions.) The resulting configuration is determined
uniquely if uncertainties in the observational input parameters and
the theoretical treatment are ignored. If these uncertainties are
taken into account we obtain a set of theoretical configurations with
the properties (I) and (II). If any one of these configurations
satisfies the conditions (III) and (IV), nothing more can be said. The
observed system may or may not be in thermal equilibrium. (The
conditions for thermal equilibrium are necessary but by no means
sufficient.) However, if configurations satisfying the contact
condition do not exist, or if all of them are thermally unstable, the
observed system is certain to be in thermal imbalance.
In the following subsections this test will be applied to a number
of observed systems. We begin with a detailed discussion of the system
BV Dra. For the other systems a short discussion will be
sufficient.
3.4. Thermal imbalance of BV Dra
For the system BV Dra (period day)
Batten & Lu (1985) determined the parameters
and found that the secondary (spectral typ F8)
is slightly hotter than the primary (F9). KR86 determined from the
colours a mean effective temperature K.
Strömgen colours (Ruci ski
1983) and the calibration of Philip & Relyea (1979) give
K. To cover this range we investigated
models with temperatures of 6000, 6100 and 6190 K.
Properties of configurations satisfying the conditions (I) and (II)
are listed in Table 1. The contact condition (III) is also
satisfied. The theoretical light curves have been fitted to the
observed light curve during the transit eclipse, cf. Fig. 4. The
temperature difference is positive and too large. This implies that
during the occultation eclipse the theoretical light curve is too
shallow. Except for these difficulties (which are unavoidable as
discussed in Sect. 3.2) the observed properties of BV Dra are
reproduced.
![[TABLE]](img81.gif)
Table 1. Theoretical configurations in thermal equilibrium for comparison with BV Dra
![[FIGURE]](img82.gif) |
Fig. 4. The light curve of the last model in Table 1 in comparison with the observed light curve of BV Dra
|
Condition (IV) however is violated. The configurations are
thermally unstable with an e -folding time of about
yr. This was shown in an eigenvalue analysis as
well as in evolutionary calculations. Accordingly, within the
framework of our approximations (this caveat will be made also in the
following subsections) BV Dra is certain to be in thermal
imbalance.
3.5. Thermal imbalance of BW Dra
For the system BW Dra ( day) Batten
& Lu (1985) determined the parameters .
Strömgen colours (Ruci ski
1983) and the calibration of Olsen (1984) give a mean effective
temperature K. For the primary KR86
derived an effective temperature of about 5900 K. For
temperatures in this range, conditions (I) and (II) give evolved
( ) configurations of mass
. Since the contact condition is violated
( ), thermal equilibrium can be excluded. In the
generalised (formal) thermal stability problem the models are unstable
on a time scale of about yr.
3.6. Thermal imbalance of W UMa
For the system W UMa ( day)
Ruci ski et al. (1993)
determined from 1989 data the parameters , a
mean temperature of K and the mass
. The light curve (e.g. Linnell 1991) shows that
the inclination is very high. Accordingly, there is little freedom in
the mass. Using these values of and adopting
the metallicity we obtain an evolved
( ) configuration with a mean temperature of 6370
K. The contact condition is violated ( ). For
larger values of Z the temperature is lower but F is
still larger. For these reasons thermal equilibrium can be excluded.
The configurations are unstable on a time scale of about
yr.
3.7. Thermal imbalance of AH Vir
The system AH Vir ( day) has also a very
high inclination. Lu &
Ruci ski (1993) determined the
parameters , a mean temperature of 5300 K and a
mass of . Adopting this mass and the metallicity
we obtain an evolved ( )
configuration which is much too hot ( K) and in
severe conflict with the contact condition ( ).
If the metallicity is increased, the temperature decreases but the
conflict with the contact condition increases. Accordingly,
AH Vir is in thermal imbalance. The configurations are unstable
on a time scale of about yr.
3.8. Thermal imbalance of AB And
For the system AB And ( day) Hrivnak
(1988) determined the parameters . In a light
curve analysis he found . Using these
parameters, the present light curve synthesis is not able to reproduce
the observed light curve. In the theoretical light curve the
difference between the two minima is too large on account of the
temperature difference.
The observed light curve shows that the inclination is very high.
We calculated models of mass and mean
temperatures between 5450 K (the primary's temperature adopted by
Hrivnak) and 5800 K. The theoretical light curve is always too
shallow. The models are evolved ( ) and satisfy
the contact condition ( ). All of them are
thermally unstable with an e -folding time of
yr. Accordingly, AB And is in thermal
im
3.9. Thermal imbalance of V508 Oph
So far we discussed W-type systems. The A-type system V508 Oph
( ) has parameters similar to those of
AB And and also a very high inclination. Lu (1986) and Lapasset
& Gómez (1990) found and determined
a mean temperature between 5800 and 6000 K. We calculated models with
these parameters and the mass . They are
evolved ( ) and satisfy the contact condition
( ). The theoretical light curves are too
shallow. All models are unstable on a time scale of
yr. We conclude that V508 Oph is in
thermal imbalance.
3.10. Thermal imbalance of OO Aql
The A-type system OO Aql ( day) has one
of the largest mass ratios. Hrivnak (1989) determined the parameters
and a temperature between 5500 and 6000 K. The
light curve indicates that the inclination is very high. We
investigated models in hydrostatic equilibrium with
. Adopting the metallicity
we obtain an evolved ( )
model in severe conflict with the contact condition
( ) and with a mean temperature of 4390 K which
is much too low. Decreasing Z we obtain models with higher
temperature but even lower degree of contact. Thermal equilibrium can
therefore be excluded. The configurations are unstable on a time scale
of about yr.
© European Southern Observatory (ESO) 1997
Online publication: July 8, 1998
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