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Centaurus X-3 was discovered in May 1967 during a survey of the southern sky
with a sounding rocket carrying
proportional counters (Chodil et al. (1967)). Observations with Uhuru later showed
that the X-ray flux was modulated by regular pulsations (Giacconi et al. (1971)) with
a 4.8 s period. On the basis of Doppler variations in its pulse period
observed with Uhuru, Cen X-3 was the first of the X-ray sources to be
established as a binary (Schreier et al. (1972)).
The X-ray eclipses which occur every 2.1 days suggest
a high inclination angle i. Assuming an eclipse half angle of 40o,
Conti (1978) estimated the radius of the companion Rc to be
12.5 R
and
i > 80o. Clark et al. (1988) estimated the eclipse
half angle as 32.9o and derived a mass
of
(1.23
0.60)M
for the neutron star. After reviewing the
available data van Kerkwijk et al. (1995) derived the 95% confidence values
Mx = 1.09+0.57-0.52M
,
Mc = 18.9+4.0-1.8M
,
Rc = 11.1+1.8-1.1R
, and
i > 66o.
The companion is a highly reddened O-type star known as V779 Cen or
Krzeminski's star. From the optical
reddening a distance of
8 kpc has been inferred, with a lower limit of
6.2 kpc .
Because Cen X-3 has not been detected in radio there is no dispersion measure
to compare with this and the distance is uncertain.
Day and Tennant (1991) used the EXOSAT ME to observe soft emission during two eclipses. They interpreted
this as a dust-scattered halo and calculated the distance to the source as
5.4
0.3 kpc. The absolute distance to the source does not affect
any of the results of this work except the calculated luminosities.
For convenience the distance to Cen X-3 will be taken to be 8 kpc.
The binary parameters of Cen X-3 have been well determined
(Joss and Rappaport (1984); Nagase et al. (1992) and references therein).
The pulsar is spinning up with
/P
2.3 x 10-4 yr-1 (Nagase et al. (1992)). This is due to the accretion of
matter with a high specific angular momentum (Ghosh and Lamb (1979a,b); Ghosh et al. (1977)).
The orbital period is decreasing with
/Porb
- 1.74 x 106 yr-1 (Nagase et al. (1992))
due to unstable tidal dissipation (Kelley et al. (1983)).
Next: 2. Mass Transfer
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Damian Audley
1998-09-04