Astron. Astrophys. 358, 572-574 (2000)
1. Background
Ori C is the brightest and hottest
member of the Orion Trapezium cluster at the heart of the bright HII
nebula M42. Previous optical/UV observations going back many years
(Conti 1972; Walborn 1981; Walborn & Panek 1984; Stahl et al.
1993; Walborn & Nichols 1994; Stahl et al. 1996) have shown that
Ori C may be the O-star equivalent of
a magnetic oblique rotator. Recent X-ray observations (Gagné et
al. 1997; Babel & Montmerle 1997) indicate a modulation in the
15.4 day rotation cycle, with a likely surface magnetic field of
several 100 G. In an attempt to detect the magnetic field via Zeeman
splitting using high resolution optical spectropolarimetry in circular
mode, Donati & Wade (1999) have reported null detections with 250
G 1 error bars for any longitudinal
component of a surface magnetic field averaged over the stellar disk.
If the field is a dipole, the pole strength must be below some 1800 G.
This null result is in agreement with the estimation of an upper
threshold for Be by Eversberg et al. (1998).
Donati & Wade (1999) also noted the unexpected discovery of
strong, time-variable continuum circular polarisation in the optical
spectrum of Ori C, reaching values as
high as 3.8%! As support for the reliability of this result, they note
the presence of depolarisation structure associated with the strong
nebular emission lines. They conclude that the continuum polarisation
must be produced within the immediate (spatially unresolved)
circumstellar (CS) environment of the star. Eversberg et al. (1998)
failed to detect any depolarisation in the strong
H nebular line, although they possibly
could have, had they had higher resolution and S/N.
Among the possible causes of this unusual continuum polarisation,
Donati & Wade invoked some kind of CS disk as the most likely
explanation. However, the level of linear continuum
polarisation should be even larger, contrary to the previous
observations of Leroy & Leborgne (1987), despite the latter
authors' reporting of variability.
© European Southern Observatory (ESO) 2000
Online publication: June 8, 2000
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