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The magnetic field and wind confinement of  θ1  Orionis C
J.-F. Donati 1 J. Babel 2 T. J. Harries 3 I. D. Howarth 4 P. Petit 1 M. Semel 5
  1 Laboratoire d'Astrophysique, Observatoire Midi-Pyrénées, 14 Av. E. Belin, F-31400 Toulouse, France,   2 36 rue des Battieux 2000 Neuchatel, Switzerland,   3 School of Physics, University of Exeter, Stocker Road, Exeter EX4 4QL,   4 Department of Physics and Astronomy, University College of London, London and   5 DASOP, Observatoire de Paris-Meudon, 5 place J. Janssen, F-92195 Meudon Principal Cédex, France
Correspondence to jean-francois.donati@obs-mip.frJ-FD
Correspondence to petit@obs-mip.frPP
Correspondence to babeljr@bluewin.chJB
Correspondence to th@astro.ex.ac.ukTJH
Correspondence to idh@star.ucl.ac.ukIDH
Correspondence to semel@obspm.frMS
 

1 Note that this assumption may not be entirely consistent with the results obtained above, indicating for instance that the disc may be opaque only beyond Rd and within RA (see Section 5.2); this point is, however, not completely clear, as it depends critically on the actual fate of the plasma piling up in the disc. We therefore preferred to keep the problem as simple as possible and avoid the introduction of additional parameters, at least until more direct constraints are available from observations.

 

2 The stellar eclipse is not totally achromatic though, since the different regions of the spectra do not come from the same spatial regions (harder X-rays being produced in hotter parts of the post-shock region).

Copyright 2002 Blackwell Science Ltd

ABSTRACT

We report the detection, through spectropolarimetric observations, of a strong dipolar magnetic field of presumably fossil origin at the surface of the very young O star  θ1  Ori C. The Stokes V signatures we detect are variable with time, the variations being consistent with rotational modulation. A detailed modelling of our observations indicates that this dipole field has an intensity of  1.1±0.1 kG  and is inclined at  42°±6°  with respect to the rotation axis (assumed to be inclined at 45° to the line of sight). We find, in particular, that the positive magnetic pole comes closest to the observer when the variable Hα emission component observed on this star reaches maximum strength. This discovery represents the first definite detection of a magnetic field in an O star, as well as the first detection of a fossil field in a very young star.

We also investigate in this paper the magnetic confinement of the radiatively driven wind of  θ1  Ori C in the context of the magnetically confined wind-shock model of Babel & Montmerle. In the case of  θ1  Ori C, this model predicts the formation of a large magnetosphere (extending as far as  2–3R∗) , consisting of a very hot post-shock region (with temperatures in excess of 10 MK and densities of about  1010–1011 cm-3 generated by the strong collision of the wind streams from both stellar magnetic hemispheres, as well as a dense cooling disc forming in the magnetospheric equator. We find that this model includes most of the physics required to obtain a satisfactory level of agreement with the extensive data sets available for  θ1  Ori C in the literature (and, in particular, with the recent X-ray data and the phase-resolved spectroscopic observations of ultraviolet and optical wind lines) provided that the mass-loss rate of  θ1  Ori C is at least 5 times smaller than that predicted by radiatively driven wind models. We finally show how new observations with the XMM or Chandra spacecraft could help us constrain this model much more tightly and thus obtain a clear picture of how magnetic fields can influence the winds of hot stars.


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