期刊
MONTHLY NOTICES OF THE ROYAL ASTRONOMICAL SOCIETY
卷 389, 期 1, 页码 75-85出版社
WILEY-BLACKWELL PUBLISHING, INC
DOI: 10.1111/j.1365-2966.2008.13575.x
关键词
stars: early-type; stars: individual: zeta Ori A; stars: magnetic fields; stars: rotation; stars: winds, outflows
资金
- French National Research Agency (ANR) [ANR-06-BLAN-0105]
- Agence Nationale de la Recherche (ANR) [ANR-06-BLAN-0105] Funding Source: Agence Nationale de la Recherche (ANR)
We report here the detection of a weak magnetic field of 50-100 G on the 09.7 superguiant zeta Orionis A (zeta Ori A), using spectropolarimetric observations obtained with NARVAL at the 2-m Telescope Bernard Lyot atop Pic du Midi (France). zeta Ori A is the third O star known to host a magnetic field (along with theta(1) Ori C and HD 191612), and the first detection on a 'normal' rapidly rotating O star. The magnetic field of zeta Ori A is the weakest magnetic field ever detected on a massive star. The measured field is lower than the thermal equipartition limit (about 100 G). By filling non-local thermodynamic equilibrium (NLTE) model atmospheres to our spectra, we determined that zeta Ori A is a 40 M(circle dot) star with a radius of 25 R(circle dot) and an age of about 5-6 Myr, showing no surface nitrogen enhancement and losing mass at a rate of about 2 x 10(-6) M(circle dot) yr(-1). The magnetic topology of zeta Ori A is apparently more complex than a dipole and involves two main magnetic polarities located on both sides of the same hemisphere; our data also suggest that zeta Ori A rotates in about 7.0 d and is about 40 degrees away from pole-on to an Earth-based observer. Despite its weakness, the detected magnetic field significantly affects the wind structure; the corresponding Alfven radius is however very close to the surface, thus generating a different rotational modulation in wind lines than that reported on the two other known magnetic O stars. The rapid rotation of zeta Ori A with respect to theta(1) Ori C appears as a surprise, both stars having similar unsigned magnetic fluxes (once rescaled to the same radius); it may suggest that the subequipartition field detected on zeta Ori A is not a fossil remnant (as opposed to that of theta(1) Ori C and HD 191612), but the result of an exotic dynamo action produced through magnetohydrodynamics (MHD) instabilities.
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