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Astronomy & Astrophysics

Publication date: 2017-07-01
Volume: 605
Publisher: EDP Sciences

Author:

Buysschaert, Bram
Neiner, C ; Briquet, M ; Aerts, Conny

Keywords:

MAMSIE - 670519;info:eu-repo/grantAgreement/EC/H2020/670519, Science & Technology, Physical Sciences, Astronomy & Astrophysics, stars: magnetic field, stars: rotation, stars: oscillations, stars: individual: HD43317, stars: early-type, ROTATING MAGNETOSPHERE MODEL, MAIN-SEQUENCE STARS, DIFFERENTIAL ROTATION, MASSIVE STARS, GRAVITY MODES, STELLAR OSCILLATIONS, ACTIVE STARS, SPACED DATA, ROAP STARS, B-STARS, astro-ph.SR, 0201 Astronomical and Space Sciences, 5101 Astronomical sciences, 5107 Particle and high energy physics, 5109 Space sciences

Abstract:

Large-scale magnetic fields at the surface of massive stars do not only influence the outer-most layers of the star, but also have consequences for the deep interior, only observationally accessible through asteroseismology. We performed a detailed characterization of the dipolar magnetic field at the surface of the B3.5V star HD 43317, a SPB/$\beta$ Cep hybrid pulsator, by studying the rotationally modulated magnetic field of archival and new Narval spectropolarimetry. Additionally, we employed a grid-based approach to compare the Zeeman signatures with model profiles. By studying the rotational modulation of the He lines in both the Narval and HARPS spectroscopy caused by co-rotating surface abundance inhomogeneities, we updated the rotation period to $0.897673\pm0.000004$d. The inclination angle between the rotation axis and the observer's line of sight remains ill-defined, because of the low level of variability in Stokes V and deformations in the intensity profiles by stellar pulsation modes. The obliquity angle between the rotation and magnetic axes is constrained to $\beta \in [67,90]^{\circ}$, and the strength of the dipolar magnetic field is of the order of 1kG to 1.5kG. This magnetic field at the stellar surface is sufficiently strong to warrant a uniformly rotating radiative envelope, causing less convective core overshooting, which should be visible in future forward seismic modeling.