Asteroseismic detection of a predominantly toroidal magnetic field in the deep interior of the main-sequence F star KIC 9244992
Masao Takata, Simon J. Murphy, Donald W. Kurtz, Hideyuki Saio, Hiromoto Shibahashi
TL;DR
Using four years of Kepler data, this work detects a strong internal magnetic field in the main-sequence F star KIC 9244992 by analyzing the asymmetry of high-order gravity-mode splittings. The authors develop a tripartite model incorporating rotation, magnetic effects, and an aspherical glitch, and show that rotation alone cannot explain the observed asymmetries. The inferred field is predominantly toroidal (B_φ^min ≈ 92 kG) with a much weaker radial component (B_r^min ≈ 3.5 kG) confined near the core, and the glitch localizes to a layer just outside the convective core where the chemical gradient is steep. These results imply efficient angular-momentum transport inconsistent with several radiative-dynamo scenarios and point to fossil fields or merger-related origins, marking the first seismic detection of a deep interior magnetic field in a main-sequence star.
Abstract
An asteroseismic analysis has revealed a magnetic field in the deep interior of a slowly-rotating main-sequence F star KIC9244992, which was observed by the Kepler spacecraft for four years. The star shows clear asymmetry of frequency splittings of high-order dipolar gravity modes, which cannot be explained by rotation alone, but are fully consistent with a model with rotation, a magnetic field and a discontinuous structure (glitch). Careful examination of the frequency dependence of the asymmetry allows us to put constraints on not only the radial component of the magnetic field, but also its azimuthal (toroidal) component. The lower bounds of the root-mean-squares of the radial and azimuthal components in the radiative region within 50 per cent in radius, which have the highest sensitivity in the layers just outside the convective core with a steep gradient of chemical compositions, are estimated to be $\mathsf{B}_{\mathrm{r}}^{\min}=3.5 \pm 0.1$ kG and $\mathsf{B}_φ^{\min}=92 \pm 7$ kG, respectively. The much stronger azimuthal component than the radial one is consistent with the significant contribution of the differential rotation although the star has almost uniform rotation at present. The estimated field strengths are too strong to be explained by dynamo mechanisms in the radiative zone associated with the magnetic Tayler instability. The aspherical glitch is found to be located in the innermost radiative layers where there is a steep gradient of chemical composition. The first detection of magnetic fields in the deep interior of a main-sequence star sheds new light on the problem of stellar magnetism, for which there remain many uncertainties.
