4.7 Article

THE MAGNETIC FURNACE: INTENSE CORE DYNAMOS IN B STARS

Journal

ASTROPHYSICAL JOURNAL
Volume 829, Issue 2, Pages -

Publisher

IOP PUBLISHING LTD
DOI: 10.3847/0004-637X/829/2/92

Keywords

convection - dynamo - magnetohydrodynamics (MHD) - stars; massive

Funding

  1. NCAR Advanced Study Program
  2. NASA through Theoretical and Computational Astrophysics Network (TCAN) grant [NNX14AB56G]
  3. NASA through Heliophysics grants [NNX11AJ36, NNX13AG18G]
  4. ERC [207430 STARS2]
  5. CNRS/INSU via Programmes National Soleil-Terre and Physique Stellaire
  6. NASA [g26133, s0943]
  7. NSF [CNS-0821794]
  8. University of Colorado Boulder
  9. NASA [686798, NNX14AB56G] Funding Source: Federal RePORTER

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The dynamo action achieved in the convective cores of main-sequence massive stars is explored here through three-dimensional (3D) global simulations of convective core dynamos operating within a young 10 M-circle dot B-type star, using the anelastic spherical harmonic code. These simulations capture the inner 65% of this star by radius, encompassing the convective nuclear-burning core (about 23% by radius) and a portion of the overlying radiative envelope. Eight rotation rates are considered, ranging from 0.05% to 16% of the surface breakup velocity, thereby capturing both convection that barely senses the effects of rotation and other situations in which the Coriolis forces are prominent. The vigorous dynamo action realized within all of these turbulent convective cores builds magnetic fields with peak strengths exceeding a megagauss, with the overall magnetic energy (ME) in the faster rotators reaching super-equipartition levels compared to the convective kinetic energy (KE). The core convection typically involves turbulent columnar velocity structures roughly aligned with the rotation axis, with magnetic fields threading through these rolls and possessing complex linkages throughout the core. The very strong fields are able to coexist with the flows without quenching them through Lorentz forces. The velocity and magnetic fields achieve such a state by being nearly co-aligned, and with peak magnetic islands being somewhat displaced from the fastest flows as the intricate evolution proceeds. As the rotation rate is increased, the primary force balance shifts from nonlinear advection balancing Lorentz forces to a magnetostrophic balance between Coriolis and Lorentz forces.

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