Magneto-elastic oscillations of neutron stars: exploring different magnetic field configurations

TL;DR

This study investigates how different magnetic field configurations in neutron stars affect magneto-elastic oscillations, helping to explain observed quasi-periodic oscillations in magnetar giant flares.

Contribution

It extends previous models by analyzing various magnetic field configurations and their impact on Alfvén spectra and QPOs in magnetars.

Findings

Estimated magnetic field strengths between 8x10^14 G and 4x10^15 G.

Most observed QPOs can be explained by magneto-elastic oscillations.

Crust-confined magnetic fields are less favored due to difficulty explaining low-frequency QPOs.

Abstract

We study magneto-elastic oscillations of highly magnetized neutron stars (magnetars) which have been proposed as an explanation for the quasi-periodic oscillations (QPOs) appearing in the decaying tail of the giant flares of soft gamma-ray repeaters (SGRs). We extend previous studies by investigating various magnetic field configurations, computing the Alfv\'en spectrum in each case and performing magneto-elastic simulations for a selected number of models. By identifying the observed frequencies of 28 Hz (SGR 1900+14) and 30 Hz (SGR 1806-20) with the fundamental Alfv\'en QPOs, we estimate the required surface magnetic field strength. For the magnetic field configurations investigated (dipole-like poloidal, mixed toroidal-poloidal with a dipole-like poloidal component and a toroidal field confined to the region of field lines closing inside the star, and for poloidal fields with an additional quadrupole-like component) the estimated dipole spin-down magnetic fields are between 8x10^14 G and 4x10^15 G, in broad agreement with spin-down estimates for the SGR sources producing giant flares. A number of these models exhibit a rich Alfv\'en continuum revealing new turning points which can produce QPOs. This allows one to explain most of the observed QPO frequencies as associated with magneto-elastic QPOs. In particular, we construct a possible configuration with two turning points in the spectrum which can explain all observed QPOs of SGR 1900+14. Finally, we find that magnetic field configurations which are entirely confined in the crust (if the core is assumed to be a type I superconductor) are not favoured, due to difficulties in explaining the lowest observed QPO frequencies (f<30 Hz).