Solar abundance corrections derived through 3D magnetoconvection simulations
D. Fabbian, E. Khomenko, F. Moreno-Insertis, and {\AA}. Nordlund

TL;DR
This study uses 3D magnetoconvection simulations to quantify how magnetic fields influence solar element abundance measurements, revealing that magnetic flux can cause significant corrections in derived iron abundances.
Contribution
It provides the first detailed quantification of magnetic effects on solar abundance determinations using realistic 3D simulations and spectral synthesis.
Findings
Magnetic flux causes up to 0.1 dex correction in Fe abundance.
Zeeman broadening and temperature stratification modifications have opposite effects.
Magnetic effects are significant for precise solar and stellar abundance analysis.
Abstract
We explore the effect of the magnetic field when using realistic three-dimensional convection experiments to determine solar element abundances. By carrying out magnetoconvection simulations with a radiation-hydro code (the Copenhagen stagger code) and through a-posteriori spectral synthesis of three Fe I lines, we obtain evidence that moderate amounts of mean magnetic flux cause a noticeable change in the derived equivalent widths compared with those for a non-magnetic case. The corresponding Fe abundance correction for a mean flux density of 200 G reaches up to ~0.1 dex in magnitude. These results are based on space- and time-averaged line profiles over a time span of 2.5 solar hours in the statistically stationary regime of the convection. The main factors causing the change in equivalent widths, namely the Zeeman broadening and the modification of the temperature stratification, act…
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