A self consistent chemically stratified atmosphere model for the roAp star 10 Aquilae

TL;DR

This paper develops a self-consistent atmospheric model for the roAp star 10 Aquilae, incorporating vertical chemical stratification and magnetic effects to improve the understanding of pulsation and atmospheric parameters.

Contribution

It introduces a novel method combining high-resolution spectroscopy and stratification modeling to accurately determine atmospheric parameters of a chemically peculiar star.

Findings

Identified significant vertical abundance gradients for multiple elements.

Determined precise fundamental parameters: Teff=7550 K, log g=3.8.

Revealed diverse stratification profiles, from steep to wide gradients.

Abstract

Context: Chemically peculiar A type (Ap) stars are a subgroup of the CP2 stars which exhibit anomalous overabundances of numerous elements, e.g. Fe, Cr, Sr and rare earth elements. The pulsating subgroup of the Ap stars, the roAp stars, present ideal laboratories to observe and model pulsational signatures as well as the interplay of the pulsations with strong magnetic fields and vertical abundance gradients. Aims: Based on high resolution spectroscopic observations and observed stellar energy distributions we construct a self consistent model atmosphere, that accounts for modulations of the temperature-pressure structure caused by vertical abundance gradients, for the roAp star 10 Aquilae (HD 176232). We demonstrate that such an analysis can be used to determine precisely the fundamental atmospheric parameters required for pulsation modelling. Methods: Average abundances were derived for 56 species. For Mg, Si, Ca, Cr, Fe, Co, Sr, Pr, and Nd vertical stratification profiles were empirically derived using the ddafit minimization routine together with the magnetic spectrum synthesis code synthmag. Model atmospheres were computed with the LLModels code which accounts for the individual abundances and stratification of chemical elements. Results: For the final model atmosphere Teff=7550 K and log g=3.8 were adopted. While Mg, Si, Co and Cr exhibit steep abundance gradients Ca, Fe and Sr showed much wider abundance gradients between log tau_5000=-1.5 and 0.5. Elements Mg and Co were found to be the least stratified, while Ca and Sr showed strong depth variations in abundance of up to ~ 6 dex.