An ISO/SWS study of the dust composition around S stars

TL;DR

This study uses high-resolution ISO/SWS spectra to analyze dust composition around S stars, revealing new features and differences from O-rich AGB stars, suggesting variations in dust mineralogy and non-stoichiometry.

Contribution

It provides the first detailed comparison of S star dust spectra with O-rich AGB stars using improved spectral data, discovering new emission features and proposing a link to non-stoichiometric silicates.

Findings

Discovery of new dust emission features in S stars.

Significant spectral differences between S stars and O-rich AGB stars.

Variation in peak positions linked to dust composition and non-stoichiometry.

Abstract

We investigate the composition of the solid-state materials in the winds around S-type AGB stars. The S stars produce dust in their wind that bears a resemblance to the dust produced in some O-rich AGB stars. However, the reported resemblance is mostly based on IRAS/LRS spectra with limited spectral resolution, sensitivity, and wavelength coverage. We investigate the dust composition around S stars using ISO/SWS data that surpass the previous studies in terms of spectral resolution and wavelength coverage. We compare the dust spectra from the 9 sources with the O-rich AGB spectra and a subset of M super-giants. We constructed average dust emission spectra of the different categories. We report the discovery of several previously unreported dust emission features in the S star spectra. The long wavelength spectra of W Aql and pi1 Gru exhibit the "30" micrometer feature attributed to MgS. Two sources exhibit a series of emission bands between 20 and 40 micrometer that we tentatively ascribe to Diopside. We show that the 10-20 micrometer spectra of the S stars are significantly different from the O-rich AGB stars. The O-rich stars exhibit a structured emission feature that is believed to arise from amorphous silicate and aluminium-oxide. The S stars lack the substructure found in the O-rich stars. Instead they show a smooth peak with a varying peak-position from source to source. We suggest that this feature is caused by a family of related material, whose exact composition determines the peak position. The observed trend mimics the laboratory trend of non-stoichiometric silicates. In this scenario the degree of non-stoichiometry is related to the Mg to SiO4 ratio, in other words, to the amount of free O available during the dust grain growth.