Oxygen and iron in interstellar dust: an X-ray investigation

TL;DR

This study uses X-ray observations to analyze the chemical composition and crystallinity of interstellar dust, focusing on oxygen and iron, revealing dominant Mg-rich silicates and significant iron depletion in the ISM.

Contribution

It introduces new X-ray dust extinction cross sections from laboratory data and applies them to analyze dust composition along multiple sight-lines in the Galaxy.

Findings

Mg-rich amorphous pyroxene dominates dust composition (~70%)

Approximately 15% of dust column density is metallic iron

Over 90% of iron is depleted into dust, while oxygen depletion is mild

Abstract

Understanding the chemistry of the interstellar medium (ISM) is fundamental for the comprehension of the Galactic and stellar evolution. X-rays provide an excellent way to study the dust chemical composition and crystallinity along different sight-lines in the Galaxy. In this work we study the dust grain chemistry in the diffuse regions of the interstellar medium in the soft X-ray band (<1 keV). We use newly calculated X-ray dust extinction cross sections, obtained from laboratory data, in order to investigate the oxygen K and iron L shell absorption. We explore the XMM-Newton and Chandra spectra of 5 low-mass X-ray binaries located in the Galactic plane, and we model the gas and dust features of oxygen and iron simultaneously. The dust samples used for this study include silicates with different Mg:Fe ratios, sulfides, iron oxides and metallic iron. Most dust samples are in both amorphous and crystalline lattice configuration. The extinction cross sections have been computed using Mie scattering approximation and assuming a power law dust size distribution. We find that the Mg-rich amorphous pyroxene (Mg0.75Fe0.25SiO3) represents the largest fraction of dust towards most of the X-ray sources, about 70% on average. Additionally, we find that ~15% of the dust column density in our lines of sight is in Fe metallic. We do not find strong evidence for ferromagnetic compounds, such as Fe3O4 or iron sulfides (FeS, FeS2). Our study confirms that the iron is heavily depleted from the gas phase into solids; more than 90% of iron is in dust. The depletion of neutral oxygen is mild, between 10-20% depending on the line of sight.