arXiv subjects

S. Zeidler

Publications and source records attributed to S. Zeidler.

2 recordsLinked to original sources

arXiv2016

Absorption and scattering by interstellar dust in the silicon K-edge of GX 5-1

We study the absorption and scattering of X-ray radiation by interstellar dust particles, which allows us to access the physical and chemical properties of dust. The interstellar dust composition is not well understood, especially on the densest sight lines of the Galactic Plane. X-rays provide a powerful tool in this study. We present newly acquired laboratory measurements of silicate compounds taken at the Soleil synchrotron facility in Paris using the Lucia beamline. The dust absorption profiles resulting from this campaign were used in this pilot study to model the absorption by interstellar dust along the line of sight of the low-mass X-ray binary (LMXB) GX 5-1. The measured laboratory cross-sections were adapted for astrophysical data analysis and the resulting extinction profiles of the Si K-edge were implemented in the SPEX spectral fitting program. We derive the properties of the interstellar dust along the line of sight by fitting the Si K-edge seen in absorption in the spectrum of GX 5-1. We measured the hydrogen column density towards GX 5-1 to be $3.40\pm0.1\times10^{22} \rm cm^{-2}$. The best fit of the silicon edge in the spectrum of GX 5-1 is obtained by a mixture of olivine and pyroxene. In this study, our modeling is limited to Si absorption by silicates with different Mg:Fe ratios. We obtained an abundance of silicon in dust of $4.0\pm0.3\times10^{-5}$ per H atom and a lower limit for total abundance, considering both gas and dust, of $>4.4\times10^{-5}$ per H atom, which leads to a gas to dust ratio of >0.22. Furthermore, an enhanced scattering feature in the Si K-edge may suggest the presence of large particles along the line of sight.

astro-ph.GA↗

arXiv2008

Far-infrared spectra of hydrous silicates at low temperatures - Providing laboratory data for Herschel and ALMA

Hydrous silicates occur in various cosmic environments, and are among the minerals with the most pronounced bands in the far infrared (FIR) spectral region. Given that Herschel and ALMA will open up new possibilities for astronomical FIR and sub-mm spectroscopy, data characterizing the dielectric properties of these materials at long wavelengths are desirable. We aimed at examining the FIR spectra of talc, picrolite, montmorillonite, and chamosite, which belong to four different groups of phyllosilicates. We tabulated positions and band widths of the FIR bands of these minerals depending on the dust temperature. By means of powder transmission spectroscopy, spectra of the examined materials were measured in the wavelength range 25-500 mum at temperatures of 300, 200, 100, and 10 K. Room-temperature measurements yield the following results. For talc, a previously unknown band, centered at 98.5 mum, was found, in addition to bands at 56.5 and 59.5 mum. For montmorillonite, several bands at wavelengths <110 mum were detected, including a band at 105 mum with an FWHM of about 10 mum. Picrolite shows a sharp 77 mum FIR band. Chamosite is characterized by bands in the 72-92 mum range, and a prominent band at 277 mum. At decreasing temperature, most of the bands shift to shorter wavelengths. Examining a potential counterpart of the 105mum band in the spectra of HD 142527 and HD 100546, we find that the broad band in the spectra of these young stars - extending from 85 to 125 mum - cannot be due to montmorillonite or any of the hydrous silicates we studied, since these materials have sharper bands in the FIR wavelength range than previously assumed, especially at low temperatures.

astro-ph↗