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Pixie Dust: The Silicate Features in the Diffuse Interstellar Medium
Author(s) -
J. E. Chiar,
A. G. G. M. Tielens
Publication year - 2006
Publication title -
the astrophysical journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.376
H-Index - 489
eISSN - 1538-4357
pISSN - 0004-637X
DOI - 10.1086/498406
Subject(s) - silicate , extinction (optical mineralogy) , cosmic dust , interstellar medium , astrophysics , physics , pyroxene , interplanetary dust cloud , absorption (acoustics) , presolar grains , analytical chemistry (journal) , mineralogy , olivine , stars , astronomy , chemistry , galaxy , nucleosynthesis , solar system , optics , chromatography
We have analyzed the 9.7 and ``18'' micron interstellar silicate absorptionfeatures along the line of sight toward four heavily extincted galactic WC-typeWolf-Rayet (WR) stars. We construct two interstellar extinction curves from1.25 to 25 micron using near-IR extinction measurements from the literaturealong with the silicate profiles of WR 98a (representing the local ISM) and GCS3 (representing the Galactic Center). We have investigated the mineralogy ofthe interstellar silicates by comparing extinction profiles for amorphoussilicates with olivine and pyroxene stochiometry to the 9.7 and ``18'' micronabsorption features in the WR 98a spectrum. In this analysis, we haveconsidered solid and porous spheres and a continuous distribution ofellipsoids. While it is not possible to simultaneously provide a perfect matchto both profiles, we find the best match requires a mixture of these two typesof compounds. We also consider iron oxides, aluminosilicates and silicatecarbide (SiC) as grain components. Iron oxides cannot be accommodated in theobserved spectrum, while the amount of Si in SiC is limited to <4%. Finally, wediscuss the cosmic elemental abundance constraints on the silicate mineralogy,grain shape and porosity.Comment: 34 pages, 8 figures, 7 table

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