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Crystalline Silicate Feature of the Vega-like Star HD 145263
Author(s) -
Mitsuhiko Honda,
Hirokazu Kataza,
Y. Okamoto,
Takashi Miyata,
Takuya Yamashita,
Shigeyuki Sako,
Takuya Fujiyoshi,
Meguru Ito,
Yoko Okada,
Itsuki Sakon,
Takashi Onaka
Publication year - 2004
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 - 10.1086/423242
Subject(s) - planetesimal , physics , silicate , forsterite , stars , meteorite , astrophysics , circumstellar dust , t tauri star , herbig ae/be star , olivine , cosmic dust , planetary system , solar system , planet , vega , astronomy , astrobiology , k type main sequence star , geochemistry , geology
We have observed the 8-13 $\mu$m spectrum (R$\sim$250) of the Vega-like starcandidate HD145263 using Subaru/COMICS. The spectrum of HD145263 shows thebroad trapezoidal silicate feature with the shoulders at 9.3 $\mu$m and 11.44$\mu$m, indicating the presence of crystalline silicate grains. This detectionimplies that crystalline silicate may also be commonly present around Vega-likestars. The 11.44 $\mu$m feature is slightly shifted to a longer wavelengthcompared to the usual 11.2-3 $\mu$m crystalline forsterite feature detectedtoward Herbig Ae/Be stars and T Tauri stars. Although the peak shift due to theeffects of the grain size can not be ruled out, we suggest that Fe-bearingcrystalline olivine explains the observed peak wavelength fairly well.Fe-bearing silicates are commonly found in meteorites and most interplanetarydust particles, which originate from planetesimal-like asteroids. According tostudies of meteorites, Fe-bearing silicate must have been formed in asteroidalplanetesimals, supporting the scenario that dust grains around Vega-like starsare of planetesimal origin, if the observed 11.44 $\mu$m peak is due toFe-bearing silicates.Comment: accepted for Publication in ApJ

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