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A&A 406, 783-788 (2003)
DOI: 10.1051/0004-6361:20030750
Experimental study of amorphous silicate formation
S. Wada1, Y. Murata1, A. T. Tokunaga2 and J. Watanabe11 Department of Applied Physics and Chemistry, The University of Electro-Communications, Chofugaoka, Chofu, Tokyo 182-8585, Japan
2 Institute for Astronomy, University of Hawaii, 2680 Woodlawn Dr., Honolulu, HI 96822, USA
(Received 29 January 2003 / Accepted 13 May 2003)
Abstract
Broad infrared bands at 10 and 18
m have often been
observed around oxygen-rich evolved stars, and these are thought to
arise from amorphous silicate dust grains. In order to study the
formation mechanism of silicate dust grains, we have analyzed
synthesized silicate dust analogs by reflection absorption infrared
spectroscopy (RAIRS) and X-ray photoelectron spectroscopy (XPS). The
dust analog was produced from SiO and Mg vapors in O
2. The
analyses showed that an amorphous silicate is formed at about
temperature of 650 K through O-deficient silicate formation.
However, when the substrate temperature was below 650 K, the main product
is a mixture of SiO
x and MgO, where
. Our experimental
results indicate that temperature is an important factor for amorphous
silicate formation in the circumstellar environment of oxygen-rich
evolved stars.
Key words: ISM: dust, extinction -- circumstellar matter -- stars: mass loss -- methods: laboratory
Offprint request: S. Wada, wada@e-one.uec.ac.jp
© ESO 2003
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