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ABUNDANT CIRCUMSTELLAR SILICA DUST AND SiO GAS CREATED BY A GIANT HYPERVELOCITY COLLISION IN THE ~12 MYR HD172555 SYSTEM

C. M. Lisse et al 2009 ApJ 701 2019-2032   doi: 10.1088/0004-637X/701/2/2019  Help

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C. M. Lisse1,8, C. H. Chen2, M. C. Wyatt3, A. Morlok4,9, I. Song5, G. Bryden6 and P. Sheehan7
1 JHU-APL, 11100 Johns Hopkins Road, Laurel, MD 20723, USA
2 STScI, 3700 San Martin Drive, Baltimore, MD 21218, USA
3 Institute of Astronomy, University of Cambridge, Madingley Road, Cambridge CB3 0HA, UK
4 The Open University, Milton Keynes, MK7 6AA, UK
5 Department of Physics and Astronomy, The University of Georgia, Athens, GA 30602, USA
6 Jet Propulsion Laboratory, 4800 Oak Grove Drive, Pasadena, CA 91109, USA
7 Department of Physics and Astronomy, University of Rochester, Rochester, NY, USA
8 Address for correspondence: Planetary Exploration Group, Space Department, Johns Hopkins University, Applied Physics Laboratory, 11100 Johns Hopkins Road, Laurel, MD 20723, USA.
9 Current address: CRPG-CNRS, UPR2300, 15 rue Notre Dame des Pauvres, BP20, 54501 Vandoeuvre les Nancy, France.
E-mail: carey.lisse@jhuapl.edu, cchen@stsci.edu, wyatt@ast.cam.ac.uk, A.Morlok@open.ac.uk, song@uga.edu, Geoffrey.Bryden@jpl.nasa.gov and psheeha2@mail.rochester.edu

ABSTRACT. The fine dust detected by infrared (IR) emission around the nearby β Pic analog star HD172555 is very peculiar. The dust mineralogy is composed primarily of highly refractory, nonequilibrium materials, with approximately three quarters of the Si atoms in silica (SiO2) species. Tektite and obsidian lab thermal emission spectra (nonequilibrium glassy silicas found in impact and magmatic systems) are required to fit the data. The best-fit model size distribution for the observed fine dust is dn/da = a –3.95±0.10. While IR photometry of the system has stayed stable since the 1983 IRAS mission, this steep a size distribution, with abundant micron-sized particles, argues for a fresh source of material within the last 0.1 Myr. The location of the dust with respect to the star is at 5.8 ± 0.6 AU (equivalent to 1.9 ± 0.2 AU from the Sun), within the terrestrial planet formation region but at the outer edge of any possible terrestrial habitability zone. The mass of fine dust is 4 × 1019-2 × 1020 kg, equivalent to a 150-200 km radius asteroid. Significant emission features centered at 4 and 8 μm due to fluorescing SiO gas are also found. Roughly 1022 kg of SiO gas, formed by vaporizing silicate rock, is also present in the system, and a separate population of very large, cool grains, massing 1021-1022 kg and equivalent to the largest sized asteroid currently found in the solar system's main asteroid belt, dominates the solid circumstellar material by mass. The makeup of the observed dust and gas, and the noted lack of a dense circumstellar gas disk, strong stellar X-ray activity, and an extended disk of β meteoroids argues that the source of the observed circumstellar materials is a giant hypervelocity (>10 km s–1) impact between large rocky planetesimals, similar to the ones which formed the Moon and which stripped the surface crustal material off of Mercury's surface.

Key words: astrochemistry; infrared: stars; planetary systems: formation; planetary systems: protoplanetary disks; radiation mechanisms: thermal; techniques: spectroscopic

Print publication: Issue 2 (2009 August 20)
Received 2008 November 24, accepted for publication 2009 June 16
Published 2009 August 7

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