Contents of: VI/111/./abstract/JSTAUFFE_ASTARS_5.abs

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 A detailed understanding of the genesis of planets is one of the
 major goals for the astronomical community, equal in import to
 investigation of the origin of the universe as a whole.  IRAS
 provided the first important step towards such an understanding
 with the discovery of resolved dust disks surrounding three nearby
 A stars (Beta Pic, Fomalhaut and Vega).  Models constructed
 to explain these data have concluded that the dust responsible for
 the infrared emission seen by IRAS is most plausibly produced by
 collisions of larger planetesimals, perhaps during an evolutionary
 phase similar to the "era of maximum bombardment" when the planets
 in our solar system were assembled, and thus that these disks
 are signatures of planet formation.

 The next critical steps in deepening our understanding would be
 to establish the fraction of stars which ultimately produce
 "debris disks", and to infer the time history of planetesimal
 collisions from observations of the evolution of these disks.

 We propose a program aimed at achieving these goals from ISO PHT
 observations of a sample of about 60 A stars selected from four
 nearby open clusters spanning a range of ages from the epoch just
 following the end of the disk accretion phase (t   5 - 10 Myr) to
 an age comparable to that of Vega and Beta Pic.  We will measure
 the entire sample at 60 microns and do a subset of the stars in
 the two youngest clusters at 25, 60 and 100 microns.  When
 combined with ground-based JHK and 10 micron photometry, these
 observations will allow us to measure the timescale for the inner
 disk clearing which is observed in the three prototype A stars.
 This program is complementary to the extant GTO program because
 it samples stars in a critical age range: 5 < t < 30 Myr.