A&A 395, 297-303 (2002)
DOI: 10.1051/0004-6361:20021265
ESO large program on physical studies of Transneptunian Objects and Centaurs: Visible photometry - First results
H. Boehnhardt1, A. Delsanti1, 2, A. Barucci2, O. Hainaut1, A. Doressoundiram2, M. Lazzarin3, L. Barrera4, C. de Bergh2, K. Birkle5, E. Dotto6, 7, K. Meech8, J. E. Ortiz9, J. Romon2, T. Sekiguchi10, N. Thomas11, G. P. Tozzi12, J. Watanabe10 and R. M. West131 European Southern Observatory ESO, Alonso de Cordova 3107, Santiago de Chile, Chile
2 Observatoire de Paris-Meudon, 5 place Jules Janssen, 92195 Meudon Cedex, France
3 Astronomical Observatory of Padova, Vicolo dell' Osservatorio 5, 35122 Padova, Italy
4 Institute for Astronomy, Universidad Catolica del Norte, Antofagasta, Chile
5 Max-Planck-Institut für Astronomie, Königstuhl 17, 69117 Heidelberg, Germany
6 INAF - Observatorio Astronomico di Torino, Strada Osservatorio 20, 10025 Pino Torinese (TO), Italy
7 INAF - Osservatorio Astronomico di Roma, via Frascati 33, 00040 Monteporzio Catone (Roma), Italy
8 University of Hawaii, 2680 Woodlawn Drive, Honolulu, Hawaii 96822, USA
9 Instituto de Astronomia de Andalucia, PO Box 3004, 18080 Granada, Spain
10 National Astronomical Observatory, Osawa 2-21-1, Mitaka, Tokyo, Japan
11 Max-Planck-Institut für Aeronomie, Postfach 20, 37189 Katlenburg-Lindau, Germany
12 Osservatorio Astrofisico di Arcetri, Largo E. Fermi 5, 50125 Firenze, Italy
13 European Southern Observatory ESO, Karl-Schwarzschild-Str. 2, 85748 Garching, Germany
(Received 7 May 2002 / Accepted 30 August 2002)
Abstract
We present the first results of
BVRI photometry of Transneptunian
Objects (TNOs) and Centaurs obtained through the ESO Large Program on physical
studies of these icy bodies in the outer solar system. In total 28 objects
were observed of which 18 are new measurements.
Combining our new
BVRI photometry with the data summary published
by Hainaut & Delsanti (2002) results in a database of 94 objects: 45 Cubewanos,
22 Plutinos, 13 scattered disk objects, 14 Centaurs.
The reddening range seems to be similar
among the four dynamical classes (
-5 to 55%/l00 nm) and only one outlier
(1994 ES
2) exists. The spectral gradient distribution of the Cubewanos
peaks between 25 to 35%/l00 nm, while for the three other types the maximum
seems to fall below 20%/l00 nm. A clustering
of red Cubewanos with perihelia beyond ~41 AU in low eccentricity and
low inclination orbit suggests that these objects are less affected by the
physical processes that potentially produce neutral colors, i.e. resurfacing
by collision and by intrinsic activity. For Cubewanos and scattered disk
objects, the range of reddening increases with decreasing perihelion distance
and with increasing orbital excitation. A correlation of the spectral
slope with inclination is present for Cubewanos and scattered
disk objects, and is non-existent for the other dynamical types. It is
unclear whether these trends (or their absence) are discriminative for the
correctness of the resurfacing scenarios. If intrinsic activity is
responsible for resurfacing, the start of the effect inside ~41 AU from
the Sun may be indicative for the driving agent, while in the collision
scenario the survival of the red Cubewano cluster in the central region
of the Kuiper-Belt argues for the existence of a population of bodies the
surface of which is heavily radiation processed without impact resurfacing.
Key words: Kuiper-Belt -- minor planets, asteroids -- techniques: photometric
Offprint request: H. Boehnhardt, hboehnha@eso.org
© ESO 2002

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