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A&A 466, 1153-1158 (2007)
DOI: 10.1051/0004-6361:20066276
Surface heterogeneity of 2005 UD from photometric observations
D. Kinoshita1, K. Ohtsuka2, T. Sekiguchi3, J. Watanabe3, T. Ito3, H. Arakida4, T. Kasuga3, S. Miyasaka5, R. Nakamura6, and H.-C. Lin11 Institute of Astronomy, National Central University, 300 Jhongda Rd., Jhongli, Taoyuan, 32001, Taiwan
e-mail: kinoshita@astro.ncu.edu.tw
2 Tokyo Meteor Network, 1-27-5 Daisawa, Setagaya, Tokyo, 155-0032, Japan
3 National Astronomical Observatory of Japan, 2-21-1 Osawa, Mitaka, Tokyo, 181-8588, Japan
4 Waseda University, 1-6-1 Nishi-Waseda, Shinjuku, Tokyo, 169-8050, Japan
5 Tokyo Metropolitan Government, 2-8-1 Nishi-Shinjuku, Shinjuku, Tokyo, 163-8001, Japan
6 Grid Technology Research Center, National Institute of Advanced Industrial Science and Technology, Central 2, 1-1-1 Umezono, Tsukuba, Ibaraki, 305-8568, Japan
(Received 20 August 2006 / accepted 28 November 2006)
Abstract
Context.The recently discovered Apollo-type near-Earth asteroid 2005 UD has
been suggested to be a fragment of (3200) Phaethon.
Aims.To test this hypothesis, we carried out photometric observations of
2005 UD using the 1-m telescope at Lulin Observatory.
Methods.Multi-color photometry was used to compare the surface
properties of (3200) Phaethon and 2005 UD. Surface-color
variation due to the rotation was also examined.
Results.The time-resolved differential photometry showed clear brightness
variation, and the lightcurve was fitted with a rotation
period of 5.23 h and an amplitude of 0.44 mag. Using
this rotational lightcurve, we derived the surface colors of 2005
UD. The surface of 2005 UD exhibits colors similar to those of F-
and B-type asteroids, which is consistent with (3200)
Phaethon. Furthermore, the (R-I) color of 2005 UD shows
variation during the rotation of the body.
Conclusions.The similarity of surface colors between (3200) Phaethon and 2005
UD observationally supports the hypothesis that 2005 UD is likely to
be a fragment of (3200) Phaethon. A simple explanation for the
inhomogeneity of the surface is that we see the surface and
subsurface of the precursor object. Another explanation is the
topographical structure that such as a large crater causes on this
heterogeneous surface.
Key words: minor planets, asteroids -- comets: general -- meteors, meteoroids -- techniques: photometric
© ESO 2007
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