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Abstract

The orbital parameters of a satellite revolving around 22 Kalliope indicate that the bulk density of this main-belt asteroid is 2.37 ± 0.4 grams per cubic centimeter. M-type asteroids such as Kalliope are thought to be the disrupted metallic cores of differentiated bodies. The lowdensity indicates that Kalliope cannot be predominantly composed of metal and may be composed of chondritic material with ∼30% porosity. The satellite orbit is circular, suggesting that Kalliope and its satellite have different internal structures and tidal dissipation rates. The satellite may be an aggregate of impact ejecta from an earlier collision with Kalliope.

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References and Notes

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We are grateful to M. Britton for follow-up observations at Palomar and to P. Goldreich, T. Ahrens, and M. Pritchard for insightful discussions. J.L.M. thanks S. Kulkarni for financial support. Some of the data presented here were obtained at the W. M. Keck Observatory, which is operated as a scientific partnership among the California Institute of Technology, the University of California, and the National Aeronautics and Space Administration. The observatory was made possible by the generous financial support of the W. M. Keck Foundation. We extend special thanks to those of Hawaiian ancestry on whose sacred mountain we are privileged to be guests. Without their generous hospitality, many of the observations presented here would not have been possible.

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Published In

Science
Volume 300 | Issue 5627
20 June 2003

Submission history

Received: 17 April 2003
Accepted: 19 May 2003
Published in print: 20 June 2003

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J. L. Margot* [email protected]
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA.
M. E. Brown
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA.

Notes

*
To whom correspondence should be addressed. E-mail: [email protected]

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