The American Astronomical Society (AAS), established in 1899 and based in Washington, DC, is the major organization of professional astronomers in North America. Its membership of about 7,000 individuals also includes physicists, mathematicians, geologists, engineers, and others whose research and educational interests lie within the broad spectrum of subjects comprising contemporary astronomy. The mission of the AAS is to enhance and share humanity's scientific understanding of the universe.
Volatile Loss and Retention on Kuiper Belt Objects
E. L. Schaller andM. E. Brown
Published 2007 March 14 • © 2007. The American Astronomical Society. All rights reserved. Printed in U.S.A.
The Astrophysical Journal,Volume 659,Number 1Citation E. L. Schaller and M. E. Brown 2007ApJ659 L61DOI 10.1086/516709
E. L. Schaller
AFFILIATIONS
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125
M. E. Brown
AFFILIATIONS
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125
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- Received2006 November 6
- Accepted2007 February 23
- Published2007 March 14
Abstract
Recent discoveries have shown that the very largest Kuiper Belt objects—Eris, 2005 FY9, and Sedna—are coated in methane and may contain other volatile ices as well. New detailed observations show that even within this class of volatile-rich bodies, unexpected differences exist in their surface compositions. 2005 FY9, a body approximately 60% the size of Pluto, with a reflectance spectrum similarly dominated by methane, has a surface depleted in molecular nitrogen by at least an order of magnitude with respect to Pluto. We find that the existence of this new class of volatile-rich objects, the lack of volatiles on most Kuiper Belt objects, and even the otherwise peculiar surface of 2005 FY9 can be explained as a consequence of atmospheric escape of volatile compounds. While previous studies of the surface compositions of objects in the Kuiper Belt have found no explainable patterns, atmospheric escape appears to provide a first-order explanation of the range of surface spectra seen on bodies in the outer solar system.
