Reviews in Mineralogy & Geochemistry Vol. 68, pp. XXX-XXX, 2008 12 Copyright © Mineralogical Society of America Oxygen and Asteroids Thomas H. Burbine1, Andrew S. Rivkin2, Sarah K. Noble3, Thais Mothé-Diniz4, William F. Bottke5, Timothy J. McCoy6, M. Darby Dyar1, and Cristina A. Thomas7 1Dept. of Astronomy, Mount Holyoke College, South Hadley, MA 01075, U.S.A. 2Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, U.S.A. 3NASA Johnson Space Center, Houston, TX 77058, U.S.A. 4Observatoire de Paris, 92195 Meudon Cedex, France 5Southwest Research Institute, Boulder, CO 80302, U.S.A. 6Department of Mineral Sciences, National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560-0119, U.S.A. 7Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, U.S.A. contact e-mail:
[email protected] ABSTRACT Hundreds of thousands of asteroids have been discovered in the asteroid belt and in near- Earth space. Oxygen is an abundant element in meteorites and presumably in most asteroids. Spectral refl ectance measurements of asteroids in the visible and near-infrared can identify oxygen-bearing minerals such as those found in the olivine, pyroxene, and serpentine groups due to their distinctive absorption features. Interpretation of the mineralogy of asteroids is complicated by the effects of space weathering, which tends to redden and darken the surfaces of asteroids. Asteroids are primarily classifi ed into a number of taxonomic classes and subclasses according to their spectral properties in the visible wavelength region. However, asteroids with similar spectral properties in the visible may have different spectral properties in the near- infrared and, therefore, different interpreted mineralogies.