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A radar survey of M- and X-class asteroids
Authors:Michael K Shepard  Beth Ellen Clark  Ellen S Howell  Jon D Giorgini  Steven J Ostro  Brian Warner  Petr Pravec  Thomas Bennett  Raoul Behrend  Josep Coloma  Andrew Rivkin
Institution:a Department of Geography and Geosciences, Bloomsburg University of Pennsylvania, 400 E. Second St., Bloomsburg, PA 17815, USA
b Ithaca College, Ithaca, NY 14853, USA
c NAIC/Arecibo Observatory, HC 3 Box 53995, Arecibo, PR 00612, USA
d University of Maine at Farmington, Farmington, ME 04938, USA
e Jet Propulsion Laboratory, Pasadena, CA 91109, USA
f Space Science Institute, La Canada, CA 91011-3364, USA
g Palmer Divide Observatory/Space Science Institute, Colorado Springs, CO, USA
h Carbuncle Hill Observatory, Greene, RI, USA
i Astronomical Institute, Academy of Sciences of the Czech Republic, Ondrejov, CZ-25165, Czech Republic
j Florida Gulf Coast University, Ft. Meyers, FL 33965, USA
k TAROT, Haute-Provence Observatory, St.-Michel l'Observatoire, France
l TAROT, Centre d'Astronomie de St.-Michel l'Observatoire, France
m Agrupacion Astronomica de Sabadell, Sabadell, Barcelona, Spain
n Osservatorio Astronomico Vallemare di Borbona, Rome, Italy
o Johns Hopkins Applied Physics Laboratory, Laurel, MD 20723, USA
Abstract:We observed ten M- and X-class main-belt asteroids with the Arecibo Observatory's S-band (12.6 cm) radar. The X-class asteroids were targeted based on their albedos or other properties which suggested they might be M-class. This work brings the total number of main-belt M-class asteroids observed with radar to 14. We find that three of these asteroids have rotation rates significantly different from what was previously reported. Based on their high radar albedo, we find that only four of the fourteen—16 Psyche, 216 Kleopatra, 758 Mancunia, and 785 Zwetana—are almost certainly metallic. 129 Antigone has a moderately high radar albedo and we suggest it may be a CH/CB/Bencubbinite parent body. Three other asteroids, 97 Klotho, 224 Oceana, and 796 Sarita have radar albedos significantly higher than the average main belt asteroid and we cannot rule out a significant metal content for them. Five of our target asteroids, 16 Psyche, 129 Antigone, 135 Hertha, 758 Mancunia, and 785 Zwetana, show variations in their radar albedo with rotation. We can rule out shape and composition in most cases, leaving variations in thickness, porosity, or surface roughness of the regolith to be the most likely causes. With the exception of 129 Antigone, we find no hydrated M-class asteroids (W-class; Rivkin, A.S., Howell, E.S., Lebofsky, L.A., Clark, B.E., Britt, D.T., 2000. Icarus 145, 351-368) to have high radar albedos.
Keywords:Asteroids  Asteroids  composition  Surfaces  asteroids
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