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Near-infrared spectroscopic survey of B-type asteroids: Compositional analysis
Authors:J de León  N Pinilla-Alonso  H Campins  J Licandro  GA Marzo
Institution:1. Instituto de Astrofísica de Andalucía – CSIC, Glorieta de la Astronomía s/n, E-18008 Granada, Spain;2. Instituto Nacional de Ciência e Tecnologia de Astrofísica, Rua do Matão, 1226 – sala 201/F – Cidade Universitária, Sao Paolo, Brazil;3. SETI Institute – 189 Bernardo Ave., Suite 100, Mountain View, CA 94043, USA;4. Observatório do Valongo: Ladeira Pedro Antonio, 43, 20080-090 Rio de Janeiro, Brazil;5. University of Central Florida, Physics Department, P.O. Box 162385, Orlando, FL 32816.2385, USA;6. Instituto de Astrofísica de Canarias, C/Vía Láctea s/n, E-38205 La Laguna, Spain;7. Departamento de Astrofísica, Universidad de La Laguna (ULL), E-38205 La Laguna, Spain;8. ENEA, C.R. Casaccia, Via Anguillarese 301, 00123 Roma, Italy
Abstract:We present near-infrared spectra of 23 B-type asteroids obtained with the NICS camera-spectrograph at the 3.56 m Telescopio Nazionale Galileo. We also compile additional visible and near-infrared spectra of another 22 B-type asteroids from the literature. A total of 45 B-types are analyzed. No significant trends in orbital properties of our sample were detected when compared with all known B-types and all known asteroids. The reflectance spectra of the asteroids in the 0.8–2.5 μm range show a continuous shape variation, from a monotonic negative (blue) slope to a positive (red) slope. This continuous spectral trend is filling the gap between the two main groups of B-types published by Clark et al. (2010]. J. Geophys. Res., 115, 6005–6027). We found no clear correlations between the spectral slope and the asteroids’ sizes or heliocentric distances. We apply a clustering technique to reduce the volume of data to six optimized “average spectra” or “centroids”, representative of the whole sample. These centroids are then compared against meteorite spectra from the RELAB database. We found carbonaceous chondrites as the best meteorite analogs for the six centroids. There is a progressive change in analogs that correlates with the spectral slope: from CM2 chondrites (water-rich, aqueously altered) for the reddest centroid, to CK4 chondrites (dry, heated/thermally altered) for the bluest one.
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