The origin of (90) Antiope from component-resolved near-infrared spectroscopy

被引:11
作者
Marchis, F. [1 ,2 ,3 ]
Enriquez, J. E. [1 ]
Emery, J. P. [4 ]
Berthier, J. [3 ]
Descamps, P. [3 ]
Vachier, F. [3 ]
机构
[1] SETI Inst, Carl Sagan Ctr, Mountain View, CA 94043 USA
[2] Univ Calif Berkeley, Dept Astron, Berkeley, CA 94720 USA
[3] CNRS, Observ Paris, Inst Mecan Celeste & Calcul Ephemerides, UMR8028, F-75014 Paris, France
[4] Univ Tennessee, Knoxville, TN 37996 USA
基金
美国国家科学基金会;
关键词
Asteroids; Surfaces; Adaptive optics; Satellites of asteroids; Spectroscopy; ORGANICS; SURFACE; PHOBOS; ICE;
D O I
10.1016/j.icarus.2011.02.011
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The origin of the similarly-sized binary Asteroid (90) Antiope remains an unsolved puzzle. To constrain the origin of this unique double system, we recorded individual spectra of the components using SPIFFI, a near-infrared integral field spectrograph fed by SINFONI, an adaptive optics module available on VLT-UT4. Using our previously published orbital model, we requested telescope time when the separation of the components of (90) Antiope was larger than 0.087", to minimize the contamination between components, during the February 2009 opposition. Several multi-spectral data-cubes in J band (SNR = 40) and H + K band (SNR = 100) were recorded in three epochs and revealed the two components of (90) Antiope. After developing a specific photometric extraction method and running an error analysis by Monte-Carlo simulations, we successfully extracted reliable spectra of both components from 1.1 to 2.4 mu m taken on the night of February 21, 2009. These spectra do not display any significant absorption features due to mafic mineral, ices, or organics, and their slopes are in agreement with both components being C- or Cb-type asteroids. Their constant flux ratio indicates that both components' surface reflectances are quite similar, with a 1-sigma variation of 7%. By comparison with 2MASS J, H, K color distribution of observed Themis family members, we conclude that both bodies were most likely formed at the same time and from the same material. The similarly-sized system could indeed be the result of the breakup of a rubble-pile proto-Antiope into two equal-sized bodies, but other scenarios of formation implying a common origin should also be considered. (C) 2011 Elsevier Inc. All rights reserved.
引用
收藏
页码:252 / 264
页数:13
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