2018A&A...618A.170L


Query : 2018A&A...618A.170L

2018A&A...618A.170L - Astronomy and Astrophysics, volume 618A170-170 (2018/1-0)

The visible and near-infrared spectra of asteroids in cometary orbits.

LICANDRO J., POPESCU M., DE LEON J., MORATE D., VADUVESCU O., DE PRA M. and ALI-LAGOA V.

Abstract (from CDS):

Context. Dynamical and albedo properties suggest that asteroids in cometary orbits (ACOs) are dormant or extinct comets. Their study provides new insights for understanding the end-states of comets and the size of the comet population.
Aims. We intend to study the visible and near-infrared (NIR) spectral properties of different ACO populations and compare them to the independently determined properties of comets.
Methods. We select our ACOs sample based on published dynamical criteria and present our own observational results obtained using the 10.4m Gran Telescopio Canarias (GTC), the 4.2m William Herschel Telescope (WHT), the 3.56m Telescopio Nazionale Galileo (TNG), and the 2.5m Isaac Newton Telescope (INT), all located at the El Roque de los Muchachos Observatory (La Palma, Spain), and the 3.0m NASA Infrared Telescope Facility (IRTF), located at the Mauna Kea Observatory, in Hawaii. We include in the analysis the spectra of ACOs obtained from the literature. We derive the spectral class and the visible and NIR spectral slopes. We also study the presence of hydrated minerals by studying the 0.7µm band and the UV-drop below 0.5µm associated with phyllosilicates.
Results. We present new observations of 17 ACOs, 11 of them observed in the visible, 2 in the NIR and 4 in the visible and NIR. We also discuss the spectra of 12 ACOs obtained from the literature. All but two ACOs have a primitive-like class spectrum (X or D-type). Almost 100% of the ACOs in long-period cometary orbits (Damocloids) are D-types. Those in Jupiter family comet orbits (JFC-ACOs) are ∼60% D-types and ∼40% X-types. The mean spectral slope S' of JFC-ACOs is 9.7±4.6%/1000Å and for the Damocloids this is 12.2±2.0%/1000Å. No evidence of hydration on the surface of ACOs is found from their visible spectra. The spectral slope and spectral class distribution of ACOs is similar to that of comets.
Conclusions. The spectral taxonomical classification and the spectral slope distribution of ACOs, and the lack of spectral features indicative of the presence of hydrated minerals on their surface, strongly suggest that ACOs are likely dormant or extinct comets.

Abstract Copyright: © ESO 2018

Journal keyword(s): comets: general - minor planets, asteroids: general - techniques: spectroscopic - methods: observational

Simbad objects: 14

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Number of rows : 14
N Identifier Otype ICRS (J2000)
RA
ICRS (J2000)
DEC
Mag U Mag B Mag V Mag R Mag I Sp type #ref
1850 - 2026
#notes
1 HD 28099 BY* 04 26 40.1217122952 +16 44 48.885808416 8.98 8.78 8.12 7.56 7.23 G2+V 450 0
2 HD 29714 PM* 04 41 42.6209425200 +22 37 23.824694316   9.98 9.32     G5V 12 0
3 HD 283886 * 04 51 00.6318387768 +24 07 21.573684120   10.48 9.88     G5 18 0
4 HD 259516 PM* 06 34 19.1789591112 +31 00 40.931433972   9.85 9.23     ~ 11 0
5 HD 292561 * 06 51 33.7279522392 -00 11 31.525152072 11.277 11.183 10.574 10.226 9.905 F8 69 0
6 HD 56513 PM* 07 18 28.8688480320 +27 15 10.269640980   8.70   7.6   G2V 69 0
7 HD 79078 * 09 12 24.0749513016 +14 43 40.284024132   10.03 9.40     G2V 12 0
8 BD+00 2717 Em* 10 57 04.0451198496 -00 13 12.886813308 10.822 10.567 9.903 9.537 9.206 F9 87 0
9 BD+00 3383 * 15 38 16.2782442528 +00 15 21.660013476   11.10 10.50     ~ 36 0
10 HD 142801 * 15 56 55.4364195480 -12 58 10.013939184   10.60 9.97     G2V 18 0
11 HD 144821 PM* 16 08 16.5824683968 -13 46 08.592923640   8.08 7.48     G2V 35 0
12 BD-00 4074 * 20 43 11.9568455592 +00 26 13.074647820   10.63 9.90     F8 50 0
13 HD 198273 PM* 20 49 29.4223614433 -08 39 09.007701794   9.02 8.45     G2V 42 0
14 HD 206938 PM* 21 45 30.3036763536 +00 40 39.837258264   9.93 9.20     G5V 12 0

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