Techniques d'observation spectroscopique d'astéroïdes
Techniques d'observation spectroscopique d'astéroïdes
Techniques d'observation spectroscopique d'astéroïdes
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6<br />
Spectral properties of near-Earth asteroids<br />
tel-00785991, version 1 - 7 Feb 2013<br />
This chapter presents spectra of eight NEAs (1917, 8567, 16960, 164400, 188452, 2010 TD54, 5620, and<br />
2001 SG286 ) obtained using the NASA telescope IRTF equipped with the spectro-imager SpeX. The analysis<br />
of these spectra includes taxonomic classification, comparison with laboratory spectra from Relab database,<br />
and for the S-type objects the correspondent mineralogical models. I also attempted to interpret our data<br />
using a space-weathering model.<br />
The taxonomic classification of five objects was reviewed and a corresponding type was assigned to the other<br />
three asteroids that were not classified before. I found that (1917) Cuyo, (8567) 1996 HW1, (16960) 1998<br />
QS52, (188452) 2004 HE62, and 2010 TD54 are in the S-complex. For these S-type asteroids a good matching<br />
was found with spectra of ordinary chondrites meteorites.<br />
The asteroids (5620) Jasonwheeler and 2001 SG286 were classified as D-type objects. The spectrum of (5620)<br />
Jasonwheeler is similar to spectra of carbonaceous chondrite meteorites. The results found for the two objects<br />
confirm their primitive properties obtained in several other spectral intervals.<br />
Four of the observed objects have delta - V lower than 7 km/sec, which make them suitable targets in terms of<br />
propulsion for a future spacecraft mission.<br />
Near-Earth Asteroids (NEAs) are a continuously changing population of small bodies with<br />
orbits that come close to the Earth’s orbit. Their chaoticity defines them as a critical population,<br />
while several important gravitational field (those of the Sun, Jupiter, and the inner planets) are<br />
superimposed influencing their orbital movement.<br />
Because of the relatively short lifetime of these objects, it is necessary to understand the<br />
dynamical mechanisms of supplying those bodies which are lost (due to expulsion from the<br />
Solar System, falling into the Sun or on the telluric planets) and their reservoirs of objects from<br />
the Main Belt. According to Gladman et al. [2000] the median lifetime of the NEAs is 10 Myr.<br />
On the other hand, NEAs are among the most accessible bodies in the Solar System in terms<br />
of the spacecraft propulsion requirements to reach them. In this sense, the knowledge of the<br />
ensemble of physical parameters for these objects, including their composition, is a critical<br />
point in defining any mission scientific objectives. Currently, several programs (like Marco-<br />
Polo-R, Osiris-REx, Hayabusa2) are under development for space exploration of NEAs.<br />
Another point is that the objects in near-Earth space are a valuable source of information as<br />
they represent a mixture of the different populations of small bodies: main-belt asteroids and<br />
cometary nuclei [DeMeo & Binzel, 2008], and a link with meteorites [Vernazza et al., 2008,