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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,

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