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Techniques d'observation spectroscopique d'astéroïdes

Techniques d'observation spectroscopique d'astéroïdes

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CHAPTER 7. SPECTRAL PROPERTIES OF MAIN BELT ASTEROIDS 115<br />

Table 7.3: Solar analogs used for data reduction, their airmass at the moment of observations and their relative<br />

distance to the object.<br />

Asteroid Solar Analogue Air mass Distance [ ◦ ]<br />

(9147) Kourakuen HD940 1.280 11.5<br />

(854) Frostia G104-335 1.070 11.3<br />

(1333) Cevenola HD127913 1.055 10.1<br />

(1333) Cevenola HD127913 1.031 10.2<br />

(3623) Chaplin HD73708 1.025 6.6<br />

(3623) Chaplin HD73708 1.018 6.6<br />

(10484) Hecht Land115-271 1.200 19.5<br />

(31569) 1999 FL18 Land115-271 1.200 15.1<br />

tel-00785991, version 1 - 7 Feb 2013<br />

The following stars were observed and used as solar analogs: HD940, G104-335, HD127913,<br />

HD73708 and L115-256 (Table 7.3). Our choice was to observe the solar analogue as close<br />

as possible to the target (bellow 20 o ). The differential airmass between the asteroid and the<br />

standard was usually restricted to less than 0.16. The stars were chosen using the tool available<br />

on IRTF website 1 . An exception was made for (10484) Hecht and (31569) 1999 FL18,<br />

where the data reduction were performed using L115-271, commonly used in NIR spectral<br />

measurements.<br />

G104-335, HD127913, HD73708 are G2V type, while HD940 is a K0 star [Høg et al., 2000,<br />

Cutri et al., 2003, Landolt, 1992]. HD 940 was chosen as trade-off between the spectral type,<br />

airmass, and its relative distance to (9147) Kourakuen.<br />

The data reduction followed the procedure described in chapter 3. For the computation of<br />

the final reflectance (ratio between the asteroid spectrum and the star spectrum) is considered<br />

the similar dynamic regimes of the detector [Vacca et al., 2004, Rayner et al., 2003].<br />

7.2 (9147) Kourakuen - a V-type asteroid outside Vesta family<br />

One of the most interesting asteroid family is the one of (4) Vesta. Located in the inner asteroid<br />

belt, the origins of this family is in a collision event that excavated a large crater in the<br />

surface of asteroid (4) Vesta [Asphaug, 1997]. The presence of such a crater in the south hemisphere<br />

of the asteroid has been confirmed by HST images [Thomas et al., 1997] and recently<br />

by NASA’s Dawn spacecraft. This crater, called Rheasilvia, has 505 Km in diameter and is one<br />

of the largest craters in the Solar System. The latest estimates indicate that the cratering event<br />

occurred at least 1.2 Gyr ago [Carruba et al., 2005].<br />

(4) Vesta is particularly interesting because it is the only large asteroid showing a basaltic<br />

crust [McCord et al., 1970]. Basaltic asteroids are believed to derive from bodies whose interiors<br />

reached the melting temperature of silicate rocks and subsequently differentiated<br />

[Gaffey et al., 2002]. Thus, (4) Vesta is a differentiated object with a basaltic crust and exposed<br />

mantle material [Gaffey, 1997] that survived during the Solar System history. It is considered<br />

1 http://irtfweb.ifa.hawaii.edu/cgi-bin/spex/find_a0v.cgi

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