Techniques d'observation spectroscopique d'astéroïdes

Techniques d'observation spectroscopique d'astéroïdes Techniques d'observation spectroscopique d'astéroïdes

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34 CHAPTER 1. WHY ASTEROIDS? tel-00785991, version 1 - 7 Feb 2013 Figure 1.1: A field obtained with INT-WFC on February 28, 2012. Ten asteroids were identified (marked with pink), from which only three were known at the moment of the observation. The size of the field is (15 arcmin x 15 arcmin) In January 1801, the abbot Giuseppe Piazzi discovered Ceres, a small body at just the right distance. In 1802 Heinrich Olbers discovered Pallas at the same orbital distance. In the following years, Juno (1804) and Vesta (1807) were discovered also at similar orbital distances with Ceres and Pallas. These bodies were too small to be classified as planets, but the gap was filled. At the beginning of the XIX century, only comets were known to be small objects orbiting the Sun, but they appear like diffuse objects. Herschel, one of the most known astronomers at that time called these objects (Ceres, Palas, Juno, Vesta) asteroids (from Greek "asteroeides"). In this way it was underlined their different appearance - point sources ("star-like") unresolved by the telescopes, compared with the comets which show extended comas. The first theory of the origin of asteroids, was developed by Olbers in 1803, who suggested that they are fragments of a planet that had been broken to pieces and additional fragments will be found. This prediction became popular, while other asteroids were discovered orbiting at the same solar distance. With the increasing number of these new findings the hypothesis that they could be fragments of an exploded planet became very popular. In the middle of the 20th century Otto Johannes Schmidt proposed that asteroids represented an arrested stage of planet formation and have never been assembled into a large body. This is now the most plausible hypothesis. The apparition of photography, offered new means for finding new asteroids. The method consists in comparison of photographic films of the same region of the sky taken at different time intervals. The vast majority of the objects recorded on films were stars and galaxies and

CHAPTER 1. WHY ASTEROIDS? 35 tel-00785991, version 1 - 7 Feb 2013 their images were located in the same relative positions on all photographic films. Because a moving asteroid would be in a slightly different position on each picture exposure and the background stars and galaxies were not, it could be identified. Nowadays the charge coupled devices (CCD) are used instead of photography. While, the CCD technology is more sensitive and accurate than the older photographic methods, the modern discovery technique itself is rather similar. Separated by several minutes, three or more CCD images are taken of the same region of the sky. These images are then compared to see if any asteroid has systematically moved to different positions on each of the separate images (Fig. 1.1). For a newly discovered object, the separation of the asteroid location from one image to another, the direction it appears to be traveling, and its brightness allow to estimate its orbital characteristics and roughly its size. For example, an object that appears to be moving very rapidly from one image to the next one, is almost certainly very close to the Earth. Computeraided analyses of the CCD images have replaced the older, manual techniques for all the current asteroid search programs. Fig. 1.1 shows a field obtained with INT-WFC (Isaac Newton Telescope, Wide Field Camera) on the night of February 28, 2012. Ten asteroids could be identified in this field by taking consecutive images at an interval of five minutes. At the moment of the observation only three of the identified asteroids were known. Thanks to this technological development, during the last decades the total numbers of the asteroids discovered had grown exponentially. Among the most important surveys dedicated to asteroid detection (particularly to Near Earth Asteroids) are those leaded by the United States (CSS, LINEAR, Spacewatch, LONEOS and NEAT) which have been using large field, mostly 1m class telescopes. In the Europe the most important programs were: ASIAGO/ADAS in Italy and Germany, CINEOS in Italy, KLENOT in the Czech Republic, NEON in Finland. An example of successfully observing run is the one performed by [Boattini et al., 2004]. During two short runs at ESO (European Southern Observatory) LaSilla, they employed the MPG (Max Planck Gesellschaft) 2.2m telescope as a search facility, and the NTT (New Technology Telescope) 3.5m as a follow-up telescope to survey faint asteroids beyond 22 magnitude, for three observing nights. The authors observed about 700 Main Belt asteroids as faint as V 22 magnitude. They exposed between 60s and 150s in the R(red) band. To conclude this section, as of August 13, 2012 there are 588,219 observed asteroids from which 333,841 have the orbits well determined (as a consequence they were numbered) 2 . 1.3 Distribution and diversity of asteroids Asteroids are often grouped according to their orbital parameters. Fig. 1.2 shows the distribution of the asteroids as a function of their heliocentric distance. The majority of asteroids are 2 http://www.naic.edu/~nolan/astorb.html

CHAPTER 1. WHY ASTEROIDS? 35<br />

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

their images were located in the same relative positions on all photographic films. Because<br />

a moving asteroid would be in a slightly different position on each picture exposure and the<br />

background stars and galaxies were not, it could be identified.<br />

Nowadays the charge coupled devices (CCD) are used instead of photography. While, the<br />

CCD technology is more sensitive and accurate than the older photographic methods, the modern<br />

discovery technique itself is rather similar. Separated by several minutes, three or more<br />

CCD images are taken of the same region of the sky. These images are then compared to see<br />

if any asteroid has systematically moved to different positions on each of the separate images<br />

(Fig. 1.1).<br />

For a newly discovered object, the separation of the asteroid location from one image to<br />

another, the direction it appears to be traveling, and its brightness allow to estimate its orbital<br />

characteristics and roughly its size. For example, an object that appears to be moving very<br />

rapidly from one image to the next one, is almost certainly very close to the Earth. Computeraided<br />

analyses of the CCD images have replaced the older, manual techniques for all the current<br />

asteroid search programs.<br />

Fig. 1.1 shows a field obtained with INT-WFC (Isaac Newton Telescope, Wide Field Camera)<br />

on the night of February 28, 2012. Ten asteroids could be identified in this field by taking<br />

consecutive images at an interval of five minutes. At the moment of the observation only three<br />

of the identified asteroids were known.<br />

Thanks to this technological development, during the last decades the total numbers of the<br />

asteroids discovered had grown exponentially. Among the most important surveys dedicated to<br />

asteroid detection (particularly to Near Earth Asteroids) are those leaded by the United States<br />

(CSS, LINEAR, Spacewatch, LONEOS and NEAT) which have been using large field, mostly<br />

1m class telescopes. In the Europe the most important programs were: ASIAGO/ADAS in<br />

Italy and Germany, CINEOS in Italy, KLENOT in the Czech Republic, NEON in Finland.<br />

An example of successfully observing run is the one performed by [Boattini et al., 2004].<br />

During two short runs at ESO (European Southern Observatory) LaSilla, they employed the<br />

MPG (Max Planck Gesellschaft) 2.2m telescope as a search facility, and the NTT (New Technology<br />

Telescope) 3.5m as a follow-up telescope to survey faint asteroids beyond 22 magnitude,<br />

for three observing nights. The authors observed about 700 Main Belt asteroids as faint as V<br />

22 magnitude. They exposed between 60s and 150s in the R(red) band.<br />

To conclude this section, as of August 13, 2012 there are 588,219 observed asteroids from<br />

which 333,841 have the orbits well determined (as a consequence they were numbered) 2 .<br />

1.3 Distribution and diversity of asteroids<br />

Asteroids are often grouped according to their orbital parameters. Fig. 1.2 shows the distribution<br />

of the asteroids as a function of their heliocentric distance. The majority of asteroids are<br />

2 http://www.naic.edu/~nolan/astorb.html

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