Techniques d'observation spectroscopique d'astéroïdes
Techniques d'observation spectroscopique d'astéroïdes Techniques d'observation spectroscopique d'astéroïdes
32 CHAPTER 1. WHY ASTEROIDS? tel-00785991, version 1 - 7 Feb 2013 of years [Yin et al., 2002]. After this period strong solar winds begin to clear dust from the Solar System, leaving the minor bodies and planets with a paucity of new material to accumulate. The asteroids are remnants of the planetesimal population that once formed the planets. Even if some of the asteroids were affected by thermal and dynamical evolution and by collisions, most of them did not suffer a significant geological evolution preserving the physical evidences related to the first 200 million years of the Solar System history . Currently, there is a wide diversity of bodies in the Solar System, thus in order to facilitate their studies and the discussions some definitions are required for different categories. The definitions of a planet, dwarf planet, and of a small body given below were assigned in Resolution 5 and 6 of the IAU (International Astronomical Union) 2006 General Assembly 1 . According to this resolution, a planet is a a celestial body that: a) is in orbit around the Sun, b) has sufficient mass for its self-gravity to overcome rigid body forces so that is assumes a hydrostatic equilibrium - nearly round shape, and c) has cleared the neighborhood around its orbit. A dwarf planet is a celestial body that a) is in orbit around the Sun, b) has sufficient mass for its self-gravity to overcome rigid body forces so that is assumes a hydrostatic equilibrium - nearly round shape, c) has not cleared the neighborhood around its orbit, and d) is not a satellite of a planet. Plutoids are dwarf planets with a semi-major axis greater than that of Neptune. All other objects except satellites orbiting the planets shall be referred collectively as small bodies of Solar System (are also called minor planets). Following these definitions, there are eight planets in our Solar System: Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, and Neptune. Pluto is a dwarf planet, also as Ceres, Haumea, Makemake, and Eris. Ceres is located in the asteroid belt, while all others have semimajor axes greater than that of Neptune. The categories of small bodies of Solar System include asteroids, trans-neptunian objects (denoted TNOs), comets and other small bodies. The size of the objects ranges from dust grains and small coherent rocks up to hundreds of kilometers size boulders. These categories are briefly presented bellow. The statistic data is taken from Minor Planet Center (MPC) website (http://www.minorplanetcenter.org/iau/mpc.html). Asteroids are referred to being rocky minor planets that orbit the Sun at distances ranging from interior to Earth’s orbit up to Jupiter’s orbit [de Pater & Lissauer, 2010]. Comets are ice-rich bodies for which the volatile constituents sublimate during close approaches to the Sun. They are characterized by a nucleus - the inner part of the body, the coma - the spherical halo of sublimated material surrounding the nucleus, and two tails: a dust tail trailing opposite the comet’s trajectory and an ion tail in the anti-Sun direction. Centaurs are icy bodies orbiting between (and in some cases also cross) the orbits of Jupiter and Neptune. There are 64 known Centaurs as of August 12, 2012. Centaurs are on chaotic 1 http://www.iau.org/
CHAPTER 1. WHY ASTEROIDS? 33 tel-00785991, version 1 - 7 Feb 2013 orbits with high eccentricities and/or inclinations. Dynamical calculations show that they are transitioning from the trans-neptunian region [de Pater & Lissauer, 2010]. TNOs are small bodies of the Solar System whose orbits lie partly or entirely beyond the orbit of Neptune. There are 1,044 known TNOs as of August 12, 2012. The existence of a disk of numerous small bodies exterior to the major planets was postulated by K. E. Edgeworth and by G. P. Kuiper. Therefore, this ensemble is referred as the Edgeworth-Kuiper belt. All small bodies (excepting the comets) with well-determined orbits are designated by a number (in a chronological order of the discoveries) and additionally can receive a name, e.g., (1) Ceres, (7986) Romania, (99942) Apophis, (134340) Pluto. After an object is discovered, but the orbit is not well determined, it receives a provisional designation. This designation is related to the date of discovery of the object: the first four characters indicate the year, followed by a space, then a letter to show the half of the month (A for January 1-15, K for May 16-31, I is omitted), followed by another letter to show the order of discovery within the half month (A for 1st, Z for 25). If a large number of the asteroids are discovered in certain half month, an additional number completes the designation, e.g: 2012 AA, 2001 SG286, 2005 UJ516. The next sections of this chapter discuss the discovery of the asteroids and the diversity of these small bodies, while this thesis concerns their composition using spectroscopy. 1.2 The Discovery Of Asteroids The roots of asteroid studies can be found at the end of the 16th century when the German mathematician and astronomer, Johannes Kepler realized that the distance between Mars and Jupiter was not proportional to the distances between other planets. He concluded that it must be another planet, undiscovered yet, occupying this part of the Solar System: "Inter Jovem et Martem interposui planetam" (Kepler 1596). Further studies of the relative distances of the planets from the Sun were made 170 years later when Johan Daniel Titius noted that the sequence of the distances from the Sun of the known planets could be fitted by a geometric progression. The relation was published by Johan Elert Bode in 1772, and today the modern formulation of the Titius-Bode empirical law is: r n = 0.4+0.3∗2 n (1.1) where r n is the semi-major axis of the n-th planet. Here, the units are considered such that the Earth’s semi-major axis is equal to 1. It can be identified Mercury for n = -1, Venus for n = 0, Earth for n = 1, Mars for n = 2, Jupiter for n = 4, and Saturn for n = 5. After the discovery of the planet Uranus (made by Sir William Herschel in 1781) at a solar distance close to the solution n = 6, the regularity in the planetary location was considered a primary feature of the Solar System. At that moment the searching for the "missing planet" with n = 3 began.
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32 CHAPTER 1. WHY ASTEROIDS?<br />
tel-00785991, version 1 - 7 Feb 2013<br />
of years [Yin et al., 2002]. After this period strong solar winds begin to clear dust from the Solar<br />
System, leaving the minor bodies and planets with a paucity of new material to accumulate.<br />
The asteroids are remnants of the planetesimal population that once formed the planets.<br />
Even if some of the asteroids were affected by thermal and dynamical evolution and by collisions,<br />
most of them did not suffer a significant geological evolution preserving the physical<br />
evidences related to the first 200 million years of the Solar System history .<br />
Currently, there is a wide diversity of bodies in the Solar System, thus in order to facilitate<br />
their studies and the discussions some definitions are required for different categories. The definitions<br />
of a planet, dwarf planet, and of a small body given below were assigned in Resolution<br />
5 and 6 of the IAU (International Astronomical Union) 2006 General Assembly 1 .<br />
According to this resolution, a planet is a a celestial body that: a) is in orbit around the<br />
Sun, b) has sufficient mass for its self-gravity to overcome rigid body forces so that is assumes<br />
a hydrostatic equilibrium - nearly round shape, and c) has cleared the neighborhood around its<br />
orbit.<br />
A dwarf planet is a celestial body that a) is in orbit around the Sun, b) has sufficient mass<br />
for its self-gravity to overcome rigid body forces so that is assumes a hydrostatic equilibrium -<br />
nearly round shape, c) has not cleared the neighborhood around its orbit, and d) is not a satellite<br />
of a planet. Plutoids are dwarf planets with a semi-major axis greater than that of Neptune. All<br />
other objects except satellites orbiting the planets shall be referred collectively as small bodies<br />
of Solar System (are also called minor planets).<br />
Following these definitions, there are eight planets in our Solar System: Mercury, Venus,<br />
Earth, Mars, Jupiter, Saturn, Uranus, and Neptune. Pluto is a dwarf planet, also as Ceres,<br />
Haumea, Makemake, and Eris. Ceres is located in the asteroid belt, while all others have<br />
semimajor axes greater than that of Neptune.<br />
The categories of small bodies of Solar System include asteroids, trans-neptunian objects<br />
(denoted TNOs), comets and other small bodies. The size of the objects ranges from dust grains<br />
and small coherent rocks up to hundreds of kilometers size boulders. These categories are<br />
briefly presented bellow. The statistic data is taken from Minor Planet Center (MPC) website<br />
(http://www.minorplanetcenter.org/iau/mpc.html).<br />
Asteroids are referred to being rocky minor planets that orbit the Sun at distances ranging<br />
from interior to Earth’s orbit up to Jupiter’s orbit [de Pater & Lissauer, 2010].<br />
Comets are ice-rich bodies for which the volatile constituents sublimate during close approaches<br />
to the Sun. They are characterized by a nucleus - the inner part of the body, the coma<br />
- the spherical halo of sublimated material surrounding the nucleus, and two tails: a dust tail<br />
trailing opposite the comet’s trajectory and an ion tail in the anti-Sun direction.<br />
Centaurs are icy bodies orbiting between (and in some cases also cross) the orbits of Jupiter<br />
and Neptune. There are 64 known Centaurs as of August 12, 2012. Centaurs are on chaotic<br />
1 http://www.iau.org/