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Techniques d'observation spectroscopique d'astéroïdes

Techniques d'observation spectroscopique d'astéroïdes

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List of Figures<br />

1.1 A field obtained with INT-WFC on February 28, 2012. Ten asteroids were identified<br />

(marked with pink), from which only three were known at the moment of<br />

the observation. The size of the field is (15 arcmin x 15 arcmin) . . . . . . . . 34<br />

1.2 a) The position of asteroids in the inner part of the Solar System (Source:<br />

http://en.wikipedia.org/). b)The distribution of asteroids in a representation<br />

(a,e)- bottom and (a,sini) - top, a is the semi-major axis and i the<br />

inclination [Nedelcu, 2010]. . . . . . . . . . . . . . . . . . . . . . . . . . . . 36<br />

1.3 The flowchart of Mega-Precovery [Vaduvescu et al., 2012]. . . . . . . . . . . . 39<br />

1.4 The first part of the Minor Planet Electronic Circular issued for the orbit recovery<br />

of the asteroid 2007 ES. . . . . . . . . . . . . . . . . . . . . . . . . . . . . 41<br />

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

2.1 The diffraction pattern produced by a diffraction grating having b=d = 5µm<br />

and N=1000. Different wavelengths are considered. . . . . . . . . . . . . . . . 45<br />

2.2 The atmospheric transmission above Mauna Kea for the wavelength ranges 0.9<br />

- 2.7 µm with a water vapor column of 1.6 mm and an air mass of 1 (Source:<br />

http://www.gemini.edu/?q=node/10789). . . . . . . . . . . . . . . 46<br />

2.3 The field of quasar PG1634+706 (north is at bottom of the figure). The object<br />

and its spectrum are surrounded by a rectangle. In this image it can be distinguish<br />

the zero order (objects are dots) and the first order (light is dispersed) -<br />

Popescu et al. [2012a]. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 48<br />

2.4 a) PG1634 + 706 spectrum obtained after data reduction and continuum subtraction;<br />

b) the correlation coefficient between quasar spectrum and the template<br />

spectrum shifted with different z [Popescu et al., 2012a]. . . . . . . . . . 49<br />

2.5 The components of the radiation received from 1km square lunar mare area<br />

(dark basaltic plain on Moon formed by ancient volcanic eruptions) having an<br />

albedo of 006, considering the average Earth-Moon distance, phase angle 0, T<br />

= 395K. The flux is measured in Watts per square meter per micron. Source<br />

McCord & Adams [1977] . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 51<br />

2.6 Reflectance spectra of several meteoritic important minerals: a) Spinel, b) Pyroxene,<br />

c) Olivine, d) Iron-Nickel alloy. . . . . . . . . . . . . . . . . . . . . . 52<br />

3.1 a) The 3m NASA InfraRed Telescope Facility at the Mauna Kea Observatory<br />

on Hawaii. b) SpeX instrument mounted to IRTF telescope. As scale, SpeX is<br />

1.4m tall and weighs 478kg. . . . . . . . . . . . . . . . . . . . . . . . . . . . 58<br />

3.2 The data reduction procedure for NIR spectra obtained with IRTF/SpeX [Nedelcu,<br />

2010]. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 60

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