Techniques d'observation spectroscopique d'astéroïdes
Techniques d'observation spectroscopique d'astéroïdes Techniques d'observation spectroscopique d'astéroïdes
104 CHAPTER 6. SPECTRAL PROPERTIES OF NEAR-EARTH ASTEROIDS tel-00785991, version 1 - 7 Feb 2013 Oct 2010 [Hicks & Rhoades, 2010]. Preliminary measurements were done by Hicks & Rhoades [2010]. They found a rotational period of 42.0 sec, which implies that this small NEA is the most rapidly rotating natural body known in the Solar System. They also measured the object’s average colors (B-R = 1.284±0.045 mag; V-R = 0.461±0.030 mag; R-I = 0.344±0.022 mag). These are compatible with an S-type spectral classification. The NIR spectrum of 2010 TD54 is plotted in Fig. 6.5a. Using the MIT-SMASS online tool for Bus-DeMeo taxonomy, this asteroid is classified as belonging to a S complex, of subtypes Sr or Sq. An end class Q is also proposed but with a lower coefficient. By using the M4AST method, this spectrum can be classified to be between Sv and Sr classes (Fig. 6.5b). It has a fairly prominent feature around 1 µm and another around 2 µm. When considering these two results and the depth of the two absorption bands, I found that the Sr type provides a more accurate description for this object. The slope for this NIR spectrum is 0.062 µm −1 . The matching with meteorite spectra (Fig. 6.5c) shows that the best fit is a spectrum for a sample from Saratov - an ordinary chondrite meteorite with a low content of Fe (L4). This sample contains particles with sizes between 10 and 45 µm (Sample ID: MB-CMP-028-B). The spectrum can also be closely fitted with spectra of powdered samples from the meteorites Mirzapur and Rio Negro, which are also L ordinary chondrites. Modelling the space weathering effects, a C s = -0.223 µm can be computed, which describes a relatively fresh surface. This agrees with the small bodies having relatively young surfaces, and Earth encounters are one of the origins for rejuvenating surfaces on near-Earth asteroids [Binzel et al., 2010]. Removing the exponential continuum and comparing again with spectra from the Relab database, it can be found a good fit to the spectrum with those of ordinary chondrite meteorites with high level of Fe, from petrologic class 4 (H4 - Olivine-Bronzite). Spectra of meteorites such as Gruneberg (Fig. 6.5d), Queen’s Mercy, or Ochansk match the unweathered spectrum of this asteroid (Table 6.4). 6.2.6 (164400) 2005 GN59 This asteroid has an absolute magnitude H = 17.40, derived from astrometric observations. The synodic period of the asteroid was estimated to be 38.62±0.01 hrs [Vander Haagen, 2011], but the monomodal solution of 19.31±0.01 hrs cannot be totally excluded. A preliminary spectrum of this object was presented by Birlan et al. [2009], while Taylor et al. [2009] presented thermal emission data corroborated with radar observations. From these radar observations, Taylor et al. [2009] discovered that this object has a two-lobed 0.35 by 1.1 km shape, with non-convex surface features. Dynamically, (164400) 2005 GN59 is an Apollo asteroid. Its calculated ∆V = 6.002 km/s make this asteroid a possible target in terms of propulsion for spacecraft mission. The NIR spectrum of 164400 was obtained in August 28, 2008 for a total integration time
CHAPTER 6. SPECTRAL PROPERTIES OF NEAR-EARTH ASTEROIDS 105 tel-00785991, version 1 - 7 Feb 2013 of 480 sec. While the spectrum is quite noisy, in order to obtain information about its taxonomic class, a five order polynomial function is used to reproduce the real data. The values for reflectance corresponding to wavelengths between 1.7 and 2 µm were excluded due to high noise caused by atmospheric turbulence (Fig. 6.6). Both the MIT-SMASS on-line tool and the M4AST routine classifies this object as an L- type. However, the K taxonomic class is also a reasonable match to our data (Fig. 6.6). An additional NIR spectrum of this object was obtained by the MIT-UH-IRTF Joint Campaign for NEO Spectral Reconnaissance 2 . This spectrum has higher S/N than the one presented in Fig. 6.6. The classification of this additional spectrum is between Sq and Q types, while a K taxonomic class was proposed as a third solution. The L taxonomic class is also considered as a possible solution by the MIT-SMASS on-line tool. Relative Reflectance 1.8 1.6 1.4 1.2 1 0.8 0.6 0.4 0.2 (164400) 2005 GN59 Spectrum Poly. fit L K 0.5 1 1.5 2 2.5 Wavelength [um] Figure 6.6: NIR spectrum of (164400) 2005 GN59 and its taxonomic classification. The difference between the spectrum presented here and the one from MIT-UH-IRTF Joint Campaign, is caused by the SNR. For our spectrum [Popescu et al., 2011], I did not take into account the feature between 1.7 and 2 µm. A visible spectrum would again help distinguish between the five possible solutions for the NIR part of the spectrum. The spectrum of 2005 GN59 is noisy and I did not attempt to compare it with the Relab database and the de-reddening model. 6.3 Spectral properties of two primitive NEAs Asteroids with low albedo are considered to contain the most primitive materials. They are found in the C, D, T and other dark taxonomic classes. The only images of such type of asteroid were those of (253) Mathilde, obtained by NEAR space-mission [Clark et al., 1999]. This asteroid surface reflects only three percent of the Sun’s light, making it twice as dark as a chunk of coal. Such a dark surface is believed to have carbon-rich material that has not been altered by planetary formation processes. A strong correlation between the asteroid taxonomical classes and their heliocentric distance was showed based on the samples studied until now. The high albedo asteroids (like those of E and S type) can be found in the inner part of the main belt while, on the other hand C type are 2 htt p ://smass.mit.edu/minus.html
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104 CHAPTER 6. SPECTRAL PROPERTIES OF NEAR-EARTH ASTEROIDS<br />
tel-00785991, version 1 - 7 Feb 2013<br />
Oct 2010 [Hicks & Rhoades, 2010].<br />
Preliminary measurements were done by Hicks & Rhoades [2010]. They found a rotational<br />
period of 42.0 sec, which implies that this small NEA is the most rapidly rotating natural<br />
body known in the Solar System. They also measured the object’s average colors (B-R =<br />
1.284±0.045 mag; V-R = 0.461±0.030 mag; R-I = 0.344±0.022 mag). These are compatible<br />
with an S-type spectral classification.<br />
The NIR spectrum of 2010 TD54 is plotted in Fig. 6.5a. Using the MIT-SMASS online tool<br />
for Bus-DeMeo taxonomy, this asteroid is classified as belonging to a S complex, of subtypes<br />
Sr or Sq. An end class Q is also proposed but with a lower coefficient. By using the M4AST<br />
method, this spectrum can be classified to be between Sv and Sr classes (Fig. 6.5b). It has a<br />
fairly prominent feature around 1 µm and another around 2 µm. When considering these two<br />
results and the depth of the two absorption bands, I found that the Sr type provides a more<br />
accurate description for this object. The slope for this NIR spectrum is 0.062 µm −1 .<br />
The matching with meteorite spectra (Fig. 6.5c) shows that the best fit is a spectrum for a<br />
sample from Saratov - an ordinary chondrite meteorite with a low content of Fe (L4). This<br />
sample contains particles with sizes between 10 and 45 µm (Sample ID: MB-CMP-028-B).<br />
The spectrum can also be closely fitted with spectra of powdered samples from the meteorites<br />
Mirzapur and Rio Negro, which are also L ordinary chondrites.<br />
Modelling the space weathering effects, a C s = -0.223 µm can be computed, which describes<br />
a relatively fresh surface. This agrees with the small bodies having relatively young surfaces,<br />
and Earth encounters are one of the origins for rejuvenating surfaces on near-Earth asteroids<br />
[Binzel et al., 2010]. Removing the exponential continuum and comparing again with spectra<br />
from the Relab database, it can be found a good fit to the spectrum with those of ordinary<br />
chondrite meteorites with high level of Fe, from petrologic class 4 (H4 - Olivine-Bronzite).<br />
Spectra of meteorites such as Gruneberg (Fig. 6.5d), Queen’s Mercy, or Ochansk match the<br />
unweathered spectrum of this asteroid (Table 6.4).<br />
6.2.6 (164400) 2005 GN59<br />
This asteroid has an absolute magnitude H = 17.40, derived from astrometric observations. The<br />
synodic period of the asteroid was estimated to be 38.62±0.01 hrs [Vander Haagen, 2011], but<br />
the monomodal solution of 19.31±0.01 hrs cannot be totally excluded.<br />
A preliminary spectrum of this object was presented by Birlan et al. [2009], while Taylor et al.<br />
[2009] presented thermal emission data corroborated with radar observations. From these radar<br />
observations, Taylor et al. [2009] discovered that this object has a two-lobed 0.35 by 1.1 km<br />
shape, with non-convex surface features.<br />
Dynamically, (164400) 2005 GN59 is an Apollo asteroid. Its calculated ∆V = 6.002 km/s<br />
make this asteroid a possible target in terms of propulsion for spacecraft mission.<br />
The NIR spectrum of 164400 was obtained in August 28, 2008 for a total integration time