Techniques d'observation spectroscopique d'astéroïdes
Techniques d'observation spectroscopique d'astéroïdes Techniques d'observation spectroscopique d'astéroïdes
124 CHAPTER 7. SPECTRAL PROPERTIES OF MAIN BELT ASTEROIDS Relative Reflectance 1.2 1.15 1.1 1.05 1 0.95 0.9 0.85 0.8 (1333) Cevenola 0.75 0.8 1 1.2 1.4 1.6 1.8 2 2.2 2.4 Wavelength [um] (a) Relative Reflectance 1.2 1.15 1.1 1.05 1 0.95 0.9 0.85 0.8 0.75 (1333) Cevenola 0.8 1 1.2 1.4 1.6 1.8 2 2.2 2.4 Wavelength [um] (b) Figure 7.3: The NIR spectra with the error-bars for (1333) Cevenola; a) obtained in March 12, 2007; b) obtained in March 13, 2007. The spectra are normalized to 1.25 µm. nomia family (including Cevenola) were studied spectroscopically in the visible region by Lazzaro et al. [1999]. Based on the visible spectrum, 41 of them were classified as S-type objects, while three asteroids exhibit flat spectra and were considered as intruders. Considering these samples in the frame of the Bus-DeMeo taxonomy [DeMeo et al., 2009], only three objects are re-observed in the near-infrared region. The visible spectrum was reported by Lazzaro et al. [2004] in the framework of S 3 OS 2 survey, and the analysis of spectral data places the asteroid into the S (S q more precisely) complex. The Eunomia family is actually dominated by objects displaying S-type spectra. Two NIR spectra were obtained for this asteroid (Fig. 7.3), on two consecutive nights, separated by 24 hours. The spectrum of March 12, 2007 is the result of the combination of individual spectra of 120 seconds each, for the total integration time of 1.4667hrs. The second spectrum was obtained in March 13, 2007 for the total integration time of 40min. Consequently, a S/N of 50 and 20 was estimated. The two NIR spectra are very similar. I made an average spectrum between the two spectra of (1333) Cevenola and I merged with the visible part from S 3 OS 2 (Fig. 7.4a). The SMASS-MIT online tool classifies this spectrum as an Sq type in Bus-DeMeo taxonomy. The Sq type has a wide 1-micron absorption band with evidence of a feature near 1.3 µm like the Q-type, except the 1-micron feature is more shallow for the Sq [DeMeo et al., 2009]. Among the solutions proposed by M4AST for taxonomic classification of this spectrum are also the Q and K types. This is due to the fact that the spectrum is not as reddened as for Sq type in the infrared part (Fig. 7.4b ). Using the G13 taxonomy [Birlan et al., 1996a], it can be found that this spectrum belongs to S-complex, being in the class 2 of this taxonomy. The class 2 of G13 taxonomy includes asteroids like (7) Iris, (11) Parthenope, (26) Proserpina, (27) Euterpe. The taxonomic type found for this asteroid spectrum, allows the application of space weathtel-00785991, version 1 - 7 Feb 2013
CHAPTER 7. SPECTRAL PROPERTIES OF MAIN BELT ASTEROIDS 125 Relative Reflectance (a) 1.2 1.15 1.1 1.05 1 0.95 0.9 0.85 0.8 0.75 0.7 (1333) Cevenola :V (1333) Cevenola :NIR 0.5 1 1.5 2 2.5 Wavelength [um] Relative Reflectance (b) 1.2 1.15 1.1 1.05 1 0.95 0.9 0.85 0.8 Cevenola 0.75 Sq Q 0.7 K 0.5 1 1.5 2 2.5 Wavelength [um] 0.23 0.22 0.25 0.24 tel-00785991, version 1 - 7 Feb 2013 Relative Reflectance (c) 0.21 0.2 0.19 0.18 0.17 0.16 Cevenola Saratov met. 0.5 1 1.5 2 2.5 Wavelength [um] Relative Reflectance (d) 0.23 0.22 0.21 0.2 0.19 0.18 Cevenola Hamlet #1 met. 0.5 1 1.5 2 2.5 Wavelength [um] Figure 7.4: a) The visible and the averaged NIR spectrum of(1333) Cevenola; b) A polynomial fit for the V+NIR spectrum of (1333) Cevenola compared with the theoretical spectra of Sq, Q and K taxonomic types; c) the comparison between the spectrum of (1333) Cevenola and the spectrum of a sample from Saratov meteorite; d) the comparison between the spectrum of (1333) Cevenola and the spectrum of a sample from Hamlet#1 meteorite. ering model proposed by Brunetto et al. [2006]. Thus, fitting the spectrum with an exponential continuum I found C s = -0.133 µm, corresponding to a relatively fresh surface. The C s value gives the number of displacements per cm 2 , d = 0.45×10 19 displacements/cm 2 . Comparing the original spectrum of (1333) Cevenola with all laboratory spectra from Relab, M4AST found matches with ordinary chondrite meteorites (L and LL subtypes, and petrologic classes 4 and 5). In terms of standard deviation and correlation coefficient, the best matches where those of samples from Saratov, Hamlet #1 (Fig. 7.4) and Paranaiba. These meteorites are ordinary chondrites with low iron content. I compared also the de-reddened spectrum of (1333) Cevenola to laboratory spectra from Relab. In this case, the four methods used give relatively different solutions. The spectral solutions that can be selected are the spectrum of a sample from Denver meteorite and the spectrum of a sample from Hamlet #1 meteorite. Both meteorites are ordinary chondrites with low iron content.
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124 CHAPTER 7. SPECTRAL PROPERTIES OF MAIN BELT ASTEROIDS<br />
Relative Reflectance<br />
1.2<br />
1.15<br />
1.1<br />
1.05<br />
1<br />
0.95<br />
0.9<br />
0.85<br />
0.8<br />
(1333) Cevenola<br />
0.75<br />
0.8 1 1.2 1.4 1.6 1.8 2 2.2 2.4<br />
Wavelength [um]<br />
(a)<br />
Relative Reflectance<br />
1.2<br />
1.15<br />
1.1<br />
1.05<br />
1<br />
0.95<br />
0.9<br />
0.85<br />
0.8<br />
0.75<br />
(1333) Cevenola<br />
0.8 1 1.2 1.4 1.6 1.8 2 2.2 2.4<br />
Wavelength [um]<br />
(b)<br />
Figure 7.3: The NIR spectra with the error-bars for (1333) Cevenola; a) obtained in March 12, 2007; b) obtained<br />
in March 13, 2007. The spectra are normalized to 1.25 µm.<br />
nomia family (including Cevenola) were studied spectroscopically in the visible region by<br />
Lazzaro et al. [1999]. Based on the visible spectrum, 41 of them were classified as S-type<br />
objects, while three asteroids exhibit flat spectra and were considered as intruders. Considering<br />
these samples in the frame of the Bus-DeMeo taxonomy [DeMeo et al., 2009], only three<br />
objects are re-observed in the near-infrared region.<br />
The visible spectrum was reported by Lazzaro et al. [2004] in the framework of S 3 OS 2 survey,<br />
and the analysis of spectral data places the asteroid into the S (S q more precisely) complex.<br />
The Eunomia family is actually dominated by objects displaying S-type spectra.<br />
Two NIR spectra were obtained for this asteroid (Fig. 7.3), on two consecutive nights, separated<br />
by 24 hours. The spectrum of March 12, 2007 is the result of the combination of individual<br />
spectra of 120 seconds each, for the total integration time of 1.4667hrs. The second<br />
spectrum was obtained in March 13, 2007 for the total integration time of 40min. Consequently,<br />
a S/N of 50 and 20 was estimated. The two NIR spectra are very similar. I made an average<br />
spectrum between the two spectra of (1333) Cevenola and I merged with the visible part from<br />
S 3 OS 2 (Fig. 7.4a).<br />
The SMASS-MIT online tool classifies this spectrum as an Sq type in Bus-DeMeo taxonomy.<br />
The Sq type has a wide 1-micron absorption band with evidence of a feature near 1.3 µm<br />
like the Q-type, except the 1-micron feature is more shallow for the Sq [DeMeo et al., 2009].<br />
Among the solutions proposed by M4AST for taxonomic classification of this spectrum are<br />
also the Q and K types. This is due to the fact that the spectrum is not as reddened as for Sq<br />
type in the infrared part (Fig. 7.4b ). Using the G13 taxonomy [Birlan et al., 1996a], it can<br />
be found that this spectrum belongs to S-complex, being in the class 2 of this taxonomy. The<br />
class 2 of G13 taxonomy includes asteroids like (7) Iris, (11) Parthenope, (26) Proserpina, (27)<br />
Euterpe.<br />
The taxonomic type found for this asteroid spectrum, allows the application of space weathtel-00785991,<br />
version 1 - 7 Feb 2013