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Techniques d'observation spectroscopique d'astéroïdes

Techniques d'observation spectroscopique d'astéroïdes

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46 CHAPTER 2. WHY SPECTROSCOPY?<br />

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

Figure 2.2: The atmospheric transmission above Mauna Kea for the wavelength ranges 0.9 - 2.7 µm with a water<br />

vapor column of 1.6 mm and an air mass of 1 (Source: http://www.gemini.edu/?q=node/10789).<br />

several other components into the instrument called spectrometer. Usually, the designs of spectrometers<br />

incorporate the following basic components: an entrance slit to reduce the overlap<br />

between adjacent wavelengths and to reduce the background noise, collimators to produce parallel<br />

beams of light, a dispersive element, a focusing element to produce focused images of the<br />

slit for different wavelengths of the spectrum, and a detector.<br />

2.2 Spectroscopy and atmospheric transparency<br />

The observation of celestial bodies using different types of ground-based telescopes is possible<br />

in the regions of electromagnetic spectrum for which the atmosphere is transparent. There are<br />

two spectral windows which allow the observation: the optical (V) up to the mid-infrared(the<br />

near-infrared 0.8 - 2.5 µm interval is denoted as NIR) and the radio one. The X-rays and ultraviolet<br />

wavelengths are blocked due to absorption by ozone and oxygen, while the far infrared<br />

radiation is blocked mainly due to absorption by water and carbon dioxide.<br />

While in the optical wavelength region the atmosphere is almost completely transparent, in<br />

the near-infrared there are absorption bands of water vapors making some regions like 1.4-1.5<br />

µm and 1.8-2.0 µm poorly transparent (Fig. 2.2). Because of the effects of the atmosphere, observations<br />

with space telescopes, such as the Hubble and Spitzer telescopes, are very valuable.<br />

Another important difference between the V and NIR spectral intervals is the fact that the<br />

sky is brighter in the NIR region. For example in the J, H, K filters 1 the estimated sky background<br />

has 15.7, 13.6, respectively 13 mag/arcsec 2 . Additional, important variations of the sky<br />

background could be observed in the intervals of tens of arc minutes of the sky.<br />

1 Wide band filters centered on 1.25 µm (J), 1.65 µm (H), 2.2 µm (K)

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