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From version < 3.1 >
edited by ahirtl
on 2018/02/13 11:50
To version < 2.1 >
edited by Barry Bishop
on 2018/02/11 12:49
>
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Summary

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1 1  === Details ===
2 2  
3 -|**Acronym**|Field spectrometry
4 -|**Description**|Acquisition of reflectance and radiance spectra in an environment analogous to Mars
5 -|**Principal Investigator (PI)**|Eleonora Ammannito
6 -|**Organisation** |Agenzia Spaziale Italiana
3 +|**Acronym**|
4 +|**Description**|
5 +|**Principal Investigator (PI)**|
6 +|**Organisation** |
7 7  
8 8  === Summary ===
9 9  
10 -VIS-NIR reflectance spectroscopy is the major technique used so far to identify mineralogical phases present on the surface of Mars. However, the interpretation of reflectance spectra is subject to a deep understanding of the contest in which the measurements have been acquired. The co-existence of different minerals (Brossard et al. 2016), the temperature (Singer & Roush 1985) and illumination (Mustard & Pieters, 1989) - just to cite few examples - can significantly alter the shape of absorption features of minerals leading to mistakes in the determination of the composition of the site under analysis.
11 11  
12 12  === Objectives ===
13 13  
14 -The scope of our proposal is to acquire spectra in a realistic Martian-like environment along with ancillary information like temperature and illumination conditions to check the reliability of mineralogical interpretation.
15 15  
16 16  === Experiment Data ===
17 17  
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