From version 1.1 >
edited by Barry Bishop
on 2018/02/11 10:30
To version < 3.1 >
edited by ahirtl
on 2018/02/13 11:50
>
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2 -
3 3  === Details ===
4 4  
5 -|**Acronym**|
6 -|**Description**|
7 -|**Principal Investigator (PI)**|
8 -|**Organisation** |
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
9 9  
10 10  === Summary ===
11 11  
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.
12 12  
13 13  === Objectives ===
14 14  
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  
18 18  |=Date|=Files
19 -
19 +|[[2018-02-03>>https://mission.oewf.org/archive_downloads/amadee18/06-FieldSpectrometry/2018-02-03]]|8 'asd' files
20 +|[[2018-02-04>>https://mission.oewf.org/archive_downloads/amadee18/06-FieldSpectrometry/2018-02-04]]|6 'asd' files
21 +|[[2018-02-09>>https://mission.oewf.org/archive_downloads/amadee18/06-FieldSpectrometry/2018-02-09]]|21 'asd' files
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