CIVA

被引:37
作者
Bibring, J.-P. [1 ]
Lamy, P.
Langevin, Y.
Soufflot, A.
Berthe, M.
Borg, J.
Poulet, F.
Mottola, S.
机构
[1] Inst Astrophys Spatiale, Orsay, France
[2] Lab Astrophys Marseille, Marseille, France
[3] DLR, IWP, Berlin, Germany
关键词
cometary composition; in situ imaging; microscopic analyses;
D O I
10.1007/s11214-006-9135-5
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
CIVA (Comet Infrared and Visible Analyser) is an integrated set of imaging instruments, designed to characterize the 360 degrees panorama (CIVA-P) as seen from the Rosetta Lander Philae, and to stud), surface and subsurface samples (CIVA-M). CIVA-P is a panoramic stereo camera, while CIVA-M is an optical microscope coupled to a near infrared microscopic hyperspectral imager. CIVA shares a common Imaging Main Electronics (IME) with ROLIS. CIVA-P will characterize the landing site, with an angular sampling (IFOV) of 1.1 mrad: each pixel will image a I rnm size feature at the distance of the landing legs, and a few rnetres at the local horizon. The panorama will be mapped by 6 identical miniaturized micro-cameras covering contiguous FOV, with their optical axis 60 degrees apart. Stereoscopic capability will be provided by an additional micro-camera, identical to and co-aligned with one of the panoramic micro-camera, with its optical axis displaced by 10 cm. CIVA-M combines two ultra-compact and miniaturised microscopes, one operating in the visible and one constituting an IR hyperspectral imaging spectrometer: they will characterize, by non-destructive analyses, the texture, the albedo, the molecular and the mineralogical composition of each of the samples provided by the Sample Drill and Distribution (SD2) system. For the optical microscope, the spatial sampling is 7 mu m: for the IR, the spectral range (1 -4 mu m and the spectral sampling (5 nm) have been chosen to allow identification of most minerals, ices and organics, on each pixel, 40 um in size. After being studied by CIVA, the sample could be analysed by a subsequent experiment (PTOLEMY and/or COSAC). The process would be repeated for each sample obtained at different depths and/or locations.
引用
收藏
页码:397 / 412
页数:16
相关论文
共 10 条
  • [1] Perennial water ice identified in the south polar cap of Mars
    Bibring, JP
    Langevin, Y
    Poulet, F
    Gendrin, A
    Gondet, B
    Berthé, M
    Soufflot, A
    Drossart, P
    Combes, M
    Bellucci, G
    Moroz, V
    Mangold, N
    Schmitt, B
    [J]. NATURE, 2004, 428 (6983) : 627 - 630
  • [2] Bibring JP., 2004, AGUSTIN CHICARRO SCI, P37
  • [3] INFRARED SOUNDING OF COMET HALLEY FROM VEGA-1
    COMBES, M
    MOROZ, VI
    CRIFO, JF
    LAMARRE, JM
    CHARRA, J
    SANKO, NF
    SOUFFLOT, A
    BIBRING, JP
    CAZES, S
    CORON, N
    CROVISIER, J
    EMERICH, C
    ENCRENAZ, T
    GISPERT, R
    GRIGORYEV, AV
    GUYOT, G
    KRASNOPOLSKY, VA
    NIKOLSKY, YV
    ROCARD, F
    [J]. NATURE, 1986, 321 (6067) : 266 - 268
  • [4] Hanner MS, 2004, SPACE SCI S, P555
  • [5] Irvine WM, 2004, SPACE SCI S, P25
  • [6] THE ORGANIC-COMPONENT IN DUST FROM COMET HALLEY AS MEASURED BY THE PUMA MASS-SPECTROMETER ON BOARD VEGA-1
    KISSEL, J
    KRUEGER, FR
    [J]. NATURE, 1987, 326 (6115) : 755 - 760
  • [7] No signature of clear CO2 ice from the 'cryptic' regions in Mars' south seasonal polar cap
    Langevin, Yves
    Doute, Sylvain
    Vincendon, Mathieu
    Poulet, Francois
    Bibring, Jean-Pierre
    Gondet, Brigitte
    Schmitt, Bernard
    Forget, F.
    [J]. NATURE, 2006, 442 (7104) : 790 - 792
  • [8] Olivine and pyroxene, diversity in the crust of Mars
    Mustard, JF
    Poulet, F
    Gendrin, A
    Bibring, JP
    Langevin, Y
    Gondet, B
    Mangold, N
    Bellucci, G
    Altieri, F
    [J]. SCIENCE, 2005, 307 (5715) : 1594 - 1597
  • [9] Phyllosilicates on Mars and implications for early martian climate
    Poulet, F
    Bibring, JP
    Mustard, JF
    Gendrin, A
    Mangold, N
    Langevin, Y
    Arvidson, RE
    Gondet, B
    Gomez, C
    [J]. NATURE, 2005, 438 (7068) : 623 - 627
  • [10] Weidenschilling SJ, 2004, SPACE SCI S, P97