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    Mercury: Mid-infrared (3-13.5 micrometers) observations show heterogeneous composition, presence of intermediate and basic soil types, and pyroxene

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    Author
    Sprague, A. L.
    Emery, J. P.
    Donaldson, K. L.
    Russell, R. W.
    Lynch, D. K.
    Mazuk, A. L.
    Issue Date
    2002-01-01
    Keywords
    Mercury
    Mauna Kea
    Hawaii
    thermal emission
    spectra
    silicate soils
    asteroids
    
    Metadata
    Show full item record
    Citation
    Sprague, A. L., Emery, J. P., Donaldson, K. L., Russell, R. W., Lynch, D. K., & Mazuk, A. L. (2002). Mercury: Mid‐infrared (3–13.5 micrometers) observations show heterogeneous composition, presence of intermediate and basic soil types, and pyroxene. Meteoritics & Planetary Science, 37(9), 1255-1268.
    Publisher
    The Meteoritical Society
    Journal
    Meteoritics & Planetary Science
    URI
    http://hdl.handle.net/10150/655566
    DOI
    10.1111/j.1945-5100.2002.tb00894.x
    Additional Links
    https://meteoritical.org/
    Abstract
    The Aerospace Corporation's Broadband Array Spectrograph System (BASS) mounted on the NASA Infrared Telescope Facility (IRTF) on Mauna Kea, Hawaii was used to obtain spectral measurements of Mercury's thermal emission on March 21, 1998 (45-85 degrees longitude), and on May 12, 1998 (68-108 degrees longitude). The spectra show heterogeneous composition on Mercury's surface between longitudes 45-85 degrees and about 68-108 degrees. These observations include measurements from 3-6 micrometers, a spectral region not previously covered by mid-infrared spectroscopy. Excellent quality data were obtained in the atmospheric windows between 3-4.2 and 4.6-5.5 micrometers. These wavelength regions exhibit high emissivity characteristic of a regolith with strong thermal gradients maintained in a vacuum environment with spectra dominated by grain sizes of about ~30 micrometers. Emission peaks are present at 3.5 and 5 micrometers in the 45-85 degrees longitude data. The 5 micrometer peak has been tentatively attributed to clino-pyroxene. Data were also obtained in the 7.5-13.5 micrometers spectral region. Spectra obtained during both observing periods show well-defined emissivity maxima (EM) in the spectral vicinity (between 7.7-9.2 micrometers) of the Christiansen frequency of silicate soils. The location of the EM for longitudes 45-85 degrees (7.9 micrometers) is consistent with a surface composition of intermediate SiO2 content. The overall spectral shape is similar to that obtained previously at the same location with different instrumentation. In the region 68-108 degrees longitude, three EM are observed at 7.8, 8.2, and 9.2 micrometers, indicating the presence of distinctly different surface composition from the other location. Comparisons of these data to other mid-infrared spectra of Mercury's surface and asteroids, and of the different instrumentation used in observations are included.
    Type
    Article
    text
    Language
    en
    ISSN
    1945-5100
    ae974a485f413a2113503eed53cd6c53
    10.1111/j.1945-5100.2002.tb00894.x
    Scopus Count
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    Meteoritics & Planetary Science, Volume 37, Number 9 (2002)

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