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    Characteristics of cometary dust tracks in Stardust aerogel and laboratory calibrations

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    Author
    Burchell, M. J.
    Fairey, S. A. J.
    Wozniakiewicz, P.
    Brownlee, D. E.
    Hörz, F.
    Kearsley, A. T.
    See, T. H.
    Tsou, P.
    Westphal, A.
    Green, S. F.
    Trigo-Rodríguez, J. M.
    Domingúez, G.
    Show allShow less
    Issue Date
    2008-01-01
    Keywords
    impact processes
    cometary nucleus
    cometary dust
    Stardust Mission
    
    Metadata
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    Citation
    Burchell, M. J., Fairey, S. A. J., Wozniakiewicz, P., Brownlee, D. E., Hörz, F., Kearsley, A. T., ... & Domingúez, G. (2008), Characteristics of cometary dust tracks in Stardust aerogel and laboratory calibrations. Meteoritics & Planetary Science, 43(1-2), 23-40.
    Publisher
    The Meteoritical Society
    Journal
    Meteoritics & Planetary Science
    URI
    http://hdl.handle.net/10150/656380
    DOI
    10.1111/j.1945-5100.2008.tb00608.x
    Additional Links
    https://meteoritical.org/
    Abstract
    The cometary tray of the NASA Stardust spacecraft’s aerogel collector was examined to study the dust captured during the 2004 flyby of comet 81P/Wild 2. An optical scan of the entire collector surface revealed 256 impact features in the aerogel (width >100 micrometers). Twenty aerogel blocks (out of a total of 132) were removed from the collector tray for a higher resolution optical scan and 186 tracks were observed (track length >50 micrometers and width >8 micrometers). The impact features were classified into three types based on their morphology. Laboratory calibrations were conducted that reproduced all three types. This work suggests that the cometary dust consisted of some cohesive, relatively strong particles as well as particles with a more friable or low cohesion matrix containing smaller strong grains. The calibrations also permitted a particle size distribution to be estimated for the cometary dust. We estimate that approximately 1200 particles bigger than 1 micrometer struck the aerogel. The cumulative size distribution of the captured particles was obtained and compared with observations made by active dust detectors during the encounter. At large sizes (>20 micrometers) all measures of the dust are compatible, but at micrometer scales and smaller discrepancies exist between the various measurement systems that may reflect structure in the dust flux (streams, clusters etc.) along with some possible instrument effects.
    Type
    Article
    text
    Language
    en
    ISSN
    1945-5100
    ae974a485f413a2113503eed53cd6c53
    10.1111/j.1945-5100.2008.tb00608.x
    Scopus Count
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    Meteoritics & Planetary Science, Volume 43, Number 1-2 (2008)

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