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    Three-dimensional textural and compositional analysis of particle tracks and fragmentation history in aerogel

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    Author
    Ebel, D. S.
    Greenberg, M.
    Rivers, M. L.
    Newville, M.
    Issue Date
    2009-01-01
    Keywords
    comets chemical composition
    aerogel
    Three dimensional imaging
    tomography
    
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    Citation
    Ebel, D. S., Greenberg, M., Rivers, M. L., & Newville, M. (2009). Three‐dimensional textural and compositional analysis of particle tracks and fragmentation history in aerogel. Meteoritics & Planetary Science, 44(10), 1445-1463.
    Publisher
    The Meteoritical Society
    Journal
    Meteoritics & Planetary Science
    URI
    http://hdl.handle.net/10150/656620
    DOI
    10.1111/j.1945-5100.2009.tb01185.x
    Additional Links
    https://meteoritical.org/
    Abstract
    We report analyses of aerogel tracks using (1 synchrotron X-ray computed microtomography (XRCMT), (2) laser confocal scanning microscopy (LCSM), and (3) synchrotron radiation X-ray fluorescence (SRXRF) of particles and their paths resulting from simulated hypervelocity impacts (1-2), and a single ~1 mm aerogel track from the Stardust cometary sample collector (1-3). Large aerogel pieces can be imaged sequentially, resulting in high spatial resolution images spanning many tomographic fields of view (lambda-tomography). We report calculations of energy deposited, and tests on aromatic hydrocarbons showing no alteration in tomography experiments. Imaging at resolutions from ~17 to ~1 micron/pixel edge (XRCMT) and to <100 nm/ pixel edge (LCSM) illustrates track geometry and interaction of particles with aerogel, including rifling, particle fragmentation, and final particle location. We present a 3-D deconvolution method using an estimated point-spread function for aerogel, allowing basic corrections of LCSM data for axial distortion. LCSM allows rapid, comprehensive, non-destructive, high information return analysis of tracks in aerogel keystones, prior to destructive grain extraction. SRXRF with LCSM allows spatial correlation of grain size, chemical, and mineralogical data. If optical methods are precluded in future aerogel capture missions, XRCMT is a viable 3D imaging technique. Combinations of these methods allow for complete, nondestructive, quantitative 3-D analysis of captured materials at high spatial resolution. This data is fundamental to understanding the hypervelocity particle-aerogel interaction histories of Stardust grains.
    Type
    Article
    text
    Language
    en
    ISSN
    1945-5100
    ae974a485f413a2113503eed53cd6c53
    10.1111/j.1945-5100.2009.tb01185.x
    Scopus Count
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    Meteoritics & Planetary Science, Volume 44, Number 10 (2009)

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