Abstract
JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 109,
E12S04,
13 PP., 2004
doi:10.1029/2004JE002318
The dust mass distribution of comet 81P/Wild 2
Planetary and Space Sciences Research Institute, Open University, Walton Hall, Milton Keynes, UK
Planetary and Space Sciences Research Institute, Open University, Walton Hall, Milton Keynes, UK
Planetary and Space Sciences Research Institute, Open University, Walton Hall, Milton Keynes, UK
Planetary and Space Sciences Research Institute, Open University, Walton Hall, Milton Keynes, UK
Laboratory for Astrophysics and Space Research, Enrico Fermi Institute, University of Chicago, Chicago, Illinois, USA
Laboratory for Astrophysics and Space Research, Enrico Fermi Institute, University of Chicago, Chicago, Illinois, USA
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA
Lockheed Martin Space Systems, Denver, Colorado, USA
Astronomy Department, University of Washington, Seattle, Washington, USA
The Dust Flux Monitor Instrument (DFMI) made direct measurements of the dust environment in the mass range 10−14 < m < 10−5 kg at comet 81P/Wild 2 during the Stardust flyby on 2 January 2004. We describe the techniques for derivation of the particle
mass distribution, including updated calibration for the acoustic subsystem. The dust coma is characterized by “swarms” and
“bursts” of particles with large variations of flux on small spatial scales, which may be explained by jets and fragmentation.
The mass of the dust coma is dominated by larger particles, as was found for comets 1P/Halley and 26P/Grigg-Skjellerup. However,
almost 80% of the particles were detected many minutes after closest approach at a distance of ∼4000 km, where small grains
dominated the detected mass flux. The mass distribution varies on small spatial scales with location in the coma, consistent
with the jets and fragmentation inferred from the highly heterogeneous dust spatial distribution. The cumulative mass distribution
index α (where the number of particles of mass m or larger, N(m)
m
−α) in the coma ranges from 0.3 to 1.1. It is possible that jets and fragmentation occur in all comets but have not previously
been well observed due to the limitations of detectors and flyby geometry. We estimate that 2800 ± 500 particles of diameter
15 μm or larger impacted the aerogel collectors, the largest being ∼6 × 10−7 kg (diameter ∼1 mm), which dominates the total collected mass. Of these, only 500 ± 200, representing just 3% of the collected
mass, originated in the far postencounter region.
Received 9 July 2004; accepted 8 November 2004; published 22 December 2004.
Citation: (2004), The dust mass distribution of comet 81P/Wild 2, J. Geophys. Res., 109, E12S04, doi:10.1029/2004JE002318.
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