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Interior structure of Neptune - Comparison with UranusMeasurements of rotation rates and gravitational harmonics of Neptune made with the Voyager 2 spacecraft allow tighter constraints on models of the planet's interior. Shock measurements of material that may match the composition of Neptune, the so-called planetary 'ice', have been carried out to pressures exceeding 200 gigapascals (2 megabars). Comparison of shock data with inferred pressure-density profiles for both Uranus and Neptune shows substantial similarity through most of the mass of both planets. Analysis of the effect of Neptune's strong differential rotation on its gravitational harmonics indicates that differential rotation involves only the outermost few percent of Neptune's mass.
Document ID
19910064577
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Hubbard, W. B.
(Arizona, University Tucson, United States)
Nellis, W. J.
(Arizona Univ. Tucson, AZ, United States)
Mitchell, A. C.
(Arizona Univ. Tucson, AZ, United States)
Holmes, N. C.
(Arizona Univ. Tucson, AZ, United States)
Mccandless, P. C.
(Lawrence Livermore National Laboratory Livermore, CA, United States)
Limaye, S. S.
(Wisconsin, University Madison, United States)
Date Acquired
August 14, 2013
Publication Date
August 9, 1991
Publication Information
Publication: Science
Volume: 253
ISSN: 0036-8075
Subject Category
Lunar And Planetary Exploration
Accession Number
91A49200
Funding Number(s)
CONTRACT_GRANT: W-7405-ENG-48
CONTRACT_GRANT: NASA ORDER W-16180
CONTRACT_GRANT: NAGW-1555
Distribution Limits
Public
Copyright
Other

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