Author:
Zuber Maria T.,Park Ryan S.,Elkins-Tanton Linda T.,Bell J. F.,Bruvold Kristoffer N.,Bercovici David,Bills Bruce G.,Binzel Richard P.,Jaumann R.,Marchi Simone,Raymond Carol A.,Roatsch T.,Wang Charles C.,Weiss Benjamin P.,Wenkert Daniel,Wieczorek Mark A.
Abstract
AbstractThe objective of the NASA Psyche mission gravity science investigation is to map the mass distribution within asteroid (16) Psyche to elucidate interior structure and to resolve the question of whether this metal-rich asteroid represents a remnant metal core or whether it is a primordial body that never melted. Measurements of gravity will be obtained via the X-band telecommunication system on the Psyche spacecraft, collected from progressively lower mapping altitudes. Orbital gravity will allow an estimate of $GM$
G
M
to better than 0.001 km3 s−2. A spherical harmonic model of gravity to degree and order 10 will be achievable and, in concert with spherical harmonic data sets from topography and magnetometry, as well as surface composition data, will provide information regarding the spatial and radial distribution of mass that will be used to constrain the origin and evolution of (16) Psyche.
Funder
Jet Propulsion Laboratory
Massachusetts Institute of Technology
Publisher
Springer Science and Business Media LLC
Subject
Space and Planetary Science,Astronomy and Astrophysics
Cited by
10 articles.
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