Letter | Published:

A partially differentiated interior for (1) Ceres deduced from its gravity field and shape

Nature volume 537, pages 515517 (22 September 2016) | Download Citation


Remote observations of the asteroid (1) Ceres from ground- and space-based telescopes have provided its approximate density and shape, leading to a range of models for the interior of Ceres, from homogeneous to fully differentiated1,2,3,4,5,6. A previously missing parameter that can place a strong constraint on the interior of Ceres is its moment of inertia, which requires the measurement of its gravitational variation1,7 together with either precession rate8,9 or a validated assumption of hydrostatic equilibrium10. However, Earth-based remote observations cannot measure gravity variations and the magnitude of the precession rate is too small to be detected9. Here we report gravity and shape measurements of Ceres obtained from the Dawn spacecraft, showing that it is in hydrostatic equilibrium with its inferred normalized mean moment of inertia of 0.37. These data show that Ceres is a partially differentiated body, with a rocky core overlaid by a volatile-rich shell, as predicted in some studies1,4,6. Furthermore, we show that the gravity signal is strongly suppressed compared to that predicted by the topographic variation. This indicates that Ceres is isostatically compensated11, such that topographic highs are supported by displacement of a denser interior. In contrast to the asteroid (4) Vesta8,12, this strong compensation points to the presence of a lower-viscosity layer at depth, probably reflecting a thermal rather than compositional gradient1,4. To further investigate the interior structure, we assume a two-layer model for the interior of Ceres with a core density of 2,460–2,900 kilograms per cubic metre (that is, composed of CI and CM chondrites13), which yields an outer-shell thickness of 70–190 kilometres. The density of this outer shell is 1,680–1,950 kilograms per cubic metre, indicating a mixture of volatiles and denser materials such as silicates and salts14. Although the gravity and shape data confirm that the interior of Ceres evolved thermally1,4,6, its partially differentiated interior indicates an evolution more complex than has been envisioned for mid-sized (less than 1,000 kilometres across) ice-rich rocky bodies.

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This research was carried out in part at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration. We thank the Dawn operations team for the development, cruise, orbital insertion and operations of the Dawn spacecraft at Ceres. R.S.P. thanks W. M. Folkner, E. M. Mazarico, and M. D. Rayman for comments and suggestions. N.R. is grateful to the CNU, Section 34, for supporting a six-month full-time research project through CRCT-2015 funding delivered by the MESR and acknowledges funding from the French National Programme of Planetology (PNP). M.J.T. acknowledges funding by the CNES. Government sponsorship acknowledged. All rights reserved.

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  1. Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109, USA

    • R. S. Park
    • , A. S. Konopliv
    • , B. G. Bills
    • , J. C. Castillo-Rogez
    • , C. A. Raymond
    •  & A. T. Vaughan
  2. IMCCE, Observatoire de Paris—PSL Research University, Sorbonne Universités—UPMC Université Paris 06, Université Lille 1, CNRS, 77 avenue Denfert-Rochereau, 75014 Paris, France

    • N. Rambaux
  3. Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA

    • A. I. Ermakov
    •  & M. T. Zuber
  4. Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA

    • R. R. Fu
  5. Institut de Recherche en Astrophysique et Planetologie, Université de Toulouse, CNRS, UPS, Toulouse, France

    • M. J. Toplis
  6. Institute of Geophysics and Planetary Physics, University of California, Los Angeles, California 90095-1567, USA

    • C. T. Russell
  7. Max Planck Institute for Solar System Research, Goettingen, Germany

    • A. Nathues
  8. Institute of Planetary Research, DLR, Department of Planetary Geodesy, Rutherfordstrasse 2, 12489 Berlin, Germany

    • F. Preusker


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R.S.P., A.S.K. and A.T.V. performed data analysis and calibration. R.S.P., B.G.B., N.R., J.C.C.-R., C.A.R., A.I.E., M.T.Z., R.R.F., M.J.T., C.T.R., A.N. and F.P. contributed to the interpretation of the data. All authors contributed to the discussion of the results and to writing the paper.

Competing interests

The authors declare no competing financial interests.

Corresponding author

Correspondence to R. S. Park.

The gravity science and framing camera data is available through the PDS Small Bodies Node website (http://sbn.pds.nasa.gov/data_sb/missions/dawn).

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