The nonmagnetic nucleus of comet 67P/Churyumov-Gerasimenko

Author:

Auster Hans-Ulrich1,Apathy Istvan2,Berghofer Gerhard3,Fornacon Karl-Heinz1,Remizov Anatoli14,Carr Chris5,Güttler Carsten6,Haerendel Gerhard7,Heinisch Philip1,Hercik David1,Hilchenbach Martin6,Kührt Ekkehard8,Magnes Werner3,Motschmann Uwe89,Richter Ingo1,Russell Christopher T.10,Przyklenk Anita1,Schwingenschuh Konrad3,Sierks Holger7,Glassmeier Karl-Heinz17

Affiliation:

1. Institut für Geophysik und extraterrestrische Physik, Technische Universität Braunschweig, Mendelssohnstrasse 3, D-38106 Braunschweig, Germany.

2. Centre for Energy Research, Hungarian Academy of Sciences, H-1121 Konkoly Thege Street 29-33, Budapest, Hungary.

3. Space Research Institute, Austrian Academy of Sciences, Schmiedlstrasse 6, A-8042 Graz, Austria.

4. Space Research Institute, Russian Academy of Sciences, Moscow, Profsoyuznaja Street 84/32, 117810 Moscow, Russia.

5. Imperial College London, Exhibition Road, London SW7 2AZ, UK.

6. Max-Planck-Institut für Sonnensystemforschung, Justus-von-Liebig-Weg 3, D-37077 Göttingen.

7. Max-Planck-Institute für Extraterrestrische Physik, Giessenbachstrasse, D-85741 Garching bei München.

8. German Aerospace Center (DLR), Institute of Planetary Research, D-12489 Berlin, Rutherfordstrasse 2, Germany.

9. Institut für Theoretische Physik, Technische Universität Braunschweig, Mendelssohnstrasse 3, D-38106 Braunschweig, Germany.

10. Institute of Geophysics and Planetary Physics, University of California, Los Angeles, Los Angeles, CA 90095-1567, USA.

Abstract

Knowledge of the magnetization of planetary bodies constrains their origin and evolution, as well as the conditions in the solar nebular at that time. On the basis of magnetic field measurements during the descent and subsequent multiple touchdown of the Rosetta lander Philae on the comet 67P/Churyumov-Gerasimenko (67P), we show that no global magnetic field was detected within the limitations of analysis. The Rosetta Magnetometer and Plasma Monitor (ROMAP) suite of sensors measured an upper magnetic field magnitude of less than 2 nanotesla at the cometary surface at multiple locations, with the upper specific magnetic moment being <3.1 × 10 −5 ampere–square meters per kilogram for meter-size homogeneous magnetized boulders. The maximum dipole moment of 67P is 1.6 × 10 8 ampere–square meters. We conclude that on the meter scale, magnetic alignment in the preplanetary nebula is of minor importance.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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