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Cited by 260

The DOI matches its Crossref record; 78 of the 78 references it cites were found in a registry or an index.

Planetary magnetic fields

Open access
Stevenson, D J·1983·Reports on Progress in Physics

Abstract

As a consequence of the smallness of the electronic fine structure constant, the characteristic time scale for the free diffusive decay of a magnetic field in a planetary core is much less than the age of the Solar System, but the characteristic time scale for thermal diffusion is greater than the age of the Solar System. Consequently, primordial fields and permanent magnetism are small and the only means of providing a substantial planetary magnetic field is the dynamo process. This requires a large region which is fluid, electrically conducting and maintained in a non-uniform motion that includes a substantial RMS vertical component. The attributes of fluidity and conductivity are readily provided in the deep interiors of all planets and most satellites, either in the form of an Fe alloy with a low eutectic temperature (e.g. Fe-S-O in terrestrial bodies and satellites) or by the occupation of conduction states in fluid hydrogen or 'ice' (H 2 O-NH 3 -CH 4 ) in giant planets. It is argued that planetary dynamos are almost certainly maintained by convection (compositional and/or thermal).

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Metadata

Authors
Stevenson, D. J.
Venue
Reports on Progress in Physics
Published
1983-05-01
Volume
46
Issue
5
Pages
555-620
ISSN
  • 0034-4885 (ISSN-L)
  • 1361-6633
OpenAlex
W1991634161
Cited by
260
References
78
FWCI
1.84
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Planetary magnetic fields. https://app.cochat.ai/papers/10.1088/0034-4885/46/5/001
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Stevenson, D. J. (1983). Planetary magnetic fields. Reports on Progress in Physics. https://doi.org/10.1088/0034-4885/46/5/001

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