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Giant Planet Formation

Dynamical Stability of a Massive Envelope

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Comparative Planetology with an Earth Perspective

Abstract

There are two antithetic works on the formation stage of giant planets. Bodenheimer and Pollack (1986) showed with numerical calculation that giant planets are formed through quasi-static contraction of massive envelopes. On the other hand, Wuchterl (1991) obtained the results that giant planets should undergo a dynamical phase and cannot have massive envelopes like the present Jupiter and Saturn because dynamical oscillation would eject envelope mass.

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References

  • Bodenheimer, P. and Pollack, J. B. (1986). Calculations of the Accretion and Evolution of Giant Planets: The.effects of Solid Cores ICARUS. 67, 391–408.

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© 1995 Springer Science+Business Media Dordrecht

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Tajima, N., Nakagawa, Y. (1995). Giant Planet Formation. In: Chahine, M.T., A’Hearn, M.F., Rahe, J., Solomon, P., Nickle, N.L. (eds) Comparative Planetology with an Earth Perspective. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-1092-3_7

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  • DOI: https://doi.org/10.1007/978-94-017-1092-3_7

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-90-481-4636-9

  • Online ISBN: 978-94-017-1092-3

  • eBook Packages: Springer Book Archive

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