Definition
Core accretion is the standard model for giant planet formation. The core accretion model proposes that the formation of giant planets starts with core formation followed by gas accretion. First, small bodies continually collide to form larger ones, eventually reaching the stage of protoplanetary cores, which are essentially large planetary embryos that form in the giant planet region. Cores that reach masses of a few Earth masses begin to accrete gas from the protoplanetary disk, slowly at first, and then at a runaway rate when the gaseous envelope’s mass becomes comparable to the core mass. Cores, therefore, represent the “seeds” of gas giant and ice giant planets in this model. An alternative model for giant planet formation is disk instability that proposes that giant planets form via a local gravitational collapse in the disk, which can later be followed by core formation and accretion of solids.
References and Further Reading
Lissauer JJ, Stevenson DJ (2007) Formation of giant planets. In: Reipurth B, Jewitt D, Keil K (eds) Protostars and planets V. University of Arizona Press, Tucson, pp 591–606, 951 pp
Pollack JB, Hubickyj O, Bodenheimer P, Lissauer JJ, Podolak M, Greenzweig Y (1996) Formation of the giant planets by concurrent accretion of solids and gas. Icarus 124:62–85
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Raymond, S.N. (2014). Core Accretion, Model for Giant Planet Formation. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_353-4
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DOI: https://doi.org/10.1007/978-3-642-27833-4_353-4
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