Definition
Primordial heat is the internal heat energy accumulated by dissipation in a planet during its first few million years of evolution. The main contributions to the primordial heat are accretional energy – the energy deposited by infalling planetesimals – and differentiation energy. The latter is mainly released by core formation and is basically potential energy that is dissipated upon formation of a gravitationally stable layering of the planet. In addition to the primordial heat, the planet’s internal heat source is mainly provided by the radioactive decay of long-lived unstable isotopes such as 238U, 235U, 232Th, and 40K and by latent heat.
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© 2011 Springer-Verlag Berlin Heidelberg
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Breuer, D. (2011). Primordial Heat. In: Gargaud, M., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-11274-4_1274
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DOI: https://doi.org/10.1007/978-3-642-11274-4_1274
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-11271-3
Online ISBN: 978-3-642-11274-4
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