Planet heating prevents inward migration of planetary cores

Pablo Benítez-Llambay, Frédéric Masset (), Gloria Koenigsberger and Judit Szulágyi
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Pablo Benítez-Llambay: IATE, Observatorio Astronómico, Universidad Nacional de Córdoba
Frédéric Masset: Instituto de Ciencias Físicas, Universidad Nacional Autónoma de México, Avenidad Universidad s/n
Gloria Koenigsberger: Instituto de Ciencias Físicas, Universidad Nacional Autónoma de México, Avenidad Universidad s/n
Judit Szulágyi: University of Nice-Sophia Antipolis, CNRS, Observatoire de la Côte d'Azur

Nature, 2015, vol. 520, issue 7545, 63-65

Abstract: Abstract Planetary systems are born in the disks of gas, dust and rocky fragments that surround newly formed stars. Solid content assembles into ever-larger rocky fragments that eventually become planetary embryos. These then continue their growth by accreting leftover material in the disk. Concurrently, tidal effects in the disk cause a radial drift in the embryo orbits, a process known as migration1,2,3,4. Fast inward migration is predicted by theory for embryos smaller than three to five Earth masses5,6,7. With only inward migration, these embryos can only rarely become giant planets located at Earth's distance from the Sun and beyond8,9, in contrast with observations10. Here we report that asymmetries in the temperature rise associated with accreting infalling material11,12 produce a force (which gives rise to an effect that we call ‘heating torque’) that counteracts inward migration. This provides a channel for the formation of giant planets8 and also explains the strong planet–metallicity correlation found between the incidence of giant planets and the heavy-element abundance of the host stars13,14.

Date: 2015
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DOI: 10.1038/nature14277

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