4.7 Article

Tidal Downsizing model - IV. Destructive feedback in planets

期刊

出版社

OXFORD UNIV PRESS
DOI: 10.1093/mnras/stw1404

关键词

planets and satellites: formation; protoplanetary discs; planetary systems

资金

  1. STFC
  2. Science and Technology Facilities Council [ST/K000373/1, ST/M006948/1, ST/M007073/1] Funding Source: researchfish
  3. STFC [ST/H00856X/1, PP/E00119X/1, ST/N000757/1, ST/H002235/1, ST/K000373/1, ST/M007073/1, ST/M006948/1, ST/K001000/1] Funding Source: UKRI

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The role of negative feedback from a massive solid core on its massive gas envelope in the Tidal Downsizing scenario of planet formation is investigated via one-dimensional planet evolution models followed by population synthesis calculations. It is shown that cores more massive than similar to 10 M-circle plus release enough energy to reverse contraction of their parent gas envelopes, culminating in their destruction. This process may help to explain why observed gas giant planets are so rare, why massive cores are so ubiquitous, and why there is a sharp rollover in the core mass function above similar to 20 M-circle plus. Additionally, the short time-scales with which these massive cores are assembled in TD may help explain formation route of Uranus, Neptune and the suspected HL Tau planets. Given the negative role of cores in assembly of gas giants in the model, an antimony is found between massive cores and gas giants: cores in survived gas giant planets are on average less massive than cores free of massive envelopes. In rare circumstances when core feedback self-regulates, extremely metal-rich gas giants, such as CoRoT-20b, a gas giant made of heavy elements by up to similar to 50 per cent, can be made.

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