Please use this identifier to cite or link to this item: http://hdl.handle.net/2381/19104
Title: Grain sedimentation inside giant planet embryos
Authors: Nayakshin, Sergei
First Published: 11-Nov-2010
Publisher: Oxford University Press (OUP)
Citation: Monthly Notices of the Royal Astronomical Society , 2010, 408 (4), pp. 2381-2396
Abstract: In the context of massive fragmenting protoplanetary discs, Boss suggested that grains can grow and sediment inside giant planet embryos formed at R∼ 5 au away from the star. Several authors since then criticized the suggestion. Convection may prevent grain sedimentation, and the embryos cannot even form so close to the parent star as cooling is too inefficient at these distances. Here we reconsider the grain sedimentation process suggested by Boss but inside an embryo formed, as expected in the light of the cooling constraints, at R∼ 100 au. Such embryos are much less dense and are also cooler. We make analytical estimates of the process and also perform simple spherically symmetric radiation hydrodynamics simulations to test these ideas. We find that convection in our models does not become important before a somewhat massive (∼ an Earth mass; this is clarified in a followup paper) solid core is built. Turbulent mixing slows down dust sedimentation but is overwhelmed by grain sedimentation when the latter grows to a centimetres size. The minimum time required for dust sedimentation to occur is a few thousand years, and is a strong function of the embryo’s mass, dust content and opacity. An approximate analytical criterion is given to delineate conditions in which a giant embryo contracts and heats up faster than dust can sediment. As Boss et al., we argue that core formation through grain sedimentation inside the giant planet embryos may yield an unexplored route to form giant gas and giant ice planets. The present model also stands at the basis of Paper III, where we study the possibility of forming terrestrial planet cores by tidal disruption and photoevaporation of the planetary envelope.
DOI Link: 10.1111/j.1365-2966.2010.17289.x
ISSN: 0035-8711
eISSN: 1365-2966
Links: http://hdl.handle.net/2381/19104
http://mnras.oxfordjournals.org/content/408/4/2381
Version: Publisher Version
Status: Peer-reviewed
Type: Journal Article
Rights: This article has been accepted for publication in Monthly Notices of the Royal Astronomical Society ©: 2010 the authors. Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved. Deposited with reference to the publisher’s archiving policy available on the SHERPA/RoMEO website.
Appears in Collections:Published Articles, Dept. of Physics and Astronomy

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