2019
DOI: 10.1051/0004-6361/201936351
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Exploring the conditions for forming cold gas giants through planetesimal accretion

Abstract: The formation of cold gas giants similar to Jupiter and Saturn in orbit and mass is a great challenge for planetesimal-driven core accretion models because the core growth rates far from the star are low. Here we model the growth and migration of single protoplanets that accrete planetesimals and gas. We integrated the core growth rate using fits in the literature to N-body simulations, which provide the efficiency of accreting the planetesimals that a protoplanet migrates through. We take into account three c… Show more

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Cited by 46 publications
(31 citation statements)
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“…After the successful application of the analytical growth tracks to Venus and Mars, we now turn to numerical integration of the masses and orbits of protoplanets undergoing pebble accretion, planetesimal accretion, and inward type I migration, using the code developed and presented in ( 5 , 2 ). The protoplanetary disc model is described in Materials and Methods.…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…After the successful application of the analytical growth tracks to Venus and Mars, we now turn to numerical integration of the masses and orbits of protoplanets undergoing pebble accretion, planetesimal accretion, and inward type I migration, using the code developed and presented in ( 5 , 2 ). The protoplanetary disc model is described in Materials and Methods.…”
Section: Resultsmentioning
confidence: 99%
“…The long formation time scale of gas giants and ice giants in the outer regions of protoplanetary discs by traditional planetesimal accretion (1,2) instigated the development of the pebble accretion theory in which the pebbles drifting through the protoplanetary disc are accreted rapidly by the growing protoplanets (3,4). While pebble accretion clearly aids the formation of gas giants (5), the formation of terrestrial planets has so far, with a few exceptions (6)(7)(8)(9), mainly been explored in classical N-body simulations where terrestrial planets grow by successive impacts between increasingly massive protoplanets (10).…”
Section: Introductionmentioning
confidence: 99%
“…Forming massive planetary cores of 10 M ⊕ at larger distances to the star within the lifetime of a gaseous disk is currently a challenge for planetesimal accretion models (Johansen & Bitsch 2019). A solution to this conundrum has appeared in the form of pebble accretion onto distant planetary embryos (Klahr & Bodenheimer 2006;Ormel & Klahr 2010;Lambrechts & Johansen 2012;Bitsch et al 2015;Ndugu et al 2017).…”
Section: Introductionmentioning
confidence: 99%
“…The formation of planetesimals is such a process, and the one-dimensional formation model by Lenz et al (2019) is such an attempt. Previous work on the accretion of planetesimals for planetary growth such as Johansen & Bitsch (2019), Mordasini (2018), or Ida & Lin (2004) used initial distributions of planetesimals and initially placed planetary embryos, while neglecting the presence of pebbles. Other formation models such as those of Bitsch et al (2015) or Brügger et al (2018) modeled planetary growth by the accretion of pebbles and initially set planetary embryos, while neglecting the formation, or accretion, of planetesimals.…”
Section: Introductionmentioning
confidence: 99%