2018
DOI: 10.1093/mnras/sty1607
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Self-stirring of debris discs by planetesimals formed by pebble concentration

Abstract: When a protoplanetary disc loses gas, it leaves behind planets and one or more planetesimal belts. The belts get dynamically excited, either by planets ("planet stirring") or by embedded big planetesimals ("self-stirring"). Collisions between planetesimals become destructive and start to produce dust, creating an observable debris disc. Following Kenyon & Bromley (2008), it is often assumed that self-stirring starts to operate as soon as the first ∼ 1000 km-sized embedded "Plutos" have formed. However, state-o… Show more

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Cited by 40 publications
(67 citation statements)
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References 70 publications
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“…Alternatively, according to turbulent concentration and gravitational clumping models (Johansen et al 2007;Cuzzi et al 2008) large planetesimals can form directly from the concentration of small pebbles in a protoplanetary disk. Though these models predict very rapid formation of hundred kilometer size bodies even at radii >100 au (Carrera et al 2017), additional time is needed to excite the neighbouring disk sufficiently (Krivov & Booth 2018). According to equation 34 from Krivov & Booth (2018) in this model the stirring of the belt at a time of 15 Myr needs an even lower initial surface density (x m ∼ 0.3) than in the case of the gradual buildup approach.…”
Section: Stirring Of the Diskmentioning
confidence: 94%
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“…Alternatively, according to turbulent concentration and gravitational clumping models (Johansen et al 2007;Cuzzi et al 2008) large planetesimals can form directly from the concentration of small pebbles in a protoplanetary disk. Though these models predict very rapid formation of hundred kilometer size bodies even at radii >100 au (Carrera et al 2017), additional time is needed to excite the neighbouring disk sufficiently (Krivov & Booth 2018). According to equation 34 from Krivov & Booth (2018) in this model the stirring of the belt at a time of 15 Myr needs an even lower initial surface density (x m ∼ 0.3) than in the case of the gradual buildup approach.…”
Section: Stirring Of the Diskmentioning
confidence: 94%
“…Though these models predict very rapid formation of hundred kilometer size bodies even at radii >100 au (Carrera et al 2017), additional time is needed to excite the neighbouring disk sufficiently (Krivov & Booth 2018). According to equation 34 from Krivov & Booth (2018) in this model the stirring of the belt at a time of 15 Myr needs an even lower initial surface density (x m ∼ 0.3) than in the case of the gradual buildup approach. Obviously, the initial surface density could not be arbitrarily large: ac-cording to Mustill & Wyatt (2009), x m > 10 would imply that the self-stirring scenario may not be feasible in the given system raising the suspicion that the dynamical excitation is rather related to a planet.…”
Section: Stirring Of the Diskmentioning
confidence: 94%
“…However, the growth of Pluto-sized objects at 100s of au in the disk takes too long to explain large disks seen around Gyr-old stars. One possibility is that these form directly from the protoplanetary disk (rather than from the collisional growth of smaller planetesimals), or it could be that a massive disk of ∼ 200 km planetesimals can stir itself without the need for larger bodies (Krivov and Booth 2018). If the belts do mark the outer edge of the planetary system then those planets could stir the disk through their gravitational perturbations.…”
Section: Evolution: Collisional Vs Dynamical Erosionmentioning
confidence: 99%
“…As discussed above, formation of scattered discs require planets to be present in the systems. Considering the same sample of discs from Matrà et al (2018), Krivov & Booth (2018) checked which of them do require planets as stirrers to explain the dust production. They found three such discs: HR 8799, HD 95086 and 49 Cet.…”
Section: Other Systemsmentioning
confidence: 99%
“…The excitation models of Kenyon & Bromley (2008) need Pluto sized objects to stir the disc, but the formation of these objects at the distance of the cold disc of HR 8799 would take longer than the age of the system. Even assuming smaller objects sufficiently stir the disc, self stirring is still not able to produce destructive collisions in the extended disc (Krivov & Booth 2018). This poses the question of how to explain any sort of destructive collision at these distances.…”
Section: Introductionmentioning
confidence: 99%