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Image: A. Angelich (NRAO/AUI/NSF)/ALMA (ESO/NAOJ/NRAO) The behaviour of pebbles around the snowline in protoplanetary disks University of Amsterdam Djoeke Schoonenberg SPF2, Biosphere, 15 March 2018 with Chris Ormel, Beibei Liu, Sebastiaan Krijt
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The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

May 20, 2019

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Page 1: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

Image: A. Angelich (NRAO/AUI/NSF)/ALMA (ESO/NAOJ/NRAO)

Thebehaviourofpebblesaroundthesnowlineinprotoplanetarydisks

University of AmsterdamDjoekeSchoonenberg

SPF2, Biosphere, 15 March 2018

withChrisOrmel,BeibeiLiu,SebastiaanKrijt

Page 2: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

Water snowline around V883 Ori

Cieza et al., Nature, 535, 2016 Schoonenberg, Okuzumi, & Ormel, A&A, 605, L2 (2017)

Page 3: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

Outline• Planetesimalformationbystreaminginstabilityaroundthesnowline

• FormationoftheTRAPPIST-1planets

Page 4: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

Fromdusttoplanets

Nottoscale!(noteventolog-scale)

µm

km

dust

planetesimal

planet

1e3km

Page 5: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

Streaminginstability• Mechanismtodirectlyformplanetesimalsfrompebbles

• Requireslocalsolids-to-gasratiooforderunity

Johansen,Youdin,&MacLow2009(seealsoYoudin&Goodman2005;Johansen,Henning,&Klahr2006;

Johansen&Youdin2007;Simonetal.2016;Yangetal.2017)

Krijtetal.2016(seealsoBirnstieletal.2012,Lambrechts&Johansen2014)

Page 6: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

Schoonenberg&Ormel,A&A,602,A21(2017)

Planetesimalformationoutsidethesnowline:alocaltransportmodel

constantmassfluxoficypebbles

snowline

Page 7: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

↵ = 3 · 10�3

⌧ = 3 · 10�2

Mgas = 10�8M�yr�1

Mpeb/Mgas = 0.8

e-foldingtimescale≈(rpeak-rsnow)/vgas

Schoonenberg&Ormel,A&A,602,A21(2017)

Page 8: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

Icypebbledesigns

‘single-seed’

‘many-seeds’

evaporationfront

Page 9: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

Icypebbledesigns

MichaelHammer,Astrobites

‘single-seed’

‘many-seeds’

evaporationfront

Page 10: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

↵ = 3 · 10�3

⌧ = 3 · 10�2

Mgas = 10�8M�yr�1

Mpeb/Mgas = 0.8

Schoonenberg&Ormel,A&A,602,A21(2017)‘dirt’‘freesilicates’

Many-seedsmodelenhances‘bump’andleadstoplanetesimalicefractionof~0.5

Page 11: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

FormationscenariofortheTRAPPIST-1planets

Ormel,Liu,andSchoonenberg,A&A,604,A1(2017)

Page 12: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

Grimmetal.,A&A,inpress

Page 13: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

Jack Cook/WHOI/USGS

Page 14: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

WaterfractionofTRAPPIST-1planetsdictatedbyratiooficypebbleaccretiontowater-poorpebbleaccretion

Ormel,Liu,andSchoonenberg,A&A,604,A1(2017)

Page 15: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

planetesimalformation+pebbleaccretion (nomigration/planetesimalmergers)

Page 16: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

�16

Planetesimalmergersandmigration

UsingMERCURY(Chambers1999)

Page 17: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

�17

Planetesimalmergersandmigration

UsingMERCURY(Chambers1999)

Page 18: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

�18

Planetesimalmergersandmigration

UsingMERCURY(Chambers1999)

firstplanetaryembryohascrossedsnowline

Page 19: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

↵ = 10�3

Mgas = 10�10M� yr�1

Z = 0.02

b c d e f g h

Page 20: The behaviour of pebbles around the snowline in ...€¢ Without migration, planetesimal formation is a self-limiting process (because pebble flux goes down due to pebble accretion

• PlanetesimalformationinourTRAPPIST-1modelstartsafterafew10^3years

• Firstplanetembryomigratesacrossthesnowlineafterafew10^4years

• Withoutmigration,planetesimalformationisaself-limitingprocess(becausepebblefluxgoesdownduetopebbleaccretionasplanetesimalmassgrows)

• Icypebbleaccretionversusrockypebbleaccretionaftericeline-crossingdeterminesbulkcompositionofTRAPPIST-1planets

• PRELIMINARY:waterfractionsofafewpercentseemtobefeasible

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