Formation of Planets around M & L dwarfs

Similar documents
Accretion of Planets. Bill Hartmann. Star & Planet Formation Minicourse, U of T Astronomy Dept. Lecture 5 - Ed Thommes

How do we model each process of planet formation? How do results depend on the model parameters?

Toward a Deterministic Model of Planetary Formation IV: Effects of Type-I Migration

Definitions. Stars: M>0.07M s Burn H. Brown dwarfs: M<0.07M s No Burning. Planets No Burning. Dwarf planets. cosmic composition (H+He)

Dynamically Unstable Planetary Systems Emerging Out of Gas Disks

F. Marzari, Dept. Physics, Padova Univ. Planetary migration

Origin of the Difference of the Jovian and Saturnian Satellite Systems

Planetary System Stability and Evolution. N. Jeremy Kasdin Princeton University

Introduction to extra solar planets

Ruth Murray-Clay University of California, Santa Barbara

Astronomy 405 Solar System and ISM

What is it like? When did it form? How did it form. The Solar System. Fall, 2005 Astronomy 110 1

PLANETARY FORMATION THEORY EXPLORING EXOPLANETS

Sta%s%cal Proper%es of Exoplanets

Planet formation in protoplanetary disks. Dmitry Semenov Max Planck Institute for Astronomy Heidelberg, Germany

Solar System evolution and the diversity of planetary systems

Wed. Sept. 20, Today: For Monday Sept. 25 and following days read Chapter 4 (The Moon) of Christiansen and Hamblin (on reserve).

Evolution of protoplanetary discs

planet migration driven by a planetesimal disk Solar System & extra solar planets: evidence for/against planet migration?

SIMULTANEOUS FORMATION OF GIANT PLANETS

Astronomy 405 Solar System and ISM

How Shadowing and Illumination in Disks Affect Planet Formation

Lecture 16. How did it happen? How long did it take? Where did it occur? Was there more than 1 process?

Planet Formation: theory and observations. Sean Raymond University of Colorado (until Friday) Observatoire de Bordeaux

Lecture Outlines. Chapter 15. Astronomy Today 7th Edition Chaisson/McMillan Pearson Education, Inc.

Tidal Dissipation in Binaries

Class 15 Formation of the Solar System

Migration. Phil Armitage (University of Colorado) 4Migration regimes 4Time scale for massive planet formation 4Observational signatures

Lecture 20: Planet formation II. Clues from Exoplanets

THE SEPARATION/PERIOD GAP IN THE DISTRIBUTION OF EXTRASOLAR PLANETS AROUND STARS WITH MASSES M 1.2 M

arxiv: v1 [astro-ph.ep] 20 Apr 2014

EXOPLANET LECTURE PLANET FORMATION. Dr. Judit Szulagyi - ETH Fellow

Dynamical water delivery: how Earth and rocky exoplanets get wet

Global models of planetary system formation. Richard Nelson Queen Mary, University of London

Planet disk interaction

arxiv:astro-ph/ v1 30 Oct 2006

PLANETARY MIGRATION A. CRIDA

Data from: The Extrasolar Planet Encyclopaedia.

Kozai-Lidov oscillations

The dynamical evolution of the asteroid belt in the pebble accretion scenario

PLANETARY MIGRATION. Review presented at the Protostars & Planets VI conference in Heidelberg, september 2013 (updated).

Giant Planet Formation

C. Mordasini & G. Bryden. Sagan Summer School 2015

What Have We Found? 1978 planets in 1488 systems as of 11/15/15 ( ) 1642 planets candidates (

Testing Theories of Planet Formation & Dynamical Evolution of Planetary Systems using Orbital Properties of Exoplanets

Formation of the Solar System Chapter 8

Uranus & Neptune: The Ice Giants. Discovery of Uranus. Bode s Law. Discovery of Neptune

1 Solar System Debris and Formation

Exoplanets: a dynamic field

Origin of the Solar System

Origin of high orbital eccentricity and inclination of asteroids

Chapter 15 The Formation of Planetary Systems

Observational Cosmology Journal Club

Minimum Mass Solar Nebulae, Nice model, & Planetary Migration.

Jupiter, Saturn, Uranus and Neptune: their formation in few million years

arxiv:astro-ph/ v1 13 Aug 2005

Observational Astronomy - Lecture 6 Solar System I - The Planets

Origin of the Solar System

Clicker Question: Clicker Question: Clicker Question:

Comet Science Goals II

Phys 214. Planets and Life

What s s New? Planetary Formation Scenarios Revisited: Core-Accretion versus Disk Instability. Taro Matsuo (Nagoya University)

Initial Conditions: The temperature varies with distance from the protosun.

Solar System Formation

Brown Dwarf Formation from Disk Fragmentation and Ejection

Which of the following statements best describes the general pattern of composition among the four jovian

Origins of Gas Giant Planets

The migration and growth of protoplanets in protostellar discs

Disk planet interaction during the formation of extrasolar planets

arxiv: v1 [astro-ph.ep] 14 Apr 2016

On the formation of the Martian moons from a circum-mars accretion disk

A Beta-Viscosity Model

Solar System Formation

arxiv:astro-ph/ v1 25 Aug 1998

On the formation of terrestrial planets in hot-jupiter systems. M. J. Fogg and R. P. Nelson ABSTRACT

PLANETARY MIGRATION A. CRIDA

Why is it hard to detect planets around other stars?

10/16/ Detecting Planets Around Other Stars. Chapter 10: Other Planetary Systems The New Science of Distant Worlds

Nature and Origin of Planetary Systems f p "

Solar System Formation

Today. Solar System Formation. a few more bits and pieces. Homework due

Accretion of Uranus and Neptune

9. Formation of the Solar System

Gas Disks to Gas Giants: Simulating the Birth of Planetary Systems

Terrestrial planet formation: planetesimal mixing KEVIN WALSH (SWRI)

arxiv: v1 [astro-ph.ep] 8 Apr 2010

The primordial excitation and clearing of the asteroid belt Revisited

Practical Numerical Training UKNum

Chapter 15: The Origin of the Solar System

Disc-Planet Interactions during Planet Formation

Planetary system dynamics. Planetary migration Kozai resonance Apsidal resonance and secular theories Mean motion resonances Gravitational scattering

Internal structure and atmospheres of planets

Super-Earths as Failed Cores in Orbital Migration Traps

Our Planetary System & the Formation of the Solar System

Astro 1: Introductory Astronomy

Planetary Migration: What Does It Mean for Planet Formation?

Actuality of Exoplanets Search. François Bouchy OHP - IAP

EART164: PLANETARY ATMOSPHERES

Test 4 Final Review. 5/2/2018 Lecture 25

Life in the Universe (1)

Transcription:

Formation of Planets around & L dwarfs D.N.C. Lin University of California with S. Ida, H. Li, S.L.Li, E. Thommes, I. Dobbs-Dixon, S.T. Lee,P. Garaud,. Nagasawa AAS Washington Jan 11th, 006 17 slides

Disk properties Hillenbrand Calvet 1 Disk life time is independent of * :similar available time Disk accretion rate varies as * : Less gas content 3 Disk heavy element mass varies as * 1-?Less metals

Preferred locations eteorites: Dry, chondrules & CAI s Enhancement factor > 4 Icy moons

Stellar mass dependence T(snow line) ~160K, L ~ a(snow line) ~ (L) 1/ /T ~.7( * / o ) AU V k (snow)~(/a) 1/ ~Const ; H/a ~Const Similar aspect ratio and Keplerian speed! But shorter time scales (a/v k ) for lower * Water-rich planets form near low-mass stars

From planetesimals to embryos Feeding zones: 10 r Hill Isolation mass: isolation ~Σ 1.5 a 3-1/ * Initial growth: (runaway) Shorter growth time scale at the snow line

* dependence Scaling disk models with * : a)solar system: inimum-mass nebula b)other stars: Σ(a) = Σ SN (a) h d where h d = ( * / sun ) 0,1, c)embryos with p > earth are formed outside snow line Importance of snow line: Interior to it: growth limit due to isolation Exterior to it: long growth time scale Outside the snow line: isolation ~1.3(a/1AU) 3/4 ( * / o ) 3/ earth less massive embryos τ embryos ~0.033(a/1AU) 59/0 ( * / o ) -16/15 yr longer growth time Can form >3 earth embryos outside 5AU within 10yr

Disk-planet tidal interactions type-i migration Goldreich & Tremaine (1979), Ward (1986, 1997), Tanaka et al. (00) > (0.1 1) type-ii migration Lin & Papaloizou (1985),... > (10 100) planet s perturbation τ mig, I disk torque imbalance Σ g,sn * 0.05 a Σg p o 1AU 3 3 yr viscous diffusion viscous disk accretion τ mig, II Σ Σ g,sn g p J 3 10 o a yr α * 1AU 1 1

Low-mass embryo (10 earth) Cooler and invisic disks

(ass) growth vs (orbital) decay Loss due to Type I migration yr 1AU ) ( (0).04 0 * o g g mig,i 4 3 Σ Σ a t τ Embryos migration time scale 5 11 1AU (0) ) ( g g mig,i embryo Σ Σ a t τ τ Outer embryos are better preserved only after significant gas depletion Critical-mass core: p =5 earth yr 1AU ) ( (0) 0.01 3 1 * g g I mig, Σ Σ a t o τ

Flow into the Roche potential Equation of motion: Bondi radius (R b =G p /c s ) Hill s radius (R h =( p /3 * ) 1/3 a) Disk thickness (H=c s a/v k ) R b / R h =3 1/3 ( p / * ) /3 (a/h) decreases with * DU Dt C s ρ ρ -1 + ϕ r If R b > R h,, a large decline in ρ (+ve r gradient) would be needed to overcome the tidal barrier. A small ρ at the Hill s radius would quench the accretion flow.

Reduction in the accretion rate Growth time scales: Embryos emergence time scale: ~ 0.033(a/1AU) 59/0 ( * / o ) -16/15 yr KH cooling/contraction of the envelope: ~10-4 ( p / earth ) -(3-4) yr Uninhibited Bondi accretion: ~(H/a) 4 ( * / p d )/Ω k ~10-3 yr( J / p ) Uninhibited accretion from the disk: ~ p /(d/dt)~ 10 3-4 yr( p / J ) Reduction due to Hill s barrier: >τ disk depletion Tidal barriers suppress the emergence of gas giants around low-mass stars

Gap formation & type II migration Viscous and thermal conditions Lower limiting mass for gas giants around low-mass stars yr 1AU 10 1 1 * o 3 J p g g,sn II mig, Σ Σ a α τ Neptune-mass planets can open up gaps and migrate close to the stars

Hot Neptunes around low- * stars Radial extent is determined by V k > V escape

igration-free sweeping secular resonances Resonant secular perturbation disk ~ p (Ward, Ida, Nagasawa) Ups And Transitional disks

Dynamical shake up (Nagasawa, Thommes) Bode s law: dynamically porous terrestrial planets orbits with low eccentricities with wide separation

Formation of water worlds Jupiter-Saturn secular interaction & multiple extrasolar systems Sweeping secular resonance may be more intense in low-mass stars. But the absence of gas or ice giants would leave behind dynamically-hot earth-mass objects

Summary 1. Snow line is important for the retention of heavy. Around low-mass stars, planets with mass greater than that of the earth are formed outside the snow line.. Planet-disk interaction can lead to depletion of first generation planetesimals, especially around low-mass stars 3. Self regulation led to the stellar accretion of most heavy elements, the late emergence of planets, and perhaps the inner holes inferred from SED s. 4. Around low-mass stars, gas accretion rate onto proto gas giants is also suppressed by a tidal barrier. 5. Neptune-mass embryos can open up gaps and migrate to the stellar proximity. 6. Residual planetesimals may have modest eccentricities. 7 There will be a desert of gas giants and an oasis of terrestrial planets, including short-period water worlds around dwarfs.