Depletion and excitation of the asteroid belt by migrating planets Kevin J. Walsh, Alessandro Morbidelli (SwRI,OCA-Nice) Sean N. Raymond (Obs. Bordeaux),

Slides:



Advertisements
Similar presentations
Resonant Structures due to Planets Mark Wyatt UK Astronomy Technology Centre Royal Observatory Edinburgh.
Advertisements

Origins of Regular and Irregular Satellites ASTR5830 March 19, :30-1:45 pm.
Origins of Regular and Irregular Satellites ASTR5830 March 21, :30-1:45 pm.
Late Heavy Bombardment Or, Kablooie!. The main piece of evidence for a lunar cataclysm comes from the radiometric ages of impact melt rocks that were.
Kozai Migration Yanqin Wu Mike Ramsahai. The distribution of orbital periods P(T) increases from 120 to 2000 days Incomplete for longer periods Clear.
The Grand Tack Scenario: Reconstructing The Migration History Of Jupiter And Saturn In The Disk Of Gas Alessandro Morbidelli (OCA, Nice) Kevin Walsh (SWRI,
Planetary migration F. Marzari, Dept. Physics, Padova Univ.
F. Marzari, Dept. Physics, Padova Univ. The role of migration and planet-planet scattering in shaping planetary systems.
Planet Formation Topic: Resonances Lecture by: C.P. Dullemond Literature: Murray & Dermott „Solar System Dynamics“
Planet Formation with Different Gas Depletion Timescales: Comparing with Observations Huigen Liu, Ji-lin Zhou, Su Wang Dept. of Astronomy.
 The outer planets are called Jovian or Jupiter- like.  These planets are made of gas and are several times more massive than the Earth.  The Jovian.
Dynamics of the young Solar system Kleomenis Tsiganis Dept. of Physics - A.U.Th. Collaborators: Alessandro Morbidelli (OCA) Hal Levison (SwRI) Rodney Gomes.
MINOR MEMBERS OF THE SOLAR SYSTEM: Asteroids. Images of three asteroids, taken during spacecraft flybys, shown to scale (Mathilde is 59 km wide and 47.
Ge/Ay133 What can the asteroid belt tell us about the early S.S.? ? 433 Eros Phobos.
The `Nice’ Model Öpik approximation Planet migration in a planetesimal disk The Nice model Consequences of the Nice Model: Epoch of Late Heavy Bombardment,
10Nov2006 Ge/Ay133 More on Jupiter, Neptune, the Kuiper belt, and the early solar system.
TERRESTRIAL PLANET FORMATION & THE FORMATION OF A WATER-RICH EARTH
Report from the Oort Cloud Simulations of the Formation of the Comet Reservoir Luke Dones Hal Levison Paul Weissman Martin Duncan.
Dynamics of Kuiper belt objects Yeh, Lun-Wen
Observations and models of size distribution of KBOs (summarize several articles) Yeh, Lun-Wen
Trans-Neptunian Objects and Pluto Astronomy 311 Professor Lee Carkner Lecture 21.
Eccentric Extrasolar Planets: The Jumping Jupiter Model HD217107b as imagined by Lynette Cook Stacy Teng TERPS Conference Dec. 9, 2004.
Terrestrial Planet Formation and the Delivery of Water: Theory and Simulations Dara Zeehandelaar TERPS Conference, ASTR688 December 9, 2004 Dara Zeehandelaar.
The basics of terrestrial planet formation The origin of water 1798 engraving, Pass Lecture 3 Formation of the Terrestrial Planets and Origin of Earth’s.
Lesson 8a Moons, Asteroids and Rings. Europa These interactions also keep Europa in a slight elliptical orbit as well. But since Europa is farther from.
Open problems in terrestrial planet formation
A coherent and comprehensive model of the evolution of the outer solar system Alessandro Morbidelli (OCA, Nice) Collaborators: R. Gomes, H. Levison, K.
 formation of non-resonant, multiple close-in super-Earths (which exist around 40-60% (?) of solar type stars)  N-body simulation (Ogihara & Ida 2009,
Giant Planet Accretion and Migration : Surviving the Type I Regime Edward Thommes Norm Murray CITA, University of Toronto Edward Thommes Norm Murray CITA,
Mass Distribution and Planet Formation in the Solar Nebula Steve Desch School of Earth and Space Exploration Arizona State University Lunar and Planetary.
THE LATE HEAVY BOMBARDMENT AND THE FORMATION OF THE SOLAR SYSTEM
Outer Planets.  The outer planets are called Jovian or Jupiter- like.  Made of gas and are several times MORE massive than the Earth.  Grew to present.
Outer Solar System. Planets Outer solar system is dominated entirely by the four Jovian planets, but is populated by billions of small icy objects Giant.
Lecture 3 – Planetary Migration, the Moon, and the Late Heavy Bombardment Abiol 574.
Chaotic Case Studies: Sensitive dependence on initial conditions in star/planet formation Fred C. Adams Physics Department University of Michigan With:
Orbits.
Planets in Debris Disks Renu Malhotra University of Arizona Planet-Debris co-evolution Where can debris exist? Cases: Solar system, upsilon Andromedae,
How do “Habitable” Planets Form? Sean Raymond University of Washington Collaborators: Tom Quinn (Washington) Jonathan Lunine (Arizona)
Introductory Astronomy History – Solar Nebula 1. Dust to Planetesimals Grains of dust (solids) collide and adhere Larger grains grow to 10 9 planetesimals.
David Nesvorny David Vokrouhlicky (SwRI) Alessandro Morbidelli (CNRS) David Nesvorny David Vokrouhlicky (SwRI) Alessandro Morbidelli (CNRS) Capture of.
Dynamics of comets and the origin of the solar system Origin of solar systems - 30/06/2009 Jean-Baptiste Vincent Max-Planck-Institut für Sonnensystemforschung.
in protoplanetary discs and OUTER SOLAR SYSTEM ARCHITECTURE
Formation of the Solar System. A model of the solar system must explain the following: 1.All planets orbit the sun counterclockwise 2.All planets orbit.
David Nesvorny (Southwest Research Institute) David Nesvorny (Southwest Research Institute) Capture of Irregular Satellites during Planetary Encounters.
WATER ON EARTH Alessandro Morbidelli CNRS, Observatoire de la Cote d’Azur, Nice.
Neptune’s Resonances With Kuiper Belt Objects and What It Tells Us About the Early Solar System The Origin of Pluto’s Orbit: Implications for the Solar.
1 The Pluto System in the Context of Kuiper Belt Formation & Evolution A. Morbidelli (OCA – Nice)
DYNAMICAL EVOLUTION OF THE SEINAJOKI ASTEROID FAMILY Vladimir Đošović Bojan Novaković The sixth Symposium "Mathematics and Applications" 17. October2015.
ORIGIN OF THE LATE HEAVY BOMBARDMENT OF THE TERRESTRIAL PLANETS
New Views on the Lunar Late Heavy Bombardment
Cratering in the Solar System William Bottke Southwest Research Institute Boulder, Colorado.
Collision Enhancement due to Planetesimal Binary Formation Planetesimal Binary Formation Junko Kominami Jun Makino (Earth-Life-Science Institute, Tokyo.
Terrestrial Planet Formation in Binary Star Systems ROSES Workshop 2005 February Jack J. Lissauer, NASA Ames Elisa V. Quintana, NASA Ames & Univ. Michigan.
Current structure of the TNB Alvaro Alvarez-Candal.
2012 Spring Semester Topics in Current Astronomy - Formation and Evolution of Planetary Systems - Course ID: Building 19 / Room number 207 for.
The peculiar properties of the Solar System Alessandro Morbidelli CNRS/Observatoire de la Cote d'Azur, Nice, France.
Dynamical constraints on the nature of the Late Heavy Bombardment and models of its origin A.Morbidelli Observatoire de la Cote d’Azur, Nice, France.
Circumstellar Disks at 5-20 Myr: Observations of the Sco-Cen OB Association Marty Bitner.
Figure 4. Same as Fig. 3 but for x = 5.5.
Capture of Irregular Satellites during Planetary Encounters
Figure 1. Orbital evolution of the planetesimals and Jupiter-mass planet in simulation S1. The solid points show the planetesimals. The radii of the planetesimals.
Making Our Solar System: Planetary Formation and Evolution
Formation of the Solar System
Ge/Ay133 What can the asteroid belt tell us about the early S.S.?
Solar system Sergei popov.
Ge/Ay133 What can the asteroid belt tell us about the early S.S.?
Formation of the solar system
Dust Evolution & Planet Traps: Effects on Planet Populations
The Structure of the Solar System
Solar system Sergei popov.
Presentation transcript:

Depletion and excitation of the asteroid belt by migrating planets Kevin J. Walsh, Alessandro Morbidelli (SwRI,OCA-Nice) Sean N. Raymond (Obs. Bordeaux), Dave P. O’Brien (PSI), Avi M. Mandell (GSFC)

Motivation: a solution to the Mars problem? Problem: Mars analogs are 5-10x larger than Mars in standard simulations. Raymond et al Mars analogs are bad

A solution to the Mars problem? Mars analogs are great Hansen 2009 Solution: Hansen (2009) solved this problem with ad-hoc initial conditions, a narrow annulus of material between 0.7— 1.0 AU. Question: Is there a mechanism to create these initial conditions? Problem: Mars analogs are 5-10x larger than Mars in standard simulations.

Migration of Jupiter and Saturn in a gas-disk 3:2 res Masset and Snellgrove, 2001, Morbidelli and Crida, 2007; Pierens and Nelson, 2008 For a wide range of possible gas-disk parameters Jupiter will open a gap and migrate inwards via type II migration Saturn migrates inwards, getting captured in resonance with Jupiter. Saturn in resonance with Jupiter can halt and reverse the inward migration of Jupiter. Saturn Jupiter

Jupiter’s migration - truncating the disk Jupiter migrates inward to ~1.5, Saturn migrates inward, getting captured in the 3:2 resonance with Jupiter, while increasing in mass, Saturn reaching near full mass halts their migration, and reverses it. They migrate out together as the gas-disk dissipates. Semimajor axis ?

Problem? The Asteroid Belt Jupiter’s outward migration scatters bodies into the asteroid belt Thus, seeking to produce taxonomic distributions, we envision reservoirs of primitive bodies between and beyond the giant planets. The asteroid belt provides strict constraints in its taxonomic and orbital distribution. Gradie and Tedesco 1982

Jupiter’s migration - truncating the disk Jupiter migrates inward to ~1.5, Saturn migrates inward, getting captured in the 3:2 resonance with Jupiter, while increasing in mass, Saturn reaching near full mass halts their migration, and reverses it. They migrate out together as the gas-disk dissipates. S-type C-type Semimajor axis ? ? scattered S-types

X,Y movie

Repopulating the Asteroid Belt The “S-type” bodies from the inner disk are scattered back roughly where they originated. This means that they largely repopulated the inner part of the asteroid belt region a<2.8. Semimajor axis (AU)

Asteroids Gradie and Tedesco 1982 Bodies are implanted in the asteroid belt ~10 -3 efficiency, ~10x current asteroid belt mass for an initial MMSN, ~Taxonomic distributions largely recreated Orbital distribution matches pre-LHB expectations e = i=0-25°

We We are not done. There is ~500 Myr until the LHB We have a component of high-e bodies that will accrete onto planets or could collide with each other.

Asteroid Belt implications Separate parent populations – AU and ~6-13 AU – Requires diversity in both populations to explain the significant observed diversity among asteroids. – Suggests that our primitive asteroids may originate closer to comets than our more metamorphosed asteroids Pre-Depleted asteroid belt – The asteroid belt was depleted rapidly before the gas-disk had fully dissipated. Pre-Excited asteroid belt – Asteroid belt gets its inclination distribution at this early time, – Eccentricities will be re-shuffled later (LHB) Chondrules/CAIs – Need to be formed/transported to ~ 13 AU and beyond?

Conclusions Conclusions: Jupiter migrating to 1.5 AU can solve some outstanding problems – Small mass of Mars – Physical dichotomy of the asteroid belt – Freedom for Jupiter to form very near the Snow Line Implications: – Jupiter and Saturn migrated significantly in the gas-disk: Jupiter reached 1.5 AU – The asteroid belt was repopulated from two distinct parent populations

Asteroids Gradie and Tedesco 1982 Bodies are implanted in the asteroid belt ~10 -3 efficiency, ~10x current asteroid belt mass for MMSN, ~Taxonomic distributions recreated Orbital distribution matches pre-LHB expectations e = i=0-25°

Asteroid Distributions: e and i The Grand Tack is not the last event to alter the orbital distribution in the asteroid belt. – The orbital instabilities related to the LHB will happen 500 Myr later. The sweeping of resonances across the asteroid belt when the giant planets migrate will – Deplete the population 2-5x, – Not change a distribution substantially, – Not change i distribution substantially, – Likely change the e distribution substantially,

Eccentricity Asteroids post-Grand Tack Average e = 0.2 Current-Day Asteroid belt H<10.8 Average e = 0.15

Minton & Malhotra did this for us! This analytical work found a good match for a rapid, and smooth, sweeping of resonances in τ < 1 Myr.

The post-Grand Tack distribution is similar post-Grand Tack

We don’t trust Minton, so we test this numerically…. What is the parameter space for giant planet migration? – Differing smooth migration rates, exponential with τ < 0.5 Myr τ = 0.5 Myr – match Minton et al τ = 0.2, 0.1, 0.05 Myr as a proxy for even more rapid migrations (e.g. jumping Jupiter) – “Jumping-Jupiter” migration, using the rapid and non-smooth evolution of the giant planets -> “jumping-Jupiter” Morbidelli et al “jump”

Smooth Migration τ=1e5 yr